2020
DOI: 10.5194/adgeo-54-195-2020
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Wettability of organic-rich source rocks: case study on Bazhenov Formation (Abalak-Bazhenov group)

Abstract: Abstract. In this work, we have investigated the wettability of Bazhenov Formation rock samples using a nuclear magnetic resonance (NMR), the methods of vapor adsorption, and wetting contact angle. We have conducted the petrographic description of rocks using ultra-thin sections and scanning electron microscopy (SEM). In addition, we used data on the organic content (TOC) obtained by the Rock-Eval method and the results of lithological typing on thin sections for detailed analysis of NMR and contact angle meth… Show more

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Cited by 5 publications
(3 citation statements)
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“…Two major oil-prone formations located within The Russian Federation are the of Bazhenov and Domanic Formations. Both formations are characterized by very low values of porosity, permeability and complex structure of void space [1][2][3].…”
Section: Introductionmentioning
confidence: 99%
“…Two major oil-prone formations located within The Russian Federation are the of Bazhenov and Domanic Formations. Both formations are characterized by very low values of porosity, permeability and complex structure of void space [1][2][3].…”
Section: Introductionmentioning
confidence: 99%
“…Rock microstructure and lithology were characterized through petrographical thin-section (30 μm) analysis with a ZEISS Axioscope 5 polarizing microscope. High-resolution two-dimensional (2D) microstructural visualization of the rock sample surface was done with a Thermo Fisher Scientific Quattro S scanning electron microscope (SEM). SEM images were done before aging, after aging in oil, and after treatment with surfactants to show the qualitative changes in wettability and explain the wettability alteration mechanism …”
Section: Methodsmentioning
confidence: 99%
“…According to our results, L-3 is characterized by a strong dominance of thin laminas and lenticular inclusions of kerogen (Figure 3C,G), whereas other lithological types host tiny dispersed or patchy organic matter, with a minor role of lenticular inclusions (Figure 3). Variations of organic matter shape cause differences in petrophysical properties of rocks, such as mechanical anisotropy, wettability [37], and many others. Different structure and distribution patterns are determined by organic matter type and origin, which is further investigated in the paper.…”
mentioning
confidence: 99%