Abstract
The results of an investigation of structure formation processes in mineral dispersions are given. It is shown that the thixotropic phenomenon has an important meaning in the strengthening of mineral systems without additional pressure. The conditions for achieving optimum structure under drying of mineral dispersions were revealed. The theological investigations of some minerals under high temperature was introduced, and the role of crystalline transformations of kaolinite and montmorillonite was shown affect the greatest plastic visconsity η 1 of their dispersions.
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