Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China
Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured t...
Ausführliche Beschreibung
Autor*in: |
Shi, Ruizhu [verfasserIn] |
---|
Format: |
E-Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2023 |
---|
Schlagwörter: |
---|
Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
---|
Übergeordnetes Werk: |
Enthalten in: Journal of soils and sediments - Berlin : Springer, 2001, 23(2023), 9 vom: 09. Juni, Seite 3435-3444 |
---|---|
Übergeordnetes Werk: |
volume:23 ; year:2023 ; number:9 ; day:09 ; month:06 ; pages:3435-3444 |
Links: |
---|
DOI / URN: |
10.1007/s11368-023-03555-2 |
---|
Katalog-ID: |
SPR052792099 |
---|
LEADER | 01000naa a22002652 4500 | ||
---|---|---|---|
001 | SPR052792099 | ||
003 | DE-627 | ||
005 | 20230819064812.0 | ||
007 | cr uuu---uuuuu | ||
008 | 230819s2023 xx |||||o 00| ||eng c | ||
024 | 7 | |a 10.1007/s11368-023-03555-2 |2 doi | |
035 | |a (DE-627)SPR052792099 | ||
035 | |a (SPR)s11368-023-03555-2-e | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
100 | 1 | |a Shi, Ruizhu |e verfasserin |4 aut | |
245 | 1 | 0 | |a Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China |
264 | 1 | |c 2023 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a Computermedien |b c |2 rdamedia | ||
338 | |a Online-Ressource |b cr |2 rdacarrier | ||
500 | |a © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. | ||
520 | |a Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion. | ||
650 | 4 | |a PAH speciation |7 (dpeaa)DE-He213 | |
650 | 4 | |a Karst terrain |7 (dpeaa)DE-He213 | |
650 | 4 | |a Soil properties |7 (dpeaa)DE-He213 | |
650 | 4 | |a Organic pollutant |7 (dpeaa)DE-He213 | |
700 | 1 | |a Sun, Yuchuan |4 aut | |
700 | 1 | |a Zheng, Xiaoxuan |4 aut | |
700 | 1 | |a Shen, Licheng |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Journal of soils and sediments |d Berlin : Springer, 2001 |g 23(2023), 9 vom: 09. Juni, Seite 3435-3444 |w (DE-627)373325134 |w (DE-600)2125896-X |x 1614-7480 |7 nnns |
773 | 1 | 8 | |g volume:23 |g year:2023 |g number:9 |g day:09 |g month:06 |g pages:3435-3444 |
856 | 4 | 0 | |u https://dx.doi.org/10.1007/s11368-023-03555-2 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_SPRINGER | ||
912 | |a GBV_ILN_11 | ||
912 | |a GBV_ILN_20 | ||
912 | |a GBV_ILN_22 | ||
912 | |a GBV_ILN_23 | ||
912 | |a GBV_ILN_24 | ||
912 | |a GBV_ILN_31 | ||
912 | |a GBV_ILN_32 | ||
912 | |a GBV_ILN_39 | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_60 | ||
912 | |a GBV_ILN_62 | ||
912 | |a GBV_ILN_63 | ||
912 | |a GBV_ILN_65 | ||
912 | |a GBV_ILN_69 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_73 | ||
912 | |a GBV_ILN_74 | ||
912 | |a GBV_ILN_90 | ||
912 | |a GBV_ILN_95 | ||
912 | |a GBV_ILN_100 | ||
912 | |a GBV_ILN_105 | ||
912 | |a GBV_ILN_110 | ||
912 | |a GBV_ILN_120 | ||
912 | |a GBV_ILN_138 | ||
912 | |a GBV_ILN_150 | ||
912 | |a GBV_ILN_151 | ||
912 | |a GBV_ILN_152 | ||
912 | |a GBV_ILN_161 | ||
912 | |a GBV_ILN_170 | ||
912 | |a GBV_ILN_171 | ||
912 | |a GBV_ILN_183 | ||
912 | |a GBV_ILN_187 | ||
912 | |a GBV_ILN_213 | ||
912 | |a GBV_ILN_224 | ||
912 | |a GBV_ILN_230 | ||
912 | |a GBV_ILN_250 | ||
912 | |a GBV_ILN_281 | ||
912 | |a GBV_ILN_285 | ||
912 | |a GBV_ILN_293 | ||
912 | |a GBV_ILN_370 | ||
912 | |a GBV_ILN_602 | ||
912 | |a GBV_ILN_636 | ||
912 | |a GBV_ILN_702 | ||
912 | |a GBV_ILN_2001 | ||
912 | |a GBV_ILN_2003 | ||
912 | |a GBV_ILN_2004 | ||
912 | |a GBV_ILN_2005 | ||
912 | |a GBV_ILN_2006 | ||
912 | |a GBV_ILN_2007 | ||
912 | |a GBV_ILN_2008 | ||
912 | |a GBV_ILN_2009 | ||
912 | |a GBV_ILN_2010 | ||
912 | |a GBV_ILN_2011 | ||
912 | |a GBV_ILN_2014 | ||
912 | |a GBV_ILN_2015 | ||
912 | |a GBV_ILN_2020 | ||
912 | |a GBV_ILN_2021 | ||
912 | |a GBV_ILN_2025 | ||
912 | |a GBV_ILN_2026 | ||
912 | |a GBV_ILN_2027 | ||
912 | |a GBV_ILN_2031 | ||
912 | |a GBV_ILN_2034 | ||
912 | |a GBV_ILN_2037 | ||
912 | |a GBV_ILN_2038 | ||
912 | |a GBV_ILN_2039 | ||
912 | |a GBV_ILN_2044 | ||
912 | |a GBV_ILN_2048 | ||
912 | |a GBV_ILN_2049 | ||
912 | |a GBV_ILN_2050 | ||
912 | |a GBV_ILN_2055 | ||
912 | |a GBV_ILN_2056 | ||
912 | |a GBV_ILN_2057 | ||
912 | |a GBV_ILN_2059 | ||
912 | |a GBV_ILN_2061 | ||
912 | |a GBV_ILN_2064 | ||
912 | |a GBV_ILN_2065 | ||
912 | |a GBV_ILN_2068 | ||
912 | |a GBV_ILN_2088 | ||
912 | |a GBV_ILN_2093 | ||
912 | |a GBV_ILN_2106 | ||
912 | |a GBV_ILN_2107 | ||
912 | |a GBV_ILN_2108 | ||
912 | |a GBV_ILN_2110 | ||
912 | |a GBV_ILN_2111 | ||
912 | |a GBV_ILN_2112 | ||
912 | |a GBV_ILN_2113 | ||
912 | |a GBV_ILN_2118 | ||
912 | |a GBV_ILN_2122 | ||
912 | |a GBV_ILN_2129 | ||
912 | |a GBV_ILN_2143 | ||
912 | |a GBV_ILN_2144 | ||
912 | |a GBV_ILN_2147 | ||
912 | |a GBV_ILN_2148 | ||
912 | |a GBV_ILN_2152 | ||
912 | |a GBV_ILN_2153 | ||
912 | |a GBV_ILN_2188 | ||
912 | |a GBV_ILN_2190 | ||
912 | |a GBV_ILN_2232 | ||
912 | |a GBV_ILN_2336 | ||
912 | |a GBV_ILN_2360 | ||
912 | |a GBV_ILN_2446 | ||
912 | |a GBV_ILN_2470 | ||
912 | |a GBV_ILN_2472 | ||
912 | |a GBV_ILN_2507 | ||
912 | |a GBV_ILN_2522 | ||
912 | |a GBV_ILN_2548 | ||
912 | |a GBV_ILN_4035 | ||
912 | |a GBV_ILN_4037 | ||
