What the statewide pattern says
Irrigated red-bed country
Western Oklahoma’s Permian sandstone and alluvial aquifers sit under irrigated agriculture, and state investigations have measured nitrate above the federal limit there for decades — the public-system map shows it county by county.
The western aquifers are working irrigation water. In the Rush Springs aquifer — red Permian sandstone beneath Caddo, Custer, Washita and neighboring counties — 91 percent of groundwater use is irrigation, and the state water board’s investigation found 13 of its samples above the 10 mg/L federal nitrate limit, a mean of 6.6 mg/L, and a maximum of 59.2 mg/L, with inorganic fertilizer identified as the major contributor (Oklahoma Water Resources Board, 2015).
It is not new. An earlier USGS study of the same aquifer reported a mean nitrate of 14.3 mg/L — above the federal limit as an average — and 28–31 mg/L in wells near a wastewater lagoon, traced to commercial fertilizer (Becker and Runkle, 1998). The aquifer recharges from rainfall through sandy soils, so what is spread on fields reaches the water table.
The public-system map on this page runs beyond the studied block: Garfield County (Enid) and its neighbors sit on terrace and alluvial aquifers over the same Permian red beds, and their systems report high at rates that match the Rush Springs picture. The published investigations cover the Rush Springs block directly; for the counties farther north and west this page reads the public-system data as the signal and the red-bed irrigation setting as the supported mechanism, not a certified per-county source.
The supported source reading is fertilizer nitrogen on irrigated red-bed and alluvial aquifers — not a certified source at any individual system, and the strongest regional pattern in this batch of states (Nolan and Hitt, 2006).