Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983 (1983)
Chapter: Comparison of Two-dimensional Domain and Boundary Integral Geothermal Models With Embankment Freeze-thaw Field Data
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Previous Chapter:
Hydraulic Conductivity Functions of Frozen Materials
Next Chapter: Determination of Critical Height of Railroad Embankments in the Permafrost Regions of the Qinghai-xizang Plateau
Suggested Citation:
"Comparison of Two-dimensional Domain and Boundary Integral Geothermal Models With Embankment Freeze-thaw Field Data." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
Suggested Citation:
"Comparison of Two-dimensional Domain and Boundary Integral Geothermal Models With Embankment Freeze-thaw Field Data." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
Suggested Citation:
"Comparison of Two-dimensional Domain and Boundary Integral Geothermal Models With Embankment Freeze-thaw Field Data." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
Suggested Citation:
"Comparison of Two-dimensional Domain and Boundary Integral Geothermal Models With Embankment Freeze-thaw Field Data." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
Suggested Citation:
"Comparison of Two-dimensional Domain and Boundary Integral Geothermal Models With Embankment Freeze-thaw Field Data." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
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