UNDERSTANDING TIDAL EFFECTS ON THE BIG PINE KEY FRESHWATER LENS WITH TIME-LAPSE ERT
Using electrical resistivity tomography (ERT), hourly measurements were taken over a 12-hour period on a 54-m-long profile, extending inland from the shoreline to monitor the tidally driven changes at the edge of the lens. Measurements of water level, temperature, and conductivity were made throughout the day in shallow wells adjacent to the profile. The experiment was conducted on two separate days, in July 2011 and in May 2012. Both surveys were conducted over the same time in the tidal cycle. ERT data were modeled using a time-lapse inversion scheme. For July 2011, the resistivity models show an abrupt movement of fresh water towards the shore over the period of an hour as the tide level decreased. In contrast, the May 2012 profile showed little change. The different results may be due to variations in groundwater level and precipitation. The water level observed in the wells in May 2012 was higher than the water level observed in July 2011. In addition, there was twice as much rain in the two months prior to the May survey compared to the survey in July. The results suggest that the tide has a larger influence on the saltwater/freshwater mixing at the edge of the lens under drier conditions.