2017
DOI: 10.26804/ager.2017.03.02
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Mechanisms of reservoir pore/throat characteristics evolution during long-term waterflooding

Abstract: Formation pore structure and reservoir parameters change continually during waterflooding due to sand production, clay erosion, and pressure/temperature variation, which causes great challenge in geological modeling and simulation. In this work, the XA Oilfield, a block with more than 20 years' waterflooding history, is used as an example to better understand the fundamental evolution mechanisms of reservoir pore network characteristics over long time waterflooding. We performed a large number of core analyses… Show more

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Cited by 16 publications
(4 citation statements)
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“…In accordance with the two-phase flow theory, the fluid-rock characters determine the relative permeability of each phase [26][27][28][29]. The functional relationship of the flow rate flowing into the th reservoir and the pressure can be obtained under the assumption of steady flow [27], or…”
Section: Calculation Methodmentioning
confidence: 99%
“…In accordance with the two-phase flow theory, the fluid-rock characters determine the relative permeability of each phase [26][27][28][29]. The functional relationship of the flow rate flowing into the th reservoir and the pressure can be obtained under the assumption of steady flow [27], or…”
Section: Calculation Methodmentioning
confidence: 99%
“…Therefore, the microfluidic models that better simulate the real pore structure are employed to observe the fingering phenomenon from micro insight to analyze the influence of various factors. The microfluidics can be made from various materials, such as glass, polydimethylsiloxane (PDMS), and polymethyl methacrylate (PMMA), performing different properties of simulated reservoirs as shown in Table .…”
Section: Introductionmentioning
confidence: 99%
“…The pore space character is controlled by primary sedimentation and subsequent process such as compaction and diageneses. Primary sedimentary processes determine the initial pore space configuration, which is then altered by the diagenetic process through mechanical compaction and fluid‐rock interaction (Anovitz et al., 2013; Emmanuel et al., 2015; Qiao et al., 2020; Wang et al., 2017). Resulting pore structures determine the fluid flow potential of the forming rock.…”
Section: Introductionmentioning
confidence: 99%