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首页> 外文期刊>Journal of Hydrology >Solute transport in solution conduits exhibiting multi-peaked breakthrough curves
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Solute transport in solution conduits exhibiting multi-peaked breakthrough curves

机译:溶液导管中的溶质迁移表现出多峰穿透曲线

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Solute transport in karst aquifers is primarily constrained to solution conduits where transport is rapid, turbulent, and relatively unrestrictive. Breakthrough curves generated from tracer tests are typically positively-skewed and may exhibit multiple peaks. In order to understand the circumstances under which multi-peaked positively skewed breakthrough curves occur, physical experiments utilizing single- and multiple-flow channels were conducted. Experiments also included waterfalls, short-term solute detention in pools, and flow obstructions. Results demonstrated that breakthrough curve skewness nearly always occurs to some degree but is magnified as immobile-flow regions are encountered. Multi-peaked breakthrough curves occurred when flow in the main channel became partially occluded from blockage in the main channel that forced divergence of solute into auxiliary channels and when waterfalls and detention in pools occurred. Currently, multi-peaked breakthrough curves are fitted by a multi-dispersion model in which a series of curves generated by the advection-dispersion equation are fitted to each measured peak by superimposing the measured breakthrough curve to obtain a combined model fit with a consequent set of estimated velocities and dispersions. In this paper, a dual-advection dispersion equation with first-order mass transfer between conduits was derived. The dual-advection dispersion equation was then applied to the multi-peaked breakthrough curves obtained from the physical experiments in order to obtain some insight into the operative solute-transport processes through the acquisition of a consequent set of velocities, dispersions, and related parameters. Successful application of the dual-advection, dispersion equation to a tracer test that exhibited dual peaks for a karst aquifer known to consist of two connected but mostly separate conduits confirmed the appropriateness of using a multi-dispersion type model when conditions warrant.
机译:岩溶含水层中的溶质运移主要受运移到溶液管道的约束,在该管道中,运移迅速,湍流且相对不受限制。示踪剂测试生成的穿透曲线通常呈正偏,并且可能会出现多个峰。为了了解在什么情况下会出现多峰正偏的突破曲线,我们进行了利用单流道和多流道的物理实验。实验还包括瀑布,池中短期溶质滞留和水流阻塞。结果表明,突破曲线偏斜几乎总是在某种程度上发生,但随着遇到固定流动区域而放大。当主通道中的流动部分被主通道中的堵塞物阻塞而导致溶质扩散到辅助通道中时,以及在水池中发生瀑布和滞留时,会出现多峰穿透曲线。当前,通过多分散模型拟合多峰穿透曲线,其中通过将测量的穿透曲线叠加以获得每个组合的拟合模型,从而将由对流扩散方程生成的一系列曲线拟合到每个测得的峰。估计的速度和色散。本文推导了管道之间具有一阶质量传递的对流对流扩散方程。然后,将对流弥散方程应用于从物理实验获得的多峰突破曲线,以便通过获取速度,弥散度和相关参数的集合来深入了解溶质的有效运移过程。成功地将双对流弥散方程应用于示踪剂测试,该示踪剂试验显示出一个已知由两个相连但大多为分开的导管组成的岩溶含水层的双峰,这证实了在条件允许时使用多分散类型模型的适当性。

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