1 Conventional and Unconventional Reservoir Rocks: Advances in Experiments, Modeling, and Simulations

Monday, 25 March 2019
8:00 AM - 12:00 PM
Konza Prairie Room

NUMERICAL SIMULATION OF OVERPRESSURE DURING SEDIMENTATION

Paper number: 1-11
Program: Theme Sessions
Time: 11:20 AM – 11:40 AM

Authors

  • Wenyu Zhao Presenting Author
    Missouri University of Science and Technology, Rolla, MO

Abstract

The evolution of pore pressure including overpressure during sedimentation is an important process to consider when analyzing whether high pore pressure causes rock failure. High pore pressure is caused by under-compaction due to the rapid burial of low-permeability sediments, and as a result, porosity decreases less rapidly with depth compared to normally compacted sediments where porosity decreases exponentially with depth. While under-compaction related pore pressure magnitudes have been determined empirically, in most numerical modeling approaches, the pore pressure is either applied as a static magnitude or coupled to a fluid flow simulator. This study simulates the pore pressure evolution during sediment loading and compaction using 3D porous-elastic-plastic finite element analysis. Continuous sedimentary loading is applied and the resulting compaction process is coupled to the evolution of Poisson’s ratio, bulk modulus, and permeability. Sensitivity analyses with respect to permeability and elasticity for various sedimentation rates and initial physical properties distributions are conducted. Initial results show that overpressure occurs in rock layers with a permeability lower than 10-12 m2 when the sedimentation rate is equal to or exceeds 10 mm/year. Pore space is easier to be compacted in rocks featuring a lower bulk modulus under the same effective stress. The coupled approach is applied to the mini-basin field in Gulf of Mexico and the results are in good agreement with reported porosity and pore pressure magnitudes. The presented procedure enables to couple the simulation of the effective state of stress both due to the initial burial history of a sedimentary basin as well as to subsequent deformation events and therefore provides a better assessment for rock failure analysis.

Geological Society of America Abstracts with Programs. Vol. 51, No. 2

doi: 10.1130/abs/2019SC-325816

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