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A universal hydro-mechanical coupled behavior model for clay-bearing strata-Molecular-level simulation approach
Muhammad Abdul Waheed1, Omar S Baghabra Al-Amoudi1,2, Mohammed A Al-Osta1,2
1Department of Civil and Environmental Engineering, King Fahd University of Petroleum and Minerals (KFUPM), 31261, Dhahran, Saudi Arabia.
This study developed a universal hydro-mechanical model for clay-bearing strata, enhancing predictions for geotechnical and geoenvironmental applications. The model accurately captures complex swelling-mechanical responses using molecular simulations.
Area of Science:
- Geotechnical Engineering
- Environmental Science
- Materials Science
Background:
- Clay minerals exhibit significant volume changes with water, complicating strata behavior under stress.
- Accurate prediction of hydro-mechanical responses in clay-bearing strata is crucial for engineering and environmental applications.
Purpose of the Study:
- To formulate a comprehensive hydro-mechanical behavior model for clay-bearing strata.
- To overcome limitations of existing models by incorporating detailed structural and fabric information.
Main Methods:
- Utilized Molecular Mechanics and Molecular Dynamics simulations on natural clay-bearing strata structures.
- Employed Monte Carlo techniques for structure formulation and molecular-level parameter acquisition.
- Developed a mathematical model based on simulation results to predict hydro-mechanical behavior.
Main Results:
- The model predicts hydro-mechanical behavior across diverse conditions, including various mineral compositions, salt content, pressures, and strains.
- Validated through laboratory and field tests, covering elastic and elasto-plastic regions.
- Successfully validated against existing data for swelling clays like MX-80 and FEBEX Bentonite.
Conclusions:
- The developed model demonstrates a universal applicability for predicting the hydro-mechanical behavior of clay-bearing strata.
- Enhances the reliability of engineering and geoenvironmental assessments involving clays.
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