International Journal of Current Microbiology and Applied Sciences · 2018 · 33 citations · 35 references
Natural SciencesEnvironmental SciencesSoil SciencesGeochemistrySoil ChemistrySoil SalinityEnvironmental GeochemistryGroundwater ContaminationGroundwater GeochemistrySoil ContaminationSoil GeochemistrySoil PollutionFluoridationFluoride ContaminationFluoride EnrichmentFluoride ReleaseSkeletal FluorosisSoil Mineral - Solution InteractionsSoil Solution Geochemistry
Fluoride (F-) contamination in groundwater has been recognized as a serious problem worldwide. It is estimated that more than 200 million people from 25 countries are under the dreadful fate of fluorosis, among them India and China are the two worst affected countries In India 62 million people (including 6 million children), suffer from dental, skeletal or non-skeletal fluorosis because of consumption of fluoride-contaminated water. Rajasthan is one of the most affected states with fluoride concentration in the range of 0.1-14 mg L-1. The source of fluoride in soil and water is predominantly geogenic and released by weathering of fluoride containing minerals such as fluorite and fluorapatite, while anthropogenic sources include brick industry, aluminium smelters and use of phosphatic fertilisers. The geochemistry of fluoride is mainly governed by two processes i.e. enrichment and leaching. Fluoride mobility in soil is highly dependent on the soil’s sorption capacity, which varies with pH, salinity and types of sorbents present in soil. In general, fluorine present in soil as minerals, adsorbed on clay and oxy-hydroxides, while a few amount is present as dissolved form in soil solution. Fluoride normally enters the human body through water, food, industrial exposure, drugs, cosmetics etc. The fluoride levels of food depend upon the nature of soil and quality of water used for irrigation and thus varies from place to place. Prosopis julifora is a hyper-accumulator of F- and has potential to remediate fluoride contaminated soils (Baunthiyal and Sharma, 2012). Fluoride ion concentration in drinking water can be easily detected by ion selective electrode. Various defluoridation techniques have been developed to reduce the fluoride content to the desired level including principally membrane and adsorption processes (Amor et al., 2001). Different bio-sorbents such as chitosan coated silica (Krishnaiah et al., 2009) stalks of sorghum and canola are efficient in removal of fluoride from water. Apart from these technical approaches awareness among the people needs to be created for prevention from fluoride health hazards.
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John Fawell · Water Intelligence Online · 2013 · 604 citations
Natural Resources, Environmental Sciences, Water Resources Management +17
Geochemistry and Genesis of Fluoride‐Containing Ground Waters in India
B. K. Handa · Ground Water · 1975 · 513 citations