Titlebook: Rock Mechanics; Leopold Müller Book 1972 Springer-Verlag Wien 1972 Gebirgsmechanik.Mechanics.Coulomb.design.elasticity.finite element meth

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Graphical Methods for Slope Stability Analysis,der the sliding of rigid bodies along existing or newly formed planes of weakness in two dimensions only. Three-dimensional problems can be solved by means of analytical geometry, however, these approaches are often too sophisticated for the stability problems encountered in engineering practice.

枯萎将要

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Technical Parameters of Rock and Rock Masses,ere mentioned. In this lecture, we shall examine more closely, first of all, those engineering properties of the rock masses which require to be determined in our engineering structures. It need not be emphasized that the engineering structure and the geological ground form together a physical syste

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Geology in Rock Mechanics,. Müller, who invited me to deal with a subject which is somehow a premise for understanding the substantial reasons that suggested and favoured the development of a Mechanic of rock masses, that is a Mechanic of a geological medium.

Compass

A Review of Fracture Criteria of Brittle Rock,neral phenomenon of fracture. Yet, the understanding of this phenomenon is fundamental if a material is used in any engineering design, whether the aim is to prevent failure of the structure or to promote it.

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Brittle Fracture of Rocks, loading systems. At failure their resitance to carry load rapidly drops to zero. This behaviour is commonly known as the “brittle” behaviour of rocks. Only recently it was recognized that such a behaviour is largely due to the rapid release of stored strain energy from the specimen-machine system (

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摇摆

Fibrillation

Friction Properties and Frictional Behavior of Rock Separation Planes,be applied to the mechanical behaviour of rock masses near the earth’s surface. The concept of discontinuum mechanics was developed, in which the deformational behaviour of rock masses takes place by relative movements along discontinuities like faults, joints, bedding-planes, etc.. The separation p

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