Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.chemgeo.2009.10.003 |
Fluoride dynamics in the granitic aquifer of the Wailapally watershed, Nalgonda District, India | |
Reddy, D. V.1; Nagabhushanam, P.1; Sukhija, B. S.1; Reddy, A. G. S.2; Smedley, P. L.3 | |
通讯作者 | Reddy, D. V. |
来源期刊 | CHEMICAL GEOLOGY
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ISSN | 0009-2541 |
出版年 | 2010 |
卷号 | 269期号:3-4页码:278-289 |
英文摘要 | High concentrations of fluoride (up to 7.6 mg/L) are a recognized feature of the Wailapally granitic aquifer of Nalgonda District, Andhra Pradesh, India. The basement rocks provide abundant sources of F in the form of amphibole, biotite, fluorite and apatite. The whole-rock concentrations of F in the aquifer are in the range 240-990 mg/kg. Calcretes from the shallow weathered horizons also contain comparably high concentrations of F (635-950 mg/kg). The concentrations of water-soluble F in the granitic rocks and the calcretes are usually low (1% of the total or less) but broadly correlate with the concentrations observed in groundwaters in the local vicinity. The water-soluble fraction of fluoride is relatively high in weathered calcretes compared to fresh calcretes. Groundwater major-ion composition shows a well-defined trend with flow downgradient in the Wailapally aquifer, from Na-Ca-HCO(3)-dominated waters in the recharge area at the upper part of the catchment, through to Na-Mg-HCO(3) and ultimately to Na-HCO(3) and Na-HCO(3)-Cl types in the discharge area in the lowest part. The evolution occurs over a reach spanning some 17 km Groundwater chemistry evolves by silicate weathering reactions, although groundwaters rapidly reach equilibrium with carbonate minerals, favouring precipitation of calcite, and ultimately dolomite in the lower parts of the watershed. This precipitation is also aided by evapotranspiration. Decreasing Ca activity downgradient leads to a dominance of fluorite-undersaturated conditions and consequently to mobilisation of F. Despite the clear downgradient evolution of major-ion chemistry, concentrations of F remain relatively uniform in the fluorite-undersaturated groundwaters, most being in the range 3.0-7.6 mg/L The rather narrow range is attributed to a mechanism of co-precipitation with and/or adsorption to calcrete in the lower sections of the aquifer. The model may find application in other high-F groundwaters from granitic aquifers of semi-arid regions. (C) 2009 Elsevier B.V. All rights reserved. |
英文关键词 | Fluoride Groundwater Health Granite Soil profiles Calcrete |
类型 | Article |
语种 | 英语 |
国家 | India ; England |
收录类别 | SCI-E |
WOS记录号 | WOS:000274767600009 |
WOS关键词 | ENVIRONMENTAL CHLORIDE ; NATURAL-WATERS ; SOUTHERN INDIA ; ANDHRA-PRADESH ; GROUNDWATERS ; GEOCHEMISTRY ; GENESIS ; CONTAMINATION ; ADSORPTION ; CHINA |
WOS类目 | Geochemistry & Geophysics |
WOS研究方向 | Geochemistry & Geophysics |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/163633 |
作者单位 | 1.Natl Geophys Res Inst, Council Sci & Ind Res, Hyderabad 500606, Andhra Pradesh, India; 2.Cent Groundwater Board, Hyderabad 500029, Andhra Pradesh, India; 3.British Geol Survey, Wallingford OX10 8BB, Oxon, England |
推荐引用方式 GB/T 7714 | Reddy, D. V.,Nagabhushanam, P.,Sukhija, B. S.,et al. Fluoride dynamics in the granitic aquifer of the Wailapally watershed, Nalgonda District, India[J],2010,269(3-4):278-289. |
APA | Reddy, D. V.,Nagabhushanam, P.,Sukhija, B. S.,Reddy, A. G. S.,&Smedley, P. L..(2010).Fluoride dynamics in the granitic aquifer of the Wailapally watershed, Nalgonda District, India.CHEMICAL GEOLOGY,269(3-4),278-289. |
MLA | Reddy, D. V.,et al."Fluoride dynamics in the granitic aquifer of the Wailapally watershed, Nalgonda District, India".CHEMICAL GEOLOGY 269.3-4(2010):278-289. |
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