Time-Dependent CO(2)-Brine-Rock Interaction Effect on Sand Onset Prediction: A Case Study of Dolomite-Rich Sandstone in Air Benakat Formation, South Sumatra, Indonesia

时间依赖性二氧化碳-盐水-岩石相互作用对砂岩形成起始预测的影响:以印度尼西亚南苏门答腊艾尔贝纳卡特组富含白云石的砂岩为例

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Abstract

CO(2) injection into geological formation for carbon capture, utilization, and storage (CCUS) including enhanced oil or gas recovery provides a solution to reduce CO(2) emissions and bring on potential economic benefits. However, field operation possesses potential challenges both for injection and production wells. Operational constraints commonly considered are weighted around the injection well and related to well and formation integrity (e.g., limiting the risk of injection-induced fracturing). On the other hand, complexities of CO(2)-brine-rock interaction affect sand production phenomena in production wells. This study investigates CO(2)-brine-rock interaction to reflect CO(2) injection impact toward reservoir fluid and rocks. This study involves extensive experimental works, namely, time-lapse dry mass measurements, brine compositions and pH analysis, X-ray diffraction (XRD), scanning electron microscopy-energy-dispersive spectroscopy (SEM-EDS), petrographic thin section analysis, porosity measurements, and elastic wave velocity measurements. CO(2)-brine-rock batch experiment was designed and utilized to observe mineral dissolution, pore structure alteration, as well as rock physics alteration caused by CO(2)-brine-rock interactions. An outcrop sample of dolomite-rich sandstone in Air Benakat formation, South Sumatra, Indonesia, was used as a case study. This study shows that dolomite dissolution was observed and led to ∼6.6% porosity improvement as well as rock strength reduction (as shown by ∼4.3% of P wave and ∼6.2% of S wave reduction, respectively). The results of experimental works were then used to construct sand onset prediction model that considers rock strength alteration caused by CO(2)-brine-rock interactions. The sand onset prediction model demonstrates an acceleration of sand onset occurrence due to CO(2)-brine-rock interactions which can assist the operator to design a better sand management strategy in producer wells.

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