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.
Область исследования:
(Archived) Without section
References
- Bubnov I. G. Works on the theory of plates. Gostekhnteoretizdat, 1953.
- Vaitkovsky K. F. Mechanical properties of ice. AS USSR, 1960.
Similar articles
Peculiarities of influence of weak layers and ice on the stability of pillars
1969 V. G. Bezkaravayny, Yu. V. Shuvalov
Economic assessment of damage from losses and dilution during development of rich ores
1969 P. G. Makulov
Investigation of properties of injection solutions for reinforcing the embedment of cleaning chambers
1969 Yu. L. Minaev