2016
DOI: 10.1016/j.jngse.2016.06.014
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A microscopic characterization of wettability in shale kerogen with varying maturity levels

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Cited by 97 publications
(81 citation statements)
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“…Mechanistically, shale pore networks comprise of (a) inorganic porosity (clay and nonclay minerals) and (b) organic matter porosity where the organic pores are hydrophobic while the inorganic pores are hydrophilic [ Curtis et al ., ]. Thus, the composite wetting behavior of shale is controlled by the distribution and connectivity of organic and inorganic matter [ Hu et al ., ]. Consequently, the CO 2 ‐wet nature of high‐TOC samples (shales C and D) indicates that organic matter dominates the composite wetting behavior, while the water‐wet behavior of low TOC shale indicates mineral dominance in pore spaces.…”
Section: Resultsmentioning
confidence: 99%
“…Mechanistically, shale pore networks comprise of (a) inorganic porosity (clay and nonclay minerals) and (b) organic matter porosity where the organic pores are hydrophobic while the inorganic pores are hydrophilic [ Curtis et al ., ]. Thus, the composite wetting behavior of shale is controlled by the distribution and connectivity of organic and inorganic matter [ Hu et al ., ]. Consequently, the CO 2 ‐wet nature of high‐TOC samples (shales C and D) indicates that organic matter dominates the composite wetting behavior, while the water‐wet behavior of low TOC shale indicates mineral dominance in pore spaces.…”
Section: Resultsmentioning
confidence: 99%
“…Some experts believe that the fracturing fluid is imbition into the complex fracture network area, and the mechanisms of oil recovery after hydraulic fracturing are imbibition [9]. The evaluation of fracturing fluid effect and the theoretical model of imbibition have gradually become a research focus [10][11][12][13][14][15][16][17][18][19]. Meng et al [5] explained that the rock fracture pressure is high during hydraulic fracturing, the fracture stress after fracturing is obviously higher than the matrix pressure.…”
Section: Introductionmentioning
confidence: 99%
“…Kerogen is classified by its chemical composition, and the C/O ratio 34−36 is one of the parameters frequently used to quantify the degree of maturity. 37 Different kerogen models have been proposed, 38,39 considering the C/O ratio varying from 0.03 to 0.2, depending on the specific kerogen. Within these models, oxygens mainly belong to carboxylic (−COOH) and carbonyl (>CO) groups.…”
Section: Introductionmentioning
confidence: 99%
“…On the other hand, there are several molecular models for kerogen’s microporosity available in the literature. , However, nanoscale models of these materials are not fully developed. Kerogen is classified by its chemical composition, and the C/O ratio is one of the parameters frequently used to quantify the degree of maturity . Different kerogen models have been proposed, , considering the C/O ratio varying from 0.03 to 0.2, depending on the specific kerogen.…”
Section: Introductionmentioning
confidence: 99%