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Using Geological Facies to Estimate Chromate Sorption to Soils

机译:利用地质相估计铬酸盐对土壤的吸附

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Quantifying the extent to which contaminant metals bind to subsurface soils is important for risk assessment, the tendency for a contaminant to migrate, and developing environmental remediation strategies. Unfortunately, subsurface soils vary widely in their composition, which in turn affect their tendency to bind metals. The hypothesis of this study was predicated on how a better understanding of geological facies would reduce uncertainty associated with predicting contaminant metal sorption. Facies are layers of sediment deposited in the subsurface due to similar depositional conditions, including energy of an overlying waterway. As such, facies are expected to have similar assemblages of minerals, particle size distributions, origins of organic matter, and similar microbial population structures. These are all important factors affecting contaminant metal sorption. The approach of this study was to collect 42 composite soil samples from a 5 m by 1.5 m grid outcrop in Graniteville, South Carolina and five end-member facies samples. The fraction of each of the five facies comprising the 42 composite soil samples were estimated. Particle size distribution (gravel, sand, silt, and clay fractions), pH, organic matter (OM), iron coating content, and microbial colony forming units were determined for each composite soil and the five end-member facies soils. Because hexavalent chromium (Cr) is the most common contaminant metal in the U.S. to exceed drinking water limits, this highly toxic and soluble metal was used as a model contaminant to provide a measure of contaminant sorption. Chromium distribution coefficients (Kd = Crsoil/Crwater) were measured. Significant correlations were identified between several soil chemical and microbial properties. A significant correlation (r = 0.423; p ≤ 0.05, d.f. = 47) was also determined between measured Kd values and Kd values calculated based on knowledge of facies Kd values. Importantly, the calculated values were characterized by large amount of inherent error. Additional work is needed to determine the applicability of this approach for remediation of contaminated sites and how best to identify appropriate facies for this novel application.
机译:量化污染物金属与地下土壤的结合程度对于风险评估,污染物迁移的趋势以及制定环境修复策略非常重要。不幸的是,地下土壤的成分差异很大,进而影响了其与金属结合的趋势。这项研究的假设是基于如何更好地了解地质相将如何减少与预测污染物金属吸附有关的不确定性。相是由于相似的沉积条件(包括上覆水道的能量)而沉积在地下的沉积物层。因此,预期相具有相似的矿物组合,粒度分布,有机物来源和相似的微生物种群结构。这些都是影响污染物金属吸附的重要因素。这项研究的方法是从南卡罗来纳州Graniteville的一个5 m x 1.5 m网格露头中收集42个复合土壤样品,以及五个末端构件相样品。估计了包含42个复合土壤样品的5个相中每个相的分数。确定了每种复合土壤和5种末端成员相土壤的粒径分布(砾石,沙子,淤泥和粘土级分),pH,有机物(OM),铁涂层含量和微生物菌落形成单位。由于六价铬(Cr)是美国超过饮用水限量的最常见污染物金属,因此使用这种剧毒且可溶的金属作为模型污染物来衡量污染物的吸收。测量了铬的分布系数(Kd = Crsoil / Crwater)。在几种土壤化学和微生物特性之间发现了显着的相关性。还确定了实测Kd值与根据相Kd值的知识计算得出的Kd值之间的显着相关性(r = 0.423; p≤0.05,d.f. = 47)。重要的是,计算值的特征在于大量的固有误差。需要进行额外的工作来确定这种方法在污染场地修复中的适用性,以及如何最好地为这种新颖的应用识别合适的相。

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