Can soil respiration estimate neglect the contribution of abiotic exchange?
Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on fl...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Chen, Xi [verfasserIn] |
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E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013 |
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| Schlagwörter: |
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| Anmerkung: |
© Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of Arid Land - SP Science Press, 2012, 6(2013), 2 vom: 06. Sept., Seite 129-135 |
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| Übergeordnetes Werk: |
volume:6 ; year:2013 ; number:2 ; day:06 ; month:09 ; pages:129-135 |
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| DOI / URN: |
10.1007/s40333-013-0244-1 |
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SPR037156667 |
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| 520 | |a Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. Neglecting the abiotic module may result in overestimates of soil respiration in arid alkaline lands, which partly explains the long-sought “missing carbon sink”. | ||
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10.1007/s40333-013-0244-1 doi (DE-627)SPR037156667 (SPR)s40333-013-0244-1-e DE-627 ger DE-627 rakwb eng Chen, Xi verfasserin aut Can soil respiration estimate neglect the contribution of abiotic exchange? 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014 Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. Neglecting the abiotic module may result in overestimates of soil respiration in arid alkaline lands, which partly explains the long-sought “missing carbon sink”. soil respiration (dpeaa)DE-He213 abiotic exchange (dpeaa)DE-He213 hypothetical system (dpeaa)DE-He213 incorporated model (dpeaa)DE-He213 missing carbon sink (dpeaa)DE-He213 Wang, WenFeng aut Luo, GePing aut Ye, Hui aut Enthalten in Journal of Arid Land SP Science Press, 2012 6(2013), 2 vom: 06. Sept., Seite 129-135 (DE-627)SPR037155849 nnns volume:6 year:2013 number:2 day:06 month:09 pages:129-135 https://dx.doi.org/10.1007/s40333-013-0244-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_22 AR 6 2013 2 06 09 129-135 |
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10.1007/s40333-013-0244-1 doi (DE-627)SPR037156667 (SPR)s40333-013-0244-1-e DE-627 ger DE-627 rakwb eng Chen, Xi verfasserin aut Can soil respiration estimate neglect the contribution of abiotic exchange? 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014 Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. Neglecting the abiotic module may result in overestimates of soil respiration in arid alkaline lands, which partly explains the long-sought “missing carbon sink”. soil respiration (dpeaa)DE-He213 abiotic exchange (dpeaa)DE-He213 hypothetical system (dpeaa)DE-He213 incorporated model (dpeaa)DE-He213 missing carbon sink (dpeaa)DE-He213 Wang, WenFeng aut Luo, GePing aut Ye, Hui aut Enthalten in Journal of Arid Land SP Science Press, 2012 6(2013), 2 vom: 06. Sept., Seite 129-135 (DE-627)SPR037155849 nnns volume:6 year:2013 number:2 day:06 month:09 pages:129-135 https://dx.doi.org/10.1007/s40333-013-0244-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_22 AR 6 2013 2 06 09 129-135 |
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10.1007/s40333-013-0244-1 doi (DE-627)SPR037156667 (SPR)s40333-013-0244-1-e DE-627 ger DE-627 rakwb eng Chen, Xi verfasserin aut Can soil respiration estimate neglect the contribution of abiotic exchange? 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014 Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. Neglecting the abiotic module may result in overestimates of soil respiration in arid alkaline lands, which partly explains the long-sought “missing carbon sink”. soil respiration (dpeaa)DE-He213 abiotic exchange (dpeaa)DE-He213 hypothetical system (dpeaa)DE-He213 incorporated model (dpeaa)DE-He213 missing carbon sink (dpeaa)DE-He213 Wang, WenFeng aut Luo, GePing aut Ye, Hui aut Enthalten in Journal of Arid Land SP Science Press, 2012 6(2013), 2 vom: 06. Sept., Seite 129-135 (DE-627)SPR037155849 nnns volume:6 year:2013 number:2 day:06 month:09 pages:129-135 https://dx.doi.org/10.1007/s40333-013-0244-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_22 AR 6 2013 2 06 09 129-135 |
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10.1007/s40333-013-0244-1 doi (DE-627)SPR037156667 (SPR)s40333-013-0244-1-e DE-627 ger DE-627 rakwb eng Chen, Xi verfasserin aut Can soil respiration estimate neglect the contribution of abiotic exchange? 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014 Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. Neglecting the abiotic module may result in overestimates of soil respiration in arid alkaline lands, which partly explains the long-sought “missing carbon sink”. soil respiration (dpeaa)DE-He213 abiotic exchange (dpeaa)DE-He213 hypothetical system (dpeaa)DE-He213 incorporated model (dpeaa)DE-He213 missing carbon sink (dpeaa)DE-He213 Wang, WenFeng aut Luo, GePing aut Ye, Hui aut Enthalten in Journal of Arid Land SP Science Press, 2012 6(2013), 2 vom: 06. Sept., Seite 129-135 (DE-627)SPR037155849 nnns volume:6 year:2013 number:2 day:06 month:09 pages:129-135 https://dx.doi.org/10.1007/s40333-013-0244-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_22 AR 6 2013 2 06 09 129-135 |
