Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate
Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Jiao, Shuai [verfasserIn] Sui, Biao [verfasserIn] Wang, Hongbin [verfasserIn] Chen, Baoyu [verfasserIn] Xomphoutheb, Thidaphone [verfasserIn] Zhao, Xingmin [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Arabian journal of geosciences - Berlin : Springer, 2008, 14(2021), 3 vom: 27. Jan. |
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| Übergeordnetes Werk: |
volume:14 ; year:2021 ; number:3 ; day:27 ; month:01 |
| Links: |
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| DOI / URN: |
10.1007/s12517-021-06472-1 |
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| Katalog-ID: |
SPR042892503 |
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| 245 | 1 | 0 | |a Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate |
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| 520 | |a Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. So PN is the best tillage mode to reduce GHG emissions in soil profile under the test conditions. | ||
| 650 | 4 | |a Conventional tillage |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a No tillage |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Greenhouse gas emission |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Soil profile |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Greenhouse effect |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Sui, Biao |e verfasserin |4 aut | |
| 700 | 1 | |a Wang, Hongbin |e verfasserin |4 aut | |
| 700 | 1 | |a Chen, Baoyu |e verfasserin |4 aut | |
| 700 | 1 | |a Xomphoutheb, Thidaphone |e verfasserin |4 aut | |
| 700 | 1 | |a Zhao, Xingmin |e verfasserin |4 aut | |
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10.1007/s12517-021-06472-1 doi (DE-627)SPR042892503 (DE-599)SPRs12517-021-06472-1-e (SPR)s12517-021-06472-1-e DE-627 ger DE-627 rakwb eng 550 ASE Jiao, Shuai verfasserin aut Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. So PN is the best tillage mode to reduce GHG emissions in soil profile under the test conditions. Conventional tillage (dpeaa)DE-He213 No tillage (dpeaa)DE-He213 Greenhouse gas emission (dpeaa)DE-He213 Soil profile (dpeaa)DE-He213 Greenhouse effect (dpeaa)DE-He213 Sui, Biao verfasserin aut Wang, Hongbin verfasserin aut Chen, Baoyu verfasserin aut Xomphoutheb, Thidaphone verfasserin aut Zhao, Xingmin verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 3 vom: 27. Jan. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:3 day:27 month:01 https://dx.doi.org/10.1007/s12517-021-06472-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 3 27 01 |
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10.1007/s12517-021-06472-1 doi (DE-627)SPR042892503 (DE-599)SPRs12517-021-06472-1-e (SPR)s12517-021-06472-1-e DE-627 ger DE-627 rakwb eng 550 ASE Jiao, Shuai verfasserin aut Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. So PN is the best tillage mode to reduce GHG emissions in soil profile under the test conditions. Conventional tillage (dpeaa)DE-He213 No tillage (dpeaa)DE-He213 Greenhouse gas emission (dpeaa)DE-He213 Soil profile (dpeaa)DE-He213 Greenhouse effect (dpeaa)DE-He213 Sui, Biao verfasserin aut Wang, Hongbin verfasserin aut Chen, Baoyu verfasserin aut Xomphoutheb, Thidaphone verfasserin aut Zhao, Xingmin verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 3 vom: 27. Jan. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:3 day:27 month:01 https://dx.doi.org/10.1007/s12517-021-06472-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 3 27 01 |
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10.1007/s12517-021-06472-1 doi (DE-627)SPR042892503 (DE-599)SPRs12517-021-06472-1-e (SPR)s12517-021-06472-1-e DE-627 ger DE-627 rakwb eng 550 ASE Jiao, Shuai verfasserin aut Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. So PN is the best tillage mode to reduce GHG emissions in soil profile under the test conditions. Conventional tillage (dpeaa)DE-He213 No tillage (dpeaa)DE-He213 Greenhouse gas emission (dpeaa)DE-He213 Soil profile (dpeaa)DE-He213 Greenhouse effect (dpeaa)DE-He213 Sui, Biao verfasserin aut Wang, Hongbin verfasserin aut Chen, Baoyu verfasserin aut Xomphoutheb, Thidaphone verfasserin aut Zhao, Xingmin verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 3 vom: 27. Jan. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:3 day:27 month:01 https://dx.doi.org/10.1007/s12517-021-06472-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 3 27 01 |
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10.1007/s12517-021-06472-1 doi (DE-627)SPR042892503 (DE-599)SPRs12517-021-06472-1-e (SPR)s12517-021-06472-1-e DE-627 ger DE-627 rakwb eng 550 ASE Jiao, Shuai verfasserin aut Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. So PN is the best tillage mode to reduce GHG emissions in soil profile under the test conditions. Conventional tillage (dpeaa)DE-He213 No tillage (dpeaa)DE-He213 Greenhouse gas emission (dpeaa)DE-He213 Soil profile (dpeaa)DE-He213 Greenhouse effect (dpeaa)DE-He213 Sui, Biao verfasserin aut Wang, Hongbin verfasserin aut Chen, Baoyu verfasserin aut Xomphoutheb, Thidaphone verfasserin aut Zhao, Xingmin verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 3 vom: 27. Jan. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:3 day:27 month:01 https://dx.doi.org/10.1007/s12517-021-06472-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 3 27 01 |
