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On the solute transport in an aquifer-aquitard system.

机译:关于溶质在含水层-阿奎塔尔体系中的传输。

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摘要

This dissertation is composed of five chapters and three major contributions are presented in Chapter II, III and IV.; Chapter I provided a review of studies on solute transport in aquifer-aquitard system. If the aquitard is considered, two categories of methods address the diffusive flux between the aquifer and aquitard: the old method treats the diffusive flux as a volumetric source in the governing equation of the solute transport in the aquifer; the new method treats the aquifer-aquitard boundary as a strict physical boundary with the requirement of continuity of solute concentration and the vertical flux. The new method is adopted throughout this study.; In Chapter II, a review of numerical techniques on Inverse Laplace Transform is provided. By careful comparison between several popular algorithms, the multiple precision Stehfest algorithm is chosen as the method to inverse out solutions on solute transport in Laplace domain throughout this dissertation.; In Chapter III, solutions were obtained for two dimensional solute transport in an aquifer-aquitard system with a divergent radial flow field, which can treat different types of solute input function and advection, longitudinal and transverse dispersion in the aquifer, vertical diffusion in the aquitard, retardation and radioactive decay in the aquifer and aquitard are taken into account. Mass exchange via diffusion between the aquifer and aquitard are investigated. The effects of hydrologic properties of the aquitard on solute transport are analyzed. Comparisons were made between the results from this study and those from previous studies. The diffusion along the aquifer-aquitard boundary was treated as a volumetric source term, and proved these solutions yield more accurate solute concentration, while those from previous studies tend to overestimate solute concentration in the aquitard, and underestimate the concentration in the aquifer.; In Chapter IV, solutions were derived for the transport of radioactive isotopes in an aquifer-aquitard system with regional flow field. This study focused on the effects of different solute transport processes on the results of groundwater age dating using radiometric techniques.; Chapter V summarized the remaining problems in this study and directions for future researches.
机译:本论文共分五章,第二,三,四章分别提出了三个主要贡献。第一章回顾了含水层-阿奎塔尔体系中溶质运移的研究。如果考虑到水族箱,则有两种方法可以解决含水层和水族箱之间的扩散通量:旧方法将扩散通量视为含水层中溶质运移控制方程式中的体积源。新方法将含水层-阿奎塔尔边界视为严格的物理边界,要求溶质浓度和垂直通量具有连续性。在整个研究过程中采用了新方法。在第二章中,对拉普拉斯逆变换的数值技术进行了回顾。通过对几种常用算法的仔细比较,本文选择多精度Stehfest算法作为反推拉普拉斯域溶质运移解的方法。在第三章中,获得了在具有径向流场发散的含水层-阿奎塔尔系统中二维溶质运移的解决方案,该系统可以处理不同类型的溶质输入函数和对流,含水层中的纵向和横向扩散,在含水层中的垂直扩散。 ,考虑了含水层和阿基塔尔的阻滞和放射性衰变。研究了通过含水层和脱水层之间的扩散进行的质量交换。分析了水母的水文性质对溶质运移的影响。本研究结果与先前研究结果进行了比较。沿含水层-含水层边界的扩散被视为体积源项,并证明这些溶液产生更准确的溶质浓度,而先前研究的那些倾向于高估含水层中的溶质浓度,而低估了含水层中的浓度。在第四章中,导出了在具有局部流场的含水层-阿奎塔尔系统中放射性同位素的运输解决方案。这项研究的重点是采用放射技术对不同溶质运移过程对地下水年龄测年结果的影响。第五章总结了本研究尚存在的问题和今后的研究方向。

著录项

  • 作者

    Bian, Aiguo.;

  • 作者单位

    Texas A&M University.;

  • 授予单位 Texas A&M University.;
  • 学科 Geology.; Hydrology.
  • 学位 Ph.D.
  • 年度 2007
  • 页码 100 p.
  • 总页数 100
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;水文科学(水界物理学);
  • 关键词

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