Investigation on the Impact Fracture Mechanism of Rock in Microgravity Environment Using the Continuum-Discontinuum Element Method

IF 1.8 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Qunlei Zhang, Jin Fang, Chun Feng, Mintao Jia, Pengda Cheng, Shuang Wang
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Abstract

In-depth analysis of asteroid samples will provide a key scientific basis for understanding its evolution history, resource utilization, and life origin. Obtaining rock samples from asteroids is getting more and more attention. However, successful sampling in asteroid is difficult due to extremely complex environmental conditions. In this paper, the dynamic processes of rock failure by sampling device are investigated by a continuum-discontinuum element method (CDEM) to instruct the rock sampling in asteroid. The deformation and failure of rock samples under different conditions (impact speeds, impact positions, rock cut-slot numbers, cut-slot spacings, cut-slot depths and cut-slot widths, etc.) are analyzed, and the relationships between the rock failure and hammer impact method are obtained. The results show that the cut-slot formed by grinding wheel increases the free surface of rock sample, which is beneficial to impact fracture and asteroid sampling. The relative distance between cut-slot free surface and impact position significantly affects the rock fracture under impact loading. The fracture degree of rock with single cut-slot is obviously smaller than that of rock with double cut-slots, the cut-slot scheme of double grinding wheels is more suitable for asteroid sampling. Under the impact loading, the rock fracture is negatively correlated with the cut-slot spacing formed by double grinding wheel cutting, the effective spacing of double cut-slots is 12 mm. The fracture unit number of rock varies nonlinearly with an increase of the depth from impact position, there is an optimal cut-slot depth corresponding to a certain impact velocity, and the rock crushing efficiency of asteroid sampling can be improved as the cut-slot depth matches the crack propagation depth.
利用连续-非连续单元法研究微重力环境下岩石的冲击断裂机理
对小行星样本的深入分析将为了解其演化历史、资源利用和生命起源提供重要的科学依据。从小行星上获取岩石样本正受到越来越多的关注。然而,由于环境条件极其复杂,在小行星上成功采样十分困难。本文采用连续-非连续单元法(CDEM)研究了取样装置破坏岩石的动态过程,以指导小行星岩石取样。分析了不同条件(冲击速度、冲击位置、岩石切槽数、切槽间距、切槽深度和切槽宽度等)下岩石样品的变形和破坏过程,并得出了岩石破坏与锤击法之间的关系。结果表明,砂轮形成的切槽增加了岩样的自由表面,有利于冲击破裂和小行星取样。切槽自由表面与冲击位置之间的相对距离对冲击载荷下的岩石断裂有显著影响。单切槽岩石的断裂程度明显小于双切槽岩石,双砂轮的切槽方案更适合小行星取样。在冲击载荷作用下,岩石断裂与双砂轮切割形成的切槽间距呈负相关,双切槽的有效间距为 12 mm。岩石的断裂单元数随距离撞击位置深度的增加而非线性变化,存在与一定撞击速度相对应的最佳切槽深度,当切槽深度与裂纹扩展深度相匹配时,小行星取样的岩石破碎效率可以提高。
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来源期刊
Lithosphere
Lithosphere GEOCHEMISTRY & GEOPHYSICS-GEOLOGY
CiteScore
3.80
自引率
16.70%
发文量
284
审稿时长
>12 weeks
期刊介绍: The open access journal will have an expanded scope covering research in all areas of earth, planetary, and environmental sciences, providing a unique publishing choice for authors in the geoscience community.
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