Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field

Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperat...
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Autor*in:	Chen, Zhaozhi [verfasserIn] Wang, Bingyu [verfasserIn] Wang, Jinyang [verfasserIn] Pan, Genxing [verfasserIn] Xiong, Zhengqin [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2016

Schlagwörter:	Soil organic matter decomposition Soil organic matter quality Temperature sensitivity Paddy field Global change

Übergeordnetes Werk:	Enthalten in: Environmental monitoring and assessment - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981, 188(2016), 10 vom: 02. Sept.
Übergeordnetes Werk:	volume:188 ; year:2016 ; number:10 ; day:02 ; month:09

Links:	Volltext

DOI / URN:	10.1007/s10661-016-5563-1

Katalog-ID:	SPR012269050

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520			\|a Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperature sensitivity for decomposition of labile (Q10-L) and recalcitrant (Q10-R) SOMs by comparing the time required to decompose a given amount of C at 25 and 35 °C. Soils were collected from a paddy field that was subjected to four treatments: ambient $ CO_{2} $ and temperature, elevated $ CO_{2} $ (500 μmol/mol), enhanced temperature (+2 °C), and their combination. The results showed that the temperature sensitivity of SOM decomposition increased with increasing SOM recalcitrance in this paddy soil (Q10-L = 2.21 ± 0.16 vs. Q10-R = 2.78 ± 0.42; mean ± SD). Elevated $ CO_{2} $ and enhanced temperature showed contrasting effects on the temperature sensitivity of SOM decomposition. Elevated $ CO_{2} $ stimulated Q10-R but had no effect on Q10-L; in contrast, enhanced temperature increased Q10-L but had no effect on Q10-R. Furthermore, the elevated $ CO_{2} $ combined with enhanced temperature treatment significantly increased Q10-L and Q10-R by 18.9 and 10.2 %, respectively, compared to the ambient conditions. Results suggested that the responses of SOM to temperature, especially for the recalcitrant SOM pool, were altered by climate changes. The greatly enhanced temperature sensitivity of SOM decomposition by elevated $ CO_{2} $ and temperature indicates that more $ CO_{2} $ will be released to the atmosphere and losses of soil C may be even greater than that previously expected in paddy field.
650		4	\|a Soil organic matter decomposition \|7 (dpeaa)DE-He213
650		4	\|a Soil organic matter quality \|7 (dpeaa)DE-He213
650		4	\|a Temperature sensitivity \|7 (dpeaa)DE-He213
650		4	\|a Paddy field \|7 (dpeaa)DE-He213
650		4	\|a Global change \|7 (dpeaa)DE-He213
700	1		\|a Wang, Bingyu \|e verfasserin \|4 aut
700	1		\|a Wang, Jinyang \|e verfasserin \|4 aut
700	1		\|a Pan, Genxing \|e verfasserin \|4 aut
700	1		\|a Xiong, Zhengqin \|e verfasserin \|4 aut
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912			\|a GBV_ILN_187
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
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912			\|a GBV_ILN_250
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912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
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Indexfelder

