Calculation of limit spans of unshored frozen roofs
Authors:
Abstract
A characteristic feature of deposits located in the permafrost zone is cementation of rock blocks with ice, which fills interlayer cracks and cracks that cut through rock layers, which promotes consolidation of layers and leads to an increase in the bearing capacity of the massif as a whole.
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References
- Bubnov I. G. Works on the theory of plates. Gostekhnteoretizdat, 1953.
- Vaitkovsky K. F. Mechanical properties of ice. AS USSR, 1960.
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