author_facet Laegdsmand, Mette
Moldrup, Per
Schjønning, Per
Laegdsmand, Mette
Moldrup, Per
Schjønning, Per
author Laegdsmand, Mette
Moldrup, Per
Schjønning, Per
spellingShingle Laegdsmand, Mette
Moldrup, Per
Schjønning, Per
Soil Science Society of America Journal
Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
Soil Science
author_sort laegdsmand, mette
spelling Laegdsmand, Mette Moldrup, Per Schjønning, Per 0361-5995 1435-0661 Wiley Soil Science http://dx.doi.org/10.2136/sssaj2011.0043 <jats:p>Solute diffusivity in soil plays a major role in many important processes with relation to plant growth and environmental issues. Soil solute diffusivity is affected by the volumetric water content as well as the morphological characteristics of water‐filled pores. The solute diffusivity in intact soil samples from two different tillage treatments (soil from below the depth of a harrow treatment and soil from within a moldboard plowed plow layer) was estimated based on concentration profiles using a newly developed method. The method makes use of multiple tracers (two sets of counterdiffusing tracers) for a better determination of the diffusivity. The diffusivity was higher in the below‐till soil than the plowed soil at the same soil water matric potential due to higher water content but also due to higher continuity and lower tortuosity of the soil pores. We measured identical solute diffusivities independent of the tracer set used. We analyzed the whole data set using Archie's law and found a linear relation between Archie's exponent and the logarithm of the soil water matric suction in centimeters of water (pF). An analysis of seven data sets from the literature showed that this was a general trend for soils with moderate to low clay contents.</jats:p> Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential Soil Science Society of America Journal
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title Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_unstemmed Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_full Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_fullStr Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_full_unstemmed Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_short Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_sort solute diffusivity in undisturbed soil: effects of soil water content and matric potential
topic Soil Science
url http://dx.doi.org/10.2136/sssaj2011.0043
publishDate 2012
physical 51-60
description <jats:p>Solute diffusivity in soil plays a major role in many important processes with relation to plant growth and environmental issues. Soil solute diffusivity is affected by the volumetric water content as well as the morphological characteristics of water‐filled pores. The solute diffusivity in intact soil samples from two different tillage treatments (soil from below the depth of a harrow treatment and soil from within a moldboard plowed plow layer) was estimated based on concentration profiles using a newly developed method. The method makes use of multiple tracers (two sets of counterdiffusing tracers) for a better determination of the diffusivity. The diffusivity was higher in the below‐till soil than the plowed soil at the same soil water matric potential due to higher water content but also due to higher continuity and lower tortuosity of the soil pores. We measured identical solute diffusivities independent of the tracer set used. We analyzed the whole data set using Archie's law and found a linear relation between Archie's exponent and the logarithm of the soil water matric suction in centimeters of water (pF). An analysis of seven data sets from the literature showed that this was a general trend for soils with moderate to low clay contents.</jats:p>
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author Laegdsmand, Mette, Moldrup, Per, Schjønning, Per
author_facet Laegdsmand, Mette, Moldrup, Per, Schjønning, Per, Laegdsmand, Mette, Moldrup, Per, Schjønning, Per
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container_issue 1
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description <jats:p>Solute diffusivity in soil plays a major role in many important processes with relation to plant growth and environmental issues. Soil solute diffusivity is affected by the volumetric water content as well as the morphological characteristics of water‐filled pores. The solute diffusivity in intact soil samples from two different tillage treatments (soil from below the depth of a harrow treatment and soil from within a moldboard plowed plow layer) was estimated based on concentration profiles using a newly developed method. The method makes use of multiple tracers (two sets of counterdiffusing tracers) for a better determination of the diffusivity. The diffusivity was higher in the below‐till soil than the plowed soil at the same soil water matric potential due to higher water content but also due to higher continuity and lower tortuosity of the soil pores. We measured identical solute diffusivities independent of the tracer set used. We analyzed the whole data set using Archie's law and found a linear relation between Archie's exponent and the logarithm of the soil water matric suction in centimeters of water (pF). An analysis of seven data sets from the literature showed that this was a general trend for soils with moderate to low clay contents.</jats:p>
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spelling Laegdsmand, Mette Moldrup, Per Schjønning, Per 0361-5995 1435-0661 Wiley Soil Science http://dx.doi.org/10.2136/sssaj2011.0043 <jats:p>Solute diffusivity in soil plays a major role in many important processes with relation to plant growth and environmental issues. Soil solute diffusivity is affected by the volumetric water content as well as the morphological characteristics of water‐filled pores. The solute diffusivity in intact soil samples from two different tillage treatments (soil from below the depth of a harrow treatment and soil from within a moldboard plowed plow layer) was estimated based on concentration profiles using a newly developed method. The method makes use of multiple tracers (two sets of counterdiffusing tracers) for a better determination of the diffusivity. The diffusivity was higher in the below‐till soil than the plowed soil at the same soil water matric potential due to higher water content but also due to higher continuity and lower tortuosity of the soil pores. We measured identical solute diffusivities independent of the tracer set used. We analyzed the whole data set using Archie's law and found a linear relation between Archie's exponent and the logarithm of the soil water matric suction in centimeters of water (pF). An analysis of seven data sets from the literature showed that this was a general trend for soils with moderate to low clay contents.</jats:p> Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential Soil Science Society of America Journal
spellingShingle Laegdsmand, Mette, Moldrup, Per, Schjønning, Per, Soil Science Society of America Journal, Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential, Soil Science
title Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_full Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_fullStr Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_full_unstemmed Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_short Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
title_sort solute diffusivity in undisturbed soil: effects of soil water content and matric potential
title_unstemmed Solute Diffusivity in Undisturbed Soil: Effects of Soil Water Content and Matric Potential
topic Soil Science
url http://dx.doi.org/10.2136/sssaj2011.0043