Title

Effect of inorganic acid concentration on sandstone surface chemistry examined via nuclear magnetic resonance

Document Type

Journal Article

Publication Title

Journal of Physical Chemistry C

Volume

126

Issue

26

First Page

10863

Last Page

10871

Publisher

ACS

School

Centre for Sustainable Energy and Resources

RAS ID

51951

Comments

Karunarathne, C. I., Al-Yaseri, A. Z., Keshavarz, A., & Iglauer, S. (2022). Effect of inorganic acid concentration on sandstone surface chemistry examined via nuclear magnetic resonance. The Journal of Physical Chemistry C, 126(26), 10863-10871. https://doi.org/10.1021/acs.jpcc.2c01706

Abstract

Despite rock surface charge being a critical component in predicting the reservoir behavior, the subsurface characteristics are still poorly understood, specially, those of sandstones, which are of key economic importance in the oil and gas industry. Even though a rock surface is originally considered to be neutrally charged, surface charges are created in the presence of water and dissolved ions. Moreover, a major proportion of sandstone reservoirs are composed of silica which creates surface charges through dissociation of silanols in the presence of water and/or acids. Rock subsurface chemistry is a primary factor that determines the variability of several key reservoir parameters (e.g., capillary pressures or residual saturations). Nuclear magnetic resonance (NMR) is a well-established tool with which such rock surface chemistry can be measured in situ. For example, surface charge is a vital characteristic with which single-phase and multiphase fluid flow behavior can be predicted (e.g., it determines colloidal stabilities or streaming potentials); the surface charge/surface potential is thus highly significant for a wide range of applications and processes, for example, enhanced oil/gas recovery, hydrogen/CO2geo-storage, or contaminant transport. This study provides novel insights into fundamental rock surface chemistry and how this is influenced by the acidity of the aqueous phase in the subsurface. Specifically, we systematically examined sandstone surface chemistry as a function of mineral acid concentration via NMR T2response measurements. For this, Bentheimer sandstone samples were treated with aqueous hydrochloric acid solutions of different concentrations, and NMR T2distribution measurements were performed for the initial and treated samples. The results indicated that higher concentrations of hydrochloric acid (and thus more surface protonation) yielded much shorter T2relaxation times compared to lower concentrations. This work thus provides fundamental information about in situ sandstone surface chemistry and therefore aids in the basic understanding and implementation of key geologic questions and engineering projects.

DOI

10.1021/acs.jpcc.2c01706

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