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Winter overflow from ice gorging on shallow streams
Deals with ice gorge occurring during coldest part of winter on streams too turbulent to permit formation of crystalline surface ice; but frazil and anchor ice are formed in such quantities that stream becomes viscous mixture, resulting in rise of water and causing overflow. Discusses increasing flow of such streams during winter months by release of artificially stored water. (see also discussion by H. B. Muckleston vol. 48, no. 2, Feb. 1922, pp. 385-386)
Winter overflow from ice gorging on shallow streams
Deals with ice gorge occurring during coldest part of winter on streams too turbulent to permit formation of crystalline surface ice; but frazil and anchor ice are formed in such quantities that stream becomes viscous mixture, resulting in rise of water and causing overflow. Discusses increasing flow of such streams during winter months by release of artificially stored water. (see also discussion by H. B. Muckleston vol. 48, no. 2, Feb. 1922, pp. 385-386)
Winter overflow from ice gorging on shallow streams
Am. Soc. Civ. Engrs., Proc
Stevens, J.C. (author)
1922
20 pages
11 Figs.
Article (Journal)
English
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Winter Overflow from Ice Gorging on Shallow Streams
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