“…The general chemical structure of vermiculites is X 4 (Y 2–3 )O 10 (OH) 2 M·nH 2 O, where X is a Si or Al, Y is Mg 2+ , Fe 2+ or Fe 3+ , Al 3+ and M is an exchangeable by Mg 2+ , Ca 2+ , Ba 2+ , Na + , and K + . X responds to a tetrahedral sheet, which is usually silica, and Y responds to an octahedral, usually magnesia [ 26 , 27 ].…”