利用神经网络推断MgO的剪切特性

IF 1.8 3区 地球科学 Q2 MINERALOGY European Journal of Mineralogy Pub Date : 2023-01-17 DOI:10.5194/ejm-35-45-2023
Ashim Rijal, L. Cobden, J. Trampert, H. Marquardt, J. Jackson
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引用次数: 2

摘要

摘要地幔矿物的剪切特性对于解释地震横波速度,从而推断行星内部的组成和动力学至关重要。剪切波速和弹性张量分量,由此可以计算剪切模量,通常在模拟地球(或行星)内部压力和温度条件的实验室中测量。将剪切模量与压力(和温度)联系起来的函数形式拟合到测量值中,并用于在数据覆盖的范围内进行内插和外推。假设函数形式提供了先验信息,对预测剪切模量及其不确定性的约束可能在很大程度上取决于假设的先验而不是数据。在本研究中,我们提出了一种数据驱动的方法,在这种方法中,我们训练一个神经网络来从实验数据中学习压力、温度和剪切模量之间的关系,而不需要先验地规定函数形式。我们提出了一个MgO的应用程序,但如果有足够的数据来训练神经网络,同样的方法也适用于任何其他矿物。在低压下,MgO的剪切模量很好地受到数据的约束。然而,我们的结果表明,即使在室温下,不同的实验结果也不一致,可以看到网络预测的概率密度函数出现多峰和发散趋势。此外,尽管显式有限应变方程与神经网络预测的可能性基本一致,但也存在与网络给出的范围偏离的区域。在这些区域,无论地球的行为(或数据的行为)如何,方程形式的先验假设都提供了剪切模量的约束。在没有报告实际不确定性的情况下,在根据这些已定义的状态方程解释地震模型时,人们可能会变得过于自信。相比之下,训练后的神经网络提供了对实验数据的合理逼近,并量化了实验误差、插值不确定性、数据稀疏性和不同实验的不一致性带来的不确定性。
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Shear properties of MgO inferred using neural networks
Abstract. Shear properties of mantle minerals are vital for interpreting seismic shear wave speeds and therefore inferring the composition and dynamics of a planetary interior. Shear wave speed and elastic tensor components, from which the shear modulus can be computed, are usually measured in the laboratory mimicking the Earth's (or a planet's) internal pressure and temperature conditions. A functional form that relates the shear modulus to pressure (and temperature) is fitted to the measurements and used to interpolate within and extrapolate beyond the range covered by the data. Assuming a functional form provides prior information, and the constraints on the predicted shear modulus and its uncertainties might depend largely on the assumed prior rather than the data. In the present study, we propose a data-driven approach in which we train a neural network to learn the relationship between the pressure, temperature and shear modulus from the experimental data without prescribing a functional form a priori. We present an application to MgO, but the same approach works for any other mineral if there are sufficient data to train a neural network. At low pressures, the shear modulus of MgO is well-constrained by the data. However, our results show that different experimental results are inconsistent even at room temperature, seen as multiple peaks and diverging trends in probability density functions predicted by the network. Furthermore, although an explicit finite-strain equation mostly agrees with the likelihood predicted by the neural network, there are regions where it diverges from the range given by the networks. In those regions, it is the prior assumption of the form of the equation that provides constraints on the shear modulus regardless of how the Earth behaves (or data behave). In situations where realistic uncertainties are not reported, one can become overconfident when interpreting seismic models based on those defined equations of state. In contrast, the trained neural network provides a reasonable approximation to experimental data and quantifies the uncertainty from experimental errors, interpolation uncertainty, data sparsity and inconsistencies from different experiments.
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来源期刊
CiteScore
2.80
自引率
9.50%
发文量
40
审稿时长
6-12 weeks
期刊介绍: EJM was founded to reach a large audience on an international scale and also for achieving closer cooperation of European countries in the publication of scientific results. The founding societies have set themselves the task of publishing a journal of the highest standard open to all scientists performing mineralogical research in the widest sense of the term, all over the world. Contributions will therefore be published primarily in English. EJM publishes original papers, review articles and letters dealing with the mineralogical sciences s.l., primarily mineralogy, petrology, geochemistry, crystallography and ore deposits, but also biomineralogy, environmental, applied and technical mineralogy. Nevertheless, papers in any related field, including cultural heritage, will be considered.
期刊最新文献
Re-equilibration of quartz inclusions in garnet H2 mobility and redox control in open vs. closed hydrothermal oceanic systems – evidence from serpentinization experiments The use of MgO–ZnO ceramics to record pressure and temperature conditions in the piston–cylinder apparatus Incorporation and substitution of ions and H2O in the structure of beryl Compressibility and thermal expansion of magnesium phosphates
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