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Geochemical and Geomechanical Alterations Related to Rock-Fluid-Proppant Interactions in the Niobrara Formation

机译:与铌渣形成中岩石液相传的地球化学和地质力学改变

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Fracture conductivity degradation results from damage mechanisms and fluid interactions that occur during and after hydraulic fracturing treatments. Rock softening and associated proppant embedment are among the damage mechanisms affecting this degradation. The aim of this research study is to understand the physico- chemical interactions between fracturing fluid and formation to investigate the associated geomechanical property changes taking place in the Niobrara shale, a calcium carbonate rich formation, during and after hydraulic fracturing treatments. Experimental tests were carried out on Niobrara core samples to investigate the effects of chemical interactions between the formation, fracturing fluid, and proppant along with static and dynamic geomechanical property changes. The samples were characterized using X-Ray Diffraction (XRD), X-Ray Fluorescence (XRF), and Field-Emission Scanning Electron Microscopy (FESEM). Two sets of experiments were conducted: fluid chemical interactions with crushed rock and proppant, and geomechanical property variations in intact core samples. In the first set of experiments the changes in the composition of the solution were monitored as a function of saturation time. In the second set, the variations in the dynamic and static mechanical properties were examined in intact core plugs before and after they were saturated. Best practices for hydraulic fracturing fluid selection are established by incorporating the impact of the fracturing fluid on geochemical composition and geomechanical property changes in the formation. This study provides an insight into how each selected fluid formulation yields unique interactions with the mineral composition of the formation. Distilled water shows to be more prone to dissolve elements affecting the strength of the rock, whereas 2% brine solutions, especially 2% KCl, dissolve elements that could be the source of scales, fines migration, other types of undesired precipitations, as well as elements related to organic matter in the reservoir rock. A comparison of the dynamic and static elastic moduli and fluid chemistry data obtained pre- and post- treatment indicate that there is a correlation between softening of the formation and the chemical interactions taking place in the rock. FE-SEM images further support this interpretation. Hydraulic fracture treatment effectiveness in tight reservoirs can be improved by integrating multidisciplinary data. This study provides detailed geomechanical and geochemical analyses capturing associated changes in the rock and the fluid composition when they interact with each other. It also introduces a correlation between mineralogy and the mechanical properties of the rock proposing a simple approach to improve the fluid selection in hydraulic fracturing operations.
机译:裂缝传导性降解的结果从期间和之后水力压裂处理中发生的损伤机制和流体的相互作用。岩石软化和相关的支撑剂嵌入是影响这种退化的损伤机制中。这项研究的目的是了解压裂液和地层,调查发生在奈厄布拉勒页岩,碳酸钙丰富的地层,期间和之后水力压裂相关的地质力学特性变化之间的物理化学相互作用。实验测试进行了上奈厄布拉勒岩心样品,调查与静态和动态地质力学特性的变化而压裂液的支撑剂之间形成化学相互作用,以及效果。使用X射线衍射(XRD),X-射线荧光(XRF),以及场致发射扫描电子显微镜(FESEM)对样品进行表征。进行了两组实验:用碎石和支撑剂,以及完整的岩心样品的地质力学特性的变化流体的化学反应。在第一组实验中的溶液的组合物中的变化作为饱和时间的函数进行监控。在第二组中,动态和静态机械性能的变化之前完整芯插头进行了检查,他们被饱和后。水力压裂流体选择最佳做法是通过将压裂流体的地球化学组成和地层中的地质力学特性变化的影响建立。这项研究提供深入了解每个所选流体制剂如何产生与地层的矿物组合物的独特的相互作用。蒸馏水示出了要更容易溶解影响岩石的强度的元素,而2%的盐水溶液中,特别是2%的KCl,溶解可能是秤,微粒运移,其它类型的不期望的沉淀的的源元件,以及在储集岩有关的有机物的元件。动态和静态弹性模量和得到的前和后处理流体化学数据的比较表明,有形成和发生在岩石中的化学相互作用的软化之间的相关性。 FE-SEM图像进一步支持这种解释。在致密储层水力压裂处理的有效性可以通过整合多学科数据得到改善。本研究提供了详细的地质力学和地球化学分析捕获在岩石和相关的变化的流体组合物当它们与彼此交互。它还引入了矿物学和岩石的提出一种简单的方法,以提高在水力压裂作业的流体选择的机械性能之间的相关性。

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