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Abstract
Karst landscapes are known for their carbonate rock, unique hydrological features and susceptibility to rapid dissolution, contamination and unpredictable groundwater flow. In these regions surface water availability is limited, causing groundwater to be the primary source for drinking water and irrigation. This study focuses on understanding the dissolution of carbonate rock, surface-groundwater interactions and water quality within Tumbling Rock Cave, Alabama. This research utilizes a variety of analytical methods to characterize the carbonate rock and water quality within the cave, but also to understand the surface- groundwater interactions and make predictions about calcite dissolution. Results from this study aim to contribute to the elementary field of karst hydrology by predicting water avail- ability and quality, and to provide broader implications for managing these vital resources.