Geochemistry of organic matter in river waters of the Amur basin, Russia
Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Levshina, S. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2016 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 75(2016), 5 vom: 24. Feb. |
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| Übergeordnetes Werk: |
volume:75 ; year:2016 ; number:5 ; day:24 ; month:02 |
| Links: |
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| DOI / URN: |
10.1007/s12665-015-5202-0 |
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| Katalog-ID: |
SPR026727005 |
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| 520 | |a Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. In the summer of 2011 and 2012, fluxes of TOC over the Amur River to the Amur Liman were 9.168 × $ 10^{3} $ and 11.029 × $ 10^{3} $ t C/day, respectively. | ||
| 650 | 4 | |a River water |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Organic matter |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Humic substances |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Suspended matter |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Organic matter flux |7 (dpeaa)DE-He213 | |
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10.1007/s12665-015-5202-0 doi (DE-627)SPR026727005 (SPR)s12665-015-5202-0-e DE-627 ger DE-627 rakwb eng Levshina, S. verfasserin (orcid)0000-0003-3748-1138 aut Geochemistry of organic matter in river waters of the Amur basin, Russia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. In the summer of 2011 and 2012, fluxes of TOC over the Amur River to the Amur Liman were 9.168 × $ 10^{3} $ and 11.029 × $ 10^{3} $ t C/day, respectively. River water (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Humic substances (dpeaa)DE-He213 Suspended matter (dpeaa)DE-He213 Organic matter flux (dpeaa)DE-He213 Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 5 vom: 24. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:5 day:24 month:02 https://dx.doi.org/10.1007/s12665-015-5202-0 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_4012 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 5 24 02 |
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10.1007/s12665-015-5202-0 doi (DE-627)SPR026727005 (SPR)s12665-015-5202-0-e DE-627 ger DE-627 rakwb eng Levshina, S. verfasserin (orcid)0000-0003-3748-1138 aut Geochemistry of organic matter in river waters of the Amur basin, Russia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. In the summer of 2011 and 2012, fluxes of TOC over the Amur River to the Amur Liman were 9.168 × $ 10^{3} $ and 11.029 × $ 10^{3} $ t C/day, respectively. River water (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Humic substances (dpeaa)DE-He213 Suspended matter (dpeaa)DE-He213 Organic matter flux (dpeaa)DE-He213 Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 5 vom: 24. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:5 day:24 month:02 https://dx.doi.org/10.1007/s12665-015-5202-0 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_4012 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 5 24 02 |
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10.1007/s12665-015-5202-0 doi (DE-627)SPR026727005 (SPR)s12665-015-5202-0-e DE-627 ger DE-627 rakwb eng Levshina, S. verfasserin (orcid)0000-0003-3748-1138 aut Geochemistry of organic matter in river waters of the Amur basin, Russia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. In the summer of 2011 and 2012, fluxes of TOC over the Amur River to the Amur Liman were 9.168 × $ 10^{3} $ and 11.029 × $ 10^{3} $ t C/day, respectively. River water (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Humic substances (dpeaa)DE-He213 Suspended matter (dpeaa)DE-He213 Organic matter flux (dpeaa)DE-He213 Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 5 vom: 24. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:5 day:24 month:02 https://dx.doi.org/10.1007/s12665-015-5202-0 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_4012 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 5 24 02 |
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10.1007/s12665-015-5202-0 doi (DE-627)SPR026727005 (SPR)s12665-015-5202-0-e DE-627 ger DE-627 rakwb eng Levshina, S. verfasserin (orcid)0000-0003-3748-1138 aut Geochemistry of organic matter in river waters of the Amur basin, Russia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. In the summer of 2011 and 2012, fluxes of TOC over the Amur River to the Amur Liman were 9.168 × $ 10^{3} $ and 11.029 × $ 10^{3} $ t C/day, respectively. River water (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Humic substances (dpeaa)DE-He213 Suspended matter (dpeaa)DE-He213 Organic matter flux (dpeaa)DE-He213 Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 5 vom: 24. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:5 day:24 month:02 https://dx.doi.org/10.1007/s12665-015-5202-0 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_4012 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 5 24 02 |
