Inferring groundwater flow and recharge from time series analysis of storm responses in a karst aquifer of southeastern Kentucky (USA) | Déduction de l'écoulement des eaux souterraines et de la recharge à partir de l’analyse des séries chronologiques des réponses aux orages dans un aquifère karstique du sud-est du Kentucky (USA) Inferencia del flujo de agua subterránea y la recarga a partir del análisis de series de tiempo de las respuestas de tormentas en un acuífero kárstico del sudeste de Kentucky (EE. UU.) 通过对(美国)肯塔基州东南部一岩溶含水层暴雨响应的时间序列分析推断地下水流和补给 Determinação do fluxo e recarga das águas subterrâneas a partir da análise de series históricas de tempestades em um aquífero cárstico no sudeste de Kentucky (EUA)
2018
Tagne, G. V. | Dowling, C.
Epigenic karst systems exhibit strong connectivity to surface recharge. In land use dominated by extensive agriculture and farming, epigenic karst aquifers are highly vulnerable to surface contaminants from point and nonpoint sources. Currently, the karstic landscapes of the southeastern Kentucky platform (USA) are impacted by agriculture and the rapid proliferation of concentrated-animal-feeding operations. Analysis of karst aquifer responses to storm events provides qualitative information regarding aquifer–recharge flow paths and groundwater residence time, and knowledge of spatial and temporal variations in recharge and flow is crucial to the understanding of the fate of surface contaminants. Time-series correlation analyses on long-term physicochemical data recorded at the outlet of Grayson Gunnar Cave, an epigenic karst system located along the Cumberland escarpment in southeastern Kentucky, revealed the existence of two separate conduit branches responding 4–8 h apart from each other. Recorded storm response times range from 4 h for flushing and dilution to 7 h for recovery. An estimated 6 million L of stored groundwater is discharged from both branches during major storms, and the fastest responding branch accounts for the majority (80%) of the groundwater reserve being discharged through the spring. As evidenced by groundwater residence time (7 days), recharge is likely characterized by localized infiltration of rain water from subsurface sinkholes to the conduit branches with no contribution of regional or lateral groundwater flow.
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