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recharge to the cave drips. Despite there being large seasonal shifts in the isotopic composition of rain waters collected above the cave, the oxygen isotope composition for both drip sites have remained nearly equal and constant at –8.0 ± 0.1‰. This value is similar to the cool-season amount-weighted average of precipitation collected at the surface, and thus supports the hypothesis of a cool-season recharge bias to the drips.

Investigating Vadose Zone Hydrology in a Karst Terrain Through Hydrograph and Chemical Time-Series of Cave Drips at Grand Caverns, Virginia