Abstract
The influence of adhesive forces on the structure of sedimentation layers has been considered. A theoretical model allowing calculation of the porosity of a sedimentation layer as a function of the particle size, the layer thickness, and the adhesive‐force level has been developed. Experiments in which these variables were changed have been carried out. The adhesive force was varied by changing the concentration of the electrolyte. A quantitative agreement between theory and experiment is observed for the porosity as a function of the particle size and the layer thickness; for the porosity as a function of the adhesive force this agreement is qualitative.
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Dueck, J.G., Purevjav, D. & Kilimnik, D.Y. A Contribution to the Theory of Porosity of Fine‐Grained Sediments. Journal of Engineering Physics and Thermophysics 77, 93–102 (2004). https://doi.org/10.1023/B:JOEP.0000020722.04941.c5
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DOI: https://doi.org/10.1023/B:JOEP.0000020722.04941.c5