Thermal degradation features of soil humic acid sub-fractions in pyrolytic treatment and their relation to molecular signatures
Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soi...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Guo, Fei [verfasserIn] Qin, Shuai [verfasserIn] Xu, Lei [verfasserIn] Bai, Yingchen [verfasserIn] Xing, Baoshan [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2020 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: The science of the total environment - Amsterdam [u.a.] : Elsevier Science, 1972, 749 |
|---|---|
| Übergeordnetes Werk: |
volume:749 |
| DOI / URN: |
10.1016/j.scitotenv.2020.142318 |
|---|
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| 520 | |a Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soil source may provide a series of promising objects to understand SOM at molecular level and the resulting patterns in SOM pyrolysis. We first propose a novel insight into pyrolysis mechanism response to molecular signatures using electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with thermogravimetric analysis (TGA) to study six humic acid (HA) sub-fractions extracted from a forest soil. The findings indicate that decomposition of soil HA occurs systematically due to molecular signatures. The decomposition can be categorized as carboxyl controlled (below 280 °C), lipid-dominated (280–450 °C) and condensed aromatics-dominated processes (450–700 °C). Predominant reaction mechanism of all HA sub-fractions was random nucleation (α > 0.25). Lipid in HA tend to initiate multiple nuclei in thermal degradation, while condensed aromatics tend to initiate and grow centering single random point in higher conversion rate (α > 0.75). Bridging the molecular signature and thermogravimetry reveals that the pyrolysis stage below 350 °C should be divided into two distinct processes related to the carboxylic group and lipid compounds, although this stage has conventionally been considered as a single process. The N element of HA was mostly preserved in the condensed aromatics which was mainly pyrolyzed above 450 °C, suggesting that pyrolysis below 450 °C is a preferable remediation treatment considering nitrogen fertility preservation. The observed molecular-level pyrolysis patterns can be applied as a targeted remediation procedure for contaminated soils and can improve the understanding of SOM thermal behaviors at the molecular level. | ||
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| 650 | 4 | |a Humic acid sub-fractions | |
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10.1016/j.scitotenv.2020.142318 doi (DE-627)ELV00486591X (ELSEVIER)S0048-9697(20)35847-2 DE-627 ger DE-627 rda eng 333.7 610 DE-600 43.12 bkl 43.13 bkl 44.13 bkl Guo, Fei verfasserin aut Thermal degradation features of soil humic acid sub-fractions in pyrolytic treatment and their relation to molecular signatures 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soil source may provide a series of promising objects to understand SOM at molecular level and the resulting patterns in SOM pyrolysis. We first propose a novel insight into pyrolysis mechanism response to molecular signatures using electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with thermogravimetric analysis (TGA) to study six humic acid (HA) sub-fractions extracted from a forest soil. The findings indicate that decomposition of soil HA occurs systematically due to molecular signatures. The decomposition can be categorized as carboxyl controlled (below 280 °C), lipid-dominated (280–450 °C) and condensed aromatics-dominated processes (450–700 °C). Predominant reaction mechanism of all HA sub-fractions was random nucleation (α > 0.25). Lipid in HA tend to initiate multiple nuclei in thermal degradation, while condensed aromatics tend to initiate and grow centering single random point in higher conversion rate (α > 0.75). Bridging the molecular signature and thermogravimetry reveals that the pyrolysis stage below 350 °C should be divided into two distinct processes related to the carboxylic group and lipid compounds, although this stage has conventionally been considered as a single process. The N element of HA was mostly preserved in the condensed aromatics which was mainly pyrolyzed above 450 °C, suggesting that pyrolysis below 450 °C is a preferable remediation treatment considering nitrogen fertility preservation. The observed molecular-level pyrolysis patterns can be applied as a targeted remediation procedure for contaminated soils and can improve the understanding of SOM thermal behaviors at the molecular level. Soil Humic acid sub-fractions Thermal feature FT-ICR MS Oil spill Pyrolytic remediation Qin, Shuai verfasserin aut Xu, Lei verfasserin aut Bai, Yingchen verfasserin aut Xing, Baoshan verfasserin (orcid)0000-0003-2028-1295 aut Enthalten in The science of the total environment Amsterdam [u.a.] : Elsevier Science, 1972 749 Online-Ressource (DE-627)306591456 (DE-600)1498726-0 (DE-576)081953178 1879-1026 nnns volume:749 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 43.12 Umweltchemie 43.13 Umwelttoxikologie 44.13 Medizinische Ökologie AR 749 |
| spelling |
