碳酸盐岩溶蚀缝洞储层数字岩石建模与弹性模拟

Digital rock modeling and elastic simulations of fractured-vuggy carbonate reservoirs

  • 摘要:
    目的 塔里木盆地的深层碳酸盐岩溶蚀缝洞储层广泛发育,刻画含缝洞系统碳酸盐岩储层的地震岩石物理特征对有利储集体的勘探发现和钻井开发具有重要的指导意义。当溶蚀缝洞的充填状态发生变化时,其弹性和衰减特征具有显著差异。
    方法 基于塔里木盆地碳酸盐岩地层露头剖面中溶蚀缝洞系统的几何结构特征和充填特征的地质认识,提出了溶蚀缝洞体系数字岩石的构建方法。在物理相似比的指导下,利用动态应力应变数值模拟计算数字岩石的频散和衰减特征,并分析溶洞充填物的类型和含量、缝胶结物的含量以及缝洞含水饱和度发生改变时,数字岩石的频散和衰减的变化特征及其背后的物理机制。
    结果和结论 溶洞充填物与溶蚀缝胶结物的含量变化对速度和衰减均产生显著影响。溶洞充填物类型对速度的影响较为明显,而对衰减的影响相对较弱。当缝洞含水饱和度发生变化时,速度呈现单调变化趋势,而衰减则表现出复杂的跳变特征。速度作为表征数字岩石内部结构平均特性的参数,其与缝洞内充填物之间具有较强的相关性;而衰减则对数字岩石局部结构内的流体赋存状态具有较高敏感性。研究成果可用于指导深层碳酸盐岩溶蚀缝洞储层的定量地震解释、属性优选和速度建模,支撑深层碳酸盐岩储层的高精度地球物理刻画。

     

    Abstract:
    Objective The Tarim Basin exhibits extensively distributed deep fractured-vuggy carbonate reservoirs. Therefore, determining the seismic and petrophysical characteristics of carbonate reservoirs with a fracture and vug system will provide significant guidance for the exploration, discovery, drilling, and exploitation of favorable reservoirs in the basin. Variations in the filling state of dissolution fractures and vugs will lead to significantly different elastic and attenuation characteristics of the reservoirs.
    Methods Based on geological insights into the geometric structural and filling characteristics of the dissolution fracture-vug system in the outcrop sections of carbonate strata in the Tarim Basin, this study proposed a digital rock modeling method for dissolution fracture-vug systems. Guided by physical similarity, this study calculated the dispersion and attenuation characteristics of digital rocks using dynamic stress-strain numerical simulations. Moreover, this study analyzed the wave dispersion and attenuation, as well as the underlying physical mechanisms, varying with the type and volume fraction of vug fillings, the volume fraction of fracture cements, and the gas saturation of fractures and vugs.
    Results and Conclusions  Changes in the volume fractions of vug fillings and fracture cements significantly affected the wave velocity and attenuation in the reservoirs. The type of vug fillings produced a more pronounced impact on the wave velocity than the wave attenuation. In the case of varying gas saturation, the wave velocity manifested a monotonic variation trend, while the wave attenuation displayed complex jump characteristics. Wave velocity, as a parameter for characterizing the average properties of the internal structures of digital rocks, exhibited a strong correlation with vug fillings. In contrast, the wave attenuation was highly sensitive to the occurrence state of fluids within local structures of digital rocks. The results of this study can guide the quantitative seismic interpretation, selection of optimal attributes, and velocity modeling for deep fractured-vuggy carbonate reservoirs, supporting the high-precision geophysical characterization of these reservoirs.

     

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