The Arbuckle-Simpson aquifer is located in central southern Oklahoma and covers nearly 520 square miles (OWRB, Groundwater Studies, 2019). This area can be seen in Figure 1 and is composed of the following counties: Carter, Coal, Johnston, Murray, and Pontotoc. These counties combined make up a total population of nearly 117,000 people (United States Census Bureau, 2018).
The climate of southern Oklahoma is most comparable to a humid, subtropical climate with temperatures ranging between thirty to ninety degrees (US Climate Climate Data, 2020). The change in temperature and precipitation over the year is shown in Figure 2. The area averages 38 inches of rain annually. The Arbuckle-Simpson aquifer is considered an extremely sensitive water resource as there are no rivers or streams that flow into the aquifer, making precipitation the only significant form of recharge (Osborn, Arbuckle Simpson Hydrology Study Final Report to the U.S. Bureau of Reclamation, 2009).
The Arbuckle-Simpson aquifer discharges to a variety of different streams and creeks, as seen in Figure 6. The largest amounts of water are discharged to Blue River (Figure 3), Byrd Mills Spring, Delaware Creek, Mill Creek, Pennington Creek (Figure 4), Sheep Creek, Honey Creek (Figure 5), Travertine Creek, and Rock Creek (Osborn, Arbuckle Simpson Hydrology Study Final Report to the U.S. Bureau of Reclamation, 2009).