author_variant	z c zc b w bw j w jw g p gp z x zx
matchkey_str	article:15732959:2016----::otatnefcsflvtdo2nwrigneprtrsniiiyfolraimted
hierarchy_sort_str	2016
bklnumber	30.00 43.00
publishDate	2016
allfields	10.1007/s10661-016-5563-1 doi (DE-627)SPR012269050 (SPR)s10661-016-5563-1-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Chen, Zhaozhi verfasserin aut Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperature sensitivity for decomposition of labile (Q10-L) and recalcitrant (Q10-R) SOMs by comparing the time required to decompose a given amount of C at 25 and 35 °C. Soils were collected from a paddy field that was subjected to four treatments: ambient $ CO_{2} $ and temperature, elevated $ CO_{2} $ (500 μmol/mol), enhanced temperature (+2 °C), and their combination. The results showed that the temperature sensitivity of SOM decomposition increased with increasing SOM recalcitrance in this paddy soil (Q10-L = 2.21 ± 0.16 vs. Q10-R = 2.78 ± 0.42; mean ± SD). Elevated $ CO_{2} $ and enhanced temperature showed contrasting effects on the temperature sensitivity of SOM decomposition. Elevated $ CO_{2} $ stimulated Q10-R but had no effect on Q10-L; in contrast, enhanced temperature increased Q10-L but had no effect on Q10-R. Furthermore, the elevated $ CO_{2} $ combined with enhanced temperature treatment significantly increased Q10-L and Q10-R by 18.9 and 10.2 %, respectively, compared to the ambient conditions. Results suggested that the responses of SOM to temperature, especially for the recalcitrant SOM pool, were altered by climate changes. The greatly enhanced temperature sensitivity of SOM decomposition by elevated $ CO_{2} $ and temperature indicates that more $ CO_{2} $ will be released to the atmosphere and losses of soil C may be even greater than that previously expected in paddy field. Soil organic matter decomposition (dpeaa)DE-He213 Soil organic matter quality (dpeaa)DE-He213 Temperature sensitivity (dpeaa)DE-He213 Paddy field (dpeaa)DE-He213 Global change (dpeaa)DE-He213 Wang, Bingyu verfasserin aut Wang, Jinyang verfasserin aut Pan, Genxing verfasserin aut Xiong, Zhengqin verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 188(2016), 10 vom: 02. Sept. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:188 year:2016 number:10 day:02 month:09 https://dx.doi.org/10.1007/s10661-016-5563-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_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 30.00 ASE 43.00 ASE AR 188 2016 10 02 09
spelling	10.1007/s10661-016-5563-1 doi (DE-627)SPR012269050 (SPR)s10661-016-5563-1-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Chen, Zhaozhi verfasserin aut Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperature sensitivity for decomposition of labile (Q10-L) and recalcitrant (Q10-R) SOMs by comparing the time required to decompose a given amount of C at 25 and 35 °C. Soils were collected from a paddy field that was subjected to four treatments: ambient $ CO_{2} $ and temperature, elevated $ CO_{2} $ (500 μmol/mol), enhanced temperature (+2 °C), and their combination. The results showed that the temperature sensitivity of SOM decomposition increased with increasing SOM recalcitrance in this paddy soil (Q10-L = 2.21 ± 0.16 vs. Q10-R = 2.78 ± 0.42; mean ± SD). Elevated $ CO_{2} $ and enhanced temperature showed contrasting effects on the temperature sensitivity of SOM decomposition. Elevated $ CO_{2} $ stimulated Q10-R but had no effect on Q10-L; in contrast, enhanced temperature increased Q10-L but had no effect on Q10-R. Furthermore, the elevated $ CO_{2} $ combined with enhanced temperature treatment significantly increased Q10-L and Q10-R by 18.9 and 10.2 %, respectively, compared to the ambient conditions. Results suggested that the responses of SOM to temperature, especially for the recalcitrant SOM pool, were altered by climate changes. The greatly enhanced temperature sensitivity of SOM decomposition by elevated $ CO_{2} $ and temperature indicates that more $ CO_{2} $ will be released to the atmosphere and losses of soil C may be even greater than that previously expected in paddy field. Soil organic matter decomposition (dpeaa)DE-He213 Soil organic matter quality (dpeaa)DE-He213 Temperature sensitivity (dpeaa)DE-He213 Paddy field (dpeaa)DE-He213 Global change (dpeaa)DE-He213 Wang, Bingyu verfasserin aut Wang, Jinyang verfasserin aut Pan, Genxing verfasserin aut Xiong, Zhengqin verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 188(2016), 10 vom: 02. Sept. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:188 year:2016 number:10 day:02 month:09 https://dx.doi.org/10.1007/s10661-016-5563-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_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 30.00 ASE 43.00 ASE AR 188 2016 10 02 09
