Dmitriy A. Martyushev , Inna N. Ponomareva , Vasiliy I. Chernykh , Shadfar Davoodi , Yousef Kazemzadeh , Tianshou Ma
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Petrophysical analyses using multi-scale X-ray computed tomography, field emission scanning electron microscopy, and X-ray diffraction were conducted on samples both before and after the well killing simulation. The experiments were performed using real samples of cores, crude oil, and the killing fluid. The results from this study indicate that low-mineralized water (practically fresh water) is a carbonate rock solvent. Such water causes the dissolution of rock components, the formation of new calcite crystals and amoeba-like secretions, and the migration of small particles (clay, quartz, and carbonates). The formation of deep channels was also recorded. The assessment reveals that the change in the pH of the killing fluid indicates that the observed mineral reactions were caused by carbonate dissolution. These combined phenomena led to a decrease in the total number of voids in the core samples, which was 25% on average, predominantly among voids measuring between 45 and 70 μm in size. The change in the pore distribution in the bulk of the samples resulted in decreases in porosity of 1.8% and permeability of 67.0% in the studied core samples. The results from this study indicate the unsuitability of low-mineralized water as a well killing fluid in carbonate reservoirs. The composition of the killing fluid should be optimized, for example, in terms of the ionic composition of water, which we intend to investigate in future research.</p></div>","PeriodicalId":100469,"journal":{"name":"Energy Geoscience","volume":"5 4","pages":"Article 100340"},"PeriodicalIF":3.6000,"publicationDate":"2024-08-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2666759224000556/pdfft?md5=45700afc99fe54653649ba54d514b699&pid=1-s2.0-S2666759224000556-main.pdf","citationCount":"0","resultStr":"{\"title\":\"Impacts of interactions with low-mineralized water on permeability and pore behavior of carbonate reservoirs\",\"authors\":\"Dmitriy A. Martyushev , Inna N. Ponomareva , Vasiliy I. 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The experiments were performed using real samples of cores, crude oil, and the killing fluid. The results from this study indicate that low-mineralized water (practically fresh water) is a carbonate rock solvent. Such water causes the dissolution of rock components, the formation of new calcite crystals and amoeba-like secretions, and the migration of small particles (clay, quartz, and carbonates). The formation of deep channels was also recorded. The assessment reveals that the change in the pH of the killing fluid indicates that the observed mineral reactions were caused by carbonate dissolution. These combined phenomena led to a decrease in the total number of voids in the core samples, which was 25% on average, predominantly among voids measuring between 45 and 70 μm in size. The change in the pore distribution in the bulk of the samples resulted in decreases in porosity of 1.8% and permeability of 67.0% in the studied core samples. The results from this study indicate the unsuitability of low-mineralized water as a well killing fluid in carbonate reservoirs. 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引用次数: 0
摘要
实验室过滤实验用于研究有效的油井杀井,同时将其对周围岩石的影响降至最低。本实验研究的新颖之处在于将岩石样本与杀井液长时间接触七天,这与俄罗斯彼尔姆边疆区油田的平均修井时间相当。我们的研究结果表明,影响岩石与杀软液相互作用的关键因素包括杀软液的化学成分、碳酸盐岩的矿物成分、储层压力和温度以及接触时间。使用多尺度 X 射线计算机断层扫描、场发射扫描电子显微镜和 X 射线衍射对杀井模拟前后的样本进行了岩石物理分析。实验使用了真实的岩心、原油和杀井液样本。研究结果表明,低矿化度水(实际上是淡水)是一种碳酸盐岩溶剂。这种水会导致岩石成分溶解,形成新的方解石晶体和阿米巴状分泌物,以及小颗粒(粘土、石英和碳酸盐)的迁移。此外,还记录到深层水道的形成。评估显示,杀戮液 pH 值的变化表明,观察到的矿物反应是由碳酸盐溶解引起的。这些综合现象导致岩心样本中的空隙总数减少,平均减少 25%,主要集中在 45 至 70 μm 大小的空隙中。样本主体孔隙分布的变化导致所研究岩心样本的孔隙率下降了 1.8%,渗透率下降了 67.0%。研究结果表明,低矿化度水不适合作为碳酸盐岩储层的杀井液。应优化杀井液的成分,例如水的离子成分,我们打算在今后的研究中对此进行调查。
Impacts of interactions with low-mineralized water on permeability and pore behavior of carbonate reservoirs
Laboratory filtration experiments are employed to investigate effective well killing while minimizing its impacts on surrounding rocks. The novelty of this experimental study lies in the prolonged exposure of rock samples to the killing fluid for seven days, corresponding to the average duration of well workovers in the oilfields in Perm Krai, Russia. Our findings indicate that critical factors influencing the interactions between rocks and the killing fluid include the chemical composition of the killing fluid, the mineralogical composition of the carbonate rocks, reservoir pressure and temperature, and the contact time. Petrophysical analyses using multi-scale X-ray computed tomography, field emission scanning electron microscopy, and X-ray diffraction were conducted on samples both before and after the well killing simulation. The experiments were performed using real samples of cores, crude oil, and the killing fluid. The results from this study indicate that low-mineralized water (practically fresh water) is a carbonate rock solvent. Such water causes the dissolution of rock components, the formation of new calcite crystals and amoeba-like secretions, and the migration of small particles (clay, quartz, and carbonates). The formation of deep channels was also recorded. The assessment reveals that the change in the pH of the killing fluid indicates that the observed mineral reactions were caused by carbonate dissolution. These combined phenomena led to a decrease in the total number of voids in the core samples, which was 25% on average, predominantly among voids measuring between 45 and 70 μm in size. The change in the pore distribution in the bulk of the samples resulted in decreases in porosity of 1.8% and permeability of 67.0% in the studied core samples. The results from this study indicate the unsuitability of low-mineralized water as a well killing fluid in carbonate reservoirs. The composition of the killing fluid should be optimized, for example, in terms of the ionic composition of water, which we intend to investigate in future research.