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粘土-水体系聚沉结构的形成过程和力学性质为很多人所研究,无论在油井钻探时、在土壤加固时(如沙漠改良,地基加固等)以及在陶瓷工业中均离下开粘土力学性质的研究,同时这种研究能解决一系列土壤学、土质学、工程地质学的重大理論问题,能阐明許多工艺过程中的物理化学原理。由于土壤胶体分散体系是个单相或多相分散在另一相的微不均匀体系和具有巨大表面的体系,物貭在高分散状态及在表面层内时,往往表现出异乎寻常的
The formation process and mechanical properties of the clayey-water system coalescence structure have been studied by many people. Whether in the process of oil well drilling, the mechanical properties of clays under soil consolidation (such as desert improvement, foundation reinforcement, etc.) and in the ceramic industry At the same time, this research can solve a series of major theoretical problems in soil science, soil science and engineering geology, and can clarify the physicochemical principles of many processes. Since soil colloidal dispersion is a heterogeneous system with a single phase or multiple phases dispersed in another phase and a system with a large surface, objects often exhibit extraordinary properties in a highly dispersed state and in the surface layer