2021
DOI: 10.1016/j.petrol.2020.107673
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CO2/brine interfacial tension and rock wettability at reservoir conditions: A critical review of previous studies and case study of black shale from Malaysian formation

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Cited by 88 publications
(47 citation statements)
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“…Interfacial tension measurements were conducted using a view chamber drop shape analyzer (model: DSA-100, Kruss). The pendant drop method 34 was followed to evaluate CH 4 /aqueous solution IFT. The required pressure and temperature at the view chamber were first attained.…”
Section: Shale Samplementioning
confidence: 99%
“…Interfacial tension measurements were conducted using a view chamber drop shape analyzer (model: DSA-100, Kruss). The pendant drop method 34 was followed to evaluate CH 4 /aqueous solution IFT. The required pressure and temperature at the view chamber were first attained.…”
Section: Shale Samplementioning
confidence: 99%
“…Thus, it is clear that a precise evaluation of shale wettability is extremely important for successful hydrocarbon exploitation from shale reservoirs. Currently, the contact angle method is frequently used to measure shale wettability under different operating conditions, , while spontaneous imbibition has also been extensively studied recently, and some NMR investigations have been conducted. , However, only a few studies have used molecular dynamics simulations to examine shale wettability. , One key factor that limits the understanding of shale rocks is their complex microstructure, , including organic matter, minerals, and microfractures. ,, Consequently, a precise shale wettability characterization may not be possible without a detailed understanding of the associated shale microstructure. Furthermore, no single imaging technique is capable to capture the shale rock microstructure fully and accurately, rather a multiscale correlative imaging approach is required. ,, …”
Section: Introductionmentioning
confidence: 99%
“…The current literature suggests that shale rocks demonstrate a mixed-wet behavior where the inorganic mineral matter is hydrophilic, while the organic matter is hydrophobic, and this hydrophobicity increases with shale total organic carbon (TOC). , However, there are other observations too where shales were found to be water-wet, and the associated wetting behavior was not influenced by shale TOC, thus suggesting a complex wetting behvaior of shales. On the contrary, the wettability of conventional geomaterials, for example, sandstones, and pure minerals are relatively better understood and evaluated. For instance, a wide body of literature agrees that pure clean quartz surfaces are strongly water-wet, while pure calcite is relatively less water-wet (at ambient conditions), and the water-wetness is typically reduced at elevated CO 2 injection pressures. , …”
Section: Introductionmentioning
confidence: 99%
“…Data were collected over a 2θ range of 2-90° at a scan rate of 0.02°/2 s. TOC was determined using the TOC device (Multi N/C 3100 Analytic Jena, Germany). BET surface was measured using surface area instrument (Tristar II Series, Micromeritics, USA), with N2 as the adsorbate gas at 77 K [19][20][21][22][23][24].…”
Section: Methodsmentioning
confidence: 99%