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Updated: Jul 11, 2026

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Published on: September 26, 2016
An interpretation of potential scale dependence of the effective matrix diffusion coefficient
1Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California, United States. hhliu@lbl.gov
Scale-dependent matrix diffusion in fractured rock is influenced by local flow loops and fracture geometry. Numerical experiments reveal these factors enhance the effective matrix diffusion coefficient with increasing test scale.
Area of Science:
- Geosciences
- Hydrogeology
- Rock Mechanics
Background:
- Matrix diffusion is crucial for solute transport in fractured rock.
- Previous field tracer tests show enhanced effective matrix diffusion coefficients with increasing scale.
Purpose of the Study:
- Investigate mechanisms behind scale-dependent matrix diffusion.
- Understand the influence of flow path geometry and local flow loops.
Main Methods:
- Numerical experiments simulating solute transport in fractured rock.
- Discrete fracture network flow simulations for water velocity distribution.
- Particle-tracking scheme and impulse-response function for solute transport calculation.
- Matching breakthrough curves to analytical solutions for parameter up-scaling.
Main Results:
- Local flow loops and matrix diffusion contribute to scale dependence.
- Scaling properties of flow path geometry play a significant role.
- Effective matrix diffusion coefficient increases with test scale.
Conclusions:
- A combination of local flow loops, matrix diffusion, and geometric scaling explains observed scale dependence.
- Numerical experiments provide insights into up-scaled transport parameters.
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