“…Similarly, the heats of adsorption at infinite dilution at 298 K for all three water models were close to each other: 33.2, 31.0, and 29.7 kJ/mol for the SPC, MSPC/E, and SPC/exp-6 models, respectively, which are all in good agreement with various experimental work ,,,, and with the value of 32.5 kJ/mol calculated by Demontis et al However, when the vapor-phase adsorption isotherms at 298 K were calculated for the three water models, it was seen that water−water−silicalite three-body interactions had a significant impact on the accuracy of the simulations. Isotherms for the three different models are shown in Figure , in comparison with the previous experimental data ,− that exhibit significant variations due to the differences in samples used, where the effects of various defects, their distribution, and their crystal size are significant. The steep water uptake in experimental isotherms may be attributed to capillary condensation occurring in the mesoporosity or macroporosity of the zeolite sample .…”