The surface nuclear magnetic resonance (SNMR) technology is a method that detecting the underground water directly at surface.
地面核磁共振(SNMR)技术是目前世界上直接用来寻找地下水的技术。
After discussing the basic inversion problem, this paper achieve the 1d SNMR Tikhonov regularization inverse by conjugate gradient method.
本文在讨论反演基本问题的基础上，用共轭梯度法实现了核磁共振的一维正则化反演。
It comments emphatically on three advanced geophysical exploration methods of multi-electrode geoelectric measurement, ground penetrating radar and SNMR.
着重评述多电极地电探测、地面穿透雷达、地面核磁共振三种先进的地球物理探测方法。
The features of Surface Nuclear Magnetic Resonance(SNMR) signal for underground water and the sources and characters of the spike noise distortion are analyzed.
首先分析了地面核磁共振信号的特征和奇异噪声的来源与特点，提出了相应的消除方法并进行了仿真研究。
The features of Surface Nuclear Magnetic Resonance(SNMR) signal for underground water and the sources and characters of the spike noise distortion are analyzed.
首先分析了地面核磁共振信号的特征和奇异噪声的来源与特点，提出了相应的消除方法并进行了仿真研究。
应用推荐