912 | |a GBV_ILN_4046 | ||
912 | |a GBV_ILN_4112 | ||
912 | |a GBV_ILN_4125 | ||
912 | |a GBV_ILN_4126 | ||
912 | |a GBV_ILN_4242 | ||
912 | |a GBV_ILN_4246 | ||
912 | |a GBV_ILN_4249 | ||
912 | |a GBV_ILN_4251 | ||
912 | |a GBV_ILN_4305 | ||
912 | |a GBV_ILN_4306 | ||
912 | |a GBV_ILN_4307 | ||
912 | |a GBV_ILN_4313 | ||
912 | |a GBV_ILN_4322 | ||
912 | |a GBV_ILN_4323 | ||
912 | |a GBV_ILN_4324 | ||
912 | |a GBV_ILN_4325 | ||
912 | |a GBV_ILN_4326 | ||
912 | |a GBV_ILN_4328 | ||
912 | |a GBV_ILN_4333 | ||
912 | |a GBV_ILN_4334 | ||
912 | |a GBV_ILN_4335 | ||
912 | |a GBV_ILN_4336 | ||
912 | |a GBV_ILN_4338 | ||
912 | |a GBV_ILN_4393 | ||
912 | |a GBV_ILN_4700 | ||
951 | |a AR | ||
952 | |d 23 |j 2023 |e 9 |b 09 |c 06 |h 3435-3444 |
author_variant |
r s rs y s ys x z xz l s ls |
---|---|
matchkey_str |
article:16147480:2023----::pcainnifunigatroplcciaoaihdoabn |
hierarchy_sort_str |
2023 |
publishDate |
2023 |
allfields |
10.1007/s11368-023-03555-2 doi (DE-627)SPR052792099 (SPR)s11368-023-03555-2-e DE-627 ger DE-627 rakwb eng Shi, Ruizhu verfasserin aut Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion. PAH speciation (dpeaa)DE-He213 Karst terrain (dpeaa)DE-He213 Soil properties (dpeaa)DE-He213 Organic pollutant (dpeaa)DE-He213 Sun, Yuchuan aut Zheng, Xiaoxuan aut Shen, Licheng aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 9 vom: 09. Juni, Seite 3435-3444 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:9 day:09 month:06 pages:3435-3444 https://dx.doi.org/10.1007/s11368-023-03555-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 9 09 06 3435-3444 |
spelling |
10.1007/s11368-023-03555-2 doi (DE-627)SPR052792099 (SPR)s11368-023-03555-2-e DE-627 ger DE-627 rakwb eng Shi, Ruizhu verfasserin aut Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion. PAH speciation (dpeaa)DE-He213 Karst terrain (dpeaa)DE-He213 Soil properties (dpeaa)DE-He213 Organic pollutant (dpeaa)DE-He213 Sun, Yuchuan aut Zheng, Xiaoxuan aut Shen, Licheng aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 9 vom: 09. Juni, Seite 3435-3444 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:9 day:09 month:06 pages:3435-3444 https://dx.doi.org/10.1007/s11368-023-03555-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 9 09 06 3435-3444 |
allfields_unstemmed |
10.1007/s11368-023-03555-2 doi (DE-627)SPR052792099 (SPR)s11368-023-03555-2-e DE-627 ger DE-627 rakwb eng Shi, Ruizhu verfasserin aut Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion. PAH speciation (dpeaa)DE-He213 Karst terrain (dpeaa)DE-He213 Soil properties (dpeaa)DE-He213 Organic pollutant (dpeaa)DE-He213 Sun, Yuchuan aut Zheng, Xiaoxuan aut Shen, Licheng aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 9 vom: 09. Juni, Seite 3435-3444 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:9 day:09 month:06 pages:3435-3444 https://dx.doi.org/10.1007/s11368-023-03555-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 9 09 06 3435-3444 |
allfieldsGer |
10.1007/s11368-023-03555-2 doi (DE-627)SPR052792099 (SPR)s11368-023-03555-2-e DE-627 ger DE-627 rakwb eng Shi, Ruizhu verfasserin aut Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion. PAH speciation (dpeaa)DE-He213 Karst terrain (dpeaa)DE-He213 Soil properties (dpeaa)DE-He213 Organic pollutant (dpeaa)DE-He213 Sun, Yuchuan aut Zheng, Xiaoxuan aut Shen, Licheng aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 9 vom: 09. Juni, Seite 3435-3444 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:9 day:09 month:06 pages:3435-3444 https://dx.doi.org/10.1007/s11368-023-03555-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 9 09 06 3435-3444 |
allfieldsSound |
10.1007/s11368-023-03555-2 doi (DE-627)SPR052792099 (SPR)s11368-023-03555-2-e DE-627 ger DE-627 rakwb eng Shi, Ruizhu verfasserin aut Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion. PAH speciation (dpeaa)DE-He213 Karst terrain (dpeaa)DE-He213 Soil properties (dpeaa)DE-He213 Organic pollutant (dpeaa)DE-He213 Sun, Yuchuan aut Zheng, Xiaoxuan aut Shen, Licheng aut Enthalten in Journal of soils and sediments Berlin : Springer, 2001 23(2023), 9 vom: 09. Juni, Seite 3435-3444 (DE-627)373325134 (DE-600)2125896-X 1614-7480 nnns volume:23 year:2023 number:9 day:09 month:06 pages:3435-3444 https://dx.doi.org/10.1007/s11368-023-03555-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 23 2023 9 09 06 3435-3444 |
language |
English |
source |
Enthalten in Journal of soils and sediments 23(2023), 9 vom: 09. Juni, Seite 3435-3444 volume:23 year:2023 number:9 day:09 month:06 pages:3435-3444 |
sourceStr |
Enthalten in Journal of soils and sediments 23(2023), 9 vom: 09. Juni, Seite 3435-3444 volume:23 year:2023 number:9 day:09 month:06 pages:3435-3444 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
PAH speciation Karst terrain Soil properties Organic pollutant |
isfreeaccess_bool |
false |
container_title |
Journal of soils and sediments |
authorswithroles_txt_mv |
Shi, Ruizhu @@aut@@ Sun, Yuchuan @@aut@@ Zheng, Xiaoxuan @@aut@@ Shen, Licheng @@aut@@ |
publishDateDaySort_date |
2023-06-09T00:00:00Z |
hierarchy_top_id |
373325134 |
id |
