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Determination of pore size distribution and hydraulic properties using nuclear magnetic resonance relaxometry:A comparative study of laboratory methods

机译:核磁共振弛豫法测定孔径分布和水力性质:实验室方法的比较研究

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摘要

In this study, we evaluate the feasibility of using nuclear magnetic resonance CNMR) relaxometry measurements to characterize pore size distribution and hydraulic properties in four porous samples with different texture and composition. We compare NMR with two classical techniques based on water retention and mercury intrusion measurements. Both T_2 and T_1 NMR relaxation measurements at 6.47 MHz were carried out for three saturated model samples (medium sand, fine sand, and a homogenous sand/kaolin clay mixture) and one saturated natural silt loam soil. Cumulative pore size distribution functions and mean pore diameters were calculated assuming average surface relaxivity parameters and a cylindrical capillary model of the pores. The mean pore diameters derived from T_2 and T_1 distributions as well as the cumulative pore size distribution functions agree satisfactorily with those derived from mercury intrusion and retention curves. The observed deviations are due to limitations of each method, sample preparation, and sample composition. To evaluate the influence of the variations observed in the hydraulic properties of the samples, the pore size distribution functions were scaled back to water retention functions, and the van Genuchten hydraulic parameters were estimated by inversion using the RETC software. The comparison shows that both T_2 and T_1 NMR relaxation measurements can be used to estimate pore size distribution and mean pore diameter, as well as the retention function and corresponding hydraulic properties.
机译:在这项研究中,我们评估了使用核磁共振弛豫法测量表征四个具有不同质地和组成的多孔样品的孔径分布和水力特性的可行性。我们将NMR与基于保水率和压汞法的两种经典技术进行比较。对三个饱和模型样品(中砂,细砂和均质砂/高岭土混合物)和一种饱和天然粉壤土在6.47 MHz处进行了T_2和T_1 NMR弛豫测量。假设平均表面弛豫参数和孔的圆柱毛细模型,计算累积的孔径分布函数和平均孔径。由T_2和T_1分布得出的平均孔径以及累积的孔径分布函数与由汞侵入和保留曲线得出的平均孔径令人满意。观察到的偏差是由于每种方法,样品制备和样品组成的限制。为了评估观察到的水硬性变化的影响,将孔径分布函数缩小为保水率函数,并使用RETC软件通过反演来估算van Genuchten水力学参数。比较结果表明,T_2和T_1 NMR弛豫测量均可用于估算孔径分布和平均孔径,以及保留功能和相应的水硬性。

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  • 来源
    《Water resources research》 |2010年第11期|p.W11510.1-W11510.11|共11页
  • 作者单位

    Agrospherc Institute, ICG-4, Forschungszentrum Julich, D-52425 Julich,Germany;

    Agrospherc Institute, ICG-4, Forschungszentrum Julich, D-52425 Julich,Germany;

    Macromolecular Chemistry Department, RWTHAachen University, D-52074, Aachen, Germany.;

    Department of Technical Physics II, Ilmcnau University of Technology, D-98684 Ilmenau, Germany.;

    Agrospherc Institute, ICG-4, Forschungszentrum Julich, D-52425 Julich,Germany;

    Agrospherc Institute, ICG-4, Forschungszentrum Julich, D-52425 Julich,Germany;

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