Colloid-chemical characterization of clayey rocks
Authors:
Abstract
In engineering geology, clayey rocks are considered as some multiphase systems consisting of mineral particles, water and air. The mineral particles, forming the skeleton of the rock, are in most cases the main constituent of the rock. Water and air fill the spaces between the mineral particles in the rock pores. The rock pores may contain only air or only water, or air and water together. In some cases, the water filling the rock pores may be in a solid state (as ice). The degree of moisture in the clay rocks changes their state and they can be two or three or in some cases even four-phase systems.
Область исследования:
Geology
References
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