基于地球数据统计反演的行星内部精细模型计算算法

IF 1 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
I. A. Boronin, T. V. Gudkova
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引用次数: 0

摘要

摘要-直到最近,行星内部结构的模型是基于直接问题的解决方案,输入行星引力场(质量,转动惯量,潮汐洛夫数k2)和假定的行星地球化学组成。为了使不同的模型参数与观测量相一致,求解逆问题是很重要的。本研究的目标之一是设计和实现一种计算算法,该算法允许简单快速地添加新的输入数据。首先,从一组观测数据中构造计算算法,确定行星内部参数的径向分布。然后,利用贝叶斯统计方法,提出了反问题,并使用马尔可夫链蒙特卡罗(MCMC)方法求解。求解反问题的概率方法大大简化了模型参数与观测值和先验数据的匹配。贝叶斯统计方法允许我们考虑模型的初始信息和观测数据之间的对应关系。在重力资料反演的经典模型实例上对所开发的计算算法进行了验证。数值实验结果以图形形式给出。求解该问题的算法具有每个马尔可夫链的计算完全独立于其他马尔可夫链的特点。这个问题很容易均匀地分布在计算机或集群的所有核心上。这大大减少了计算算法的运行时间,这在未来输入参数数量增加时非常重要。在第二步的工作中,计划使用所提出的计算算法从已知的观测数据中找到行星内部的参数分布。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Computational Algorithm for Detailing Models of Planetary Interior Based on Statistical Inversion of Geodata

Computational Algorithm for Detailing Models of Planetary Interior Based on Statistical Inversion of Geodata

Abstract—Until recently, the model of the interior structure of a planet was specified based on the solution of the direct problem with input data on the planetary gravitational field (mass, moment of inertia, tidal Love numbers k2) and the presumed geochemical composition of the planet. To reconcile the different model parameters with the observed quantities, it is important to solve the inverse problem. One of the goals of this study is to design and implement a computational algorithm that allows for easy and fast addition of new input data. At the first step, a computational algorithm is constructed to determine the radial distributions of the parameters of the planet’s interior from a set of observational data. Using the Bayesian statistics approach, we then formulate the inverse problem and solve it using the Markov chain Monte Carlo (MCMC) method. The probabilistic approach to solving the inverse problem greatly simplifies the matching of model parameters that satisfy the observations and the a priori data. The Bayesian statistics approach allows us to take into account the correspondence between the initial information about the model and the observed data. The developed computational algorithm was tested on the classical model example of gravity data inversion. The results of the numerical experiment are presented graphically. The algorithm for solving the problem has the peculiarity that each Markov chain is computed completely independently of the others. The problem is easily distributed evenly over all the cores of a computer or a cluster. This greatly reduces the running time of the computational algorithm, which is important in the future when the number of input parameters increases. At the second step of the work, it is planned to use the presented computational algorithm to find parameter distributions in the interior of planets from the known observational data.

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来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
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