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MULTI-ELEMENT ANALYSES OF PRIVATE WELLS ON THE ST. REGIS MOHAWK NATION (AKWESASNE)

机译:ST上私人井的多元素分析。里格斯·莫哈克族(阿克瓦萨涅)

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One hundred and fifty four well water samples from private wells on the St. Regis Mohawk Nation (Akwesasne) were collected for multi-element analyses to determine the quality of drinking water. An additional thirty-five samples were analyzed for quality control including method blanks, standards, and duplicates, and confirm the high quality of the data collected. In twenty-six instances drinking water standards established by the Environmental Protection Agency (EPA) for various elements were exceeded. Secondary standards for manganese (n = 19) and total dissolved solids (TDS; n = 24) were most often violated. One well exceeded the EPA Maximum Contaminant Level (MCL) for Mercury, one well exceeded the MCL for Arsenic, and one well exceeded the action level for Lead. Several wells had concentrations near the EPA primary MCL for Arsenic. The source(s) of these contaminants is unknown and could be natural. Sodium was found in all wells sampled and had an average concentration of 67 ppm; however, relatively high values of >400 ppm were also measured. A wide variation in water chemistry was noted suggesting potable water is drawn from more than one source. Major chemical trends can be explained by infiltration of water through unconsolidated glacial deposits into a confined rock aquifer (Ogdensburg Dolostone) containing a source of soluble evaporite minerals contributing to enhanced concentrations of elements such as bromine, chlorine, lithium, magnesium, potassium, sodium, and strontium and characterized by a Ca:Mg ratio of ~60:40. There is no evidence for widespread impact to groundwater resources in the wells sampled; however, this statement applies only to inorganic compounds.
机译:收集了来自瑞吉莫霍克族(Akwesasne)的私人井中的一百四十四口井水样品,进行多元素分析,以确定饮用水的质量。对另外的35个样品进行了质量控制分析,包括方法空白,标准品和重复样品,并确认了所收集数据的高质量。在超过26种情况下,超过了环境保护局(EPA)为各种元素制定的饮用水标准。经常违反锰(n = 19)和总溶解固体(TDS; n = 24)的二级标准。一口水银超过了EPA的最大污染物限量(MCL),一口水超过了砷的MCL,一口超出了铅的行动水平。几个孔的浓度接近EPA砷的主要MCL。这些污染物的来源未知,可能是自然的。在所有采样的孔中均发现钠,其平均浓度为67 ppm。但是,也测量到了较高的值,即> 400 ppm。注意到水化学变化很大,表明饮用水取自多种来源。主要化学趋势可以解释为:水通过未固结的冰川沉积物进入密闭岩石含水层(Ogdensburg Dolostone),该含水层中含有可溶性蒸发矿物,有助于提高元素的浓度,例如溴,氯,锂,镁,钾,钠,和锶,其特征是Ca:Mg比约为60:40。没有证据表明采样井对地下水资源有广泛影响。但是,该声明仅适用于无机化合物。

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