To the dynamics of saturated soils
UDC
624.1+622.258EDN
XECYWJAbstract
There are considered the deformation processes in the soil body, resulting under the pulse action. Saturated soils play an important role in the study of such processes. This feature is related to short-term action. As a result of short-term action of excessive pressure, redistribution of water and air in the soil does not have time to occur and deformation is realized due to the air compression (reduction of water-ratio) and partially elastic compression of water and mineral matrix. In the low moisture soils mineral matrix receives most of the dynamic load, with considerable friction between the particles that prevents their mutual displacement and repacking, and hence the development of volumetric deformation. Increasing humidity results in improved particles repacking and increased density. However, at high rates of soil moisture, water receives dynamic load, which deformation is elastic and soil compaction reduces. Therefore, there is optimum moisture rate under dynamic loading, which achieves the highest packing. From the analysis of experimental curves it shows that this value is approximately equal to the optimum moisture content of 20%. The ability to achieve maximum compaction of soil at the optimum moisture content is at the core of the explosive method of soil compaction. The paper shows the results of soil compaction on the experimental plots. We describe the details of the research. It confirmed the effectiveness of the method.
Keywords:
water-saturated ground, shock wave, distortion, dynamic loading, thinning, compaction, humidityReferences
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Dates
Submitted
May 4, 2016
Accepted
June 16, 2016
Published
December 22, 2016
How to Cite
[1]
Kamalyan, S.R., Kamalyan, R.Z., To the dynamics of saturated soils. Ecological Bulletin of Research Centers of the Black Sea Economic Cooperation, 2016, № 4, pp. 52–60.
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Copyright (c) 2016 Камалян С.Р., Камалян Р.З.
This work is licensed under a Creative Commons Attribution 4.0 International License.
