摘要: The adsorption data of Gorbach et al. (Adsorption 10(1): 29–46, 2004) and Morris (J. Colloid Interface Sci. 28: 149–155, 1968) for the water on 4A zeolite pellets is re-analyzed. Model isotherms are derived considering a two site hypothesis, one α cage β cage. Four simple model fitted to data. Both dual Toth or Langmuir isotherm fit adequately. optimized standard enthalpy entropy parameters from surprising 1/3rd that observed calorimetrically, positive, physical impossibility. Substituting calorimetric corrected differential sorption values resulting in varying significantly with temperature. This variation postulated be due either hydration formation, clathrate formation clusters such as dimers, trimers, etc.