Paths of stress, temperature, and chemical potential are known to strongly influence the evolution of the transport properties of rocks. This is especially true where the materials are fractured, and permeability is strongly coupled to relatively small
changes in fracture apertures, that may in turn be driven by changes in stress or chemical potential.
Long Term Flow Through Tests
Long term flow through tests provide measurements of:
By your continued use of our website you agree to Core Lab's usage of cookies. More Information