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    三合村区块沙三段稠油储层电阻率差异性分析及启示

    • 摘要: 沾化凹陷三合村区块沙三段深层稠油储层电阻率响应复杂,表现为测井电阻率曲线有高有低,影响因素不明,严重影响流体性质的测井判别和饱和度评价。笔者利用岩性描述、物性、X衍射、生产测试及测井等资料,对沙三段稠油储层进行“四性”特征及相互关系研究,深入探讨电阻率差异性及影响因素。结果表明:稠油储层岩性以细砂岩为主,矿物成分主要为石英,含少量长石和黏土,属于中-高孔、中-高渗储层;含砾粗砂岩和含砾中砂岩物性最好,含砾细砂岩和细砂岩次之,砾岩最差;富含油和油浸样品物性较好,而油斑和油迹物性差,其中富含油主要分布于含砾细砂岩,油浸、油斑主要发育于细砂岩、中砾岩;电阻率差异主要体现在不同的岩性上,含砾石稠油层电阻率值普遍高于40Ω·m,而细砂岩稠油层通常低于30Ω·m,电阻率响应受岩性、物性、含油性和油水赋存状态的综合影响,特别是同一岩性表现的电阻率差异受稠油、水相互赋存的影响不容忽视。基于上述对储层特征和电阻率影响因素的剖析,为稠油有效储层电阻率下限取值、饱和度测井评价甚至类似稠油油藏开发提供了一定的依据和启示。

       

      Abstract: The resistivity response of the deep heavy oil reservoirs in the Third Member of the Shahejie Formation in the Sanhe Village Block, Zhanhua Sag, is complex, characterized by both high and low logging resistivity curves. The influencing factors are unclear, which severely affects the logging discrimination of fluid properties and saturation evaluation. Using data such as lithological descriptions, physical properties, X-ray diffraction, production tests, and well logs, this study investigates the “four-property” characteristics and their interrelationships in the heavy oil reservoirs of the Third Member of the Shahejie Formation, and thoroughly explores the resistivity differences and their influencing factors. The results show that the heavy oil reservoirs are predominantly composed of fine sandstone, with mineral composition mainly quartz, along with small amounts of feldspar and clay, classifying them as medium-high porosity and medium-high permeability reservoirs. Among these, gravelly coarse sandstone and gravelly medium sandstone exhibit the best physical properties, followed by gravelly fine sandstone and fine sandstone, while conglomerate shows the poorest. Samples rich in oil and those that are oil-soaked have better physical properties, whereas samples with oil stains and oil traces have poor physical properties. Oil-rich samples are mainly distributed in gravelly fine sandstone, while oil-soaked and oil-stained samples are primarily developed in fine sandstone and medium conglomerate. The resistivity differences are mainly reflected in different lithologies: the resistivity value of gravel-bearing heavy oil layers is generally higher than 40 Ω·m, whereas that of fine sandstone heavy oil layers is usually below 30 Ω·m. The resistivity response is comprehensively influenced by lithology, physical properties, oil-bearing property, and the occurrence state of oil and water. Particularly, the resistivity differences observed within the same lithology, influenced by the mutual occurrence of heavy oil and water, cannot be ignored. Based on the above analysis of reservoir characteristics and factors influencing resistivity, this study provides a certain basis and implications for determining the lower limit of effective reservoir resistivity in heavy oil reservoirs, saturation logging evaluation, and even the development of similar heavy oil reservoirs.

       

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