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Water confined in heterogeneous clay–quartz pores: Structure and dynamics from atomistic simulations
The molecular-scale behavior of water in heterogeneous clay–quartz systems is critical for understanding cementation processes in natural soils and compacted bentonite, which is crucial for oil recovery and nuclear waste disposal barriers construction. Here we investigate how heterogeneity of mixed Na-montmorillonite and α-quartz surfaces affect water structure and dynamics in nanopores of 2.5 to 60 Å in the presence of different surface functional groups. The results show that surface roughness alters water orientation and hydrogen bonding, with surface effects extending up to 15 Å. Water mobility is decreases with quartz addition in nano-channels due to strong surface hydrogen bond networks. For pores larger than 20 Å , the heterogeneous system behaves as a linear combination of its components, while smaller pores exhibit non-additive behavior due to the greater effect of short-range van der Waals interactions.