• The undulation degree of rock tensile fracture surfaces is critically influenced by the initial fracture angle, with a threshold at 45° separating high and low undulation intervals.
• Quantitative indices for relative undulation degree, undulation frequency, and matching degree were developed to characterize fracture surface morphology.
• A direct relationship was established between fracture surface undulation changes and gas flow guidance, enabling quantitative characterization of gas flow stability, tortuosity, and uniformity.
• Numerical models validated the proposed indices, confirming their utility in predicting gas flow patterns in fractured rock strata.
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