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Three-dimensional electrical resistivity model of a nuclear waste disposal site

机译:核废料处置场的三维电阻率模型

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A three-dimensional (3D) modeling study was completed on a very large electrical resistivity survey conducted at a nuclear waste site in eastern Washington. The acquisition included 47 pole–pole twodimensional (2D) resistivity profiles collected along parallel and orthogonal lines over an area of 850 m×570 m. The data were geo-referenced and inverted using EarthImager3D (EI3D). EI3D runs on a Microsoft 32-bit operating system (e.g. WIN-2K, XP) with a maximum usable memory of 2 GB. The memory limits the size of the domain for the inversion model to 200 m×200 m, based on the survey electrode density. Therefore, a series of increasing overlapping models were run to evaluate the effectiveness of dividing the survey area into smaller subdomains. The results of the smaller subdomains were compared to the inversion results of a single domain over a larger area using an upgraded form of EI3D that incorporates multi-processing capabilities and 32 GB of RAM memory. The contours from the smaller subdomains showed discontinuity at the boundaries between the adjacent models, which do not match the hydrogeologic expectations given the nature of disposal at the site. At several boundaries, the contours of the low resistivity areas close, leaving the appearance of disconnected plumes or open contours at boundaries are not met with a continuance of the low resistivity plume into the adjacent subdomain. The model results of the single large domain show a continuous monolithic plume within the central and western portion of the site, directly beneath the elongated trenches. It is recommended that where possible, the domain not be subdivided, but instead include as much of the domain as possible given the memory of available computing resources.
机译:在华盛顿东部的一个核废料场进行的非常大的电阻率调查中完成了三维(3D)建模研究。采集的数据包括沿着850 m×570 m区域的平行线和正交线收集的47个极-极二维(2D)电阻率曲线。使用EarthImager3D(EI3D)对数据进行地理参考和反转。 EI3D在Microsoft 32位操作系统(例如WIN-2K,XP)上运行,最大可用内存为2 GB。存储器根据测量电极密度将反演模型的域大小限制为200 m×200 m。因此,运行了一系列不断增加的重叠模型来评估将调查区域划分为较小子域的有效性。使用升级的EI3D形式将较小子域的结果与较大区域中单个域的反演结果进行比较,该版本具有多种处理功能和32 GB RAM内存。较小子域的轮廓在相邻模型之间的边界处显示出不连续性,鉴于现场处置的性质,这与水文地质预期不符。在几个边界处,低电阻率区域的轮廓是封闭的,在边界处不连续的羽状流或开放轮廓的出现无法满足低电阻率羽状体进入相邻子域的连续性。单个大区域的模型结果显示,在站点的中部和西部部分,在细长沟槽的正下方,是连续的整体羽状流。建议在可能的情况下,不要对域进行细分,而是在给定可用计算资源内存的情况下,尽可能多地包含该域。

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