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10.1007/s12517-021-06472-1 doi (DE-627)SPR042892503 (DE-599)SPRs12517-021-06472-1-e (SPR)s12517-021-06472-1-e DE-627 ger DE-627 rakwb eng 550 ASE Jiao, Shuai verfasserin aut Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. So PN is the best tillage mode to reduce GHG emissions in soil profile under the test conditions. Conventional tillage (dpeaa)DE-He213 No tillage (dpeaa)DE-He213 Greenhouse gas emission (dpeaa)DE-He213 Soil profile (dpeaa)DE-He213 Greenhouse effect (dpeaa)DE-He213 Sui, Biao verfasserin aut Wang, Hongbin verfasserin aut Chen, Baoyu verfasserin aut Xomphoutheb, Thidaphone verfasserin aut Zhao, Xingmin verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 14(2021), 3 vom: 27. Jan. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:14 year:2021 number:3 day:27 month:01 https://dx.doi.org/10.1007/s12517-021-06472-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 14 2021 3 27 01 |
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English |
| source |
Enthalten in Arabian journal of geosciences 14(2021), 3 vom: 27. Jan. volume:14 year:2021 number:3 day:27 month:01 |
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Enthalten in Arabian journal of geosciences 14(2021), 3 vom: 27. Jan. volume:14 year:2021 number:3 day:27 month:01 |
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Article |
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findex.gbv.de |
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Conventional tillage No tillage Greenhouse gas emission Soil profile Greenhouse effect |
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550 |
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Arabian journal of geosciences |
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Jiao, Shuai @@aut@@ Sui, Biao @@aut@@ Wang, Hongbin @@aut@@ Chen, Baoyu @@aut@@ Xomphoutheb, Thidaphone @@aut@@ Zhao, Xingmin @@aut@@ |
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2021-01-27T00:00:00Z |
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SPR042892503 |
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To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. 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|
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Jiao, Shuai |
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Jiao, Shuai ddc 550 misc Conventional tillage misc No tillage misc Greenhouse gas emission misc Soil profile misc Greenhouse effect Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate |
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550 ASE Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate Conventional tillage (dpeaa)DE-He213 No tillage (dpeaa)DE-He213 Greenhouse gas emission (dpeaa)DE-He213 Soil profile (dpeaa)DE-He213 Greenhouse effect (dpeaa)DE-He213 |
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Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate |
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Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate |
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Jiao, Shuai Sui, Biao Wang, Hongbin Chen, Baoyu Xomphoutheb, Thidaphone Zhao, Xingmin |
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comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate |
| title_auth |
Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate |
| abstract |
Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. So PN is the best tillage mode to reduce GHG emissions in soil profile under the test conditions. |
| abstractGer |
Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. So PN is the best tillage mode to reduce GHG emissions in soil profile under the test conditions. |
| abstract_unstemmed |
Abstract Agricultural tillage practices play an important role in the production and consumption of greenhouse gases (GHGs) that contribute substantially to the global warming. To explore GHG diffusion characteristic and seek for environment-friendly tillage methods, four tillage systems consisting of continuous rotary tillage (CR), continuous no tillage (CN), ploughing-rotary tillage (PR), and ploughing-no tillage (PN) were designed, and vertical variations of GHG concentrations under different tillage systems were investigated. Mean $ CO_{2} $ concentration in the soil profile was increased significantly with the increase of soil depth. Higher soil moisture promoted $ CO_{2} $ production. However, the influence of soil temperature on the content of $ CO_{2} $ was not obvious. The concentrations of $ CH_{4} $ in soil at 0–20-cm depth were greater than that of 20–40 cm, which was mainly affected by fertilization. The trend of $ N_{2} $O concentration variation in soil was consistent with that of $ CO_{2} $. The diffusion flux of $ CO_{2} $ in soil was all positive, and it changes greatly in the whole growth cycle of maize, which had obvious correlation with precipitation. The $ CH_{4} $ diffusion flux decreased with the increase of soil depth, and the change trend of 0–20-cm soil layer diffusion flux was consistent with the gas concentration. The 20–40-cm soil layer fluctuated greatly, which was mainly affected by water content, and the whole value was negative after jointing. The trend of $ N_{2} $O diffusion flux was similar to that of $ CH_{4} $. In the whole maize growth period, except for $ CH_{4} $ in 20–40-cm soil layer, the cumulative diffusion fluxes of greenhouse gases in each treatment were all positive, indicating that the whole farmland soil was the emission source of greenhouse gases. The effect of three greenhouse gases on greenhouse effect was $ CO_{2} $ > $ N_{2} $O > $ CH_{4} $, and the comprehensive warming potential of different tillage methods was CN > CR > PR> PN. So PN is the best tillage mode to reduce GHG emissions in soil profile under the test conditions. |
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Comparative effects of long-term conventional tillage and no-till systems on greenhouse gas emissions in continuous maize monoculture soil in a semi-arid temperate climate |
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https://dx.doi.org/10.1007/s12517-021-06472-1 |
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Sui, Biao Wang, Hongbin Chen, Baoyu Xomphoutheb, Thidaphone Zhao, Xingmin |
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| score |
7.3995314 |