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Study on Surface Nuclear Magnetic Resonance Inversion

机译:表面核磁共振反演研究

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Surface nuclear magnetic resonance is widely used for groundwater exploration and aquifercharacterization. Inversion of surface nuclear magnetic resonance provides important information about aquifers, such as their depths, thickness and water content. In this paper, we simply introduced the basic principles of nuclear magnetic resonance firstly, and then we discussed the relationship between surface nuclear magnetic resonance one dimensional kernel and pulse moment, medium conductivity, depth. It was found that surface nuclear magnetic resonance maximum depth is superimposed for one value of pulse moment and has smaller maximum depth in the higher conductive medium. A water content of layers lying below highly conductive layer is severely underestimated. It was also found that the condition number of one dimensional kernel matrix is small in the insulating medium. We improved simulated annealing algorithm from parameter restrictive condition, model disturbance, adaptive optimization method, circulate method, objective function, Markov chain and so on. Finally, we inverted MRS data using singular value decomposition and improved simulated annealing algorithm.The experimental result of synthetic data shows inverting MRS data using SVD in insulating medium and improved simulated annealing algorithm are desirable.
机译:表面核磁共振被广泛用于地下水勘探和含水层特征化。表面核磁共振反演可提供有关含水层的重要信息,例如其深度,厚度和含水量。本文首先简单介绍了核磁共振的基本原理,然后讨论了表面核磁共振的一维核与脉冲矩,介质电导率,深度之间的关系。已经发现,表面核磁共振最大深度被叠加在一个脉冲矩值上,并且在较高的导电介质中具有较小的最大深度。严重低估了位于高导电层之下的层的水含量。还发现在绝缘介质中一维核矩阵的条件数较小。从参数限制条件,模型扰动,自适应优化方法,循环方法,目标函数,马尔可夫链等方面对模拟退火算法进行了改进。最后,我们利用奇异值分解和改进的模拟退火算法对MRS数据进行了反演。综合数据的实验结果表明,在绝缘介质中使用SVD对MRS数据进行反演是理想的。

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