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quick condition : ウィキペディア英語版 | quick condition The quick condition of soil is the condition when the upward water pressure gradient and water flow reduce the effective stress, i.e., cohesiveness of the soil. Sandy soils may lose their shear strength, and the soil may behave as a fluid. Cohesive soils may produce cracks with water seepage.〔''McGraw-Hill Dictionary of Architecture and Construction'', article "Quick condition"〕〔(A reference on soil mechanics ), University of the West England〕〔F.G.Bell, ''Engineering Geology'', ISBN 抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「quick condition」の詳細全文を読む
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