Joint use of singular value decomposition and Monte-Carlo simulation for estimating uncertainty in surface NMR inversion

被引:13
|
作者
Legchenko, Anatoly [1 ]
Comte, Jean-Christophe [2 ]
Ofterdinger, Ulrich [3 ]
Vouillamoz, Jean-Michel [1 ]
Lawson, Fabrice Messan Amen [4 ]
Walsh, John [5 ]
机构
[1] Univ Grenoble Alps, Inst Dev Res, IGE, Grenoble, France
[2] Univ Aberdeen, Sch Geosci, Aberdeen, Scotland
[3] Queens Univ, Belfast, Antrim, North Ireland
[4] Univ Abomey Calavi, Cotonou, Benin
[5] Coll Engn Math & Phys Sci, Sch Earth Sci, Dublin, Ireland
关键词
Hydrogeophysics; Ireland; Hard rock aquifer; Magnetic resonance sounding; MRS; Surface NMR; SNMR; NUCLEAR-MAGNETIC-RESONANCE; HARD-ROCK; WATER-RESOURCE; RESISTIVITY; RESOLUTION; RECHARGE; MRS; PRINCIPLES; AQUIFERS;
D O I
10.1016/j.jappgeo.2017.06.010
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We propose a simple and robust approach for investigating uncertainty in the results of inversion in geophysics. We apply this approach to inversion of Surface Nuclear Magnetic Resonance (SNMR) data, which is also known as Magnetic Resonance Sounding (MRS). Solution of this inverse problem is known to be non-unique. We inverse MRS data using the well-known Tikhonov regularization method, which provides an optimal solution as a trade-off between the stability and accuracy. Then, we perturb this model by random values and compute the fitting error for the perturbed models. The magnitude of these perturbations is limited by the uncertainty estimated with the singular value decomposition (SVD) and taking into account experimental errors. We use 106 perturbed models and show that the large majority of these models, which have all the water content within the variations given by the SVD estimate, do not fit data with an acceptable accuracy. Thus, we may limit the solution space by only the equivalent inverse models that fit data with the accuracy close to that of the initial inverse model. For representing inversion results, we use three equivalent solutions instead of the only one: the "best" solution given by the regularization or other inversion technic and the extreme variations of this solution corresponding to the equivalent models with the minimum and the maximum volume of water. For demonstrating our approach, we use synthetic data sets and experimental data acquired in the framework of investigation of a hard rock aquifer in the Ireland (County Donegal). (C) 2017 Elsevier B.V. All rights reserved.
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页码:28 / 36
页数:9
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