Evolutionary characteristics of RA and AF in sandstone under different numbers of freeze-thaw cycles. (a, b, c, d, and e represent N = 0, 20, 40, 60, and 80, respectively.).

Evolutionary characteristics of RA and AF in sandstone under different numbers of freeze-thaw cycles. (a, b, c, d, and e represent N = 0, 20, 40, 60, and 80, respectively.).

<p>Evolutionary characteristics of RA and AF in sandstone under different numbers of freeze-thaw cycles. (a, b, c, d, and e represent N = 0, 20, 40, 60, and 80, respectively.).</p>

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Bibliographic Details
Main Author:	Yanan Sun (316649) (author)
Other Authors:	Bing Liang (3475652) (author), Junzu Ma (15333057) (author), Jiaxu Jin (15333060) (author), Daoliang Liu (22075997) (author)
Published:	2025
Subjects:	Biophysics Cell Biology Molecular Biology Physiology Biotechnology Evolutionary Biology Geology Ecology Physical Sciences not elsewhere classified longitudinal wave velocity force chain fields cold region engineering b value shows acoustic emission tests thaw cycling conditions xlink "> freeze thaw erosion conditions continuous accumulation trend thaw erosion thaw cycles continuous process rock specimens rock samples rock mass results show peak strength particles lead numerical simulations microcracks inside microcrack types macroscopic fracture macroscopic cracking large number inhomogeneous variations increasing number increasing degree high degree fracture extension different modes different forms cracking pattern common hazard af indicates
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