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Seismic responses of tight gas sand of different water saturations: A physical model research

机译:不同水饱和饱和饱和砂砂的地震反应:物理模型研究

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Due to the low-porosity/low-permeability character of tight sand, the gas-water mixed fluids in reservoir may not be evenly distributed, therefore the fluid substitution researches based on the rock physics theory that require fluid uniform distribution are not accurate. In this paper we focus on the velocity-water saturation relationship by ultrasonic transmission measurement. On this basis we build tight gas sand physical model of different water saturations, conduct data acquisition and processing and give the variation of seismic responses. The results show that in near offset the AVO response make little variation in low water saturation period, when saturation reaches certain value the rock physical properties of tight sand appear great changes, as a result the AVO response shows bigger change, the amplitude curve of different saturations can be distinguished. But in far offset the AVO curves of different saturation intersect together. In the post-stack section, the change of water saturation give rise to the different attenuation, the amplitude ratio between top and bottom of the reservoir shows a good correspondence with saturation, therefore this parameter is a good indicator to determine the gas content of tight sand.
机译:由于紧砂的低孔隙率/低渗透率特征,在储存器中的气 - 水混合的流体可以不被均匀地分布,因此根据需要流体的均匀分布的岩石物理理论的流体替换研究是不准确的。在本文中,我们集中在通过超声透射测量速度 - 水饱和度的关系。在此基础上,我们建立不同的含水饱和度的致密砂岩气的物理模型,进行数据采集和处理,并给地震响应的变化。结果表明,在近偏移距中低水饱和期的AVO响应没有多大的变化,当饱和度达到一定值致密砂岩的岩石物理性质出现了很大的变化,其结果是AVO响应显示较大的变化,不同的振幅曲线饱和度可以区分。但在远偏移不同饱和度的AVO曲线相交在一起。在后堆叠部,水饱和度引起的不同衰减的变化,的储存节目的顶部和底部之间的振幅比与饱和度有良好的对应,因此此参数是一个很好的指标,以确定紧的气体含量沙。

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