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Published on: April 7, 2017
Measuring the permeability of open-framework gravel.
James T Ferreira1, Robert W Ritzi, David F Dominic
1Department of Earth and Environmental Sciences, Wright State University, Dayton, OH 45435, USA.
Measuring high permeability in open-framework gravel is challenging. This study used a 3 m permeameter to accurately quantify permeability (k) values ranging from 4000 to 100,000 Darcies, overcoming laboratory limitations.
Area of Science:
- Geosciences
- Environmental Science
- Hydrology
Background:
- Conventional laboratory permeameters struggle to measure high permeability (k) in materials like open-framework gravel due to insufficient head differences.
- The high k values exceed the measurement range of standard constant-head permeameters, limiting accurate characterization.
Purpose of the Study:
- To develop and validate a method for accurately measuring high permeability in open-framework gravel.
- To extend the measurement capabilities of laboratory permeameters for challenging geological materials.
Main Methods:
- Utilized a 3-meter-long permeameter to create a measurable head difference (10^-2 to 10^-3 m) for high-permeability samples.
- Collected flow data across a range from linear, laminar flow to nonlinear, laminar flow to ensure measurements were within the Darcian regime.
- Precisely measured head differences to the nearest 10^-5 m.
Main Results:
- Successfully measured permeability values for open-framework gravel ranging from 4000 to 100,000 Darcies.
- Verified that the measured k values were obtained within the Darcian flow regime, ensuring data reliability.
- Demonstrated the effectiveness of the extended-length permeameter for high-k materials.
Conclusions:
- A 3 m permeameter is effective for measuring high permeability in open-framework gravel, overcoming limitations of conventional equipment.
- The developed method provides accurate and reliable permeability data for sediments with k values up to 100,000 Darcies.
- This research advances the accurate characterization of porous media with exceptionally high hydraulic conductivity.
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