Lithological influences on occurrence of high-fluoride groundwater …
However, kaolin may also adsorb a large quantity of F − ions (Sreedevi et al., 2006). The primary kaolin deposits of the study area have F − concentration between 468 and 1722 mg kg −1; however secondary kaolin deposit at Gori has low F − quantity (270 mg kg −1), probably the F − ions have been washed out in water during ...
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