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Some studies suggest that fluoride levels in well water can exceed safe limits and pose health risks, while other studies indicate that fluoride concentrations are generally within safe limits but still require monitoring.
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Fluoride is a naturally occurring element found in various geological formations, and its presence in well water is a common phenomenon worldwide. The concentration of fluoride in groundwater can vary significantly depending on the local geology, hydrology, and human activities.
In the southern edge of the Chinese Loess Plateau, studies have shown that 64% of shallow groundwater samples exceed the fluoride limit of 1.5 mg/L, with some samples reaching up to 3.8 mg/L. This high concentration is primarily due to the dissolution of fluoride-containing minerals and prolonged water-rock interactions in the aquifer.
In the United States, data from over 38,000 wells indicate that 10.9% of domestic wells have fluoride concentrations above 0.7 mg/L, with 2.6% exceeding 2 mg/L and 0.6% surpassing 4 mg/L. The highest fluoride levels are often associated with greater pH values, total dissolved solids (TDS), and alkalinity, particularly in the western regions.
In Northern Thailand, high fluoride levels have been documented in both shallow and deep wells, with 31% of shallow wells and 35% of deep wells in certain areas containing hazardous levels of fluoride (≥1.5 mg/L). The sources of fluoride include geothermal fields and geological formations such as biotite-granite.
In the Región Lagunera of Northern Mexico, fluoride concentrations in well water range from less than 0.5 to 3.7 mg/L. Approximately 19.4% of samples exceed the 1.5 mg/L limit. There is a strong correlation between fluoride and arsenic concentrations, indicating a shared geogenic source.
A survey of wells across Saudi Arabia revealed fluoride levels ranging from 0.10 to 5.4 mg/L. About 13.96% of the wells exceeded the World Health Organization's recommended level of 1.5 mg/L, with the highest concentrations found in regions like Hadwood Shamalyah and Hail.
In the Shanmuganadhi River basin of South India, fluoride levels in groundwater vary seasonally, with concentrations ranging from 0.01 to 3.30 mg/L. The primary sources of fluoride are minerals in granitic and gneissic rocks, as well as agricultural fertilizers.
High fluoride levels in drinking water can lead to dental and skeletal fluorosis, posing significant health risks to affected populations. In regions with elevated fluoride concentrations, both adults and children are at risk of developing these conditions .
Several methods have been explored to reduce fluoride levels in well water, including:
Fluoride contamination in well water is a widespread issue influenced by natural geological processes and human activities. The variability in fluoride levels across different regions underscores the need for localized studies and tailored mitigation strategies to ensure safe drinking water. Regular monitoring and the implementation of effective fluoride-removal techniques are essential to protect public health.
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