Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing
Abstract To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes...
Ausführliche Beschreibung
Autor*in: |
Morgalev, Sergey Yu [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2022 |
---|
Schlagwörter: |
---|
Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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: Environmental science and pollution research - Springer Berlin Heidelberg, 1994, 30(2022), 1 vom: 29. Juli, Seite 823-836 |
---|---|
Übergeordnetes Werk: |
volume:30 ; year:2022 ; number:1 ; day:29 ; month:07 ; pages:823-836 |
Links: |
---|
DOI / URN: |
10.1007/s11356-022-22219-1 |
---|
Katalog-ID: |
OLC2080231863 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2080231863 | ||
003 | DE-627 | ||
005 | 20230606195406.0 | ||
007 | tu | ||
008 | 230131s2022 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/s11356-022-22219-1 |2 doi | |
035 | |a (DE-627)OLC2080231863 | ||
035 | |a (DE-He213)s11356-022-22219-1-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 570 |a 360 |a 333.7 |q VZ |
082 | 0 | 4 | |a 690 |a 333.7 |a 540 |q VZ |
084 | |a BIODIV |q DE-30 |2 fid | ||
100 | 1 | |a Morgalev, Sergey Yu |e verfasserin |4 aut | |
245 | 1 | 0 | |a Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing |
264 | 1 | |c 2022 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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 Abstract To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted. | ||
650 | 4 | |a Peat | |
650 | 4 | |a Pore water | |
650 | 4 | |a Freezing | |
650 | 4 | |a Thawing | |
650 | 4 | |a Major | |
650 | 4 | |a Trace elements | |
650 | 4 | |a Nutrients | |
650 | 4 | |a Toxicants | |
650 | 4 | |a Microorganisms | |
700 | 1 | |a Lim, Artem G. |4 aut | |
700 | 1 | |a Morgaleva, Tamara G. |4 aut | |
700 | 1 | |a Morgalev, Yuri N. |4 aut | |
700 | 1 | |a Manasypov, Rinat M. |4 aut | |
700 | 1 | |a Kuzmina, Daria |4 aut | |
700 | 1 | |a Shirokova, Liudmila S. |4 aut | |
700 | 1 | |a Orgogozo, Laurent |4 aut | |
700 | 1 | |a Loiko, Sergey V. |4 aut | |
700 | 1 | |a Pokrovsky, Oleg S. |0 (orcid)0000-0002-3155-7069 |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Environmental science and pollution research |d Springer Berlin Heidelberg, 1994 |g 30(2022), 1 vom: 29. Juli, Seite 823-836 |w (DE-627)171335805 |w (DE-600)1178791-0 |w (DE-576)038875101 |x 0944-1344 |7 nnns |
773 | 1 | 8 | |g volume:30 |g year:2022 |g number:1 |g day:29 |g month:07 |g pages:823-836 |
856 | 4 | 1 | |u https://doi.org/10.1007/s11356-022-22219-1 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a FID-BIODIV | ||
912 | |a SSG-OLC-UMW | ||
912 | |a SSG-OLC-ARC | ||
912 | |a SSG-OLC-TEC | ||
912 | |a SSG-OLC-CHE | ||
912 | |a SSG-OLC-FOR | ||
912 | |a SSG-OLC-DE-84 | ||
912 | |a GBV_ILN_252 | ||
912 | |a GBV_ILN_267 | ||
912 | |a GBV_ILN_2018 | ||
912 | |a GBV_ILN_4277 | ||
951 | |a AR | ||
952 | |d 30 |j 2022 |e 1 |b 29 |c 07 |h 823-836 |
author_variant |
s y m sy sym a g l ag agl t g m tg tgm y n m yn ynm r m m rm rmm d k dk l s s ls lss l o lo s v l sv svl o s p os osp |
---|---|
matchkey_str |
article:09441344:2022----::rcintooogncntinseasnbceiipaprwtrni |
hierarchy_sort_str |
2022 |
publishDate |
2022 |
allfields |
10.1007/s11356-022-22219-1 doi (DE-627)OLC2080231863 (DE-He213)s11356-022-22219-1-p DE-627 ger DE-627 rakwb eng 570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Morgalev, Sergey Yu verfasserin aut Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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 To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted. Peat Pore water Freezing Thawing Major Trace elements Nutrients Toxicants Microorganisms Lim, Artem G. aut Morgaleva, Tamara G. aut Morgalev, Yuri N. aut Manasypov, Rinat M. aut Kuzmina, Daria aut Shirokova, Liudmila S. aut Orgogozo, Laurent aut Loiko, Sergey V. aut Pokrovsky, Oleg S. (orcid)0000-0002-3155-7069 aut Enthalten in Environmental science and pollution research Springer Berlin Heidelberg, 1994 30(2022), 1 vom: 29. Juli, Seite 823-836 (DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 0944-1344 nnns volume:30 year:2022 number:1 day:29 month:07 pages:823-836 https://doi.org/10.1007/s11356-022-22219-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 30 2022 1 29 07 823-836 |
spelling |
10.1007/s11356-022-22219-1 doi (DE-627)OLC2080231863 (DE-He213)s11356-022-22219-1-p DE-627 ger DE-627 rakwb eng 570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Morgalev, Sergey Yu verfasserin aut Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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 To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted. Peat Pore water Freezing Thawing Major Trace elements Nutrients Toxicants Microorganisms Lim, Artem G. aut Morgaleva, Tamara G. aut Morgalev, Yuri N. aut Manasypov, Rinat M. aut Kuzmina, Daria aut Shirokova, Liudmila S. aut Orgogozo, Laurent aut Loiko, Sergey V. aut Pokrovsky, Oleg S. (orcid)0000-0002-3155-7069 aut Enthalten in Environmental science and pollution research Springer Berlin Heidelberg, 1994 30(2022), 1 vom: 29. Juli, Seite 823-836 (DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 0944-1344 nnns volume:30 year:2022 number:1 day:29 month:07 pages:823-836 https://doi.org/10.1007/s11356-022-22219-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 30 2022 1 29 07 823-836 |
