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Deformation and Shrinkage Effects on the Soil Water Release Characteristic

Gregory, Andrew S ; Bird, Nigel R.A ; Whalley, W. Richard ; Matthews, G. Peter ; Young, Iain M

Soil Science Society of America journal, 2010-07, Vol.74 (4), p.1104-1112 [Periódico revisado por pares]

Madison: Soil Science Society

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Título:
Deformation and Shrinkage Effects on the Soil Water Release Characteristic
Autor: Gregory, Andrew S ; Bird, Nigel R.A ; Whalley, W. Richard ; Matthews, G. Peter ; Young, Iain M
Assuntos: Agronomy. Soil science and plant productions ; arable soils ; Biological and medical sciences ; Compressed ; computed tomography ; Consolidation ; Deformation ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Fundamental and applied biological sciences. Psychology ; grassland soils ; Grasslands ; Mathematical analysis ; Mathematical models ; nondestructive methods ; Physical properties ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Porosity ; Porous materials ; saturated conditions ; shear stress ; Shrinkage ; simulation models ; Soil (material) ; soil aggregates ; soil matric potential ; soil pore system ; Soil science ; soil water characteristic ; soil water retention ; Soils ; Standard deviation ; Surficial geology ; topsoil ; volume ; Water and solute dynamics
É parte de: Soil Science Society of America journal, 2010-07, Vol.74 (4), p.1104-1112
Notas: http://dx.doi.org/10.2136/sssaj2009.0278
All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher. Permission for printing and for reprinting the material contained herein has been obtained by the publisher.
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Descrição: The soil water release characteristic is controlled by the soil pores and so alteration of the pore system will have an effect. We sought to examine the effects of various pore deformations in a range of arable and grassland soils from the UK. Sieved topsoil materials were compressed to 50 or 200 kPa, or remolded to simulate shear deformation at the plastic limit. They were then subjected to matric potentials from 0 to -1500 kPa using conventional tension and pressure plate apparatus. Volume changes were monitored to assess shrinkage. Further samples in the compressed state were subjected to x-ray computed tomography scanning to nondestructively characterize the soil pore system. Increasing the compression from 50 to 200 kPa mainly affected the >30-µm pores, changing a dual porous system of inter- and intraaggregate pores to one mainly dominated by intraaggregate pores, as confirmed by gravimetric water release characteristic data and the scans. Shear-deformed soils retained more water than the compressed soil and shrank more, such that they remained tension saturated at low (negative) matric potentials. We developed a function to predict the soil saturation state as a function of matric potential and porosity. This explained 28 to 63% of the variance, irrespective of the initial structural state, but up to 94% of the variation when one of the fitted parameters was allowed to vary for the different initial states. This was sufficiently systematic to suggest that a general model of the effects of soil deformation and shrinkage on the water release characteristic may be possible.
Editor: Madison: Soil Science Society
Idioma: Inglês

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Deformation and Shrinkage Effects on the Soil Water Release Characteristic

Gregory, Andrew S ; Bird, Nigel R.A ; Whalley, W. Richard ; Matthews, G. Peter ; Young, Iain M

Madison: Soil Science Society

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