T152 Energy and Mineral Resources of the Illinois Basin I
Tuesday, 6 November 2018
8:00 AM - 12:00 PM
Room 145
INTEGRATED RESERVOIR CHARACTERIZATION FOR CHEMICAL ENHANCED OIL RECOVERY, TAR SPRINGS FORMATION, ILLINOIS BASIN, U.S.A
Paper number: T152-7
Program: Technical Sessions
Time: 9:25 AM – 9:40 AM
Authors
-
Jack W. FeketePurdue University, West Lafayette, IN
-
Kenneth RidgwayPurdue University, West Lafayette, IN
-
Cliff T. JohnstonPurdue University, West Lafayette, IN
-
Nathan C. SchultheissPurdue University, West Lafayette, IN
-
Bryan ClaytonPioneer Oil Company, Inc., Vincennes, IN
Abstract
Results show the pilot study reservoir is compartmentalized by five lithofacies each characterized by distinct properties: F1 – fine grained horizontally stratified sandstone; F2 – very fine to fine grained flaser bedded sandstone; F3 – wavy bedded sandstone with very fine grained sandstone and mudstone interlayers; F4 – lenticular bedded silty mudstone; and F5 – calcite cemented sandstone. Petrophysical and geochemical results suggest horizontally stratified and flaser bedded sandstone facies represent the best reservoir injection targets. Together, lithofacies F1 and F2 have higher average porosity and permeability, possess significantly lower clay percentages, and yield the highest residual oil. Wavy bedded, lenticular bedded, and calcite-cemented sandstone facies have the poorest reservoir quality due to enhanced clay content that impairs porosity, permeability, and has led to diminished oil saturations. Clay components are distributed throughout the reservoir in varying proportions based on lithofacies and can influence not only flow parameters but interact with injected chemicals to alter fluid circulation and sweep efficiencies. This integrated approach to reservoir characterization has important implications for providing a framework for decision making concerning the future of other developed reservoirs considered close to abandonment in mature basins.
Geological Society of America Abstracts with Programs. Vol. 50, No. 6
doi: 10.1130/abs/2018AM-324251
© Copyright 2018 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.