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Application of rare earth elements for water source discrimination in Renlou coal mine, northern Anhui Province, China

机译:稀土元素在北安徽省北部煤矿水源辨别中的应用

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Rare earth element (REEs) concentrations were measured for groundwater and wall rock samples from two aquifers (sandstone and limestone aquifers) in Renlou coal mine, northern Anhui Province, China. The results indicate that groundwater from these two aquifers are rich in REEs as expressed by their Nd concentrations (0.012 and 0.008 μg/L). They all show heavy REEs enrichment with low Nd_(RN)/Yb_(RN) ratios (0.35 and 0.40) when normalized to their aquifer rocks. Y- Ho fractionation are only observed for groundwater from limestone aquifer with high Y/Ho ratio (97 in average), whereas groundwater from sandstone aquifer have low Y/Ho ratios (24 in average). The former is considered to be related to the release of Y and Ho from calcite with different partition coefficient. The similarity of some REEs between groundwater and aquifer rock, as well as the different rock composition of aquifers, provide possibility for discrimination of water sources by using REEs, and Y/Ho ratios and Eu anomalies are expected to be useful in Renlou coal mine.
机译:稀土元素(REES)浓度从北安徽省北安北部的Wenlou煤矿两种含水层(砂岩和石灰石含水层)的地下水和壁岩样。结果表明,来自这两种含水层的地下水富含其Nd浓度(0.012和0.008μg/ L)的REES。它们全部显示重型REES在含水层岩石中的低ND_(RN)/ YB_(RN)比率(0.35和0.40)。 y-ho分馏仅观察到具有高y / ho比的石灰石含水层的地下水(平均97个),而砂岩含水层的地下水具有低Y / HO比(平均24个)。前者被认为与具有不同分区系数的方解石的y和ho的释放有关。地下水和含水层岩石之间的一些簧片的相似性,以及含水层的不同岩石组成,通过使用REES来提供水源的可能性,以及Y / HO比和欧盟异常的可能性在Renlou煤矿中有用。

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