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10.1007/s12665-015-5202-0 doi (DE-627)SPR026727005 (SPR)s12665-015-5202-0-e DE-627 ger DE-627 rakwb eng Levshina, S. verfasserin (orcid)0000-0003-3748-1138 aut Geochemistry of organic matter in river waters of the Amur basin, Russia 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. In the summer of 2011 and 2012, fluxes of TOC over the Amur River to the Amur Liman were 9.168 × $ 10^{3} $ and 11.029 × $ 10^{3} $ t C/day, respectively. River water (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Humic substances (dpeaa)DE-He213 Suspended matter (dpeaa)DE-He213 Organic matter flux (dpeaa)DE-He213 Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 5 vom: 24. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:5 day:24 month:02 https://dx.doi.org/10.1007/s12665-015-5202-0 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_4012 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 5 24 02 |
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The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. 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Levshina, S. |
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Levshina, S. misc River water misc Organic matter misc Humic substances misc Suspended matter misc Organic matter flux Geochemistry of organic matter in river waters of the Amur basin, Russia |
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Geochemistry of organic matter in river waters of the Amur basin, Russia River water (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Humic substances (dpeaa)DE-He213 Suspended matter (dpeaa)DE-He213 Organic matter flux (dpeaa)DE-He213 |
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Geochemistry of organic matter in river waters of the Amur basin, Russia |
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Environmental earth sciences |
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geochemistry of organic matter in river waters of the amur basin, russia |
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Geochemistry of organic matter in river waters of the Amur basin, Russia |
| abstract |
Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. In the summer of 2011 and 2012, fluxes of TOC over the Amur River to the Amur Liman were 9.168 × $ 10^{3} $ and 11.029 × $ 10^{3} $ t C/day, respectively. © Springer-Verlag Berlin Heidelberg 2016 |
| abstractGer |
Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. In the summer of 2011 and 2012, fluxes of TOC over the Amur River to the Amur Liman were 9.168 × $ 10^{3} $ and 11.029 × $ 10^{3} $ t C/day, respectively. © Springer-Verlag Berlin Heidelberg 2016 |
| abstract_unstemmed |
Abstract Organic matter (OM) plays an important role in the biochemical C cycle and in river waters, in particular. The paper considers a huge area of the Amur basin and its subbasins. The concentrations and distribution of OM in river waters were investigated during the summer of 2008 and 2010–2012. The conducted studies identified total, dissolved and particulate organic carbon (TOC, DOC and POC), humic substances (HS)–humic acids (HA) and fulvic acids (FA), and suspended matter (SM). It was established that concentrations of OM vary significantly along the river flow and hydrological cross sections due to inflows from major tributaries originated in various physio-geographical zones. The results showed that concentrations of TOC varied from two to several tens of mg C/L, but were dominantly high. In the Upper Amur basin water, concentrations of DOC were dominant; the amount of HS was 17–48 % of DOC. Upstream of the Songhua mouth, the amount of HS (up to 60 % of DOC) was mainly due to inflows from the Zeya and Bureya running over the taiga zone. High concentrations of OM and SM were detected in the water discharge from the Songhua, the amount of HS accounted for 20 % of DOC. In the Ussuri basin, formed in the coniferous broad-leaved forest zone, concentrations of OM were lower compared to the Amur water. In the summer of 2011 and 2012, fluxes of TOC over the Amur River to the Amur Liman were 9.168 × $ 10^{3} $ and 11.029 × $ 10^{3} $ t C/day, respectively. © Springer-Verlag Berlin Heidelberg 2016 |
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Geochemistry of organic matter in river waters of the Amur basin, Russia |
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https://dx.doi.org/10.1007/s12665-015-5202-0 |
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10.1007/s12665-015-5202-0 |
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| score |
7.399846 |