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In the paper we present a macroscopic continuum model of adsorption in porous materials consisting of three components. We consider the ow of a uid component through channels of the skeleton. It serves as carrier for an adsorbate whose mass balance equation contains a source term. The source consists of two parts: a Langmuir contribution connected with bare sides on internal surfaces which becomes in equilibrium the Langmuir isotherm, and changes of the internal surface driven by the source offatcat:bitkoqqgrvcuhmy5m3iupkadn4