Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation
Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures fo...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Urakawa, Rieko [verfasserIn] Ohte, Nobuhito [verfasserIn] Shibata, Hideaki [verfasserIn] Tateno, Ryunosuke [verfasserIn] Inagaki, Yoshiyuki [verfasserIn] Oda, Tomoki [verfasserIn] Toda, Hiroto [verfasserIn] Fukuzawa, Karibu [verfasserIn] Watanabe, Tsunehiro [verfasserIn] Hishi, Takuo [verfasserIn] Oyanagi, Nobuhiro [verfasserIn] Nakata, Makoto [verfasserIn] Fukushima, Keitaro [verfasserIn] Nakanishi, Asami [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Ecological research - Bognor Regis : Wiley, 1986, 32(2016), 2 vom: 19. Dez., Seite 279-285 |
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| Übergeordnetes Werk: |
volume:32 ; year:2016 ; number:2 ; day:19 ; month:12 ; pages:279-285 |
| Links: |
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| DOI / URN: |
10.1007/s11284-016-1420-5 |
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| Katalog-ID: |
SPR018641075 |
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| 245 | 1 | 0 | |a Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation |
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| 520 | |a Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation. | ||
| 650 | 4 | |a Forest soil |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Net N mineralization rate |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Net nitrification rate |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a In situ incubation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Laboratory incubation |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Ohte, Nobuhito |e verfasserin |4 aut | |
| 700 | 1 | |a Shibata, Hideaki |e verfasserin |4 aut | |
| 700 | 1 | |a Tateno, Ryunosuke |e verfasserin |4 aut | |
| 700 | 1 | |a Inagaki, Yoshiyuki |e verfasserin |4 aut | |
| 700 | 1 | |a Oda, Tomoki |e verfasserin |4 aut | |
| 700 | 1 | |a Toda, Hiroto |e verfasserin |4 aut | |
| 700 | 1 | |a Fukuzawa, Karibu |e verfasserin |4 aut | |
| 700 | 1 | |a Watanabe, Tsunehiro |e verfasserin |4 aut | |
| 700 | 1 | |a Hishi, Takuo |e verfasserin |4 aut | |
| 700 | 1 | |a Oyanagi, Nobuhiro |e verfasserin |4 aut | |
| 700 | 1 | |a Nakata, Makoto |e verfasserin |4 aut | |
| 700 | 1 | |a Fukushima, Keitaro |e verfasserin |4 aut | |
| 700 | 1 | |a Nakanishi, Asami |e verfasserin |4 aut | |
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10.1007/s11284-016-1420-5 doi (DE-627)SPR018641075 (SPR)s11284-016-1420-5-e DE-627 ger DE-627 rakwb eng 570 630 ASE 42.00 bkl Urakawa, Rieko verfasserin aut Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation. Forest soil (dpeaa)DE-He213 Net N mineralization rate (dpeaa)DE-He213 Net nitrification rate (dpeaa)DE-He213 In situ incubation (dpeaa)DE-He213 Laboratory incubation (dpeaa)DE-He213 Ohte, Nobuhito verfasserin aut Shibata, Hideaki verfasserin aut Tateno, Ryunosuke verfasserin aut Inagaki, Yoshiyuki verfasserin aut Oda, Tomoki verfasserin aut Toda, Hiroto verfasserin aut Fukuzawa, Karibu verfasserin aut Watanabe, Tsunehiro verfasserin aut Hishi, Takuo verfasserin aut Oyanagi, Nobuhiro verfasserin aut Nakata, Makoto verfasserin aut Fukushima, Keitaro verfasserin aut Nakanishi, Asami verfasserin aut Enthalten in Ecological research Bognor Regis : Wiley, 1986 32(2016), 2 vom: 19. Dez., Seite 279-285 (DE-627)320630773 (DE-600)2023900-2 1440-1703 nnns volume:32 year:2016 number:2 day:19 month:12 pages:279-285 https://dx.doi.org/10.1007/s11284-016-1420-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_266 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_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 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_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 42.00 ASE AR 32 2016 2 19 12 279-285 |
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10.1007/s11284-016-1420-5 doi (DE-627)SPR018641075 (SPR)s11284-016-1420-5-e DE-627 ger DE-627 rakwb eng 570 630 ASE 42.00 bkl Urakawa, Rieko verfasserin aut Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation. Forest soil (dpeaa)DE-He213 Net N mineralization rate (dpeaa)DE-He213 Net nitrification rate (dpeaa)DE-He213 In situ incubation (dpeaa)DE-He213 Laboratory incubation (dpeaa)DE-He213 Ohte, Nobuhito verfasserin aut Shibata, Hideaki verfasserin aut Tateno, Ryunosuke verfasserin aut Inagaki, Yoshiyuki verfasserin aut Oda, Tomoki verfasserin aut Toda, Hiroto verfasserin aut Fukuzawa, Karibu verfasserin aut Watanabe, Tsunehiro verfasserin aut Hishi, Takuo verfasserin aut Oyanagi, Nobuhiro verfasserin aut Nakata, Makoto verfasserin aut Fukushima, Keitaro verfasserin aut Nakanishi, Asami verfasserin aut Enthalten in Ecological research Bognor Regis : Wiley, 1986 32(2016), 2 vom: 19. Dez., Seite 279-285 (DE-627)320630773 (DE-600)2023900-2 1440-1703 nnns volume:32 year:2016 number:2 day:19 month:12 pages:279-285 https://dx.doi.org/10.1007/s11284-016-1420-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_266 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_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 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_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 42.00 ASE AR 32 2016 2 19 12 279-285 |
