Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983 (1983)

Chapter: Water Migration Due To a Temperature Gradient in Frozen Soil

Previous Chapter: Uniaxial Compressive Strength of Ice Segregated From Soil
Suggested Citation: "Water Migration Due To a Temperature Gradient in Frozen Soil." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press. doi: 10.17226/28727.
Page 913
Suggested Citation: "Water Migration Due To a Temperature Gradient in Frozen Soil." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press. doi: 10.17226/28727.
Page 914
Suggested Citation: "Water Migration Due To a Temperature Gradient in Frozen Soil." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press. doi: 10.17226/28727.
Page 915
Suggested Citation: "Water Migration Due To a Temperature Gradient in Frozen Soil." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press. doi: 10.17226/28727.
Page 916
Next Chapter: Hydrologic Characteristics of Small Arctic-alpine Watersheds Central Brooks Range Alaska
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