allfields_unstemmed |
10.1007/s11356-022-22219-1 doi (DE-627)OLC2080231863 (DE-He213)s11356-022-22219-1-p DE-627 ger DE-627 rakwb eng 570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Morgalev, Sergey Yu verfasserin aut Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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 To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted. Peat Pore water Freezing Thawing Major Trace elements Nutrients Toxicants Microorganisms Lim, Artem G. aut Morgaleva, Tamara G. aut Morgalev, Yuri N. aut Manasypov, Rinat M. aut Kuzmina, Daria aut Shirokova, Liudmila S. aut Orgogozo, Laurent aut Loiko, Sergey V. aut Pokrovsky, Oleg S. (orcid)0000-0002-3155-7069 aut Enthalten in Environmental science and pollution research Springer Berlin Heidelberg, 1994 30(2022), 1 vom: 29. Juli, Seite 823-836 (DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 0944-1344 nnns volume:30 year:2022 number:1 day:29 month:07 pages:823-836 https://doi.org/10.1007/s11356-022-22219-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 30 2022 1 29 07 823-836 |
allfieldsGer |
10.1007/s11356-022-22219-1 doi (DE-627)OLC2080231863 (DE-He213)s11356-022-22219-1-p DE-627 ger DE-627 rakwb eng 570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Morgalev, Sergey Yu verfasserin aut Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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 To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted. Peat Pore water Freezing Thawing Major Trace elements Nutrients Toxicants Microorganisms Lim, Artem G. aut Morgaleva, Tamara G. aut Morgalev, Yuri N. aut Manasypov, Rinat M. aut Kuzmina, Daria aut Shirokova, Liudmila S. aut Orgogozo, Laurent aut Loiko, Sergey V. aut Pokrovsky, Oleg S. (orcid)0000-0002-3155-7069 aut Enthalten in Environmental science and pollution research Springer Berlin Heidelberg, 1994 30(2022), 1 vom: 29. Juli, Seite 823-836 (DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 0944-1344 nnns volume:30 year:2022 number:1 day:29 month:07 pages:823-836 https://doi.org/10.1007/s11356-022-22219-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 30 2022 1 29 07 823-836 |
allfieldsSound |
10.1007/s11356-022-22219-1 doi (DE-627)OLC2080231863 (DE-He213)s11356-022-22219-1-p DE-627 ger DE-627 rakwb eng 570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Morgalev, Sergey Yu verfasserin aut Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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 To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted. Peat Pore water Freezing Thawing Major Trace elements Nutrients Toxicants Microorganisms Lim, Artem G. aut Morgaleva, Tamara G. aut Morgalev, Yuri N. aut Manasypov, Rinat M. aut Kuzmina, Daria aut Shirokova, Liudmila S. aut Orgogozo, Laurent aut Loiko, Sergey V. aut Pokrovsky, Oleg S. (orcid)0000-0002-3155-7069 aut Enthalten in Environmental science and pollution research Springer Berlin Heidelberg, 1994 30(2022), 1 vom: 29. Juli, Seite 823-836 (DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 0944-1344 nnns volume:30 year:2022 number:1 day:29 month:07 pages:823-836 https://doi.org/10.1007/s11356-022-22219-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 30 2022 1 29 07 823-836 |
language |
English |
source |
Enthalten in Environmental science and pollution research 30(2022), 1 vom: 29. Juli, Seite 823-836 volume:30 year:2022 number:1 day:29 month:07 pages:823-836 |
sourceStr |
Enthalten in Environmental science and pollution research 30(2022), 1 vom: 29. Juli, Seite 823-836 volume:30 year:2022 number:1 day:29 month:07 pages:823-836 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Peat Pore water Freezing Thawing Major Trace elements Nutrients Toxicants Microorganisms |
dewey-raw |
570 |
isfreeaccess_bool |
false |
container_title |
Environmental science and pollution research |
authorswithroles_txt_mv |
Morgalev, Sergey Yu @@aut@@ Lim, Artem G. @@aut@@ Morgaleva, Tamara G. @@aut@@ Morgalev, Yuri N. @@aut@@ Manasypov, Rinat M. @@aut@@ Kuzmina, Daria @@aut@@ Shirokova, Liudmila S. @@aut@@ Orgogozo, Laurent @@aut@@ Loiko, Sergey V. @@aut@@ Pokrovsky, Oleg S. @@aut@@ |
publishDateDaySort_date |
2022-07-29T00:00:00Z |
hierarchy_top_id |
171335805 |
dewey-sort |
3570 |
id |
OLC2080231863 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2080231863</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230606195406.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">230131s2022 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11356-022-22219-1</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2080231863</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11356-022-22219-1-p</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="082" ind1="0" ind2="4"><subfield code="a">570</subfield><subfield code="a">360</subfield><subfield code="a">333.7</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">690</subfield><subfield code="a">333.7</subfield><subfield code="a">540</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">BIODIV</subfield><subfield code="q">DE-30</subfield><subfield code="2">fid</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Morgalev, Sergey Yu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</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 2022. Springer Nature