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The Formation and Model of High Fluoride Groundwater and In-situ Dispelling Fluoride Assumption in Gaomi City of Shandong Province

Zong-jun GAO( ), Zhen-hui ZHU, Xiao-di LIU, Yan-lan XU
Shandong University of Science and Technology, Qingdao, China, 266590
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Abstract

The occurrence of fluorosis in Gaomi City is among the highest regions in China. High fluoride groundwater occurrence in Quaternary sediments originated from the weathering residuals of Cretaceous volcano clastic rock. The origin of high fluoride groundwater in Gaomi City was summarized as the following 2 model: one is leaching and enrichment, the other one is evaporation and condensation in alkali condition. Based on the analysis of the local environment and the mechanism of fluoride enrichment, a method of “in- situ dispelling” was proposed and confirmed through laboratory leaching test. This might be economical and feasible method for the removal of fluorine from the local strata.

Keywords

In-situ dispelling of fluorideHigh fluorine strataHigh fluoride groundwaterExampleGaomi City, Shandong, China

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Journal of Groundwater Science and Engineering
Volume 2 Issue 2,
June 2014
Pages 34-39
DOI: 10.26599/JGSE.2014.9280016

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GAO Z-j, ZHU Z-h, LIU X-d, et al. The Formation and Model of High Fluoride Groundwater and In-situ Dispelling Fluoride Assumption in Gaomi City of Shandong Province. Journal of Groundwater Science and Engineering, 2014, 2(2): 34-39. https://doi.org/10.26599/JGSE.2014.9280016

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Published: 28 June 2014
© 2014 Journal of Groundwater Science and Engineering Editorial Office