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前言粘性土的分散性系指土体在缓慢流动的水中或在静水中,由于土粒表面薄膜水的增厚,土粒之间排斥力超过吸引力(万德华力),使得粘土胶粒进入悬液内并产生随水
Preface The dispersibility of cohesive soil refers to the soil in slow flowing water or in still water, due to the thickening of the water on the surface of the soil particles, the repulsion between the soil particles exceeds the attractive force (Wandereli) so that the clay particles Into the suspension and generated with the water