Author:
Connell D.C.,Tombs J.M.C.
Abstract
Abstract
Polycrystalline ice, growing from the melt, can exert a pressure against an extended obstacle, even though it is free to grow in other directions. Pressures of over 0.2 bar (20kN m-2) have been measured with simple apparatus. This phenomenon may be important in explaining the frost-shattering of rocks.
Publisher
Cambridge University Press (CUP)
Cited by
11 articles.
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