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EXAMINATION OF POROSITY BY NMR AND INTRUSION POROSIMETRY

机译:核磁共振和压入法测定孔隙度

摘要

Properties of a porous solid sample 19, which may be a core of rock taken from below ground are carried out using apparatus which performs both nuclear magnetic resonance (NMR) and porosimetry measurements. The apparatus has a magnet 11,12 providing a magnetic field and a radio frequency coil 20 for transmitting and/or receiving electromagnetic radiation so as to bring about NMR in the magnetic field, a pressure vessel 14, 15 to hold a sample 19 within the magnetic field, a supply of a non-wetting liquid connected to the vessel, means to apply pressure to the non-wetting liquid to force liquid into pores of the sample 19 means to measure applied pressure of the non-wetting liquid and means to measure volume thereof taken up by the sample. The pressure of non-wetting liquid may be increased in steps, using intruded liquid volume at each step to give a measurement of pore throat size using NMR at each step to give a measure of pore size such as diameter of equivalent sphere. The non-wetting liquid may be mercury and NMR may observe the Knight shift of 99 Hg.
机译:多孔固体样品 19 的特性可以使用执行核磁共振(NMR)和孔隙率测量的设备来执行,该样品可能是从地下开采的岩石的核心。该装置具有提供磁场的磁体 11,12 和用于发送和/或接收电磁辐射以便在磁场中产生NMR的射频线圈 20 。压力容器 14、15 将样品 19 保持在磁场内,与容器相连的不润湿液体的供给意味着向容器施加压力。迫使液体进入样品孔中的非润湿性液体 19 是指测量非润湿性液体施加的压力并测量其被样品吸收的体积。可以逐步增加不润湿液体的压力,在每个步骤中使用注入的液体体积以在每个步骤中使用NMR来测量孔喉的尺寸,以给出孔径的度量,例如等效球体的直径。非润湿液体可以是汞,NMR可以观察到99 Hg的奈特位移。

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