Theoretical Studies of Ice Segregation in Soil
Abstract The mathematical theory of heat conduction is applied to the analysis of ice segregation processes in soil. A diffusion equation is first employed for the flow of soil moisture. Two new quantities, the rate of ice segregation,σ and the segregation efficiency, E , are introduced. The first i...
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Cambridge University Press (CUP)
1966
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Online Access: | http://dx.doi.org/10.1017/s0022143000019274 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019274 |
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crcambridgeupr:10.1017/s0022143000019274 2024-03-03T08:46:08+00:00 Theoretical Studies of Ice Segregation in Soil Arakawa, Kiyoshi 1966 http://dx.doi.org/10.1017/s0022143000019274 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019274 en eng Cambridge University Press (CUP) Journal of Glaciology volume 6, issue 44, page 255-260 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1966 crcambridgeupr https://doi.org/10.1017/s0022143000019274 2024-02-08T08:36:15Z Abstract The mathematical theory of heat conduction is applied to the analysis of ice segregation processes in soil. A diffusion equation is first employed for the flow of soil moisture. Two new quantities, the rate of ice segregation,σ and the segregation efficiency, E , are introduced. The first is the rate of ice growth measured as mass per area per time. The latter is defined as E = σL /( K 1 ∂T 1 / ∂x − K 2 ∂T 2 / ∂x ), where L is the latent heat of fusion of ice, T 1 and K 1 are the temperature and thermal conductivity of frozen soil, and T 2 and K 2 are the temperature and thermal conductivity of unfrozen soil. Three types of soil freezing can be classified in terms of E : freezing of non-frost-susceptible soil ( E = 0), perfect segregation ( E = 1) and imperfect segregation (0 < E < 1). Finally, the mathematical boundary conditions at an advancing frost line are obtained in freezing, frost-susceptible soil ( E ≠ 0). Two parameters related to the structure of soil are pointed out, which seem to be valid criteria of frost susceptibility. The amount of frost-heaving is derived under special conditions. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 6 44 255 260 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Arakawa, Kiyoshi Theoretical Studies of Ice Segregation in Soil |
topic_facet |
Earth-Surface Processes |
description |
Abstract The mathematical theory of heat conduction is applied to the analysis of ice segregation processes in soil. A diffusion equation is first employed for the flow of soil moisture. Two new quantities, the rate of ice segregation,σ and the segregation efficiency, E , are introduced. The first is the rate of ice growth measured as mass per area per time. The latter is defined as E = σL /( K 1 ∂T 1 / ∂x − K 2 ∂T 2 / ∂x ), where L is the latent heat of fusion of ice, T 1 and K 1 are the temperature and thermal conductivity of frozen soil, and T 2 and K 2 are the temperature and thermal conductivity of unfrozen soil. Three types of soil freezing can be classified in terms of E : freezing of non-frost-susceptible soil ( E = 0), perfect segregation ( E = 1) and imperfect segregation (0 < E < 1). Finally, the mathematical boundary conditions at an advancing frost line are obtained in freezing, frost-susceptible soil ( E ≠ 0). Two parameters related to the structure of soil are pointed out, which seem to be valid criteria of frost susceptibility. The amount of frost-heaving is derived under special conditions. |
format |
Article in Journal/Newspaper |
author |
Arakawa, Kiyoshi |
author_facet |
Arakawa, Kiyoshi |
author_sort |
Arakawa, Kiyoshi |
title |
Theoretical Studies of Ice Segregation in Soil |
title_short |
Theoretical Studies of Ice Segregation in Soil |
title_full |
Theoretical Studies of Ice Segregation in Soil |
title_fullStr |
Theoretical Studies of Ice Segregation in Soil |
title_full_unstemmed |
Theoretical Studies of Ice Segregation in Soil |
title_sort |
theoretical studies of ice segregation in soil |
publisher |
Cambridge University Press (CUP) |
publishDate |
1966 |
url |
http://dx.doi.org/10.1017/s0022143000019274 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019274 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 6, issue 44, page 255-260 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000019274 |
container_title |
Journal of Glaciology |
container_volume |
6 |
container_issue |
44 |
container_start_page |
255 |
op_container_end_page |
260 |
_version_ |
1792502054732693504 |