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Near-surface seismic reflection investigations at a groundwater contamination site.

机译:地下水污染现场的近地表地震反射调查。

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A 3-D seismic reflection survey was conducted at a groundwater contamination site to adequately image the near surface (20m) at a level of detail to enhance ongoing remediation activities at the site. The site, Operable Unit 2 (OU2), located at Hill Air Force Base in Ogden, Utah has been the subject of a continuing effort to remove dense nonaqueous phase liquids (DNAPLs), solvents and degreasers, which had been dumped into trenches at the site for eight years. Subsurface maps of the near surface geology, based solely on data from the over 200 monitoring wells drilled at the site, do not provide sufficient detail of subsurface features that trap these contaminants to conduct site remediation in a cost-effective manner.; The target geologic feature for remediation, a paleochannel complex, under a surface layer of unconsolidated sands, silts and gravels, cut into a thick layer of clay. The paleochannel traps both groundwater and contaminants. The paleochannel was the focus of an earlier 2-D survey, demonstrating the viability of the site for seismic methods. Successfully imaging the channel profile in three places, results from the 2-D survey served as a testbed for planning for the 3-D survey.; The 3-D reflection survey covered an area of 37 x 95m centered over the paleochannel. After data processing, the resulting seismic volume shows a paleochannel complex with two channels from the north merging into a single channel that spreads out across the southern portion of the survey. Intersecting the channel are two displacement surfaces, origins unknown, disrupting channel flow and altering the pattern of erosion and deposition. The resulting map shows the channel complex with depth to base clay varying from 6 to 18.33m. Vertical resolution of the depth-to-clay map is 1.25m (lambda/2).; Stratigraphic analysis of the sedimentary package above the interpreted clay surface confirms the seismic interpretation. Comparison with results from a tomographic study (Azaria, 2003) and a VSP study (Gao et al., 2003) at the site confirm the reflection survey results.*; *This dissertation is a compound document (contains both a paper copy and a CD as part of the dissertation).
机译:在地下水污染现场进行了3D地震反射调查,以详细地对近地表(<20m)进行成像,以增强现场的正在进行的修复活动。位于犹他州奥格登市希尔空军基地的可操作单元2(OU2)现场一直在努力清除被倾倒在沟渠中的稠密非水相液体(DNAPLs),溶剂和脱脂剂。网站使用了八年。仅基于现场钻探的200多个监测井的数据,近地表地质的地下图没有提供足够的地下特征细节,这些特征会诱捕这些污染物以经济有效的方式进行现场修复。整治的目标地质特征是一个古河道综合体,位于未固结的沙子,淤泥和砾石的表层下,被切成厚厚的粘土层。古河道既捕集地下水,又捕集污染物。古河道是早期二维调查的重点,证明了该地点在地震方法方面的可行性。 2-D测量的结果成功地在三个地方成像,2-D测量的结果成为了3-D测量计划的测试平台。 3-D反射调查覆盖了以古河道为中心的37 x 95m区域。经过数据处理后,所产生的地震体显示出一个古河道综合体,其北部的两个河道合并成一个单一的河道,并在整个勘测的南部扩散。与通道相交的是两个位移面,其起源不明,破坏了通道流动并改变了侵蚀和沉积的模式。生成的地图显示了通道复合体,其深度与基础黏土的深度在6到18.33m之间。深度-粘土图的垂直分辨率为1.25m(λ/ 2)。对解释后的粘土表面之上的沉积物包裹的地层分析证实了地震解释。与现场层析成像研究(Azaria,2003年)和VSP研究(Gao等,2003年)的结果进行比较,证实了反射调查的结果。 *本论文是复合文件(作为论文的一部分,包含纸质副本和CD)。

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