本文作者根据胶体混合体系凝聚理论和有关的测验资料,提出了粘土矿物絮团的推理模式.根据该模式,可以计算絮团的平均容重,并可对一泥沙运动现象,例如淤泥运动的临界容重,浮泥的界限容重等,作出较合理的解释.该文的发表希望能引起有关同志的讨沦,以利该课题的深入研究. Based on the cohesive theory of colloidal mixed systems and the related test data, the authors propose a model for in silico mineral flocculation based on which the average bulk density of flocs can be calculated and the effect of a sediment movement such as the criticality of silt motion Bulk density, the limit weight of the floating mud, etc., to make a more reasonable explanation.The publication of this paper hopes to arouse the discussion of comrades in order to facilitate the in-depth study of the subject.