What the statewide pattern says
An irrigated-terrace pattern, and a slow fix
Nebraska's higher nitrate concentrates beneath irrigated cropland on the High Plains aquifer — the Central Platte above all — and even decades of mandatory groundwater rules have moved it only slowly.
Most of Nebraska draws from the High Plains (Ogallala) aquifer — well-drained sand and gravel, shallow in the river valleys, beneath some of the most intensively irrigated cropland in the country (Nolan and Hitt, 2006). The flagship hotspot is the Central Platte, where groundwater beneath irrigated terraces long averaged roughly 18 to 26 mg/L of nitrate — about double the federal limit — while bottomland nearby ran far lower: the geology showing through (Exner, Hirsh and Spalding, 2014).
Nebraska is also the state that tried to fix it with rules that bite. Its 23 locally elected Natural Resources Districts hold real regulatory authority over groundwater, and the Central Platte district imposed mandatory fertilizer-timing limits back in the 1980s. The honest lesson: even with teeth, improvement has been glacial — on the order of 0.14 to 0.26 mg/L a year — and much of the gain came from switching furrow irrigation to sprinklers, not from fertilizer rules alone. Decades-long travel times mean the ground answers slowly (Exner and others, 2014).
The supported source reading is agricultural — fertilizer on irrigated corn, delivered by irrigation recharge — not a certified source at any individual system. Statewide, the drivers split east and west: in the east, nitrate tracks sandy topsoil, well depth, and hydraulic conductivity; in the west, vadose-zone thickness and aquifer thickness. Nebraska's 2024 statewide private-well study — the largest in state history, about 3,500 wells — gives the private-well side its first full look (Nebraska DWEE, 2024).