Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils
Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian fores...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Cuevas, Jaime G. [verfasserIn] Paulino, Leandro [verfasserIn] Dörner, José [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2020 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Journal of soil science and plant nutrition - [Cham] : Springer International Publishing, 2010, 20(2020), 4 vom: 20. Mai, Seite 1859-1871 |
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| Übergeordnetes Werk: |
volume:20 ; year:2020 ; number:4 ; day:20 ; month:05 ; pages:1859-1871 |
| Links: |
|---|
| DOI / URN: |
10.1007/s42729-020-00257-3 |
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| Katalog-ID: |
SPR041887921 |
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| 520 | |a Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments. | ||
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| 650 | 4 | |a Nitrogen cycle |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Paulino, Leandro |e verfasserin |4 aut | |
| 700 | 1 | |a Dörner, José |e verfasserin |4 aut | |
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10.1007/s42729-020-00257-3 doi (DE-627)SPR041887921 (SPR)s42729-020-00257-3-e DE-627 ger DE-627 rakwb eng 630 570 ASE 580 630 ASE 48.30 bkl 58.52 bkl Cuevas, Jaime G. verfasserin aut Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments. Andisols (dpeaa)DE-He213 Denitrification (dpeaa)DE-He213 Potential mineralization (dpeaa)DE-He213 Potential nitrification (dpeaa)DE-He213 Nitrogen cycle (dpeaa)DE-He213 Paulino, Leandro verfasserin aut Dörner, José verfasserin aut Enthalten in Journal of soil science and plant nutrition [Cham] : Springer International Publishing, 2010 20(2020), 4 vom: 20. Mai, Seite 1859-1871 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:20 year:2020 number:4 day:20 month:05 pages:1859-1871 https://dx.doi.org/10.1007/s42729-020-00257-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 ASE 58.52 ASE AR 20 2020 4 20 05 1859-1871 |
| spelling |
10.1007/s42729-020-00257-3 doi (DE-627)SPR041887921 (SPR)s42729-020-00257-3-e DE-627 ger DE-627 rakwb eng 630 570 ASE 580 630 ASE 48.30 bkl 58.52 bkl Cuevas, Jaime G. verfasserin aut Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments. Andisols (dpeaa)DE-He213 Denitrification (dpeaa)DE-He213 Potential mineralization (dpeaa)DE-He213 Potential nitrification (dpeaa)DE-He213 Nitrogen cycle (dpeaa)DE-He213 Paulino, Leandro verfasserin aut Dörner, José verfasserin aut Enthalten in Journal of soil science and plant nutrition [Cham] : Springer International Publishing, 2010 20(2020), 4 vom: 20. Mai, Seite 1859-1871 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:20 year:2020 number:4 day:20 month:05 pages:1859-1871 https://dx.doi.org/10.1007/s42729-020-00257-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 ASE 58.52 ASE AR 20 2020 4 20 05 1859-1871 |
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10.1007/s42729-020-00257-3 doi (DE-627)SPR041887921 (SPR)s42729-020-00257-3-e DE-627 ger DE-627 rakwb eng 630 570 ASE 580 630 ASE 48.30 bkl 58.52 bkl Cuevas, Jaime G. verfasserin aut Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments. Andisols (dpeaa)DE-He213 Denitrification (dpeaa)DE-He213 Potential mineralization (dpeaa)DE-He213 Potential nitrification (dpeaa)DE-He213 Nitrogen cycle (dpeaa)DE-He213 Paulino, Leandro verfasserin aut Dörner, José verfasserin aut Enthalten in Journal of soil science and plant nutrition [Cham] : Springer International Publishing, 2010 20(2020), 4 vom: 20. Mai, Seite 1859-1871 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:20 year:2020 number:4 day:20 month:05 pages:1859-1871 https://dx.doi.org/10.1007/s42729-020-00257-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 ASE 58.52 ASE AR 20 2020 4 20 05 1859-1871 |
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10.1007/s42729-020-00257-3 doi (DE-627)SPR041887921 (SPR)s42729-020-00257-3-e DE-627 ger DE-627 rakwb eng 630 570 ASE 580 630 ASE 48.30 bkl 58.52 bkl Cuevas, Jaime G. verfasserin aut Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments. Andisols (dpeaa)DE-He213 Denitrification (dpeaa)DE-He213 Potential mineralization (dpeaa)DE-He213 Potential nitrification (dpeaa)DE-He213 Nitrogen cycle (dpeaa)DE-He213 Paulino, Leandro verfasserin aut Dörner, José verfasserin aut Enthalten in Journal of soil science and plant nutrition [Cham] : Springer International Publishing, 2010 20(2020), 4 vom: 20. Mai, Seite 1859-1871 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:20 year:2020 number:4 day:20 month:05 pages:1859-1871 https://dx.doi.org/10.1007/s42729-020-00257-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 ASE 58.52 ASE AR 20 2020 4 20 05 1859-1871 |
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10.1007/s42729-020-00257-3 doi (DE-627)SPR041887921 (SPR)s42729-020-00257-3-e DE-627 ger DE-627 rakwb eng 630 570 ASE 580 630 ASE 48.30 bkl 58.52 bkl Cuevas, Jaime G. verfasserin aut Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments. Andisols (dpeaa)DE-He213 Denitrification (dpeaa)DE-He213 Potential mineralization (dpeaa)DE-He213 Potential nitrification (dpeaa)DE-He213 Nitrogen cycle (dpeaa)DE-He213 Paulino, Leandro verfasserin aut Dörner, José verfasserin aut Enthalten in Journal of soil science and plant nutrition [Cham] : Springer International Publishing, 2010 20(2020), 4 vom: 20. Mai, Seite 1859-1871 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:20 year:2020 number:4 day:20 month:05 pages:1859-1871 https://dx.doi.org/10.1007/s42729-020-00257-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 ASE 58.52 ASE AR 20 2020 4 20 05 1859-1871 |
