The Turnover of Organic Carbon and Nitrogen in Soil [and Discussion]

Although the decomposition of plant material in soil is an extremely complex process, relatively simple models can give good fits to the decay process. Thus a two-compartment model gives a close representation, over the first few years, of the decay of 14C-labelled plant material in soil. A model co...

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Veröffentlicht in:Philosophical transactions of the Royal Society of London. Series B. Biological sciences 1990-09, Vol.329 (1255), p.361-368
Hauptverfasser: Jenkinson, D. S., Andrew, S. P. S., Lynch, J. M., Goss, M. J., Tinker, P. B.
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container_issue 1255
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container_title Philosophical transactions of the Royal Society of London. Series B. Biological sciences
container_volume 329
creator Jenkinson, D. S.
Andrew, S. P. S.
Lynch, J. M.
Goss, M. J.
Tinker, P. B.
description Although the decomposition of plant material in soil is an extremely complex process, relatively simple models can give good fits to the decay process. Thus a two-compartment model gives a close representation, over the first few years, of the decay of 14C-labelled plant material in soil. A model containing a single homogeneous humus compartment decomposing by a first-order process is surprisingly useful for soil organic nitrogen over periods measured in decades. More sophisticated multicompartmental models are now widely used to represent turnover in soil. One of these, the Rothamsted turnover model, is described in detail and shown to give a useful representation of data from the Rothamsted long-term field experiments.
doi_str_mv 10.1098/rstb.1990.0177
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ispartof Philosophical transactions of the Royal Society of London. Series B. Biological sciences, 1990-09, Vol.329 (1255), p.361-368
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1471-2970
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subjects Agricultural soils
Agrology
Carbon
Clay soils
Fate of Organic Materials in Soils
Grassland soils
Nitrogen
Organic soils
Soil air
Soil organic carbon
Soil organic matter
title The Turnover of Organic Carbon and Nitrogen in Soil [and Discussion]
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