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Registro Completo |
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Biblioteca(s): |
Embrapa Cerrados. |
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Data corrente: |
21/12/2017 |
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Data da última atualização: |
21/12/2017 |
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Autoria: |
YANNI, S. F.; JANZEN, H. H.; GREGORICH, E. G.; ELLERT, B. H.; LARNEY, F. J.; OLSON, B. M.; ZVOMUYA, F. |
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Afiliação: |
SANDRA F. YANNI, AGRICULTURE AND AGRI-FOOD CANADA; H. HENRY JANZEN, AGRICULTURE AND AGRI-FOOD CANADA; EDWARD G. GREGORICH, AGRICULTURE AND AGRI-FOOD CANADA; BEN H. ELLERT, AGRICULTURE AND AGRI-FOOD CANADA; FRANCIS J. LARNEY, AGRICULTURE AND AGRI-FOOD CANADA; BARRY M. OLSON, ALBERTA AGRICULTURE AND FORESTRY; FRANCIS ZVOMUYA, UNIVERSITY OF MANITOBA. |
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Título: |
Organic carbon convergence in diverse soils toward Steady State: a 21-year field bioassay. |
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Ano de publicação: |
2016 |
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Fonte/Imprenta: |
Soil Science Society of America Journal, V. 80, P. 1653-1662, Oct. 2016. |
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DOI: |
doi:10.2136/sssaj2016.07.0214 |
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Idioma: |
Inglês |
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Notas: |
The equation on page 1656 should read: If OC21> OC0 , then OCt=(OCeq-OC0) x [1-exp(-kt)]+OC0. |
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Conteúdo: |
Abstract: The response of soil organic matter (SOM) to an abrupt change in environment and management was studied in a long-term field bioassay. Thirty-six soils, with a wide range of SOM reflecting large differences in management, climate, and ecological histories, were selected and transported to a common site at Lethbridge, Alberta, Canada. The experiment included control and N-fertilized treatment plots. The plots were seeded annually to spring wheat and managed under no-till rain-fed conditions, with annual removal of aboveground residues. The soils were sampled every 7 yr and analyzed for organic C (OC), total N (TN), and light fraction C (LF-C) and N (LF-N). Most of the soils lost OC and TN over 21 yr, and the amount of loss was highly related to the original contents (9?74 g C kg−1, 1.4?6.4 g N kg−1). Similarly, LF-C and LF-N, indices of labile OM, declined in most soils, but the rate of loss was faster than for OC. In a few soils, SOM slowly increased from initially low levels. The soils seem to be progressing toward a steady state, although complete convergence of OC and TN may not occur for a century or longer based on an exponential model. Labile OM may converge within a few decades, so that these soils, conceivably, will still have widely different OC and TN but similar labile SOM, with possible implications for soil health. Our findings demonstrate the value of long-term field bioassays for improved understanding of SOM dynamics in response to management and climate change. MenosAbstract: The response of soil organic matter (SOM) to an abrupt change in environment and management was studied in a long-term field bioassay. Thirty-six soils, with a wide range of SOM reflecting large differences in management, climate, and ecological histories, were selected and transported to a common site at Lethbridge, Alberta, Canada. The experiment included control and N-fertilized treatment plots. The plots were seeded annually to spring wheat and managed under no-till rain-fed conditions, with annual removal of aboveground residues. The soils were sampled every 7 yr and analyzed for organic C (OC), total N (TN), and light fraction C (LF-C) and N (LF-N). Most of the soils lost OC and TN over 21 yr, and the amount of loss was highly related to the original contents (9?74 g C kg−1, 1.4?6.4 g N kg−1). Similarly, LF-C and LF-N, indices of labile OM, declined in most soils, but the rate of loss was faster than for OC. In a few soils, SOM slowly increased from initially low levels. The soils seem to be progressing toward a steady state, although complete convergence of OC and TN may not occur for a century or longer based on an exponential model. Labile OM may converge within a few decades, so that these soils, conceivably, will still have widely different OC and TN but similar labile SOM, with possible implications for soil health. Our findings demonstrate the value of long-term field bioassays for improved understanding of SOM dynamics in response to manag... Mostrar Tudo |
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Palavras-Chave: |
Bioenssaio; Matéria orgânica do solo. |
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Thesagro: |
Carbono; Matéria Orgânica; Mudança Climática; Química do Solo. |
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Thesaurus Nal: |
Canada. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
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001 2083339
005 2017-12-21
008 2016 bl uuuu u00u1 u #d
024 7 $adoi:10.2136/sssaj2016.07.0214$2DOI
100 1 $aYANNI, S. F.
245 $aOrganic carbon convergence in diverse soils toward Steady State$ba 21-year field bioassay.$h[electronic resource]
260 $c2016
500 $aThe equation on page 1656 should read: If OC21> OC0 , then OCt=(OCeq-OC0) x [1-exp(-kt)]+OC0.
520 $aAbstract: The response of soil organic matter (SOM) to an abrupt change in environment and management was studied in a long-term field bioassay. Thirty-six soils, with a wide range of SOM reflecting large differences in management, climate, and ecological histories, were selected and transported to a common site at Lethbridge, Alberta, Canada. The experiment included control and N-fertilized treatment plots. The plots were seeded annually to spring wheat and managed under no-till rain-fed conditions, with annual removal of aboveground residues. The soils were sampled every 7 yr and analyzed for organic C (OC), total N (TN), and light fraction C (LF-C) and N (LF-N). Most of the soils lost OC and TN over 21 yr, and the amount of loss was highly related to the original contents (9?74 g C kg−1, 1.4?6.4 g N kg−1). Similarly, LF-C and LF-N, indices of labile OM, declined in most soils, but the rate of loss was faster than for OC. In a few soils, SOM slowly increased from initially low levels. The soils seem to be progressing toward a steady state, although complete convergence of OC and TN may not occur for a century or longer based on an exponential model. Labile OM may converge within a few decades, so that these soils, conceivably, will still have widely different OC and TN but similar labile SOM, with possible implications for soil health. Our findings demonstrate the value of long-term field bioassays for improved understanding of SOM dynamics in response to management and climate change.
650 $aCanada
650 $aCarbono
650 $aMatéria Orgânica
650 $aMudança Climática
650 $aQuímica do Solo
653 $aBioenssaio
653 $aMatéria orgânica do solo
700 1 $aJANZEN, H. H.
700 1 $aGREGORICH, E. G.
700 1 $aELLERT, B. H.
700 1 $aLARNEY, F. J.
700 1 $aOLSON, B. M.
700 1 $aZVOMUYA, F.
773 $tSoil Science Society of America Journal, V. 80, P. 1653-1662, Oct. 2016.
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