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Published on: May 20, 2018
A novel numerical simulation framework for predicting pore space evolution and rock properties through sedimentation,
Bowen Ling1,2, Xingming Du1, Shuheng Du1
1Institute of Mechanics, Chinese Academy of Sciences, Beijing, 100190, China.
This study introduces a numerical simulation framework to predict rock pore space evolution during diagenesis. The model integrates mineral grain generation, deposition, compaction, and geochemical reactions, offering insights into porosity and permeability changes.
Area of Science:
- Geology
- Geochemistry
- Computational Science
Background:
- Pore space evolution significantly impacts rock physical properties, driven by diagenetic processes.
- Current research lacks predictive models for how sedimentary heterogeneity affects diagenesis and pore space evolution.
Purpose of the Study:
- To develop and demonstrate a numerical simulation framework for predicting pore-space evolution.
- To integrate mineral grain generation, deposition, compaction, fluid flow, solute transport, dissolution, and cementation.
Main Methods:
- Utilized Quartet Structure Generation Set (QSGS) for 3D mineral grain generation.
- Employed Discrete Element Method (DEM) for deposition and compaction.
- Applied Finite Volume Method (FVM) for fluid flow, geochemical reactions, and physical property computation.
Main Results:
- Simulation results for porosity-depth trends and cementation align with analytical models.
- Demonstrated framework capabilities through case studies of quartz and multi-mineral systems.
- Validated the dynamic prediction of pore-space evolution, porosity, and permeability.
Conclusions:
- The developed numerical framework is robust for dynamic prediction of rock physical properties.
- This approach offers significant potential for understanding diagenetic impacts on reservoir quality.
- Highlights the importance of integrated modeling for sedimentary basin analysis.
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