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10.1007/s11284-016-1420-5 doi (DE-627)SPR018641075 (SPR)s11284-016-1420-5-e DE-627 ger DE-627 rakwb eng 570 630 ASE 42.00 bkl Urakawa, Rieko verfasserin aut Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation. Forest soil (dpeaa)DE-He213 Net N mineralization rate (dpeaa)DE-He213 Net nitrification rate (dpeaa)DE-He213 In situ incubation (dpeaa)DE-He213 Laboratory incubation (dpeaa)DE-He213 Ohte, Nobuhito verfasserin aut Shibata, Hideaki verfasserin aut Tateno, Ryunosuke verfasserin aut Inagaki, Yoshiyuki verfasserin aut Oda, Tomoki verfasserin aut Toda, Hiroto verfasserin aut Fukuzawa, Karibu verfasserin aut Watanabe, Tsunehiro verfasserin aut Hishi, Takuo verfasserin aut Oyanagi, Nobuhiro verfasserin aut Nakata, Makoto verfasserin aut Fukushima, Keitaro verfasserin aut Nakanishi, Asami verfasserin aut Enthalten in Ecological research Bognor Regis : Wiley, 1986 32(2016), 2 vom: 19. Dez., Seite 279-285 (DE-627)320630773 (DE-600)2023900-2 1440-1703 nnns volume:32 year:2016 number:2 day:19 month:12 pages:279-285 https://dx.doi.org/10.1007/s11284-016-1420-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_266 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_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 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_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 42.00 ASE AR 32 2016 2 19 12 279-285 |
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10.1007/s11284-016-1420-5 doi (DE-627)SPR018641075 (SPR)s11284-016-1420-5-e DE-627 ger DE-627 rakwb eng 570 630 ASE 42.00 bkl Urakawa, Rieko verfasserin aut Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation. Forest soil (dpeaa)DE-He213 Net N mineralization rate (dpeaa)DE-He213 Net nitrification rate (dpeaa)DE-He213 In situ incubation (dpeaa)DE-He213 Laboratory incubation (dpeaa)DE-He213 Ohte, Nobuhito verfasserin aut Shibata, Hideaki verfasserin aut Tateno, Ryunosuke verfasserin aut Inagaki, Yoshiyuki verfasserin aut Oda, Tomoki verfasserin aut Toda, Hiroto verfasserin aut Fukuzawa, Karibu verfasserin aut Watanabe, Tsunehiro verfasserin aut Hishi, Takuo verfasserin aut Oyanagi, Nobuhiro verfasserin aut Nakata, Makoto verfasserin aut Fukushima, Keitaro verfasserin aut Nakanishi, Asami verfasserin aut Enthalten in Ecological research Bognor Regis : Wiley, 1986 32(2016), 2 vom: 19. Dez., Seite 279-285 (DE-627)320630773 (DE-600)2023900-2 1440-1703 nnns volume:32 year:2016 number:2 day:19 month:12 pages:279-285 https://dx.doi.org/10.1007/s11284-016-1420-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_266 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_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 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_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 42.00 ASE AR 32 2016 2 19 12 279-285 |
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10.1007/s11284-016-1420-5 doi (DE-627)SPR018641075 (SPR)s11284-016-1420-5-e DE-627 ger DE-627 rakwb eng 570 630 ASE 42.00 bkl Urakawa, Rieko verfasserin aut Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation. Forest soil (dpeaa)DE-He213 Net N mineralization rate (dpeaa)DE-He213 Net nitrification rate (dpeaa)DE-He213 In situ incubation (dpeaa)DE-He213 Laboratory incubation (dpeaa)DE-He213 Ohte, Nobuhito verfasserin aut Shibata, Hideaki verfasserin aut Tateno, Ryunosuke verfasserin aut Inagaki, Yoshiyuki verfasserin aut Oda, Tomoki verfasserin aut Toda, Hiroto verfasserin aut Fukuzawa, Karibu verfasserin aut Watanabe, Tsunehiro verfasserin aut Hishi, Takuo verfasserin aut Oyanagi, Nobuhiro verfasserin aut Nakata, Makoto verfasserin aut Fukushima, Keitaro verfasserin aut Nakanishi, Asami verfasserin aut Enthalten in Ecological research Bognor Regis : Wiley, 1986 32(2016), 2 vom: 19. Dez., Seite 279-285 (DE-627)320630773 (DE-600)2023900-2 1440-1703 nnns volume:32 year:2016 number:2 day:19 month:12 pages:279-285 https://dx.doi.org/10.1007/s11284-016-1420-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_266 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_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 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_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 42.00 ASE AR 32 2016 2 19 12 279-285 |