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English |
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Enthalten in Journal of soil science and plant nutrition 20(2020), 4 vom: 20. Mai, Seite 1859-1871 volume:20 year:2020 number:4 day:20 month:05 pages:1859-1871 |
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Enthalten in Journal of soil science and plant nutrition 20(2020), 4 vom: 20. Mai, Seite 1859-1871 volume:20 year:2020 number:4 day:20 month:05 pages:1859-1871 |
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Andisols Denitrification Potential mineralization Potential nitrification Nitrogen cycle |
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Journal of soil science and plant nutrition |
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Cuevas, Jaime G. @@aut@@ Paulino, Leandro @@aut@@ Dörner, José @@aut@@ |
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2020-05-20T00:00:00Z |
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We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Andisols</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Denitrification</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Potential mineralization</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Potential nitrification</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nitrogen cycle</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Paulino, Leandro</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Dörner, José</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of soil science and plant nutrition</subfield><subfield code="d">[Cham] : Springer International Publishing, 2010</subfield><subfield code="g">20(2020), 4 vom: 20. 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Cuevas, Jaime G. |
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Cuevas, Jaime G. ddc 630 ddc 580 bkl 48.30 bkl 58.52 misc Andisols misc Denitrification misc Potential mineralization misc Potential nitrification misc Nitrogen cycle Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils |
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630 570 ASE 580 630 ASE 48.30 bkl 58.52 bkl Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils Andisols (dpeaa)DE-He213 Denitrification (dpeaa)DE-He213 Potential mineralization (dpeaa)DE-He213 Potential nitrification (dpeaa)DE-He213 Nitrogen cycle (dpeaa)DE-He213 |
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ddc 630 ddc 580 bkl 48.30 bkl 58.52 misc Andisols misc Denitrification misc Potential mineralization misc Potential nitrification misc Nitrogen cycle |
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Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils |
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Elektronische Aufsätze |
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Cuevas, Jaime G. |
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10.1007/s42729-020-00257-3 |
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pathways for nitrous oxide generation in forested and agricultural zones growing on volcanic ash soils |
| title_auth |
Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils |
| abstract |
Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments. |
| abstractGer |
Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments. |
| abstract_unstemmed |
Abstract We studied the in situ relative contribution of soil nitrous oxide ($ N_{2} $O) emissions from already discovered pathways, namely the nitrification, nitrifier denitrification (ND), and heterotrophic denitrification (HD). We selected a transect from upland pastures to lowland riparian forests growing on volcanic ash soils. We used the acetylene blocking technique, and $ N_{2} $O was measured by gas chromatography. We also measured rates of potential organic matter mineralization and potential nitrification in laboratory. Potential mineralization increased from uplands to lowlands, while potential nitrification decreased in the same transect. In riparian forests, $ N_{2} $O emissions under acetylene blocking were higher than without acetylene, revealing that 22–31% of nitrogen emissions consisted of dinitrogen. Conversely, in pastures, $ N_{2} $O emissions under acetylene blocking were lower than without acetylene. Our results suggest that HD predominates in waterlogged, anoxic, and acidic soils with no nitrification, which are typical conditions for riparian soils. Conversely, $ N_{2} $O from nitrification and ND predominates in more oxic environments that are less water-saturated, have less acidic soils, and a larger nitrification rate than riparian areas (i.e., typical conditions for pasture soils). Thus, processes related to the nitrogen cycle depend on the land cover/use and soil physical-chemical properties, even in vegetation zones growing on adjacent soil types. Our results imply that different mitigation measures must be implemented to abate $ N_{2} $O emissions in different soil environments. |
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Pathways for Nitrous Oxide Generation in Forested and Agricultural Zones Growing on Volcanic Ash Soils |
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| score |
7.3974133 |