基质酸化碳酸盐岩油藏微观结构及返排分析方法

Abdullah M. Al Moajil, Bashayer Aldakkan, H. Al-badairy, S. Shen
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引用次数: 2

摘要

碳酸盐岩酸化的成功取决于流体配方的选择、储层参数、作业设计和执行。对返排废酸的分析对今后的酸化工艺改进、配方设计和工艺设计有重要意义。本文的目的是分享碳酸盐岩酸化处理后的返排分析方法,重点是固体分析。采用高分辨率环境扫描电子显微镜(ESEM)、能量色散x射线微分析(EDX)和x射线衍射(XRD)等先进的显微和光谱分析技术进行微观结构分析。反排样品用0.45µm滤纸过滤。采用ICP法对返排样品进行分析。注入的酸性配方溶解了大量方解石。返排样品中最大钙浓度为9万~ 12万mg/L。此外,在pH值为4.7-5.5的返排样品中发现了固体沉淀。石膏是分析样品中的主要化合物,而其他化合物如鳞球石、磁铁矿、石英和重晶石在单个样品中检测到。在返排初期检测到铁基化合物。在后期返排阶段发现了富钙和富硅化合物。经鉴定,铁的来源很可能是磨屑。发现重晶石和石英与铁基化合物有关。石膏和氯化钠在CaSO4和NaCl化合物之间具有不同的优势,Dourba等人(2017)描述了可能的相关性。颗粒团聚主要与钙、氯化物和硫酸盐基化合物有关。棒状和六边形颗粒主要为硅基颗粒。花颗粒和枝晶结构被检测到,可能与石膏沉淀的无定形和半水中间体有关。扫描电镜观察到硫酸盐化合物的不同结构和团聚,表明它们是通过不同的机制和环境形成的。
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Microstructural and Flowback Analysis Methodology in Matrix Acidized Carbonate Oil Reservoirs
The success of carbonate acidizing depends on the selection of proper fluid recipes, reservoir formation parameters, job design, and execution. Analysis of flowback spent acid will improve the acidizing process in future treatments, enhance the designed recipes and treatment design. The objective of this paper is to share the flowback analysis methodology following carbonate acidizing treatments with focus on solid analysis. Microstructural analysis with advanced microscopy and spectroscopy analytical techniques such as high-resolution environmental scanning electron microscopy (ESEM), energy dispersive X-ray microanalysis (EDX) and X-ray diffraction (XRD) techniques were utilized. Flowback samples were filtered through 0.45 µm filter paper. ICP was used to analyze the flowback samples. The injected acid recipes dissolved significant amount of calcite. The maximum calcium concentrations in flowback samples were 90,000-120,000 mg/L. Moreover, solid precipitates were found in flowback samples associated with pH values of 4.7-5.5. Gypsum was the dominant compound in the samples analyzed while the other compounds such as Lepidocrocite, Magnetite, Quartz, and Barite were detected in a single sample. The iron-based compounds were detected in the beginning of flowback period. Calcium and silicon rich compounds were identified in later flowback periods. The source of iron was identified to be most likely mill scale. Barite and Quartz were found to be associated with iron-based compounds. Gypsum and sodium chloride were detected with varying dominations between CaSO4 and NaCl compounds with a possible correlation as described by Dourba et al. (2017). Particles agglomerations were mainly associated with calcium, chloride and sulfate-based compounds. The rod-like and hexagonally-shaped particles were mainly found to be Si-based particles. Flower particles and dendrite structures were detected and probably associated with Gypsum precipitation amorphous and hemihydrate intermediates. The varying structures and agglomerations of sulfate compounds detected by the SEM indicated they were formed via different mechanisms and environments.
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