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On the solute transport in an aquifer-aquitard system

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.

Identiferoai:union.ndltd.org:tamu.edu/oai:repository.tamu.edu:1969.1/ETD-TAMU-1319
Date15 May 2009
CreatorsBian, Aiguo
ContributorsZhan, Hongbin
Source SetsTexas A and M University
Languageen_US
Detected LanguageEnglish
TypeBook, Thesis, Electronic Dissertation, text
Formatelectronic, application/pdf, born digital

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