allfields_unstemmed	10.1007/s10661-016-5563-1 doi (DE-627)SPR012269050 (SPR)s10661-016-5563-1-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Chen, Zhaozhi verfasserin aut Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperature sensitivity for decomposition of labile (Q10-L) and recalcitrant (Q10-R) SOMs by comparing the time required to decompose a given amount of C at 25 and 35 °C. Soils were collected from a paddy field that was subjected to four treatments: ambient $ CO_{2} $ and temperature, elevated $ CO_{2} $ (500 μmol/mol), enhanced temperature (+2 °C), and their combination. The results showed that the temperature sensitivity of SOM decomposition increased with increasing SOM recalcitrance in this paddy soil (Q10-L = 2.21 ± 0.16 vs. Q10-R = 2.78 ± 0.42; mean ± SD). Elevated $ CO_{2} $ and enhanced temperature showed contrasting effects on the temperature sensitivity of SOM decomposition. Elevated $ CO_{2} $ stimulated Q10-R but had no effect on Q10-L; in contrast, enhanced temperature increased Q10-L but had no effect on Q10-R. Furthermore, the elevated $ CO_{2} $ combined with enhanced temperature treatment significantly increased Q10-L and Q10-R by 18.9 and 10.2 %, respectively, compared to the ambient conditions. Results suggested that the responses of SOM to temperature, especially for the recalcitrant SOM pool, were altered by climate changes. The greatly enhanced temperature sensitivity of SOM decomposition by elevated $ CO_{2} $ and temperature indicates that more $ CO_{2} $ will be released to the atmosphere and losses of soil C may be even greater than that previously expected in paddy field. Soil organic matter decomposition (dpeaa)DE-He213 Soil organic matter quality (dpeaa)DE-He213 Temperature sensitivity (dpeaa)DE-He213 Paddy field (dpeaa)DE-He213 Global change (dpeaa)DE-He213 Wang, Bingyu verfasserin aut Wang, Jinyang verfasserin aut Pan, Genxing verfasserin aut Xiong, Zhengqin verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 188(2016), 10 vom: 02. Sept. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:188 year:2016 number:10 day:02 month:09 https://dx.doi.org/10.1007/s10661-016-5563-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_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 30.00 ASE 43.00 ASE AR 188 2016 10 02 09
allfieldsGer	10.1007/s10661-016-5563-1 doi (DE-627)SPR012269050 (SPR)s10661-016-5563-1-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Chen, Zhaozhi verfasserin aut Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperature sensitivity for decomposition of labile (Q10-L) and recalcitrant (Q10-R) SOMs by comparing the time required to decompose a given amount of C at 25 and 35 °C. Soils were collected from a paddy field that was subjected to four treatments: ambient $ CO_{2} $ and temperature, elevated $ CO_{2} $ (500 μmol/mol), enhanced temperature (+2 °C), and their combination. The results showed that the temperature sensitivity of SOM decomposition increased with increasing SOM recalcitrance in this paddy soil (Q10-L = 2.21 ± 0.16 vs. Q10-R = 2.78 ± 0.42; mean ± SD). Elevated $ CO_{2} $ and enhanced temperature showed contrasting effects on the temperature sensitivity of SOM decomposition. Elevated $ CO_{2} $ stimulated Q10-R but had no effect on Q10-L; in contrast, enhanced temperature increased Q10-L but had no effect on Q10-R. Furthermore, the elevated $ CO_{2} $ combined with enhanced temperature treatment significantly increased Q10-L and Q10-R by 18.9 and 10.2 %, respectively, compared to the ambient conditions. Results suggested that the responses of SOM to temperature, especially for the recalcitrant SOM pool, were altered by climate changes. The greatly enhanced temperature sensitivity of SOM decomposition by elevated $ CO_{2} $ and temperature indicates that more $ CO_{2} $ will be released to the atmosphere and losses of soil C may be even greater than that previously expected in paddy field. Soil organic matter decomposition (dpeaa)DE-He213 Soil organic matter quality (dpeaa)DE-He213 Temperature sensitivity (dpeaa)DE-He213 Paddy field (dpeaa)DE-He213 Global change (dpeaa)DE-He213 Wang, Bingyu verfasserin aut Wang, Jinyang verfasserin aut Pan, Genxing verfasserin aut Xiong, Zhengqin verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 188(2016), 10 vom: 02. Sept. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:188 year:2016 number:10 day:02 month:09 https://dx.doi.org/10.1007/s10661-016-5563-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_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 30.00 ASE 43.00 ASE AR 188 2016 10 02 09
