用预极化表面核磁共振测量土壤水分

T. Hiller, S. Costabel, R. Dlugosch, T. Radić, M. Müller‐Petke
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引用次数: 0

摘要

非饱和带的小规模研究在水文地球物理研究界引起了越来越大的兴趣。表面核磁共振(SNMR)技术虽然提供了有关饱和区含水量和渗透率的宝贵数据,但由于信号幅值较低,难以可靠地检测和解释部分饱和土壤的信号。最近,使用预极化的SNMR (SNMR- pp)技术克服了这一限制。在这里,一个强大的预极化场增强了一米以下线圈的SNMR信号,使其能够在不久的将来实现地下两米以上的土壤湿度测量。我们首次在真实土壤上进行了SNMR-PP测量,并证明了该技术在定性和定量检测土壤湿度方面的总体可行性。我们的土壤湿度测量是由独立的时域反射(TDR)数据验证。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Measuring Soil Moisture Using Surface-NMR With Prepolarization
Summary Small-scale investigations of the unsaturated zone has gained increasing interest in the hydro-geophysical research community. The technique of surface-NMR (SNMR), while providing valuable data on water content and permeability in the saturated zone, has difficulties to reliably detect and interpret signals from partly-saturated soils due to low signal amplitudes. Recently, SNMR using prepolarization (SNMR-PP) has gained interest to overcome this limitation. Here, a strong prepolarization field enhances the SNMR signal of coils with a footprint of below 1m up to a level that promises to enable soil moisture measurements in the upper two meters of the subsurface in the near future. We present the first SNMR-PP measurements on a real soil and demonstrate the general feasibility of this technique to qualitatively and quantitatively detect soil moisture. Our soil moisture measurements are validated by independent time domain reflectometry (TDR) data.
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