Vermiculite
Vermiculite (Verm) is a generally ctahedral 2:1 clay mineral with hydrated cations occupying the interlayer space. However, the negative layer charge of Verm, arising mostly from substitution of Al 3 + for Si 4 + in tetrahedral sites, is larger than that of smectite (Brigatti et al., 2013). Haley et al. (1982) observed two sharp Raman bands at 3739 cm − …
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