allfieldsSound	10.1007/s10661-016-5563-1 doi (DE-627)SPR012269050 (SPR)s10661-016-5563-1-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Chen, Zhaozhi verfasserin aut Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperature sensitivity for decomposition of labile (Q10-L) and recalcitrant (Q10-R) SOMs by comparing the time required to decompose a given amount of C at 25 and 35 °C. Soils were collected from a paddy field that was subjected to four treatments: ambient $ CO_{2} $ and temperature, elevated $ CO_{2} $ (500 μmol/mol), enhanced temperature (+2 °C), and their combination. The results showed that the temperature sensitivity of SOM decomposition increased with increasing SOM recalcitrance in this paddy soil (Q10-L = 2.21 ± 0.16 vs. Q10-R = 2.78 ± 0.42; mean ± SD). Elevated $ CO_{2} $ and enhanced temperature showed contrasting effects on the temperature sensitivity of SOM decomposition. Elevated $ CO_{2} $ stimulated Q10-R but had no effect on Q10-L; in contrast, enhanced temperature increased Q10-L but had no effect on Q10-R. Furthermore, the elevated $ CO_{2} $ combined with enhanced temperature treatment significantly increased Q10-L and Q10-R by 18.9 and 10.2 %, respectively, compared to the ambient conditions. Results suggested that the responses of SOM to temperature, especially for the recalcitrant SOM pool, were altered by climate changes. The greatly enhanced temperature sensitivity of SOM decomposition by elevated $ CO_{2} $ and temperature indicates that more $ CO_{2} $ will be released to the atmosphere and losses of soil C may be even greater than that previously expected in paddy field. Soil organic matter decomposition (dpeaa)DE-He213 Soil organic matter quality (dpeaa)DE-He213 Temperature sensitivity (dpeaa)DE-He213 Paddy field (dpeaa)DE-He213 Global change (dpeaa)DE-He213 Wang, Bingyu verfasserin aut Wang, Jinyang verfasserin aut Pan, Genxing verfasserin aut Xiong, Zhengqin verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 188(2016), 10 vom: 02. Sept. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:188 year:2016 number:10 day:02 month:09 https://dx.doi.org/10.1007/s10661-016-5563-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_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 30.00 ASE 43.00 ASE AR 188 2016 10 02 09
language	English
source	Enthalten in Environmental monitoring and assessment 188(2016), 10 vom: 02. Sept. volume:188 year:2016 number:10 day:02 month:09
sourceStr	Enthalten in Environmental monitoring and assessment 188(2016), 10 vom: 02. Sept. volume:188 year:2016 number:10 day:02 month:09
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Soil organic matter decomposition Soil organic matter quality Temperature sensitivity Paddy field Global change
dewey-raw	333.7
isfreeaccess_bool	false
container_title	Environmental monitoring and assessment
authorswithroles_txt_mv	Chen, Zhaozhi @@aut@@ Wang, Bingyu @@aut@@ Wang, Jinyang @@aut@@ Pan, Genxing @@aut@@ Xiong, Zhengqin @@aut@@
publishDateDaySort_date	2016-09-02T00:00:00Z
hierarchy_top_id	31281738X
dewey-sort	3333.7
id	SPR012269050
language_de	englisch
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author	Chen, Zhaozhi
spellingShingle	Chen, Zhaozhi ddc 333.7 bkl 30.00 bkl 43.00 misc Soil organic matter decomposition misc Soil organic matter quality misc Temperature sensitivity misc Paddy field misc Global change Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field
authorStr	Chen, Zhaozhi
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topic_title	333.7 ASE 30.00 bkl 43.00 bkl Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field Soil organic matter decomposition (dpeaa)DE-He213 Soil organic matter quality (dpeaa)DE-He213 Temperature sensitivity (dpeaa)DE-He213 Paddy field (dpeaa)DE-He213 Global change (dpeaa)DE-He213
topic	ddc 333.7 bkl 30.00 bkl 43.00 misc Soil organic matter decomposition misc Soil organic matter quality misc Temperature sensitivity misc Paddy field misc Global change
topic_unstemmed	ddc 333.7 bkl 30.00 bkl 43.00 misc Soil organic matter decomposition misc Soil organic matter quality misc Temperature sensitivity misc Paddy field misc Global change
topic_browse	ddc 333.7 bkl 30.00 bkl 43.00 misc Soil organic matter decomposition misc Soil organic matter quality misc Temperature sensitivity misc Paddy field misc Global change
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title	Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field
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title_full	Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field
author_sort	Chen, Zhaozhi
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author_browse	Chen, Zhaozhi Wang, Bingyu Wang, Jinyang Pan, Genxing Xiong, Zhengqin
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title_sort	contrasting effects of elevated $ co_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a chinese paddy field
title_auth	Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field
