Qin Shengwu, Ma Zhongjun, Jiang Chuandong, Lin Jun, Xue Yiguo, Shang Xinlei, Li Zhiqiang
College of Construction Engineering, Jilin University, Changchun 130026, China.
College of Institute of Instrument Science and Electrical Engineering, Jilin University, Changchun 130026, China.
Sensors (Basel). 2017 Sep 15;17(9):2127. doi: 10.3390/s17092127.
Due to its unique sensitivity to hydrogen protons, magnetic resonance sounding (MRS) is the only geophysical method that directly detects water and can provide nondestructive information on subsurface aquifer properties. The relationship between the surface MRS signal and the location and characteristics of aquifers using large-coil (typically 50-150 m) sensors has been discussed based on forward modelling and experiments. However, few researchers have studied underground MRS using a small-coil sensor. In this paper, a parametric study and a large-scale physical model test were conducted to shed light on the critical response characteristics of underground MRS using a small-coil sensor. The effects of the size and number of turns of the transmitter coil and receiver coil, the geomagnetic declination, the geomagnetic inclination, and the position, thickness, and water content of a water-bearing structure on the performance of the underground MRS were studied based on numerical simulations. Furthermore, we derived the kernel function and underground MRS signal curves for a water-bearing structure model based on the simulations. Finally, a large-scale physical model test on underground MRS using a small-coil sensor was performed using a physical test system for geological prediction of tunnels at Shandong University. The results show that the inversion results of the physical model test were in good agreement with the physical prototype results. Using both numerical modeling and physical model tests, this study showed that underground MRS using a small-coil sensor can be used to predict water-bearing structures in underground engineering.
由于磁共振测深(MRS)对氢质子具有独特的敏感性,它是唯一能直接探测水并能提供关于地下含水层特性的无损信息的地球物理方法。基于正演模拟和实验,已经讨论了使用大线圈(通常为50 - 150米)传感器时地表MRS信号与含水层位置和特征之间的关系。然而,很少有研究人员使用小线圈传感器研究地下MRS。本文进行了参数研究和大规模物理模型试验,以阐明使用小线圈传感器的地下MRS的关键响应特性。基于数值模拟,研究了发射线圈和接收线圈的尺寸和匝数、磁偏角、磁倾角以及含水结构的位置、厚度和含水量对地下MRS性能的影响。此外,基于模拟推导了含水结构模型的核函数和地下MRS信号曲线。最后,利用山东大学隧道地质超前预报物理试验系统,进行了使用小线圈传感器的地下MRS大规模物理模型试验。结果表明,物理模型试验的反演结果与物理原型结果吻合良好。通过数值模拟和物理模型试验,本研究表明使用小线圈传感器的地下MRS可用于预测地下工程中的含水结构。