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English |
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Enthalten in Ecological research 32(2016), 2 vom: 19. Dez., Seite 279-285 volume:32 year:2016 number:2 day:19 month:12 pages:279-285 |
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Enthalten in Ecological research 32(2016), 2 vom: 19. Dez., Seite 279-285 volume:32 year:2016 number:2 day:19 month:12 pages:279-285 |
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Forest soil Net N mineralization rate Net nitrification rate In situ incubation Laboratory incubation |
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Ecological research |
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Urakawa, Rieko @@aut@@ Ohte, Nobuhito @@aut@@ Shibata, Hideaki @@aut@@ Tateno, Ryunosuke @@aut@@ Inagaki, Yoshiyuki @@aut@@ Oda, Tomoki @@aut@@ Toda, Hiroto @@aut@@ Fukuzawa, Karibu @@aut@@ Watanabe, Tsunehiro @@aut@@ Hishi, Takuo @@aut@@ Oyanagi, Nobuhiro @@aut@@ Nakata, Makoto @@aut@@ Fukushima, Keitaro @@aut@@ Nakanishi, Asami @@aut@@ |
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2016-12-19T00:00:00Z |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR018641075</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230519162518.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201006s2016 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11284-016-1420-5</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR018641075</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s11284-016-1420-5-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">570</subfield><subfield code="a">630</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">42.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Urakawa, Rieko</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Forest soil</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Net N mineralization rate</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Net nitrification rate</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">In situ incubation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Laboratory incubation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ohte, Nobuhito</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Shibata, Hideaki</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tateno, Ryunosuke</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Inagaki, Yoshiyuki</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Oda, Tomoki</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Toda, Hiroto</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fukuzawa, Karibu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Watanabe, Tsunehiro</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Hishi, Takuo</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Oyanagi, Nobuhiro</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nakata, Makoto</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fukushima, Keitaro</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nakanishi, Asami</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">Ecological research</subfield><subfield code="d">Bognor Regis : Wiley, 1986</subfield><subfield code="g">32(2016), 2 vom: 19. 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| author |
Urakawa, Rieko |
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Urakawa, Rieko ddc 570 bkl 42.00 misc Forest soil misc Net N mineralization rate misc Net nitrification rate misc In situ incubation misc Laboratory incubation Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation |
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Urakawa, Rieko |
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1440-1703 |
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570 630 ASE 42.00 bkl Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation Forest soil (dpeaa)DE-He213 Net N mineralization rate (dpeaa)DE-He213 Net nitrification rate (dpeaa)DE-He213 In situ incubation (dpeaa)DE-He213 Laboratory incubation (dpeaa)DE-He213 |
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ddc 570 bkl 42.00 misc Forest soil misc Net N mineralization rate misc Net nitrification rate misc In situ incubation misc Laboratory incubation |
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ddc 570 bkl 42.00 misc Forest soil misc Net N mineralization rate misc Net nitrification rate misc In situ incubation misc Laboratory incubation |
