• Liquid water is a critical factor in reducing the brittleness of schist under cyclic environmental actions.
• The attenuation function model accurately predicts peak stress and elastic modulus degradation (R2 > 0.97).
• Freeze-thaw cycles in water (FTW) cause the most severe deterioration, with the shortest half-life for strength (28 cycles) and wave velocity (208 cycles).
• Damage variables for compressive strength and elastic modulus increase with cycle number, with FTW showing the highest damage after 40 cycles.
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