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Effective dispersion in temporally fluctuating flow through a heterogeneous medium
1Department of Geotechnical Engineering and Geosciences, Technical University of Catalonia (UPC), Barcelona, Spain. marco.dentz@upc.es
Summary
This study examines solute transport in fluctuating groundwater flow through heterogeneous media. Temporal flow variations enhance solute spreading, impacting dispersion coefficients and supporting remediation strategies.
Area of Science:
- Environmental science
- Hydrogeology
- Fluid dynamics
Background:
- Understanding solute transport in heterogeneous porous media is crucial for environmental remediation.
- Spatially heterogeneous media and temporally fluctuating flow conditions are common in groundwater systems.
- Existing theories often simplify flow to steady-state conditions, potentially missing key transport dynamics.
Purpose of the Study:
- To investigate the effective transport of passive solutes in temporally fluctuating flow within spatially heterogeneous media.
- To analyze the impact of temporal boundary condition fluctuations on solute dispersion.
- To develop a theoretical framework for predicting solute dispersion under complex flow conditions.
Main Methods:
- Solving the Darcy equation for incompressible fluid flow using perturbation theory.
- Distinguishing between spatial (medium heterogeneity) and temporal (boundary condition fluctuation) random processes.
- Evaluating second-order perturbation approximations for effective and ensemble dispersion coefficients.
Main Results:
- Derived dispersion coefficients include terms for local dispersion, spatial heterogeneity, and interactions between temporal fluctuations and heterogeneity.
- Temporal velocity fluctuations lead to time-evolving transverse dispersion coefficients reaching macroscopic values.
- Results are valid for moderately fluctuating fields but show wide applicability via simulations.
Conclusions:
- Temporal flow fluctuations significantly influence solute dispersion, leading to enhanced spreading.
- The findings reconcile theoretical predictions with field observations of solute transport.
- Supports remediation strategies involving temporal variations in injection/pumping rates for improved groundwater mixing.