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A geostatistical approach for quantification of contaminant mass discharge uncertainty using multilevel sampler measurements

机译:使用多级采样器测量来量化污染物质量排放不确定性的地统计学方法

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Contaminant mass discharge across a control plane downstream of a dense nonaqueous phase liquid (DNAPL) source zone has great potential to serve as a metric for the assessment of the effectiveness of source zone treatment technologies and for the development of risk-based source-plume remediation strategies. However, too often the uncertainty of mass discharge estimated in the field is not accounted for in the analysis. In this paper, a geostatistical approach is proposed to estimate mass discharge and to quantify its associated uncertainty using multilevel transect measurements of contaminant concentration (C) and hydraulic conductivity (K). The approach adapts the p-field simulation algorithm to propagate and upscale the uncertainty of mass discharge from the local uncertainty models of C and K. Application of this methodology to numerically simulated transects shows that, with a regular sampling pattern, geostatistics can provide an accurate model of uncertainty for the transects that are associated with low levels of source mass removal (i.e., transects that have a large percentage of contaminated area). For high levels of mass removal (i.e., transects with a few hot spots and large areas of near-zero concentration), a total sampling area equivalent to 6~7% of the transect is required to achieve accurate uncertainty modeling. A comparison of the results for different measurement supports indicates that samples taken with longer screen lengths may lead to less accurate models of mass discharge uncertainty. The quantification of mass discharge uncertainty, in the form of a probability distribution, will facilitate risk assessment associated with various remediation strategies.
机译:稠密非水相液体(DNAPL)源区下游控制平面上的污染物大量排放具有巨大潜力,可作为评估源区处理技术有效性和开发基于风险的源-源头补救措施的指标策略。但是,在分析中往往没有考虑到现场估计的质量排放的不确定性。在本文中,提出了一种地统计学方法来估计质量流量并使用污染物浓度(C)和水力传导率(K)的多级样线测量来量化其相关的不确定性。该方法采用p场模拟算法来传播和放大C和K局部不确定性模型中的质量排放不确定性。将该方法应用于数值模拟样条表明,采用规则的采样模式,地统计学可以提供准确的结果。与源物质去除水平低相关的样线(即,污染面积百分比很大的样线)的不确定性模型。对于高水平的质量去除(即具有少量热点和接近零浓度的大面积的样线),需要总采样面积相当于样条线的6〜7%以实现准确的不确定性建模。不同测量支持物的结果比较表明,采用更长筛网长度采集的样品可能会导致质量排放不确定性模型的准确性降低。大量排放不确定性以概率分布的形式进行量化将有助于与各种补救策略相关的风险评估。

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