Skip to main content
. 2022 Feb 9;12(2):259. doi: 10.3390/life12020259

Figure 1.

Figure 1

Two examples of typical crystal structures of common clay minerals: (a) montmorillonite, a 2:1 type smectite with layers consisting of two tetrahedral sheets and one octahedral sheet with layers separated by the interlayer space with hydrated cations; (b) kaolinite, a 1:1 type clay mineral with layers consisting of one tetrahedral and one octahedral sheet.