10.1016/j.scitotenv.2020.142318 doi (DE-627)ELV00486591X (ELSEVIER)S0048-9697(20)35847-2 DE-627 ger DE-627 rda eng 333.7 610 DE-600 43.12 bkl 43.13 bkl 44.13 bkl Guo, Fei verfasserin aut Thermal degradation features of soil humic acid sub-fractions in pyrolytic treatment and their relation to molecular signatures 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soil source may provide a series of promising objects to understand SOM at molecular level and the resulting patterns in SOM pyrolysis. We first propose a novel insight into pyrolysis mechanism response to molecular signatures using electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with thermogravimetric analysis (TGA) to study six humic acid (HA) sub-fractions extracted from a forest soil. The findings indicate that decomposition of soil HA occurs systematically due to molecular signatures. The decomposition can be categorized as carboxyl controlled (below 280 °C), lipid-dominated (280–450 °C) and condensed aromatics-dominated processes (450–700 °C). Predominant reaction mechanism of all HA sub-fractions was random nucleation (α > 0.25). Lipid in HA tend to initiate multiple nuclei in thermal degradation, while condensed aromatics tend to initiate and grow centering single random point in higher conversion rate (α > 0.75). Bridging the molecular signature and thermogravimetry reveals that the pyrolysis stage below 350 °C should be divided into two distinct processes related to the carboxylic group and lipid compounds, although this stage has conventionally been considered as a single process. The N element of HA was mostly preserved in the condensed aromatics which was mainly pyrolyzed above 450 °C, suggesting that pyrolysis below 450 °C is a preferable remediation treatment considering nitrogen fertility preservation. The observed molecular-level pyrolysis patterns can be applied as a targeted remediation procedure for contaminated soils and can improve the understanding of SOM thermal behaviors at the molecular level. Soil Humic acid sub-fractions Thermal feature FT-ICR MS Oil spill Pyrolytic remediation Qin, Shuai verfasserin aut Xu, Lei verfasserin aut Bai, Yingchen verfasserin aut Xing, Baoshan verfasserin (orcid)0000-0003-2028-1295 aut Enthalten in The science of the total environment Amsterdam [u.a.] : Elsevier Science, 1972 749 Online-Ressource (DE-627)306591456 (DE-600)1498726-0 (DE-576)081953178 1879-1026 nnns volume:749 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 43.12 Umweltchemie 43.13 Umwelttoxikologie 44.13 Medizinische Ökologie AR 749 |
| allfields_unstemmed |
10.1016/j.scitotenv.2020.142318 doi (DE-627)ELV00486591X (ELSEVIER)S0048-9697(20)35847-2 DE-627 ger DE-627 rda eng 333.7 610 DE-600 43.12 bkl 43.13 bkl 44.13 bkl Guo, Fei verfasserin aut Thermal degradation features of soil humic acid sub-fractions in pyrolytic treatment and their relation to molecular signatures 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soil source may provide a series of promising objects to understand SOM at molecular level and the resulting patterns in SOM pyrolysis. We first propose a novel insight into pyrolysis mechanism response to molecular signatures using electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with thermogravimetric analysis (TGA) to study six humic acid (HA) sub-fractions extracted from a forest soil. The findings indicate that decomposition of soil HA occurs systematically due to molecular signatures. The decomposition can be categorized as carboxyl controlled (below 280 °C), lipid-dominated (280–450 °C) and condensed aromatics-dominated processes (450–700 °C). Predominant reaction mechanism of all HA sub-fractions was random nucleation (α > 0.25). Lipid in HA tend to initiate multiple nuclei in thermal degradation, while condensed aromatics tend to initiate and grow centering single random point in higher conversion rate (α > 0.75). Bridging the molecular signature and thermogravimetry reveals that the pyrolysis stage below 350 °C should be divided into two distinct processes related to the carboxylic group and lipid compounds, although this stage has conventionally been considered as a single process. The N element of HA was mostly preserved in the condensed aromatics which was mainly pyrolyzed above 450 °C, suggesting that pyrolysis below 450 °C is a preferable remediation treatment considering nitrogen fertility preservation. The observed molecular-level pyrolysis patterns can be applied as a targeted remediation procedure for contaminated soils and can improve the understanding of SOM thermal behaviors at the molecular level. Soil Humic acid sub-fractions Thermal feature FT-ICR MS Oil spill Pyrolytic remediation Qin, Shuai verfasserin aut Xu, Lei verfasserin aut Bai, Yingchen verfasserin aut Xing, Baoshan verfasserin (orcid)0000-0003-2028-1295 aut Enthalten in The science of the total environment Amsterdam [u.a.] : Elsevier Science, 1972 749 Online-Ressource (DE-627)306591456 (DE-600)1498726-0 (DE-576)081953178 1879-1026 nnns volume:749 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 43.12 Umweltchemie 43.13 Umwelttoxikologie 44.13 Medizinische Ökologie AR 749 |
