Why Batch-0042-048 Establishes That Subsurface Thermal Inertia Controls Diurnal Groundwater Recharge Timing in Fractured Crystalline Bedrock Aquifers

为何批次0042-048确立了地下热惯性对裂隙结晶基岩含水层日尺度地下水补给时序的控制作用

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Batch-0042-048 combines fiber-optic distributed temperature sensing (DTS) with high-frequency piezometric logging across three granitic aquifer systems in southern India.
Thermal lag between surface temperature oscillations and subsurface thermal wave propagation governs the phase shift of recharge pulses relative to rainfall events.

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