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METHOD FOR ESTIMATING THE VOLUME OF CLAY (V CLAY) ON THE BASIS OF THE FORMATION DENSITY, OF THE POROSITY AND OF THE ACOUSTIC VELOCITIES IN CLAY-SANDSTONE RESERVOIRS
METHOD FOR ESTIMATING THE VOLUME OF CLAY (V CLAY) ON THE BASIS OF THE FORMATION DENSITY, OF THE POROSITY AND OF THE ACOUSTIC VELOCITIES IN CLAY-SANDSTONE RESERVOIRS
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机译:基于地层密度,孔隙度和声速的粘土-砂岩储层中粘土体积(V Clay Sub>)的估算方法
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摘要
Method of estimating the volume of clay (Vclay) characterizing a clay-sandstone reservoir, on the basis of the diagraphic recordings at the level of the well, the global density (ρb) and the velocities of the longitudinal (Vp) and transverse (Vs) waves and the porosity (ϕ). On the scale of the reservoir, one proceeds firstly with the estimation of the volumes of the acoustic velocities of the longitudinal (Vp) and transverse (Vs) waves and of the global density of the formation (ρb) on the basis of the seismic data processed in terms of amplitudes preserved by using a stratigraphic inversion. Thereafter one proceeds to the estimation of the volume of the total porosity (ϕt) on the basis of the acoustic velocities of the longitudinal (Vp) and transverse (Vs) waves and of the global density of the formation (ρb), which are generated by the inversion, using a multilinear relation. The volume of clay (Vclay) is estimated by this method by using the volumes of the seismic velocities (Vp) and (Vs), of the global density (ρb) and of the porosity (ϕ).
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机译:根据井水平的岩性记录,整体密度(ρ b ),估算表征粘土-砂岩储层的粘土(V clay Sub>)体积的方法Sub>)和纵向(V p Sub>)和横向(V s Sub>)的速度以及孔隙率(ϕ)。在储层的规模上,首先进行纵波(V p Sub>)和横波(V s Sub>)和纵波的声速体积估计。地层的整体密度(ρ b Sub>)是根据通过地层反演保留的振幅处理的地震数据得出的。然后,根据纵向(V p Sub>)和横向(V <使用多线性关系通过反演生成的Sub> s Sub>)波和地层的整体密度(ρ b Sub>)。使用地震速度(V p Sub>)和(V s Sub>)的体积,通过此方法估算粘土的体积(V clay Sub>) ),整体密度(ρ b Sub>)和孔隙率(ϕ)。
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