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10.1016/j.scitotenv.2020.142318 doi (DE-627)ELV00486591X (ELSEVIER)S0048-9697(20)35847-2 DE-627 ger DE-627 rda eng 333.7 610 DE-600 43.12 bkl 43.13 bkl 44.13 bkl Guo, Fei verfasserin aut Thermal degradation features of soil humic acid sub-fractions in pyrolytic treatment and their relation to molecular signatures 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soil source may provide a series of promising objects to understand SOM at molecular level and the resulting patterns in SOM pyrolysis. We first propose a novel insight into pyrolysis mechanism response to molecular signatures using electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with thermogravimetric analysis (TGA) to study six humic acid (HA) sub-fractions extracted from a forest soil. The findings indicate that decomposition of soil HA occurs systematically due to molecular signatures. The decomposition can be categorized as carboxyl controlled (below 280 °C), lipid-dominated (280–450 °C) and condensed aromatics-dominated processes (450–700 °C). Predominant reaction mechanism of all HA sub-fractions was random nucleation (α > 0.25). Lipid in HA tend to initiate multiple nuclei in thermal degradation, while condensed aromatics tend to initiate and grow centering single random point in higher conversion rate (α > 0.75). Bridging the molecular signature and thermogravimetry reveals that the pyrolysis stage below 350 °C should be divided into two distinct processes related to the carboxylic group and lipid compounds, although this stage has conventionally been considered as a single process. The N element of HA was mostly preserved in the condensed aromatics which was mainly pyrolyzed above 450 °C, suggesting that pyrolysis below 450 °C is a preferable remediation treatment considering nitrogen fertility preservation. The observed molecular-level pyrolysis patterns can be applied as a targeted remediation procedure for contaminated soils and can improve the understanding of SOM thermal behaviors at the molecular level. Soil Humic acid sub-fractions Thermal feature FT-ICR MS Oil spill Pyrolytic remediation Qin, Shuai verfasserin aut Xu, Lei verfasserin aut Bai, Yingchen verfasserin aut Xing, Baoshan verfasserin (orcid)0000-0003-2028-1295 aut Enthalten in The science of the total environment Amsterdam [u.a.] : Elsevier Science, 1972 749 Online-Ressource (DE-627)306591456 (DE-600)1498726-0 (DE-576)081953178 1879-1026 nnns volume:749 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 43.12 Umweltchemie 43.13 Umwelttoxikologie 44.13 Medizinische Ökologie AR 749 |
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10.1016/j.scitotenv.2020.142318 doi (DE-627)ELV00486591X (ELSEVIER)S0048-9697(20)35847-2 DE-627 ger DE-627 rda eng 333.7 610 DE-600 43.12 bkl 43.13 bkl 44.13 bkl Guo, Fei verfasserin aut Thermal degradation features of soil humic acid sub-fractions in pyrolytic treatment and their relation to molecular signatures 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soil source may provide a series of promising objects to understand SOM at molecular level and the resulting patterns in SOM pyrolysis. We first propose a novel insight into pyrolysis mechanism response to molecular signatures using electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with thermogravimetric analysis (TGA) to study six humic acid (HA) sub-fractions extracted from a forest soil. The findings indicate that decomposition of soil HA occurs systematically due to molecular signatures. The decomposition can be categorized as carboxyl controlled (below 280 °C), lipid-dominated (280–450 °C) and condensed aromatics-dominated processes (450–700 °C). Predominant reaction mechanism of all HA sub-fractions was random nucleation (α > 0.25). Lipid in HA tend to initiate multiple nuclei in thermal degradation, while condensed aromatics tend to initiate and grow centering single random point in higher conversion rate (α > 0.75). Bridging the molecular signature and thermogravimetry reveals that the pyrolysis stage below 350 °C should be divided into two distinct processes related to the carboxylic group and lipid compounds, although this stage has conventionally been considered as a single process. The N element of HA was mostly preserved in the condensed aromatics which was mainly pyrolyzed above 450 °C, suggesting that pyrolysis below 450 °C is a preferable remediation treatment considering nitrogen fertility preservation. The observed molecular-level pyrolysis patterns can be applied as a targeted remediation procedure for contaminated soils and can improve the understanding of SOM thermal behaviors at the molecular level. Soil Humic acid sub-fractions Thermal feature FT-ICR MS Oil spill Pyrolytic remediation Qin, Shuai verfasserin aut Xu, Lei verfasserin aut Bai, Yingchen verfasserin aut Xing, Baoshan verfasserin (orcid)0000-0003-2028-1295 aut Enthalten in The science of the total environment Amsterdam [u.a.] : Elsevier Science, 1972 749 Online-Ressource (DE-627)306591456 (DE-600)1498726-0 (DE-576)081953178 1879-1026 nnns volume:749 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 43.12 Umweltchemie 43.13 Umwelttoxikologie 44.13 Medizinische Ökologie AR 749 |
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thermal degradation features of soil humic acid sub-fractions in pyrolytic treatment and their relation to molecular signatures |
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Thermal degradation features of soil humic acid sub-fractions in pyrolytic treatment and their relation to molecular signatures |
