CONNECTING CONTAMINATION EVENTS TO THE SEDIMENT RECORD IN HIDDEN RIVER CAVE, KENTUCKY
This paper will explore current research taking place in Hidden River Cave to determine how water and sediment are being transported through the cave system. This further understanding of sediment transport is used to assess the impact of past contaminant input on the cave environment. Concentrations of selected contaminants were determined using water samples, sediment cores, and surface sediment samples collected in the cave. Water samples were tested for one or all of chromium (Cr(VI) and Cr(III)), aluminum, nickel and lead, with pH, water temperature, total dissolved solids and conductivity measured in situ. Sediment cores were analyzed using an Itrax core scanner to obtain elemental concentrations, radiography, and magnetic susceptibility data. Identification of distinct horizons of metal concentrations in sediment cores allows for sedimentation event correlation within the cave system. The chronology of sedimentation events was determined using Pb-210 analysis of core sediment and indicates a strong connection between historical contaminating events in the town of Horse Cave and cave sediment deposition. Sediment core analysis has thus allowed depositional patterns in the cave system to be determined and related to historic surficial processes. These findings can be applied to enhance understanding of the combined effects of landscape evolution and anthropogenic impacts which may be used to inform decision making processes for communities overlying both Hidden River Cave and other karstic cave systems.