abstract	Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperature sensitivity for decomposition of labile (Q10-L) and recalcitrant (Q10-R) SOMs by comparing the time required to decompose a given amount of C at 25 and 35 °C. Soils were collected from a paddy field that was subjected to four treatments: ambient $ CO_{2} $ and temperature, elevated $ CO_{2} $ (500 μmol/mol), enhanced temperature (+2 °C), and their combination. The results showed that the temperature sensitivity of SOM decomposition increased with increasing SOM recalcitrance in this paddy soil (Q10-L = 2.21 ± 0.16 vs. Q10-R = 2.78 ± 0.42; mean ± SD). Elevated $ CO_{2} $ and enhanced temperature showed contrasting effects on the temperature sensitivity of SOM decomposition. Elevated $ CO_{2} $ stimulated Q10-R but had no effect on Q10-L; in contrast, enhanced temperature increased Q10-L but had no effect on Q10-R. Furthermore, the elevated $ CO_{2} $ combined with enhanced temperature treatment significantly increased Q10-L and Q10-R by 18.9 and 10.2 %, respectively, compared to the ambient conditions. Results suggested that the responses of SOM to temperature, especially for the recalcitrant SOM pool, were altered by climate changes. The greatly enhanced temperature sensitivity of SOM decomposition by elevated $ CO_{2} $ and temperature indicates that more $ CO_{2} $ will be released to the atmosphere and losses of soil C may be even greater than that previously expected in paddy field.
abstractGer	Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperature sensitivity for decomposition of labile (Q10-L) and recalcitrant (Q10-R) SOMs by comparing the time required to decompose a given amount of C at 25 and 35 °C. Soils were collected from a paddy field that was subjected to four treatments: ambient $ CO_{2} $ and temperature, elevated $ CO_{2} $ (500 μmol/mol), enhanced temperature (+2 °C), and their combination. The results showed that the temperature sensitivity of SOM decomposition increased with increasing SOM recalcitrance in this paddy soil (Q10-L = 2.21 ± 0.16 vs. Q10-R = 2.78 ± 0.42; mean ± SD). Elevated $ CO_{2} $ and enhanced temperature showed contrasting effects on the temperature sensitivity of SOM decomposition. Elevated $ CO_{2} $ stimulated Q10-R but had no effect on Q10-L; in contrast, enhanced temperature increased Q10-L but had no effect on Q10-R. Furthermore, the elevated $ CO_{2} $ combined with enhanced temperature treatment significantly increased Q10-L and Q10-R by 18.9 and 10.2 %, respectively, compared to the ambient conditions. Results suggested that the responses of SOM to temperature, especially for the recalcitrant SOM pool, were altered by climate changes. The greatly enhanced temperature sensitivity of SOM decomposition by elevated $ CO_{2} $ and temperature indicates that more $ CO_{2} $ will be released to the atmosphere and losses of soil C may be even greater than that previously expected in paddy field.
abstract_unstemmed	Abstract Climate changes including elevated $ CO_{2} $ and temperature have been known to affect soil carbon (C) storage, while the effects of climate changes on the temperature sensitivity of soil organic matter (SOM) are unclear. A 365-day laboratory incubation was used to investigate the temperature sensitivity for decomposition of labile (Q10-L) and recalcitrant (Q10-R) SOMs by comparing the time required to decompose a given amount of C at 25 and 35 °C. Soils were collected from a paddy field that was subjected to four treatments: ambient $ CO_{2} $ and temperature, elevated $ CO_{2} $ (500 μmol/mol), enhanced temperature (+2 °C), and their combination. The results showed that the temperature sensitivity of SOM decomposition increased with increasing SOM recalcitrance in this paddy soil (Q10-L = 2.21 ± 0.16 vs. Q10-R = 2.78 ± 0.42; mean ± SD). Elevated $ CO_{2} $ and enhanced temperature showed contrasting effects on the temperature sensitivity of SOM decomposition. Elevated $ CO_{2} $ stimulated Q10-R but had no effect on Q10-L; in contrast, enhanced temperature increased Q10-L but had no effect on Q10-R. Furthermore, the elevated $ CO_{2} $ combined with enhanced temperature treatment significantly increased Q10-L and Q10-R by 18.9 and 10.2 %, respectively, compared to the ambient conditions. Results suggested that the responses of SOM to temperature, especially for the recalcitrant SOM pool, were altered by climate changes. The greatly enhanced temperature sensitivity of SOM decomposition by elevated $ CO_{2} $ and temperature indicates that more $ CO_{2} $ will be released to the atmosphere and losses of soil C may be even greater than that previously expected in paddy field.
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container_issue	10
title_short	Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field
url	https://dx.doi.org/10.1007/s10661-016-5563-1
remote_bool	true
author2	Wang, Bingyu Wang, Jinyang Pan, Genxing Xiong, Zhengqin
author2Str	Wang, Bingyu Wang, Jinyang Pan, Genxing Xiong, Zhengqin
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doi_str	10.1007/s10661-016-5563-1
up_date	2024-07-04T02:29:02.366Z
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Contrasting effects of elevated $ CO_{2} $ and warming on temperature sensitivity of soil organic matter decomposition in a Chinese paddy field

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