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Study on dynamic response characteristics of impact of freeze-thaw saturated marble in plateau area

To study the effects that the perennial freeze–thaw environment exerts on the dynamic mechanical properties of marble, which characterizes the Qinghai-Tibet Plateau, impact tests were conducted, and saturated marble was utilized; thus, we analyzed the effect of different loading rates on its dynamic...

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Detalles Bibliográficos
Autores principales: Huang, Wuhu, Yin, Jiandong, Li, Xianglong, Hou, Defeng, Wang, Jianguo, Zhang, Zhiping, Zuo, Ting, Jian, Ximing, Li, Wendong, Yang, Yang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10490945/
https://www.ncbi.nlm.nih.gov/pubmed/37683026
http://dx.doi.org/10.1371/journal.pone.0290628
Descripción
Sumario:To study the effects that the perennial freeze–thaw environment exerts on the dynamic mechanical properties of marble, which characterizes the Qinghai-Tibet Plateau, impact tests were conducted, and saturated marble was utilized; thus, we analyzed the effect of different loading rates on its dynamic compressive strength, fragmentation pattern, and energy-absorbing density. The results indicate the following: (1) When 42.02s(-1) ≤[Image: see text] ≤ 49.20s(-1), the degree of fragmentation and the fractal dimension of saturated state marble is greater than that of the dry state marble; when [Image: see text] <42.02s(-1) or [Image: see text] >49.20s-(1), the dry state marble exhibits greater fragmentation than the saturated marble; (2) When the saturated state marble is subjected to a specific fractal dimension, the energy-absorbing density of the marble that characterizes the saturated state is great compared with the dry state, and when the fractal dimension increases, the energy-absorbing densities that characterize the two states gradually converge. (3) The effect of water on the mechanical properties of marble has an obvious rate dependence, showing a weakening effect at low strain rates and a strengthening effect at high strain rates. In regard to the analysis pertaining to the dynamic fracture mechanism of marble under the influence of the freeze-thaw environment that characterizes the plateau, the aforementioned experimental results exhibit considerable significance.