Department of Geology, S.V. University, Tirupati, 517 502, A. P, India.
Environ Monit Assess. 2011 Jan;172(1-4):427-43. doi: 10.1007/s10661-010-1345-3. Epub 2010 Feb 6.
Fluoride-rich groundwater is well known in granite aquifers in India and the world. This study examines the fluoride content of well water in different parts of Talupula area of Anantapur district, Andhra Pradesh. It also focuses on fluorides and their relationship to water-quality parameters and their impacts on humans through groundwater resources. Most parts of the area covered in this region are inherently enriched with fluorides threatening several ecosystems. The fluoride concentration ranges between 0.78 and 6.10 mg L⁻¹. The alkaline pH and high bicarbonate are responsible for release of fluoride-bearing minerals into groundwater. The arid climate of the region, the granitic rocks and the low freshwater exchange due to periodical drought conditions are the factors responsible for the higher incidence of fluorides in the groundwater resources. Apart from these prevailing natural conditions, years of neglect and lack of restoration programs on terrestrial and aquatic environments have led to accumulative impacts on groundwater, soils, plants, and animals including humans. The people dependent on these groundwater resources are prone to dental fluorosis and mild skeletal fluorosis.
富氟地下水在印度和世界的花岗岩含水层中是众所周知的。本研究调查了安得拉邦阿南塔普尔区塔卢普拉地区不同地区井水的氟含量。它还侧重于氟化物及其与水质参数的关系,以及通过地下水资源对人类的影响。该地区大部分地区都富含氟化物,威胁着多个生态系统。氟化物浓度在 0.78 至 6.10 毫克/升之间。碱性 pH 值和高碳酸氢盐导致含氟矿物释放到地下水中。该地区干旱的气候、花岗岩岩石以及由于周期性干旱条件导致的淡水交换不足,是地下水中氟化物含量较高的原因。除了这些普遍的自然条件外,多年来对陆地和水生环境的忽视和缺乏恢复计划,导致对地下水、土壤、植物和动物(包括人类)产生累积影响。依赖这些地下水资源的人们容易患氟斑牙和轻度氟骨症。