2022
DOI: 10.1016/j.fuel.2022.125328
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New methods to evaluate impacts of osmotic pressure and surfactant on fracturing fluid loss and effect of contact angle on spontaneous imbibition data scaling in unconventional reservoirs

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Cited by 17 publications
(22 citation statements)
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“…Further, a more water-wet state leads to more snap off events [44,45], and therefore a more serious H2 loss and a smaller 𝐻 2−𝑊𝐹 . Moreover, during well shut-in, discontinuous H2 bubbles can exert strong resistance for the spontaneous imbibition of in-situ formation brine [46,47] -therefore, if RPH is present, the initial H2 concentration is higher around the wellbore region (which again results in a larger 𝐻 2−𝑊𝑃 at the beginning of each H2 withdrawal cycle). The observed 𝐻 2−𝑊𝐹 and 𝐻 2−𝑊𝑃 response to the withdrawal cycle is because 1) at the end of each H2 injection cycle, more H2 will be in place than the earlier injection cycle; and 2) at the end of each H2 withdrawal cycle, more H2 will be lost to the subsurface than the earlier withdrawal cycle [28].…”
Section: Impact Of Relative Permeability Hysteresis and Wettabilitymentioning
confidence: 99%
“…Further, a more water-wet state leads to more snap off events [44,45], and therefore a more serious H2 loss and a smaller 𝐻 2−𝑊𝐹 . Moreover, during well shut-in, discontinuous H2 bubbles can exert strong resistance for the spontaneous imbibition of in-situ formation brine [46,47] -therefore, if RPH is present, the initial H2 concentration is higher around the wellbore region (which again results in a larger 𝐻 2−𝑊𝑃 at the beginning of each H2 withdrawal cycle). The observed 𝐻 2−𝑊𝐹 and 𝐻 2−𝑊𝑃 response to the withdrawal cycle is because 1) at the end of each H2 injection cycle, more H2 will be in place than the earlier injection cycle; and 2) at the end of each H2 withdrawal cycle, more H2 will be lost to the subsurface than the earlier withdrawal cycle [28].…”
Section: Impact Of Relative Permeability Hysteresis and Wettabilitymentioning
confidence: 99%
“…The water–rock interaction between soluble minerals in the rock and water will affect the SI of water. More specifically, the soluble minerals in the rock are partially dissolved by the reaction with water, which has a certain effect on the SI of water, and the previous studies’ results show that the salinity of water also has a great influence on SI. In addition, clay minerals typically swell to a certain extent when in contact with water, complicating the pore structure of shale (e.g., blocking pores and throats) and sometimes reducing fluid migration rates. , For homogeneous porous media, the greater the tortuosity of the connected pore system, the longer the migration path of solute molecules through the same linear distance in the porous medium and the smaller the imbibition slope . Due to the strong heterogeneity and complex pore structure of shale with the coexistence of organic matter pores and inorganic pores, shale reservoirs often exhibit mixed wettability (Dalmatian wettability), which in turn affects the SI behavior. , The wettability and pore connectivity of shale reservoirs were previously evaluated by SI experiments. , However, the application of SI on the enrichment mechanism of hydrocarbons is quite limited.…”
Section: Introductionmentioning
confidence: 99%
“…43 This phenomenon is typically achieved by injecting brine solutions with different salinity compared to the formation brine. 44 The injection-induced osmotic pressure triggers the migration of water molecules from the formation water toward the injected brine, resulting in a water flow into the porous media. The influx of water displaces the oil, improves fluid mobility, and ultimately leads to enhancing oil recovery.…”
Section: ■ Introductionmentioning
confidence: 99%