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热喀斯特指地表因地下冰融化而造成的地面下沉和滑塌过程，[1]多发生在北极、青藏高原等多年冻土区。热喀斯特是多年冻土退化的表征之一，会影响工程建筑，破坏地表植被，导致生态系统退化，改变土壤的水文和碳氮循环过程等。[2]
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