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WETTABILITY ALTERATION IN LIMESTONE AND DOLOMITE WITH BRINES AND CO_2

机译:石灰石和白云石与卤水和CO_2的润湿性变化

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Wettability test is one of the most used tools for evaluating rock/fluid interaction in oils reservoir. In the present paper two carbonate outcrop rocks are evaluated for wettability alterations when subjected to brine injections of varying salinities and content of dissolved CO_2. The evaluation included a qualitative appraisal via spontaneous imbibition tests and a quantitative assessment by the Amott-Harvey procedure. Rocks refer to limestone and dolomite samples with petro-physical properties similar to the Brazilian pre-salt reservoirs. Testing fluids are a medium gravity crude oil, seawater concentration brine, formation equivalent brine and the carbonated version of these brines. Results show additional oil recovery directly associated with wettability alteration provoked by brine concentration changes. Increments in recovery were observed independently if the brine concentration decreased or increased in the replacement process. For dolomites and limestone wettability changed in the direction of turning the rock from oil-wet to neutral wet. Tests carried out with equivalent carbonated brines show that similar alteration in the wetting properties also occur. Alterations were as well independent of the increase or decrease of the salt concentration in the brine changed. However, CO_2 or its derived ions dissolved in the brines seem to inhibit the mechanism of wettability change when rocks are subject to changes in brine salt concentrations.
机译:润湿性测试是评估油藏中岩石/流体相互作用的最常用工具之一。在本文中,当注入盐度和溶解的CO_2含量不同的盐水时,评估了两个碳酸盐露头岩石的润湿性变化。评估包括通过自发吸收测试进行的定性评估和通过Amott-Harvey程序进行的定量评估。岩石是指岩石物理性质类似于巴西盐下储层的石灰岩和白云岩样品。测试流体是中等重力原油,海水浓缩盐水,地层当量盐水以及这些盐水的碳酸化形式。结果表明,与盐水浓度变化引起的润湿性变化直接相关的额外采油量。如果更换过程中盐水浓度降低或增加,则可独立观察到回收率的增加。对于白云岩和石灰石,润湿性沿将岩石从油湿变为中性湿润的方向发生了变化。用等效的碳酸盐水进行的测试表明,润湿性能也发生了类似的变化。改变也与盐水中盐浓度的增加或减少无关。然而,当岩石的盐水盐浓度发生变化时,溶解在盐水中的CO_2或其衍生离子似乎抑制了润湿性变化的机制。

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