深部岩石における熱・水・力学連成下の動的損傷特性とエネルギー散逸に関するマルチスケール研究
Qi Ping1,2, Bobo Zhang3,4
1School of Civil Engineering and Architecture, Anhui University of Science and Technology, Huainan, 232001, Anhui, China.
Scientific reports
|January 26, 2026
まとめ
深部地盤工学では、熱・水・力学(THM)連成と採掘により、岩盤破砕のリスクに直面する。本研究は、THM要因が岩盤破壊モードにどのように影響するかを明らかにし、検証済みの微小亀裂伝播モデルを導入する。
科学分野:
- 土木工学
- 岩盤力学
- マルチフィジックス工学
背景:
- 深部地盤工学における掘削は、岩盤破砕災害を受けやすい。
- THM連成と採掘の擾乱は、これらのリスクを著しく増大させる。
結論:
- THM連成は、岩盤の破壊モードと微細構造特性を著しく変化させる。
- 開発された力学モデルは、THMおよび衝撃荷重下での微小亀裂の発生を正確に予測する。
- 本研究結果は、深部地盤工学における岩盤破砕リスクを軽減するための重要な洞察を提供する。
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