“…The presence of silanol defects ((SiOH) x ; i.e., the hydrophility of a material) stabilizes H 2 O within zeolite pores and impacts adsorption energies for H 2 O within BEA and MFI zeolites. 6,7,10,14,19,20,31,[36][37][38] The literature, however, lacks an understanding for how the structures that H 2 O forms depends on the combination of zeolite topology and (SiOH) x densities. Moreover, the thermochemical properties of these H 2 O structures will likely exhibit a complex dependence on the pore diameter and (SiOH) x density, because the importance of SiOH functions may change as H 2 O loses opportunities to hydrogen bond via spatial constraints.…”