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10.1007/s40333-013-0244-1 doi (DE-627)SPR037156667 (SPR)s40333-013-0244-1-e DE-627 ger DE-627 rakwb eng Chen, Xi verfasserin aut Can soil respiration estimate neglect the contribution of abiotic exchange? 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014 Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. Neglecting the abiotic module may result in overestimates of soil respiration in arid alkaline lands, which partly explains the long-sought “missing carbon sink”. soil respiration (dpeaa)DE-He213 abiotic exchange (dpeaa)DE-He213 hypothetical system (dpeaa)DE-He213 incorporated model (dpeaa)DE-He213 missing carbon sink (dpeaa)DE-He213 Wang, WenFeng aut Luo, GePing aut Ye, Hui aut Enthalten in Journal of Arid Land SP Science Press, 2012 6(2013), 2 vom: 06. Sept., Seite 129-135 (DE-627)SPR037155849 nnns volume:6 year:2013 number:2 day:06 month:09 pages:129-135 https://dx.doi.org/10.1007/s40333-013-0244-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_22 AR 6 2013 2 06 09 129-135 |
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Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. Neglecting the abiotic module may result in overestimates of soil respiration in arid alkaline lands, which partly explains the long-sought “missing carbon sink”. © Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014 |
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Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. Neglecting the abiotic module may result in overestimates of soil respiration in arid alkaline lands, which partly explains the long-sought “missing carbon sink”. © Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014 |
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Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. Neglecting the abiotic module may result in overestimates of soil respiration in arid alkaline lands, which partly explains the long-sought “missing carbon sink”. © Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR037156667</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230328170117.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2013 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s40333-013-0244-1</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR037156667</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s40333-013-0244-1-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Chen, Xi</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Can soil respiration estimate neglect the contribution of abiotic exchange?</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2013</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Science Press, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences and Springer-Verlag Berlin Heidelberg 2014</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract This study examines the hypothesis that soil respiration can always be interpreted purely in terms of biotic processes, neglecting the contribution of abiotic exchange to $ CO_{2} $ fluxes in alkaline soils of arid areas that characterize 5% of the Earth’s total land surface. Analyses on flux data collected from previous studies suggested reconciling soil respiration as organic (root/microbial respiration) and inorganic (abiotic $ CO_{2} $ exchange) respiration, whose contributions in the total $ CO_{2} $ flux were determined by soil alkaline content. On the basis of utilizing meteorological and soil data collected from the Xinjiang and Central Asia Scientific Data Sharing Platform, an incorporated model indicated that inorganic respiration represents almost half of the total $ CO_{2} $ flux. 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Sept., Seite 129-135</subfield><subfield code="w">(DE-627)SPR037155849</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:6</subfield><subfield code="g">year:2013</subfield><subfield code="g">number:2</subfield><subfield code="g">day:06</subfield><subfield code="g">month:09</subfield><subfield code="g">pages:129-135</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s40333-013-0244-1</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_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">6</subfield><subfield code="j">2013</subfield><subfield code="e">2</subfield><subfield code="b">06</subfield><subfield code="c">09</subfield><subfield code="h">129-135</subfield></datafield></record></collection>
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