SPR052792099 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">SPR052792099</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230819064812.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230819s2023 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11368-023-03555-2</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR052792099</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s11368-023-03555-2-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Shi, Ruizhu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2023</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">PAH speciation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Karst terrain</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Soil properties</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Organic pollutant</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sun, Yuchuan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zheng, Xiaoxuan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Shen, Licheng</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of soils and sediments</subfield><subfield code="d">Berlin : Springer, 2001</subfield><subfield code="g">23(2023), 9 vom: 09. Juni, Seite 3435-3444</subfield><subfield code="w">(DE-627)373325134</subfield><subfield code="w">(DE-600)2125896-X</subfield><subfield code="x">1614-7480</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:23</subfield><subfield code="g">year:2023</subfield><subfield code="g">number:9</subfield><subfield code="g">day:09</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:3435-3444</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s11368-023-03555-2</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_32</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_138</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_171</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_183</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_187</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_250</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_281</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_636</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2001</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2007</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2008</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2009</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2020</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2026</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2031</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2039</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2048</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2049</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2050</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2055</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2056</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2057</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2061</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2088</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2093</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2106</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2107</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2108</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2144</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2188</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2232</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2360</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2446</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2470</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2472</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2507</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2522</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2548</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4246</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4326</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4328</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4334</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4393</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">23</subfield><subfield code="j">2023</subfield><subfield code="e">9</subfield><subfield code="b">09</subfield><subfield code="c">06</subfield><subfield code="h">3435-3444</subfield></datafield></record></collection>
|
author |
Shi, Ruizhu |
spellingShingle |
Shi, Ruizhu misc PAH speciation misc Karst terrain misc Soil properties misc Organic pollutant Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China |
authorStr |
Shi, Ruizhu |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)373325134 |
format |
electronic Article |
delete_txt_mv |
keep |
author_role |
aut aut aut aut |
collection |
springer |
remote_str |
true |
illustrated |
Not Illustrated |
issn |
1614-7480 |
topic_title |
Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China PAH speciation (dpeaa)DE-He213 Karst terrain (dpeaa)DE-He213 Soil properties (dpeaa)DE-He213 Organic pollutant (dpeaa)DE-He213 |
