“…It is a magnesium aluminum non-planar hydrous 2:1 phyllosilicate with modulated structure, showing a fibrous morphology resulting from the 180°inversion occurring every four silicon tetrahedra, which produces a structure of chains aligned parallel to the "a" axis, each of which has a 2:1 type structure, with exchangeable cations and reactive Si-OH groups on its surface (Bradley, 1940;Serratosa, 1978;Suarez Barrios et al, 1995) that may be involved in interactions with many different compounds. The alternation of these building blocks creates structural cavities (zeolitic channels) that lead palygorskite to have great internal surface (Casal et al, 2001). The width of the block structure is 0.64 to 0.37 nm (Fernández-Saavedra et al, 2004).…”