Capillary pressure – saturation relationships for gas shales measured using a water activity meter

B. Donnelly, E. Perfect, L. D. McKay, P. J. Lemiszki, V. H. DiStefano, L. M. Anovitz, J. McFarlane, R. E. Hale, C. L. Cheng

Research output: Contribution to journalArticlepeer-review

24 Scopus citations

Abstract

Hydraulic fracturing of gas shale formations involves pumping a large volume of fracking fluid into a hydrocarbon reservoir to fracture the rock and thus increase its permeability. The majority of the fracking fluid introduced is never recovered and the fate of this lost fluid, often called “leak off,” has become the source of much debate. Information on the capillary pressure – saturation relationship for each wetting phase is needed to simulate leak off using numerical reservoir models. The petroleum industry commonly employs air – water capillary pressure – saturation curves to predict these relationships for mixed wet reservoirs. Traditional methods of measuring this curve are unsuitable for gas shales due to high capillary pressures associated with the small pores present. A possible alternative method is the water activity meter which is used widely in the soil sciences for such measurements. However, its application to lithified material has been limited. This study utilized a water activity meter to measure air – water capillary pressures (ranging from 1.3 to 219.6 MPa) at several water saturation levels in both the wetting and drying directions. Water contents were measured gravimetrically. Seven types of gas producing shale with different porosities (2.5–13.6%) and total organic carbon contents (0.4–13.5%) were investigated. Nonlinear regression was used to fit the resulting capillary pressure – water saturation data pairs for each shale type to the Brooks and Corey equation. Data for six of the seven shale types investigated were successfully fitted (median R2 = 0.93), indicating this may be a viable method for parameterizing capillary pressure – saturation relationships for inclusion in numerical reservoir models. As expected, the different shale types had statistically different Brooks and Corey parameters. However, there were no significant differences between the Brooks and Corey parameters for the wetting and drying measurements, suggesting that hysteresis may not need to be taken into account in leak off simulations.

Original languageEnglish
Pages (from-to)1342-1352
Number of pages11
JournalJournal of Natural Gas Science and Engineering
Volume33
DOIs
StatePublished - Jul 1 2016

Funding

The authors wish to thank Consol Energy Inc. (Pittsburgh, PA) for providing the Chattanooga and Marcellus shale samples. E. Perfect acknowledges funding from David E. Jackson of BDY Environmental LLC , Nashville, TN through a Faculty Achievement Award. Work by V.H. DiStefano and L.M. Anovitz was supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, Chemical Sciences, Geosciences, and Biosciences Division.

FundersFunder number
U.S. Department of Energy
Office of Science
Basic Energy Sciences
Chemical Sciences, Geosciences, and Biosciences Division

    Keywords

    • Brooks and Corey
    • Capillary pressure
    • Porosity
    • Shale
    • Volumetric water content
    • Water activity meter

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