دورية أكاديمية
Saturated dislocations transient propagation-evolution in olivine structure under ultra high-coupled thermal-force fields
العنوان: | Saturated dislocations transient propagation-evolution in olivine structure under ultra high-coupled thermal-force fields |
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المؤلفون: | Zhu BJ(朱伯靖), Liu Chang, Shi Yaolin, Liu Xuyao |
بيانات النشر: | ELSEVIER SCIENCE BV |
سنة النشر: | 2012 |
المجموعة: | Yunnan Observatories: YNAO OpenIR (Chinese Academy of Sciences, CAS) / 中国科学院云南天文台机构知识库 |
مصطلحات موضوعية: | Saturated Dislocations Propagation-evolution, Molecular-micro-transient Scale Fracture Model, Flow Driven Pore-network Crack Model, First Principle, Ionic Fluid Transport-dehydration, Ultra High Temperature And Pressure, 地球科学::固体地球物理学, 理学, 理学::地球物理学, Engineering, Mechanics, Mechanical, FATIGUE-CRACK-INITIATION, WAVE-PROPAGATION, HIGH-TEMPERATURE, FREQUENCY RANGE, ELASTIC WAVES, MODEL, CONSOLIDATION, PERMEABILITY, DIFFRACTION, VELOCITY |
الوصف: | Based on the first principle and flow driven pore-network crack theory, the crystal size saturated dislocations transient (10−4–10−5 s) propagation–evolution in olivine structure under ultra high-coupled temperature (200–500 °C) and pressure (0.4–1 GPa) are studied on the parallel CPU&GPU platform. First, the molecular-micro-scale transient fracture model is established by using hybrid hypersingular integral equation and Lattice Boltzmann method, the hydrogen ion and oxonium ion transport–dehydration (HI–OI–TD) in olivine [(FeMg)SiO4] crystal are explored. The bond-strength–length as function of thermal-force–time fields, the limited thermal-force value for HI–OI–TD through the crystal, and the ion state water adsorption in the crystal are calculated, respectively. Then, based on the above results, the crystal size saturated dislocations/defects propagation–evolution is studied. The relationship between the stress distribution and micro-strain under different velocity–time conditions, the saturated dislocations/defects propagation–evolution as function of coupled thermal-force–time fields are obtained. All these findings can helpful understand the mechanism of the dehydration fracturing shale gas, the coal-gas outbursts, and the coseismic triggering issues. |
نوع الوثيقة: | article in journal/newspaper report |
اللغة: | English |
العلاقة: | Theoretical and Applied Fracture Mechanics; http://ir.ynao.ac.cn/handle/114a53/12322Test; https://www.sciencedirect.com/science/article/pii/S0167844212000031Test |
DOI: | 10.1016/j.tafmec.2012.02.002 |
الإتاحة: | https://doi.org/10.1016/j.tafmec.2012.02.002Test http://ir.ynao.ac.cn/handle/114a53/12322Test https://www.sciencedirect.com/science/article/pii/S0167844212000031Test |
رقم الانضمام: | edsbas.F70A13A7 |
قاعدة البيانات: | BASE |
DOI: | 10.1016/j.tafmec.2012.02.002 |
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