Email this article Mechanism specifics of the landslide-hazardous massif limit state formation and landslide block displacement
- Authors: Postoev G.P.1
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Affiliations:
- Sergeev Institute of Environmental Geoscience, Russian Academy of Sciences
- Issue: No 2 (2019)
- Pages: 13-20
- Section: NATURAL AND TECHNONATURAL PROCESSES
- URL: https://journals.eco-vector.com/0869-7809/article/view/12714
- DOI: https://doi.org/10.31857/S0869-78092019213-20
- ID: 12714
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Abstract
In the landslide cycle of deep block movement development, the landslide process starts with the separation of the new landslide block from the bedrock massif, and it ends with the block displacement until the steady landslide head is formed in the hotbed (on the landslide slope). The initial stressed state in the bedrock massif with horizontal earth surface (before the landslide block forms) is controlled by the Mohr-Coulomb criterion. The landslide hotbed forming as well as the sliding basis appearing cause the change in the initial stress state and the formation of horizontally oriented dissipative blocks-structures. The principal stresses are concentrated on the boundary surfaces of these structures (which are of a circular cylindrical shape). The limit state forms along these boundary surfaces of the appropriate block in the local massif zone on the contact with the landslide hotbed. The displacement occurs along the same surfaces, provided the equilibrium is disturbed. In forming the limit state of the head scarp massif, the adjacent part of the landslide massif (within the boundaries of the earlier separated landslide block) acts as an additional load (creates an active vertical pressure from the landslide mass weight) to the horizon of the landslide basis. The bedrock massif interacts with the slope at the stage of preparing block displacement. The block limit state is achieved in case the head scarp height reaches its critical value (the slope edge is higher than the landslide head). Under the soil masses weight in the new landslide block, separated from the bedrock massif, as it subsides, the soil crushes in a lower part of the block, which has lost its balance, in the slide basis zone. The paper considers the conditions of the new landslide block formation, the beginning of block displacement process, the mechanism of interaction between blocks, the bedrock massif and the landslide body, which consists of earlier displaced landslide blocks. The paper also provides the rationale for the soil strength changes in the process of displacement and its significance in the landslide cycle completing, with comparing the results of theoretical and experimental studies.
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About the authors
G. P. Postoev
Sergeev Institute of Environmental Geoscience, Russian Academy of Sciences
Author for correspondence.
Email: opolzen@geoenv.ru
Russian Federation, 13, str. 2, Ulanskii per., Moscow, 101000
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