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Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soil source may provide a series of promising objects to understand SOM at molecular level and the resulting patterns in SOM pyrolysis. We first propose a novel insight into pyrolysis mechanism response to molecular signatures using electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with thermogravimetric analysis (TGA) to study six humic acid (HA) sub-fractions extracted from a forest soil. The findings indicate that decomposition of soil HA occurs systematically due to molecular signatures. The decomposition can be categorized as carboxyl controlled (below 280 °C), lipid-dominated (280–450 °C) and condensed aromatics-dominated processes (450–700 °C). Predominant reaction mechanism of all HA sub-fractions was random nucleation (α > 0.25). Lipid in HA tend to initiate multiple nuclei in thermal degradation, while condensed aromatics tend to initiate and grow centering single random point in higher conversion rate (α > 0.75). Bridging the molecular signature and thermogravimetry reveals that the pyrolysis stage below 350 °C should be divided into two distinct processes related to the carboxylic group and lipid compounds, although this stage has conventionally been considered as a single process. The N element of HA was mostly preserved in the condensed aromatics which was mainly pyrolyzed above 450 °C, suggesting that pyrolysis below 450 °C is a preferable remediation treatment considering nitrogen fertility preservation. The observed molecular-level pyrolysis patterns can be applied as a targeted remediation procedure for contaminated soils and can improve the understanding of SOM thermal behaviors at the molecular level. |
| abstractGer |
Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soil source may provide a series of promising objects to understand SOM at molecular level and the resulting patterns in SOM pyrolysis. We first propose a novel insight into pyrolysis mechanism response to molecular signatures using electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with thermogravimetric analysis (TGA) to study six humic acid (HA) sub-fractions extracted from a forest soil. The findings indicate that decomposition of soil HA occurs systematically due to molecular signatures. The decomposition can be categorized as carboxyl controlled (below 280 °C), lipid-dominated (280–450 °C) and condensed aromatics-dominated processes (450–700 °C). Predominant reaction mechanism of all HA sub-fractions was random nucleation (α > 0.25). Lipid in HA tend to initiate multiple nuclei in thermal degradation, while condensed aromatics tend to initiate and grow centering single random point in higher conversion rate (α > 0.75). Bridging the molecular signature and thermogravimetry reveals that the pyrolysis stage below 350 °C should be divided into two distinct processes related to the carboxylic group and lipid compounds, although this stage has conventionally been considered as a single process. The N element of HA was mostly preserved in the condensed aromatics which was mainly pyrolyzed above 450 °C, suggesting that pyrolysis below 450 °C is a preferable remediation treatment considering nitrogen fertility preservation. The observed molecular-level pyrolysis patterns can be applied as a targeted remediation procedure for contaminated soils and can improve the understanding of SOM thermal behaviors at the molecular level. |
| abstract_unstemmed |
Pyrolysis is a promising treatment for soil remediation for rapidity and fertility preservation. But it is difficult to establish the relationship between pyrolysis behaviors and soil organic matter (SOM) structures, for SOM is a mixture of heterogeneous compounds. HA sub-fractions from the same soil source may provide a series of promising objects to understand SOM at molecular level and the resulting patterns in SOM pyrolysis. We first propose a novel insight into pyrolysis mechanism response to molecular signatures using electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) combined with thermogravimetric analysis (TGA) to study six humic acid (HA) sub-fractions extracted from a forest soil. The findings indicate that decomposition of soil HA occurs systematically due to molecular signatures. The decomposition can be categorized as carboxyl controlled (below 280 °C), lipid-dominated (280–450 °C) and condensed aromatics-dominated processes (450–700 °C). Predominant reaction mechanism of all HA sub-fractions was random nucleation (α > 0.25). Lipid in HA tend to initiate multiple nuclei in thermal degradation, while condensed aromatics tend to initiate and grow centering single random point in higher conversion rate (α > 0.75). Bridging the molecular signature and thermogravimetry reveals that the pyrolysis stage below 350 °C should be divided into two distinct processes related to the carboxylic group and lipid compounds, although this stage has conventionally been considered as a single process. The N element of HA was mostly preserved in the condensed aromatics which was mainly pyrolyzed above 450 °C, suggesting that pyrolysis below 450 °C is a preferable remediation treatment considering nitrogen fertility preservation. The observed molecular-level pyrolysis patterns can be applied as a targeted remediation procedure for contaminated soils and can improve the understanding of SOM thermal behaviors at the molecular level. |
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| score |
7.400467 |