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The aim of this paper is to summarize the experimental work carried out by IFP on rock samples taken from the Meuse/Haute Marne underground research laboratory host formation. The behavior of this clayey rock, called ''argillite,'' has been studied within the framework of Biot's mechanics of fluid saturated porous solids. Drained and undrained oedometric tests (i.e., uniaxial strain tests) have been...