topic |
misc PAH speciation misc Karst terrain misc Soil properties misc Organic pollutant |
topic_unstemmed |
misc PAH speciation misc Karst terrain misc Soil properties misc Organic pollutant |
topic_browse |
misc PAH speciation misc Karst terrain misc Soil properties misc Organic pollutant |
format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
cr |
hierarchy_parent_title |
Journal of soils and sediments |
hierarchy_parent_id |
373325134 |
hierarchy_top_title |
Journal of soils and sediments |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)373325134 (DE-600)2125896-X |
title |
Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China |
ctrlnum |
(DE-627)SPR052792099 (SPR)s11368-023-03555-2-e |
title_full |
Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China |
author_sort |
Shi, Ruizhu |
journal |
Journal of soils and sediments |
journalStr |
Journal of soils and sediments |
lang_code |
eng |
isOA_bool |
false |
recordtype |
marc |
publishDateSort |
2023 |
contenttype_str_mv |
txt |
container_start_page |
3435 |
author_browse |
Shi, Ruizhu Sun, Yuchuan Zheng, Xiaoxuan Shen, Licheng |
container_volume |
23 |
format_se |
Elektronische Aufsätze |
author-letter |
Shi, Ruizhu |
doi_str_mv |
10.1007/s11368-023-03555-2 |
title_sort |
speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest china |
title_auth |
Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China |
abstract |
Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
abstractGer |
Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
abstract_unstemmed |
Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 |
container_issue |
9 |
title_short |
Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China |
url |
https://dx.doi.org/10.1007/s11368-023-03555-2 |
remote_bool |
true |
author2 |
Sun, Yuchuan Zheng, Xiaoxuan Shen, Licheng |
author2Str |
Sun, Yuchuan Zheng, Xiaoxuan Shen, Licheng |
ppnlink |
373325134 |
mediatype_str_mv |
c |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/s11368-023-03555-2 |
up_date |
2024-07-03T14:49:08.166Z |
_version_ |
1803569749738651648 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">SPR052792099</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230819064812.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230819s2023 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11368-023-03555-2</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR052792099</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s11368-023-03555-2-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Shi, Ruizhu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Speciation and influencing factors of polycyclic aromatic hydrocarbons in soils of southwest China</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2023</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Purpose Organic pollutants’ transport, transformation, and biological effectiveness in soils depend mainly on their chemical forms. Therefore, in addition to studying the total content of pollutants, it is essential to understand the forms of organic pollutants in soils. In this study, we measured the speciations of polycyclic aromatic hydrocarbons (PAHs), including desorbing fraction, non-desorbing fraction, and bound residues, in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China. We also investigated the occurrence of PAHs in soils of the region. Moreover, we used principal component analysis (PCA) to analyze the relationship between soil properties and different speciations of PAHs in soils. The contents of ΣPAH16 ranged from 319.69–1215.64 ng/g, with a mean value of 615.02 ng/g. Desorbing fraction PAHs were significant, accounting for 34–81% of the total PAHs. The ratio of different speciations ordered as soluble > organic solvent extracted > bound residues. 2-3-ring were the major components of the total PAHs content in soils and desorbing fraction. PCA analysis determined that soil organic matter (SOM), total nitrogen (TN), and soil bulk density significantly affected the non-desorbing fraction, and pH and total organic carbon (TOC) had a significant positive correlation with the bound residues. The karst area is a complex and fragile ecosystem. The speciation of PAHs in soils is of great importance for assessing their risk and for remediation. However, most studies have focused on the concentration and distribution of PAHs in karst soils. Therefore, in this paper, we investigated the distribution of PAHs in soils in karst areas by investigating the distribution of different speciations of PAHs in soils. We also investigated the key factors influencing the distribution of different speciations. Materials and methods Ten sites were selected in Zhongliangshan karst terrain, where 0–20 cm of soil was collected and the concentrations of 16 PAHs were measured. Three speciations of 16 PAHs in soils were extracted by sequential extraction. And the standard methods recommended by the Chinese Society of Soil Science were used to determine the basic soil properties. Result and discussion In this study, we measured the speciation of PAHs in soil samples from the Zhongliangshan karst terrain in Chongqing, southwest China, including desorbing fraction, non-desorbing fraction, and bound residues. The total content of the 16 PAHs ranged from 319.69 to 1215.64 ng/g, with an average value of 615.02 ng/g. The desorbing fraction was significant, accounting for 34–81% of the total PAHs. The ratio of different speciations is ordered as desorbing fraction > non-desorbing fraction > bound residues. 