Multi-Regional Reactive Transport Due to Strong Anisotropy in Unsaturated Soils with Evolving Scales of Heterogeneity

Moo-Young, Horace K.

Lehigh University, Bethlehem, PA (United States)

关键词: Diffusion;    Anisotropy;    58 Geosciences;    Soils;    54 Environmental Sciences;   

DOI  :  10.2172/838365
RP-ID  :  EMSP-86952--2003
RP-ID  :  FG07-02ER63512
RP-ID  :  838365

美国|英语

来源: UNT Digital Library

【 摘 要 】

Current conceptualizations of state-dependent anisotropy have failed to describe field observations, and the importance of multi-region flow in strongly anisotropic soils appears to be unrecognized. It is hypothesized that under the typical conditions of arid waste sites, when strong heterogeneity is predicted, the first order small anisotropy analysis is not rigorously applicable, and non-equilibrium mass transfer governs transport. Inter-region mass transfer is dominated by local velocity variations rather than diffusion, and access to reactive sites becomes limited. Accurate representation therefore requires an analysis to transport over evolving scales of heterogeneity and complexities to account for the interacting physical and chemical processes governing sorption in anisotropic media. In order to address these issues an integrated laboratory, field-modeling study with the following objectives is proposed. (1) Determine the scale of applicability and the limitations of th e small perturbation (stochastic) approach for predicting flow and transport at arid sites with strong heterogeneity. (2) Develop an appropriately rigorous averaging approach to better quantify local scale behavior in anisotropic soils. (3) Investigate precisely a range of macroscopic flow regimes, measure accurately their three-dimensional average properties, and develop a multi-region transfer method to bridge the gap between pore-scale fluid migration and macro-scale displacement behavior under strong anisotropy. To accomplish the stated goals and objectives, the project is investigating transport processes over evolving scales of heterogeneity and complexities using three essential components of subsurface science identified here as three unique tasks. Task 1--Controlled Laboratory Studies. Task 2--Controlled Field Experiments. Task 3--Numerical Simulations Task 1 has been divided into two activities: (1) an investigation of pore-scale processes and (2) an investigation of intermediate-scale processes. Researchers at Lehigh University are focusing on part 2 of Task 1 that involves the use of a research centrifuge.