What the statewide pattern says
Sugar-beet irrigation on fast soils
Wyoming's higher nitrate is a North Platte valley story: decades of irrigated farming on highly permeable soils above a shallow alluvial aquifer that also supplies the valley towns.
Goshen County is Wyoming's most concentrated farming ground, and its nitrate problem is documented in unusual detail. The valley towns — Torrington, Lingle, Fort Laramie — draw drinking water from the North Platte alluvial aquifer, the same shallow aquifer that sits under the irrigated fields. USDA analyses rate the valley's predominant soils as high-leaching (permeability above 6 inches per hour), and University of Wyoming work has tracked nitrate in the aquifer for decades (University of Wyoming Water Resources Center).
The mechanism is partly geological bad luck. A University of Wyoming wellhead study for Torrington found that Brule Formation bedrock outcrops act as underground dams: nitrate from intensively farmed terrace land stagnates behind them, then spills through breaches straight into the floodplain aquifer that feeds the municipal wellfield. A citizen-monitoring network across the county measured nitrate up to 53.6 mg/L — more than five times the federal limit — in wells just outside the river floodplain, with concentrations peaking during the growing season (Reddy and Goertler, 1998).
The rest of the state runs low: Wyoming's map is one farm valley plus a thin scatter, including Teton County, where the signal is growth and septic on alluvial ground rather than row crops. About three-quarters of Wyoming's population drinks groundwater, so the valley's alluvial setting matters beyond the towns (Wyoming Water Resources Center).
The supported source reading is irrigated row-crop nitrogen — corn and sugar beets — on high-leaching soils over the alluvial aquifer — not a certified source at any individual system. The valley fits the national pattern of nitrate risk where heavy nitrogen input meets fast infiltration (Nolan and Hitt, 2006).