The influence of soil microstructure on hydraulic properties of hydrocarbon-contaminated freezing ground
Abstract The significance of the thermodynamic relations of ice and water within the paniculate and porous soil medium has been widely demonstrated in recent decades. The existence of unfrozen water along with ice at temperatures below 0°C, because of capillary and mineral surface forces, is respons...
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Cambridge University Press (CUP)
1999
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Online Access: | http://dx.doi.org/10.1017/s0032247400026309 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400026309 |
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crcambridgeupr:10.1017/s0032247400026309 2024-04-07T07:55:33+00:00 The influence of soil microstructure on hydraulic properties of hydrocarbon-contaminated freezing ground White, T.L. Williams, P.J. 1999 http://dx.doi.org/10.1017/s0032247400026309 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400026309 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 35, issue 192, page 25-32 ISSN 0032-2474 1475-3057 General Earth and Planetary Sciences Ecology Geography, Planning and Development journal-article 1999 crcambridgeupr https://doi.org/10.1017/s0032247400026309 2024-03-08T00:36:12Z Abstract The significance of the thermodynamic relations of ice and water within the paniculate and porous soil medium has been widely demonstrated in recent decades. The existence of unfrozen water along with ice at temperatures below 0°C, because of capillary and mineral surface forces, is responsible for the specific thermal, mechanical, and hydraulic properties of soils exposed to seasonal or perennial freezing. The introduction of a hydrocarbon contaminant into this dynamic porous medium has significant consequences for the thermodynamics of the unfrozen water–ice interactions. Techniques recently developed have allowed examination of microstructures of soils exposed to freezing. It has been shown that freeze–thaw cycles produce complex changes in particle aggregation and pore space distribution, which in turn affect soil water energy. An examination of the microstructure of a hydrocarbon-contaminated, frostaffected soil revealed differences in morphology from that of similar but uncontaminated samples. These differences are in turn responsible for differences in hydraulic conductivity between uncontaminated and contaminated freezing soils. Article in Journal/Newspaper Polar Record Cambridge University Press Polar Record 35 192 25 32 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
topic |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
spellingShingle |
General Earth and Planetary Sciences Ecology Geography, Planning and Development White, T.L. Williams, P.J. The influence of soil microstructure on hydraulic properties of hydrocarbon-contaminated freezing ground |
topic_facet |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
description |
Abstract The significance of the thermodynamic relations of ice and water within the paniculate and porous soil medium has been widely demonstrated in recent decades. The existence of unfrozen water along with ice at temperatures below 0°C, because of capillary and mineral surface forces, is responsible for the specific thermal, mechanical, and hydraulic properties of soils exposed to seasonal or perennial freezing. The introduction of a hydrocarbon contaminant into this dynamic porous medium has significant consequences for the thermodynamics of the unfrozen water–ice interactions. Techniques recently developed have allowed examination of microstructures of soils exposed to freezing. It has been shown that freeze–thaw cycles produce complex changes in particle aggregation and pore space distribution, which in turn affect soil water energy. An examination of the microstructure of a hydrocarbon-contaminated, frostaffected soil revealed differences in morphology from that of similar but uncontaminated samples. These differences are in turn responsible for differences in hydraulic conductivity between uncontaminated and contaminated freezing soils. |
format |
Article in Journal/Newspaper |
author |
White, T.L. Williams, P.J. |
author_facet |
White, T.L. Williams, P.J. |
author_sort |
White, T.L. |
title |
The influence of soil microstructure on hydraulic properties of hydrocarbon-contaminated freezing ground |
title_short |
The influence of soil microstructure on hydraulic properties of hydrocarbon-contaminated freezing ground |
title_full |
The influence of soil microstructure on hydraulic properties of hydrocarbon-contaminated freezing ground |
title_fullStr |
The influence of soil microstructure on hydraulic properties of hydrocarbon-contaminated freezing ground |
title_full_unstemmed |
The influence of soil microstructure on hydraulic properties of hydrocarbon-contaminated freezing ground |
title_sort |
influence of soil microstructure on hydraulic properties of hydrocarbon-contaminated freezing ground |
publisher |
Cambridge University Press (CUP) |
publishDate |
1999 |
url |
http://dx.doi.org/10.1017/s0032247400026309 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400026309 |
genre |
Polar Record |
genre_facet |
Polar Record |
op_source |
Polar Record volume 35, issue 192, page 25-32 ISSN 0032-2474 1475-3057 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0032247400026309 |
container_title |
Polar Record |
container_volume |
35 |
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192 |
container_start_page |
25 |
op_container_end_page |
32 |
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1795672785893195776 |