首页> 外文会议>International Symposium on Water-Rock Interaction(WRI-11) vol.1; 20040627-0702; Saratoga Springs,NY(US) >Experimental and numerical simulation of carbonate dissolution and porosity development by organic acids
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Experimental and numerical simulation of carbonate dissolution and porosity development by organic acids

机译:有机酸对碳酸盐溶解和孔隙发育的实验和数值模拟

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A series of flow-through experiments were conducted to identify and quantify the effects of acetic acid on secondary porosity generation in carbonate reservoirs during deep burial. For the acetic acid concentrations studied (typical of oil field waters), dissolution occurred as a sharp reaction front on a core scale. Along the reaction front, acetic acid dissolved the material by attacking calcite cleavage planes. Calcium concentrations measured from effluent samples indicated that the pore fluid reached its equilibrium concentration rapidly. Dissolution resulted in a bulk porosity increase of less than 0.5% after 14 days, contributed mostly by the dissolution at the core inlet. The experimental results validated predictions of reactive transport models and the theoretical derivation of dissolution patterns. Mass balance calculations suggest that the porosity increases by organic acid dissolution are not volumetrically important.
机译:进行了一系列流过实验,以识别和量化乙酸对深埋期间碳酸盐岩储层中二次孔隙生成的影响。对于所研究的乙酸浓度(典型的油田水),在核心规模上,溶解以急剧的反应前沿发生。沿着反应前沿,乙酸通过攻击方解石裂解平面溶解了物质。从废水样品中测得的钙浓度表明,孔隙流体迅速达到其平衡浓度。溶解导致14天后的总孔隙率增加小于0.5%,主要是由于岩心入口处的溶解所致。实验结果验证了反应性传输模型的预测和溶出度模式的理论推导。质量平衡计算表明,由于有机酸溶解而增加的孔隙度在体积上并不重要。

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