What the statewide pattern says
A tile-drainage pattern, with a karst edge
Iowa's higher nitrate is an agricultural pattern with two pathways: buried tile drains that send it to the rivers, and a karst northeast that sends it straight underground.
Iowa is some of the most intensively farmed ground on earth, and its defining nitrate pathway is the buried tile drain. Tile drainage turned wet prairie into cropland, but it also flushes water and nitrate to the rivers in days — which is why north-central Iowa's cities, drawing from tile-fed rivers, fight nitrate in summer even where nearby wells run low (Dubrovsky and others, 2010).
The second setting is the far northeast: the Paleozoic Plateau, Iowa's share of the Driftless karst, where sinkholes and fractured carbonate give surface nitrogen near-direct access to groundwater. Statewide, the national vulnerability work associates high nitrate with exactly this combination — heavy nitrogen input on permeable or fast-pathway ground (Nolan and Hitt, 2006).
What the public-system map cannot show is the private-well picture, and in Iowa it is studied better than almost anywhere. A USGS–National Cancer Institute model of 34,084 Iowa private wells found well depth dominates risk: mean nitrate runs about 7.7 mg/L in wells shallower than 50 feet versus about 1.0 mg/L below 500 feet, with sinkhole proximity and soil permeability behind depth (Wheeler and others, 2015).
The supported source reading is agricultural — row-crop nitrogen on drained or karst ground — not a certified source at any individual system. Iowa sits at the center of the Corn Belt nitrogen yields that the Mississippi-basin SPARROW model ranks highest in the nation (Robertson and Saad, 2021). And the ground holds decades of old nitrogen, so change arrives slowly, in years rather than seasons.