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{{#category_index:C|compaction}} Loss of porosity with increasing differential pressure, usually in a nonelastic way, e.g., by grain deformation, repacking, recrystalization, etc. The normal porosity of shales given by the Hubbert-Rubey law is


where is the initial porosity (the Atterberg limits, q.v.), c is a constant, and P is the differential pressure, the difference between the overburden pressure and the formation fluid pressure. This leads to a pressure-with-depth curve that is roughly logarithmic:


Compaction is nearly irreversible, i.e., relieving the pressure that compacted a rock does not uncompact it, but releaving the pressure is apt to produce a small change (unloading effect).