首页> 外文期刊>Journal of Contaminant Hydrology >Flow and transport in unsaturated fractured rock: effects of multiscale heterogeneity of hydrogeologic properties
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Flow and transport in unsaturated fractured rock: effects of multiscale heterogeneity of hydrogeologic properties

机译:非饱和裂隙岩中的流动与输运:水文地质特性的多尺度非均质性影响

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摘要

The heterogeneity of hydrogeologic properties at different scales may have different effects on flow and transport processes in a subsurface system. A model for the unsaturated zone of Yucca Mountain, Nevada, is developed to represent complex heterogeneity at two different scales: (1) layer scale corresponding to geologic layering and (2) local scale. The layer-scale hydrogeologic properties are obtained using inverse modeling, based on the available measurements collected from the Yucca Mountain site. Calibration results show a significant lateral and vertical variability in matrix and fracture properties. Hydrogeologic property distributions in a two-dimensional, vertical cross-section of the site are generated by combining the average layer-scale matrix and fracture properties with local-scale perturbations generated using a stochastic simulation method. The unsaturated water flow and conservative (nonsorbing) tracer transport through the cross-section are simulated for different sets of matrix and fracture property fields. Comparison of simulation results indicates that the local-scale heterogeneity of matrix and fracture properties has a considerable effect on unsaturated flow processes, leading to fast flow paths in fractures and the matrix. These paths shorten the travel time of a conservative tracer from the source (repository) horizon in the unsaturated zone to the water table for small fractions of total released tracer mass. As a result, the local-scale heterogeneity also has a noticeable effect on global tracer transport processes, characterized by an average breakthrough curve at the water table, especially at the early arrival time of tracer mass. However, the effect is not significant at the later time after 20% tracer mass reaches the water table. The simulation results also verify that matrix diffusion plays an important role in overall solute transport processes in the unsaturated zone at Yucca Mountain.
机译:不同规模的水文地质性质的非均质性可能对地下系统的流动和运输过程产生不同的影响。建立了内华达州尤卡山非饱和带的模型,以两种不同的尺度表示复杂的非均质性:(1)对应于地质分层的层尺度和(2)局部尺度。基于从尤卡山遗址收集的可用测量值,使用反演模型获得层级水文地质特性。校准结果表明,基体和断裂特性存在明显的横向和垂直变化。通过将平均层尺度矩阵和裂缝特性与使用随机模拟方法生成的局部尺度扰动相结合,可以在站点的二维垂直横截面中生成水文地质特性分布。针对不同组的基质和裂缝特性场,模拟了横断面的非饱和水流和保守(非吸附)示踪剂传输。模拟结果的比较表明,基体的局部尺度非均质性和裂缝特性对非饱和流动过程具有相当大的影响,从而导致裂缝和基体中的快速流动路径。这些路径缩短了保守示踪剂从不饱和区的源(储层)层位到地下水位的行进时间,这仅占示踪剂总释放量的一小部分。结果,局部尺度的异质性也对全球示踪剂的运输过程产生了显着影响,其特征是在地下水位,特别是在示踪剂团块的早期到达时,平均冲刺曲线。但是,在20%的示踪剂质量达到地下水位之后,以后的效果并不明显。仿真结果还证明了基质扩散在尤卡山非饱和带的整体溶质运移过程中起着重要作用。

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