any identical units of stress. The stresses are effective, that is, less the pore pressure
Holds when: The intermediate principal stress does not affect the strength (in reality it affects it a little, usually strengthening the rock). The straight line is an approximation. At large confinements the strength curve flattens, and in loose sands the cohesion is close to zero. The strength is the peak one, the greatest stress of the test. After the peak a weak rock goes on carrying part of the load.
Sand production: types, prediction and cost of the problem →