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MODELLING REFLECTION SIGNATURES OF PORE FLUIDS AND DUAL POROSITY IN CARBONATE RESERVOIRS

机译:碳酸盐岩储层中孔隙流体和双重孔隙的反射特征建模

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The motivation for this synthetic Amplitude Versus Angle (AVA) study of an isotropic carbonate reservoir consisting of a dual porosity on two scales is to identify possible seismic signatures of carbonate rocks containing various fluids and pore connection models. The reservoir is modelled for four scenarios on the basis of a general theory for visco-elastic waves, where the inclusion-based model operates with spheroidal cavities on two scales. While the total porosity of the reservoir is considered constant, the pores and cracks at the different scales are designed to be either connected or isolated. The pore systems are saturated with either gas, oil or water. Reflection coefficients are computed for a 2-layer model consisting of a cap rock of shale above the reservoir in order to analyze the effects of various pore to pore connection and pore fluid models in the double porosity systems.rnThe modelling shows how the AVA parameters change both due to varying pore to pore connection and various pore fluid saturation scenarios. If we assume estimated AVA parameters with some uncertainties, the study indicates that it should be possible to obtain measurable changes in the reflectivity due to changes of the pore connectivity also when the introduced fluid has almost equal acoustic properties as the displaced one. Such modelling studies should be of particular relevance for studying diagenetic effects on seismic signatures, as for instance, water and oil may have similar acoustic properties, but different impact on the pore system over time.
机译:对由两个尺度上的双重孔隙组成的各向同性碳酸盐岩储层进行合成振幅对角(AVA)研究的动机是,确定含有各种流体和孔隙连接模型的碳酸盐岩的可能地震特征。在粘弹性波的一般理论基础上,针对四种情况对储层进行了建模,其中基于夹杂物的模型在两个尺度上以球状腔体运行。虽然储层的总孔隙度被认为是恒定的,但不同规模的孔隙和裂缝被设计为连通或隔离的。孔隙系统充满了气体,油或水。计算一个由储层上方的页岩盖层组成的2层模型的反射系数,以分析双孔隙度系统中各种孔隙对孔隙的连接和孔隙流体模型的影响。该模型显示了AVA参数如何变化两者都是由于孔隙与孔隙之间的连接不断变化以及孔隙流体饱和度不同而引起的。如果我们假设估计的AVA参数具有一些不确定性,则研究表明,即使引入的流体具有与驱替后的流体几乎相同的声学特性,由于孔隙连通性的变化,也应该可以获得反射率的可测量变化。这样的模型研究对于研究成岩作用对地震特征的影响尤为重要,例如,水和油可能具有相似的声学特性,但随着时间的流逝对孔隙系统的影响不同。

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