Abstract
An algorithm for determining the electrical and hydrodynamic parameters of soils during their electroosmotic treatment is presented. The results of computer simulation of non-stationary physical processes occurring in clay soils during the flow of electric current without the introduction of active solutions are given.
Highlights
The physical parameters characterizing the process of electroosmotic soil treatment are the velocity of electroosmosis, coefficients of filtration kf, electroosmosis ke and electroosmotic activity ( k = k ⁄k ).Determining these characteristics by various methods requires multi-stage cumbersome measurements, the availability of special laboratory equipment [1,2,3,4,5,6,7,8], it is advisable to increase the efficiency and accuracy of assessments using an experimental-analytical research method, including computer modeling, experimental data obtained at various stages of electrical processing
The initial data for the first stage were the graphs of changes in the value of the relative resistivity (Fig. 2) [7, 9]
The stage is responsible for determining the size of the characteristic zones formed during the processing of the soil (Fig. 3)
Summary
The physical parameters characterizing the process of electroosmotic soil treatment are the velocity of electroosmosis, coefficients of filtration kf, electroosmosis ke and electroosmotic activity ( k = k ⁄k ).Determining these characteristics by various methods requires multi-stage cumbersome measurements, the availability of special laboratory equipment [1,2,3,4,5,6,7,8], it is advisable to increase the efficiency and accuracy of assessments using an experimental-analytical research method, including computer modeling, experimental data obtained at various stages of electrical processing
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