or its licensor 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">Abstract To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Peat</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pore water</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Freezing</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Thawing</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Major</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Trace elements</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nutrients</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Toxicants</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Microorganisms</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lim, Artem G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Morgaleva, Tamara G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Morgalev, Yuri N.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Manasypov, Rinat M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kuzmina, Daria</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Shirokova, Liudmila S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Orgogozo, Laurent</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Loiko, Sergey V.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Pokrovsky, Oleg S.</subfield><subfield code="0">(orcid)0000-0002-3155-7069</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Environmental science and pollution research</subfield><subfield code="d">Springer Berlin Heidelberg, 1994</subfield><subfield code="g">30(2022), 1 vom: 29. Juli, Seite 823-836</subfield><subfield code="w">(DE-627)171335805</subfield><subfield code="w">(DE-600)1178791-0</subfield><subfield code="w">(DE-576)038875101</subfield><subfield code="x">0944-1344</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:30</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:1</subfield><subfield code="g">day:29</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:823-836</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11356-022-22219-1</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_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-BIODIV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-UMW</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-ARC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-TEC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_252</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4277</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">30</subfield><subfield code="j">2022</subfield><subfield code="e">1</subfield><subfield code="b">29</subfield><subfield code="c">07</subfield><subfield code="h">823-836</subfield></datafield></record></collection>
|
author |
Morgalev, Sergey Yu |
spellingShingle |
Morgalev, Sergey Yu ddc 570 ddc 690 fid BIODIV misc Peat misc Pore water misc Freezing misc Thawing misc Major misc Trace elements misc Nutrients misc Toxicants misc Microorganisms Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing |
authorStr |
Morgalev, Sergey Yu |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)171335805 |
format |
Article |
dewey-ones |
570 - Life sciences; biology 360 - Social problems & services; associations 333 - Economics of land & energy 690 - Buildings 540 - Chemistry & allied sciences |
delete_txt_mv |
keep |
author_role |
aut aut aut aut aut aut aut aut aut aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0944-1344 |
topic_title |
570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing Peat Pore water Freezing Thawing Major Trace elements Nutrients Toxicants Microorganisms |
topic |
ddc 570 ddc 690 fid BIODIV misc Peat misc Pore water misc Freezing misc Thawing misc Major misc Trace elements misc Nutrients misc Toxicants misc Microorganisms |
topic_unstemmed |
ddc 570 ddc 690 fid BIODIV misc Peat misc Pore water misc Freezing misc Thawing misc Major misc Trace elements misc Nutrients misc Toxicants misc Microorganisms |
topic_browse |
ddc 570 ddc 690 fid BIODIV misc Peat misc Pore water misc Freezing misc Thawing misc Major misc Trace elements misc Nutrients misc Toxicants misc Microorganisms |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Environmental science and pollution research |
hierarchy_parent_id |
171335805 |
dewey-tens |
570 - Life sciences; biology 360 - Social problems & social services 330 - Economics 690 - Building & construction 540 - Chemistry |
hierarchy_top_title |
Environmental science and pollution research |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 |
title |
Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing |
ctrlnum |
(DE-627)OLC2080231863 (DE-He213)s11356-022-22219-1-p |
title_full |
Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing |
author_sort |
Morgalev, Sergey Yu |
journal |
Environmental science and pollution research |
journalStr |
Environmental science and pollution research |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science 300 - Social sciences 600 - Technology |
recordtype |
marc |
publishDateSort |
2022 |
contenttype_str_mv |
txt |
container_start_page |
823 |
author_browse |
Morgalev, Sergey Yu Lim, Artem G. Morgaleva, Tamara G. Morgalev, Yuri N. Manasypov, Rinat M. Kuzmina, Daria Shirokova, Liudmila S. Orgogozo, Laurent Loiko, Sergey V. Pokrovsky, Oleg S. |
container_volume |
30 |
class |
570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid |
format_se |
Aufsätze |
author-letter |
Morgalev, Sergey Yu |
doi_str_mv |
10.1007/s11356-022-22219-1 |
normlink |
(ORCID)0000-0002-3155-7069 |
normlink_prefix_str_mv |
(orcid)0000-0002-3155-7069 |
dewey-full |
570 360 333.7 690 540 |
title_sort |
fractionation of organic c, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing |
title_auth |
Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing |
abstract |
Abstract To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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 |
Abstract To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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 |
Abstract To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022. Springer Nature or its licensor 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_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 |
container_issue |
1 |
title_short |
Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing |
url |
https://doi.org/10.1007/s11356-022-22219-1 |
remote_bool |
false |
author2 |
Lim, Artem G. Morgaleva, Tamara G. Morgalev, Yuri N. Manasypov, Rinat M. Kuzmina, Daria Shirokova, Liudmila S. Orgogozo, Laurent Loiko, Sergey V. Pokrovsky, Oleg S. |
author2Str |
Lim, Artem G. Morgaleva, Tamara G. Morgalev, Yuri N. Manasypov, Rinat M. Kuzmina, Daria Shirokova, Liudmila S. Orgogozo, Laurent Loiko, Sergey V. Pokrovsky, Oleg S. |
ppnlink |
171335805 |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/s11356-022-22219-1 |
up_date |
2024-07-04T03:17:01.511Z |
_version_ |
1803616802851258368 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2080231863</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230606195406.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">230131s2022 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11356-022-22219-1</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2080231863</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11356-022-22219-1-p</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="082" ind1="0" ind2="4"><subfield code="a">570</subfield><subfield code="a">360</subfield><subfield code="a">333.7</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">690</subfield><subfield code="a">333.7</subfield><subfield code="a">540</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">BIODIV</subfield><subfield code="q">DE-30</subfield><subfield code="2">fid</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Morgalev, Sergey Yu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</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 2022. Springer Nature or its licensor 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">Abstract To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Peat</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pore water</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Freezing</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Thawing</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Major</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Trace elements</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nutrients</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Toxicants</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Microorganisms</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lim, Artem G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Morgaleva, Tamara G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Morgalev, Yuri N.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Manasypov, Rinat M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kuzmina, Daria</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Shirokova, Liudmila S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Orgogozo, Laurent</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Loiko, Sergey V.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Pokrovsky, Oleg S.</subfield><subfield code="0">(orcid)0000-0002-3155-7069</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Environmental science and pollution research</subfield><subfield code="d">Springer Berlin Heidelberg, 1994</subfield><subfield code="g">30(2022), 1 vom: 29. Juli, Seite 823-836</subfield><subfield code="w">(DE-627)171335805</subfield><subfield code="w">(DE-600)1178791-0</subfield><subfield code="w">(DE-576)038875101</subfield><subfield code="x">0944-1344</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:30</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:1</subfield><subfield code="g">day:29</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:823-836</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11356-022-22219-1</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_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-BIODIV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-UMW</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-ARC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-TEC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_252</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4277</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">30</subfield><subfield code="j">2022</subfield><subfield code="e">1</subfield><subfield code="b">29</subfield><subfield code="c">07</subfield><subfield code="h">823-836</subfield></datafield></record></collection>
|
score |
7.4002314 |