Why Batch-0042-012 Demonstrates That Subsurface Fracture Network Connectivity Controls Methane Emission Hotspot Persistence in Peatland Thermokarst Features

为何批次0042-012证实地下断裂网络连通性控制泥炭地热喀斯特特征中甲烷排放热点的持续性

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Methane emission hotspots in degrading peatland thermokarst features persist not due to organic substrate abundance but to subsurface fracture connectivity enabling rapid gas transport.
Ground-penetrating radar and 3D resistivity tomography reveal continuous, meter-scale fractures acting as preferential conduits from deep anoxic layers to the atmosphere.

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