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构造应力化学——慢地震震源机制解的一种可能途径*

郭谦谦, 孙静娴, 侯泉林   

  1. 中国科学院大学地球与行星科学学院 中国科学院计算地球动力学重点实验室,北京, 100049
  • 收稿日期:2024-01-03 修回日期:2024-03-27 发布日期:2024-04-07
  • 通讯作者: †E-mail: quhou@ucas.edu.cn
  • 基金资助:
    *国家自然科学基金重点国际(地区)合作研究项目(42220104008)和中国科学院大学自设项目(E3JT040103)资助

Tectonic stress chemistry- a possible perspective on focal mechanism of slow earthquakes

GUO Qianqian, SUN Jingxian, HOU Quanlin   

  1. CAS Key Laboratory of Computational Geodynamics,College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing 100049,China
  • Received:2024-01-03 Revised:2024-03-27 Published:2024-04-07

摘要: 慢地震震源机制研究主要建立在脆性变形基础上。然而高纵、横波速度比、异常高泊松比等特征表明其震源区物质粘度较大,更易发生塑性变形。固体力学研究认为塑性变形的起点是位错,塑性应变能无法释放。分子尺度上,原子通过化学键结合形成矿物。应力化学研究显示机械力可以直接作用于化学键,化学键断裂时体系位于能量高位。塑性变形的位错机制应该始于化学键的变化,再通过断裂、重组,形成亚颗粒、细粒化,能量的转化过程可能是机械能首先转化为体系内能,即原子势能;随着加载继续,原子势能突破化学键的束缚,转化为塑性应变能。化学键的重建会释放能量,塑性变形过程中可能会释放一部分化学能,这是否与慢地震有关,是个值得探索的科学命题。

关键词: 慢地震, 震源机制, 塑性变形微观机理, 塑性应变能, 构造应力化学

Abstract: Researches on the focal mechanism was mainly based on brittle deformation. However, high ratios of P-wave to S-wave velocity, anomalously high Poisson's ratios indicate that the source material of slow earthquakes is more viscous and more prone to plastic deformation. Traditional studies suggest that plastic deformation begins with dislocation, and is permanent. Therefore, the plastic strain energy cannot be released. However, it is maybe different when talked about on a microscopic molecular scale. The lithosphere is mainly constructed of silicate minerals, especially of tetracoordinated compounds with [SiO4] tetrahedrons as fundamental units. That is, within minerals are chemical bonds binding various atoms together. Therefore, the dislocation mechanism of plastic deformation may first start with the change of chemical bonds, and then the chemical bonds begin to break off and rebonding, forming sub-grains and grain size reduction. Mechanochemical study shows that the mechanical force can directly act on the chemical bond via stretching and rotating, change the bond length, angle, and finally break off the chemical bond. Quantum chemical calculations on molecular fragments of the crystalline structure in coal indicate that the carbon bond breaks off at high energy levels, when the hydroxyl group of the 6-membered benzene ring falls off to form CO and 5-membered rings. During plastic deformation, the energy conversion may be work done from mechanical energy by external forces firstly to internal energy as atomic potential energy, and then plastic strain energy. However, not all atomic potential energy could transform into plastic strain energy for the reconstruction of the chemical bond may releases energy. As a result, a little energy may be released during the plastic deformation. Whether this is related to slow earthquakes is a scientific proposition worth exploring. It may be a possible way to explore the focal mechanism of slow earthquakes by using atomic scale quantum chemistry calculation to establish a finer energy change process of crystal plastic deformation and comparing the source parameters of slow earthquakes.

Key words: Slow earthquake, focal mechanism, microscopic mechanism of plastic deformation, plastic strain energy, tectonic stress chemistry

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