Batch-0022-013: Karst Hydrological Partitioning and Subsurface Flow Path Heterogeneity
喀斯特水文分区与地下水流路径异质性
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In limestone terrains, rainwater splits instantly between rapid conduit flow and slow matrix seepage.
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Dye-tracing experiments prove some sinkholes feed springs 15 km away within hours, while others recharge local aquifers over decades.
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