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Effect of moisture content on permeability of frozen soils Item Info

Title:
Effect of moisture content on permeability of frozen soils
Authors:
Bloomsburg, G. L.; Swang, S. J.
Date Created (ISO Standard):
1969-10-16
Description:
The general subject of permeability of frozen soil and particularly the infiltration rate of frozen soil is of particular interest to hydrologists in the Northwest. A great many of our worst floods have been caused by storms occurring when the soil was frozen such that the infiltration rate was extremely slow. When this occurs, all or nearly all of the storm precipitation appears as surface runoff. Some of the more recent storms of this type were during the winters of 1962 and 1964, when there were several of these flood occurances in various sections of Idaho, eastern Oregon, and Washington. Presentation at the 16th annual meeting, Pacific Northwest Region, American Geophysical Union, at the Oregon Museum of Science and Industry, October 16 and 17, 1969.
Subjects:
soil physics soil porosity moisture content
Location:
Boise Basin
Latitude:
42.63
Longitude:
-114.53
Collection:
Boise Basin
IWRRI number:
196902
Rights:
Rights to the digital resource are held by the University of Idaho. http://www.uidaho.edu/
Publisher:
University of Idaho
Contributing Institution:
University of Idaho
Type:
Text
Format:
application/pdf
Cataloger:
wbv
Date Digitized:
2012

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Source
Preferred Citation:
"Effect of moisture content on permeability of frozen soils", Idaho Waters Digital Library, University of Idaho Library Digital Collections, https://www.lib.uidaho.edu/digital/iwdl/items/iwdl-196902.html
Rights
Rights:
Rights to the digital resource are held by the University of Idaho. http://www.uidaho.edu/