“…During silylation, silane molecules and hydrolyzed silanes entered Mt galleries and caused a prominent increase of the basal spacing [8]. Also, the intercalated silane molecules would hydrolyze to silanols due to the interlayer water of Mt and consequently condensation among themselves to form oligomers and/or with the two adjacent layers, simultaneously [10,11]. The silane oligomers act as pillars for expansion of Mt layers and the simultaneous condensation of silane (oligomers) with the two adjacent clay layers will fix the interlayer height to a certain value, resulting in a locking effect.…”