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- W2023350411 abstract "Abstract Direct measurements of ice crack velocity obtained from double cantilever beam fracture toughness specimens gave a terminal velocity of approximately 20 m/s or 0.01Cd (0.005Cs) where Cd is the dilatational wave velocity and Cs the shear wave velocity. This value is much lower than both theoretical predictions, and experimental values obtained in other brittle materials, of approximately 0.3 Cd. It is shown that this low velocity is due to the low hardness of ice compared to glasses. Crack bifurcation was not observed in any of the samples and this is explained by the low crack velocity — in other materials bifurcation only occurs at high velocities. It is concluded that fragment size in ice is, therefore, not the result of bifurcation, but rather a consequence of the various stress fields developed." @default.
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- W2023350411 date "1987-04-01" @default.
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- W2023350411 title "Preliminary measurements of terminal crack velocity in ice" @default.
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- W2023350411 doi "https://doi.org/10.1016/0165-232x(87)90004-8" @default.
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