Fast 3D forward modeling of a potential field based on spherical symmetry of gravitational potential

Author:

Sun Siyuan1ORCID,Gao Xiuhe2ORCID,Cao Xuefeng1

Affiliation:

1. China Aero Geophysical Survey & Remote Sensing Center for Natural Resources, Department of Applied Technology for Airborne Geophysical Prospecting, Beijing, China.

2. China Aero Geophysical Survey & Remote Sensing Center for Natural Resources, Department of Applied Technology for Airborne Geophysical Prospecting, Beijing, China. (corresponding author)

Abstract

A novel approach is developed to implement the forward modeling of a potential field caused by prismatic grids on gridded observations with higher efficiency and less memory. Based on the spherical symmetry of gravitational potential, we summarize the parity, symmetry, and interconversion relations from derivatives and higher derivatives of gravitational potential, which reveal that there are vast repetitive calculation and storage redundancies in conventional forward modeling of a potential field for prismatic grids, especially for cubic grids. These properties help to reduce not only the size of a single kernel matrix but also the number of necessary kernels in multicomponent forward modeling of a potential field, such as a gradient tensor field or joint inversion of a potential field. Several experiments on the synthetic and the realistic Bishop models are presented to illustrate how these properties are used in the forward modeling of gravity and magnetic gradient tensors. Based on the proposed properties, a 2D fast Fourier transform is performed to accelerate the discrete deconvolution of the kernel and the model parameters. With the new method, one single kernel can be reduced to half the number of model parameters, and the memory requirement and time cost of our method can be reduced by 1/8 and 1/2, respectively, compared with previous works. In forward modeling of six gravity gradient tensor components, only two kernels need to be computed and stored, which are 1/3 of the conventional method. These examples indicate that, with high precision, our method requires less memory and less time than conventional methods. It shows potential in the fast large-scale inversion of gravity, magnetic, and gradient tensors with limited hardware resources.

Funder

National Key Research and Development Program of China

National Science Foundation for Youth Scientists of China

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference38 articles.

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2. Processing gravity gradient data

3. Constraints in 3D gravity inversion

4. Bruun, C. E., and T. B. Nielsen, 2007, Algorithms and software for large-scale geophysical reconstructions: Master’s thesis, DTU, DK-2800 Kgs, Technical University of Denmark.

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