The water that flows from the Arbuckle-Simpson aquifer contains mainly calcium, magnesium, and bicarbonate (Christenson, S., Hunt, A.G., and Parkhurst, D.L., 2009). These elements can be contributed to the limestone and dolomite that make up the aquifer. While contaminants are not present in the majority of discharged water, certain wells have produced high levels of nitrate and and chloride that exceeded regulations for drinking water set forth by the EPA (OWRB, Geochemistry of the Arbuckle-Simpson Aquifer, 2009).
There are several activities throughout southern Oklahoma that could threaten the use of the Arbuckle-Simpson aquifer as a public drinking water supply. The two major activities that threaten the aquifer are mining activity and oil activity, as seen in Figures 14 and 15.
Limestone makes up a large portion of the Arbuckle-Simpson aquifer. Limestone is also mined to make building materials and other products. Mining can lead to metal contaminants polluting the water system.
There is a large amount of oil activity in southern Oklahoma. Many of the pipelines located in the area travel through creeks that flow from the aquifer. Oil spills from these pipelines would contaminate possible drinking water.
Fracking injects a large amount of water when preparing a new well. This water is typically locally sourced and is filled with drilling fluid and sand. The water must be disposed of once it is used. A possible fracking water spill could lead to contaminants entering the water system.