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A Test Case For The Simulation Of Three-dimensional Variable-density Flow And Solute Transport In Discretely-fractured Porous Media

机译:离散压裂多孔介质中三维变密度流和溶质运移模拟的测试案例

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摘要

A test case has been developed for three-dimensional simulations of variable-density flow and solute transport in discretely-fractured porous media. The simulation domain is a low-permeability porous matrix cube containing a single non-planar fracture. The initial solute concentration is zero everywhere. A constant solute concentration is assigned to the top of the domain, which increases near-top fluid density and induces downward density-driven flow. The test case is therefore comparable to downwelling of a dense brine below a saline disposal basin or a waste repository. Numerous fingers and distinct convection cells develop early in the fracture but the fingers later coalesce and convection becomes less apparent. To help test other variable-density flow and transport models, results of the test case are presented both qualitatively (concentration contours and velocity fields) and quantitatively (penetration depth, mass flux, total mass stored, maximum fracture and matrix velocity).
机译:已经开发了一个测试案例,用于在离散断裂的多孔介质中进行可变密度流动和溶质运移的三维模拟。模拟域是包含单个非平面裂缝的低渗透多孔基质立方体。初始溶质浓度在任何地方都为零。恒定的溶质浓度分配给畴的顶部,这会增加近顶部的流体密度并引起向下的密度驱动流。因此,该测试案例可媲美浓盐水在盐水处理池或废物处置库下方的下流。骨折早期会形成许多手指和明显的对流细胞,但手指后来合并,对流变得不太明显。为了帮助测试其他可变密度的流量和传输模型,定性(浓度轮廓和速度场)和定量(渗透深度,质量通量,存储的总质量,最大裂缝和基体速度)都给出了测试案例的结果。

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