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首页> 外文期刊>Journal of Applied Geophysics >Pore space characterization in carbonate rocks - Approach to combine nuclear magnetic resonance and elastic wave velocity measurements
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Pore space characterization in carbonate rocks - Approach to combine nuclear magnetic resonance and elastic wave velocity measurements

机译:碳酸盐岩中孔隙空间的表征-结合核磁共振和弹性波速度测量的方法

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摘要

Pore space features influence petrophysical parameters such as porosity, permeability, elastic wave velocity or nuclear magnetic resonance (NMR). Therefore they are essential to describe the spatial distribution of petrophysical parameters in the subsurface, which is crucial for efficient reservoir characterization especially in carbonate rocks. While elastic wave velocity measurements respond to the properties of the solid rock matrix including pores or fractures, NMR measurements are sensitive to the distribution of pore-filling fluids controlled by rock properties such as the pore-surface-to-pore-volume ratio. Therefore a combination of both measurement principles helps to investigate carbonate pore space using complementary information.
机译:孔隙空间特征会影响岩石物理参数,例如孔隙度,渗透率,弹性波速度或核磁共振(NMR)。因此,它们对于描述地下岩石物理参数的空间分布至关重要,这对于有效地表征油藏尤其是碳酸盐岩至关重要。尽管弹性波速度测量对包括孔隙或裂缝在内的固体岩石基质的特性作出响应,但NMR测量对受岩石特性(例如孔表面积与孔隙体积之比)控制的孔隙填充流体的分布敏感。因此,两种测量原理的组合有助于使用补充信息来研究碳酸盐孔隙空间。

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