快速的3D重力和磁性建模使用中点方程和2D FFT
Xulong Wang1, Jianxin Liu1,2,3, Jian Li4,5
1School of Geosciences and Info-Physics, Central South University, Changsha, 410083, China.
Scientific reports
|June 8, 2023
概括
这项研究引入了一种新的3D重力和磁性建模方法,使用中点方程和2D FFT. 它显著减少了计算资源,使地质物理建模更有效.
科学领域:
- 地质物理学 地质物理学
- 计算科学 计算科学
背景情况:
- 传统的3D重力和磁性建模方法需要大量的计算资源.
- 计算内核矩阵和2D离散卷积是计算密集的步骤.
研究的目的:
- 为3D重力和磁性建模开发一种新的,计算效率高的方法.
- 为了减少与传统的地球物理建模技术相关的计算负担.
主要方法:
- 结合了中点方程方法与2D快速里埃转换 (FFT).
- 应用中点方程来计算积分的体积元素.
- 使用2D FFT来有效计算重量矩阵和密度/磁化之间的卷积.
主要成果:
- 拟议的算法显著减少了计算时间和内存需求.
- 与空间波数域方法相比,效率的增长大约是两个数量级.
- 使用人工和真实地形模型的验证证实了准确性和效率.
结论:
- 这种新的方法为3D重力和磁性建模的计算效率提供了实质性的改进.
- 这种方法克服了传统方法在资源消耗方面的局限性.
- 经过验证的算法为地球物理探索和分析提供了更容易使用的工具.
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