A THERMALLY-STABLE COLD SPRING ENVIRONMENT WITH A NEGATIVE GEOTHERMAL GRADIENT: ARBUCKLE-SIMPSON AQUIFER, SOUTHERN OKLAHOMA
This study integrates spring and well data to model thermal variability in the system from the surface to the center of the aquifer at 600 meters. It is supported by spring and well data on chemistry, flow and electrical properties. The thermal modeling has focused on two primary factors known to contribute to perturbations in temperature gradients: groundwater movement and paleoclimatic signatures. Inverse one-dimensional models of temperature measurements were used to compute groundwater movement. Forward modeling was also used to determine a plausible velocity range for groundwater in this area. Paleoclimatic signatures were investigated using a one-dimensional transient conductive heat transfer model. To address paleoclimatic signatures, a model was selected for its strengths in incorporating data collected and its relative flexibility in assessing the parameters used in the model. Results show flow velocities present at rates high enough to significantly disturb the temperature gradient of this area. Paleoclimatic results show a defined warming in the subsurface of 0.4 °C in the past sixty years. These results demonstrate strong groundwater movement and paleoclimatic effects can result in a thermally stable cold spring environment.