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首页> 外文期刊>Journal of Petroleum Science & Engineering >Experimental evaluation of oxidation sensitivity in organic-rich shale reservoir
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Experimental evaluation of oxidation sensitivity in organic-rich shale reservoir

机译:有机富有的页岩储层氧化敏感性的实验评价

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Organic-rich shale reservoirs are rich in reductive minerals, such as pyrite and other organic matters. The working fluid for the development of shale gas reservoirs contains large amount of dissolved oxygen. Once the working fluid enters the organic shale reservoir, it will oxidize the reducing components, cause mineral transformation, release solid phase particles, change the pore structures, and damage the seepage capacity of organic-rich shale reservoirs. The understanding and evaluation of the oxidation sensitivity is of great significance for improving the productivity of shale reservoirs. Therefore, organic shale of the Longmaxi Formation in the Pengshui area of the southeastern Sichuan Basin (China) was taken as the research object in the current work. In order to evaluate the reservoir fluid sensitivity, experiments were conducted to evaluate the oxidation sensitivity of the organic-rich shale reservoir. The experimental results showed that oxic fluids had the highest degree of damage on the permeability of shale than the reductive and degassed fluids. The oxidation sensitivity indices, Sox, of the shale samples were found to be 65.62% and 54.88%, respectively, which are moderately strong. The mechanism for the damage of the oxidation sensitivity of shale involves the production of Fe2O3, Fe(OH)(3), FeCO3 (siderite), CaSO4 center dot 2H(2)O (dihydrate gypsum), MgSO4, other precipitated solid particles (chemicals), and the shale debris. Therefore, the pores and fractures were blocked by solid particles, resulting in the decrease in fracture width as well as the number of solid particles, which could be expelled. An appropriate concentration of oxidants has a positive effect on the permeability of organic-rich shale. The oxidation will produce macroscopic cracks and a large number of dissolution pores that significantly improved the transport capacity of the pore fracture system, and increased the permeability of the organic-rich shale.
机译:有机富含的页岩储层富含矿物质,如硫铁矿和其他有机物。用于发展页岩气藏的工作流体含有大量的溶解氧。一旦工作流体进入有机页岩储存器,它将氧化还原成分,导致矿物转化,释放固相颗粒,改变孔隙结构,损坏有机富有的页岩储存器的渗流能力。对氧化敏感性的理解和评价对于提高页岩储层的生产率具有重要意义。因此,在四川盆地(中国)的彭水地区龙马西地区的有机页岩被视为目前工作中的研究对象。为了评估储层液体敏感性,进行实验以评估有机富含物体储层的氧化敏感性。实验结果表明,对页岩的渗透率而不是还原和脱气流体具有最高程度的损伤。发现氧化敏感性索引SOX,页岩样品分别为65.62%和54.88%,其适度强。 Shale氧化敏感性损伤的机制涉及生产Fe2O3,Fe(OH)(3),FECO3(锌),CasO4中心点2H(2)O(二水合物石膏),MgSO 4,其他沉淀的固体颗粒(化学品),和页岩碎片。因此,孔隙和裂缝被固体颗粒阻断,导致裂缝宽度的降低以及可驱逐的固体颗粒的数量。适当浓度的氧化剂对有机富含物的渗透性产生了积极影响。氧化将产生宏观裂缝和大量溶出孔,可显着提高孔隙骨折系统的运输能力,并增加了有机富含物的页岩的渗透性。

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