Research on dynamic damage path of multi-layered combined coal mass under impact load

IF 4.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Physics and Chemistry of the Earth Pub Date : 2025-06-01 Epub Date: 2025-01-28 DOI:10.1016/j.pce.2025.103872
Feng Li, Chenchen Wang, Bo Xu, Dongdong Liang, Zeyu Li, Tianyi Zhang, Bincan Tian
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Abstract

In this paper, similar materials are used to prepare the multi-layered composited coal mass. Through drop hammer impact multi-layered combined coal mass test, it's found that each layer appears multiple radial cracks, local coal layer appears circumferential cracks to generate petal-shaped fragments. The number of radial and circumferential cracks and petal-like fragments first increases and then decreases with layers increase. Combining the dynamic strain response characteristics, the first layer radial plane produces compression wave in radial direction and tension wave in circumferential direction due to the loading wave. And then, the unloading wave leads to the tension wave in the radial direction and compression wave in the circumferential direction. The impact load propagates as spherical wave within the coal mass, resulting in compressive strains along the axial direction and tensile strains of the coal mass lateral face. Combined with the failure characteristics and dynamic strain response characteristics, it's clear that the radial cracks first appear in each layer, the process of unloading wave meets with plastic loading wave results in tensile stress wave in some layers to form circumferential cracks. The energy attenuation of stress waves affects the number of circumferential cracks and petal-like fragments. In the axial direction, the coal mass forms dense nuclei and undergoes splitting. The radial and circumferential cracks in the radial plane intersect with the boundary to form axial cracks, finally forming the lateral face axial failure mode with less axial cracks in the top and bottom layers, more axial cracks in the middle layers.
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冲击载荷作用下多层复合煤体动态损伤路径研究
本文采用类似材料制备多层复合煤体。通过落锤冲击多层组合煤体试验,发现每层出现多个径向裂纹,局部煤层出现周向裂纹,产生花瓣状破片。径向、周向裂纹和花瓣状碎块的数量随层数的增加先增加后减少。结合动应变响应特性,第一层径向面在加载波作用下产生径向压缩波和周向张力波。然后,卸荷波导致径向上的张力波和周向上的压缩波。冲击载荷在煤体内部以球波形式传播,产生沿轴向的压缩应变和煤体侧向面的拉伸应变。结合破坏特征和动应变响应特征可知,各层首先出现径向裂纹,卸荷波与塑性加载波相遇的过程中,部分层产生拉应力波,形成周向裂纹。应力波的能量衰减影响环向裂纹和花瓣状碎块的数量。在轴向上,煤体形成致密核并发生分裂。径向面径向裂纹和周向裂纹与边界相交形成轴向裂纹,最终形成上下两层轴向裂纹较少,中间层轴向裂纹较多的侧向面轴向破坏模式。
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来源期刊
Physics and Chemistry of the Earth
Physics and Chemistry of the Earth 地学-地球科学综合
CiteScore
5.40
自引率
2.70%
发文量
176
审稿时长
31.6 weeks
期刊介绍: Physics and Chemistry of the Earth is an international interdisciplinary journal for the rapid publication of collections of refereed communications in separate thematic issues, either stemming from scientific meetings, or, especially compiled for the occasion. There is no restriction on the length of articles published in the journal. Physics and Chemistry of the Earth incorporates the separate Parts A, B and C which existed until the end of 2001. Please note: the Editors are unable to consider submissions that are not invited or linked to a thematic issue. Please do not submit unsolicited papers. The journal covers the following subject areas: -Solid Earth and Geodesy: (geology, geochemistry, tectonophysics, seismology, volcanology, palaeomagnetism and rock magnetism, electromagnetism and potential fields, marine and environmental geosciences as well as geodesy). -Hydrology, Oceans and Atmosphere: (hydrology and water resources research, engineering and management, oceanography and oceanic chemistry, shelf, sea, lake and river sciences, meteorology and atmospheric sciences incl. chemistry as well as climatology and glaciology). -Solar-Terrestrial and Planetary Science: (solar, heliospheric and solar-planetary sciences, geology, geophysics and atmospheric sciences of planets, satellites and small bodies as well as cosmochemistry and exobiology).
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