Department of Geology, Anna University, Chennai, 600025, India.
Environ Monit Assess. 2011 Jan;172(1-4):481-92. doi: 10.1007/s10661-010-1348-0. Epub 2010 Feb 20.
Serious problems are faced in several parts of the world due to the presence of high concentration of fluoride in drinking water which causes dental and skeletal fluorosis to humans. Nalgonda district in Andhra Pradesh, India is one such region where high concentration of fluoride is present in groundwater. Since there are no major studies in the recent past, the present study was carried out to understand the present status of groundwater quality in Nalgonda and also to assess the possible causes for high concentration of fluoride in groundwater. Samples from 45 wells were collected once every 2 months and analyzed for fluoride concentration using an ion chromatograph. The fluoride concentration in groundwater of this region ranged from 0.1 to 8.8 mg/l with a mean of 1.3 mg/l. About 52% of the samples collected were suitable for human consumption. However, 18% of the samples were having less than the required limit of 0.6 mg/l, and 30% of the samples possessed high concentration of fluoride, i.e., above 1.5 mg/l. Weathering of rocks and evaporation of groundwater are responsible for high fluoride concentration in groundwater of this area apart from anthropogenic activities including irrigation which accelerates weathering of rocks.
由于饮用水中氟化物浓度过高,导致世界上许多地区都面临着严重的问题,这会给人类的牙齿和骨骼带来氟中毒。印度安得拉邦的纳尔贡达地区就是这样一个地下水氟化物浓度过高的地区。由于最近没有进行过重大研究,因此进行了本项研究,以了解纳尔贡达地区地下水水质的现状,并评估导致地下水氟化物浓度过高的可能原因。每隔两个月采集一次 45 口井的水样,使用离子色谱仪分析氟化物浓度。该地区地下水中的氟化物浓度范围为 0.1 至 8.8 毫克/升,平均值为 1.3 毫克/升。采集的样本中约有 52%适合人类饮用。然而,有 18%的样本中氟化物含量低于 0.6 毫克/升的要求限值,而 30%的样本中氟化物浓度较高,即超过 1.5 毫克/升。除了包括加速岩石风化的灌溉在内的人为活动外,岩石风化和地下水蒸发也是造成该地区地下水中氟化物浓度过高的原因。