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ddc 570 bkl 42.00 misc Forest soil misc Net N mineralization rate misc Net nitrification rate misc In situ incubation misc Laboratory incubation |
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Elektronische Aufsätze Aufsätze Elektronische Ressource |
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Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation |
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(DE-627)SPR018641075 (SPR)s11284-016-1420-5-e |
| title_full |
Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation |
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Urakawa, Rieko |
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Ecological research |
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Ecological research |
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eng |
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500 - Science 600 - Technology |
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2016 |
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Urakawa, Rieko Ohte, Nobuhito Shibata, Hideaki Tateno, Ryunosuke Inagaki, Yoshiyuki Oda, Tomoki Toda, Hiroto Fukuzawa, Karibu Watanabe, Tsunehiro Hishi, Takuo Oyanagi, Nobuhiro Nakata, Makoto Fukushima, Keitaro Nakanishi, Asami |
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Elektronische Aufsätze |
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Urakawa, Rieko |
| doi_str_mv |
10.1007/s11284-016-1420-5 |
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570 630 |
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verfasserin |
| title_sort |
estimation of field soil nitrogen mineralization and nitrification rates using soil n transformation parameters obtained through laboratory incubation |
| title_auth |
Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation |
| abstract |
Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation. |
| abstractGer |
Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation. |
| abstract_unstemmed |
Abstract We tested the potential of estimating in-field (in situ) nitrogen (N) transformation rates based on soil temperature data and N transformation parameters ($ Q_{10} $ and N transformation rates at standard temperature) obtained through laboratory incubations at three constant temperatures for 4 weeks. This test was conducted based on a comparison between in situ measurements and estimates using soils from 16 sites across 9 regions within the Japanese archipelago. The actual in situ N mineralization and nitrification rates measured using the buried-bag method at 0–50-cm-soil depth were 111 ± 34 and 106 ± 45 kg N $ ha^{−1} $ $ year^{−1} $, respectively, and estimates of both the rate and the amount were largely accurate. For rate alone, estimates were accurate in the 0–10-cm soil layer for annual and seasonal averages (except for spring–summer) whereas for amount alone, estimates were accurate to depths of 50 and 30 cm for N mineralization and nitrification, respectively. Thus, estimates of the rates and amounts were approximately equal to the actual in situ rate/amount, given the wide range of prediction intervals of the field measurement data. The differences between the estimates of N transformation rates derived from hourly measured and monthly average soil temperatures were negligible. Therefore, in situ soil N transformations, which are laborious to measure in the field, have the potential to be estimated from a combination of monthly average soil temperatures and N transformation parameters, which are relatively straightforward to obtain through laboratory incubation. |
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Estimation of field soil nitrogen mineralization and nitrification rates using soil N transformation parameters obtained through laboratory incubation |
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https://dx.doi.org/10.1007/s11284-016-1420-5 |
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Ohte, Nobuhito Shibata, Hideaki Tateno, Ryunosuke Inagaki, Yoshiyuki Oda, Tomoki Toda, Hiroto Fukuzawa, Karibu Watanabe, Tsunehiro Hishi, Takuo Oyanagi, Nobuhiro Nakata, Makoto Fukushima, Keitaro Nakanishi, Asami |
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Ohte, Nobuhito Shibata, Hideaki Tateno, Ryunosuke Inagaki, Yoshiyuki Oda, Tomoki Toda, Hiroto Fukuzawa, Karibu Watanabe, Tsunehiro Hishi, Takuo Oyanagi, Nobuhiro Nakata, Makoto Fukushima, Keitaro Nakanishi, Asami |
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| score |
7.398737 |