Crustal Imaging and Characterization Team
Rich Wanty
F/Cl ratios in waters can be used to help evaluate water sources and transport pathways. There are a few factors that govern the F/Cl systematics: 1) fluoride is uncommon in most rocks, but more common in mineral deposits, so it provides a good source term, and 2) fluoride may be reactive, so it can't necessarily be treated as a conservative solute. To further test the utility of using F/Cl ratios, existing literature was compiled and experiments were performed on fluoride adsorption onto common rock-forming minerals, such as quartz, feldspars, and micas. Dissolution of micas also may be a source term in some cases. The hypothesis that the variation in F/Cl ratios in nature exceeds the amount of F attenuation due to water-rock interactions was tested. Once the reactivity of fluoride is better understood, the assumption that F and Cl are conservative can be better tested.
Rich Wanty
Box 25046 MS 964D Denver Federal Center
Denver, CO 80225-0046
Phone: (303) 236-1819
Email: rwanty
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