2–3-ring were the major components of the total PAHs content in soils and each speciation. The PCA results show a significant effect of soil organic matter, TN, and soil bulk density on the non-desorbing fraction. pH and TOC had a relatively significant positive correlation with bound residues. Conclusions This paper investigated the contamination status of PAHs in surface soils in the karst terrain of southwest China, and the speciation of PAHs. Under the special geological structure background in karst areas, studying the occurrence forms and influencing factors of PAHs pollutants in soils is of great significance for a deeper understanding of the occurrence forms of pollutants and effective control of their diffusion.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">PAH speciation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Karst terrain</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Soil properties</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Organic pollutant</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sun, Yuchuan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zheng, Xiaoxuan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Shen, Licheng</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of soils and sediments</subfield><subfield code="d">Berlin : Springer, 2001</subfield><subfield code="g">23(2023), 9 vom: 09. Juni, Seite 3435-3444</subfield><subfield code="w">(DE-627)373325134</subfield><subfield code="w">(DE-600)2125896-X</subfield><subfield code="x">1614-7480</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:23</subfield><subfield code="g">year:2023</subfield><subfield code="g">number:9</subfield><subfield code="g">day:09</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:3435-3444</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s11368-023-03555-2</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_32</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_138</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_171</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_183</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_187</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_250</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_281</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_636</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2001</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2007</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2008</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2009</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2020</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2026</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2031</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2039</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2048</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2049</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2050</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2055</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2056</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2057</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2061</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2088</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2093</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2106</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2107</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2108</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2144</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2188</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2232</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2360</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2446</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2470</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2472</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2507</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2522</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2548</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4246</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4326</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4328</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4334</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4393</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">23</subfield><subfield code="j">2023</subfield><subfield code="e">9</subfield><subfield code="b">09</subfield><subfield code="c">06</subfield><subfield code="h">3435-3444</subfield></datafield></record></collection>
|
score |
7.3993597 |