What the statewide pattern says
Tile drains protect the middle; the edges answer
Illinois' elevated systems concentrate along the Mississippi River corridor — Madison, St. Clair, Adams, Hancock, Henderson counties — and in scattered shallow sand-and-gravel and thin-cover settings, while the deep Mahomet aquifer that supplies much of east-central Illinois runs below detection.
Illinois' 154 mapped systems above the natural-background band form two visible corridors: the Mississippi River edge from Adams and Hancock through Madison and St. Clair — the American Bottoms — and a scatter of shallow-aquifer counties across the interior, led by McLean, Peoria, Winnebago and Vermilion. More than 1.1 million people are served by Illinois systems at or above 1.00 mg/L.
The state's defining mechanism is artificial drainage. Most Illinois farmland is tile-drained, and tile short-circuits infiltrating water to streams instead of letting it soak to the water table — a major reason nitrate rarely reaches deep aquifers under the corn belt (USGS Lower Illinois River Basin NAWQA). The same study drew the depth line: all 30 deep Mahomet aquifer samples ran below 0.10 mg/L, while 7 percent of shallow wells exceeded the federal limit, at 11 to 77 mg/L, every one of them less than 50 feet deep.
The deep Mahomet's protection is physical, not chemical: thick clay-rich till separates it from the surface, and age-dating near Clinton found recharge older than 1953 even in shallow permeable units above the aquifer (USGS SIR 2015-5159). Where that till is thin or the sand and gravel reaches the surface — the Mississippi bluffs, the Havana Lowlands, the Kankakee sands — the shield drops. The Illinois State Water Survey names the sources directly: nitrate from fertilizers and septic systems, tracked in shallow-aquifer studies across Kane, Lake and Will counties (ISWS Water Resource Systems).
The supported source reading is row-crop and septic nitrogen on shallow sand and gravel where tile drainage cannot intercept it — not a certified source at any individual system (Nolan and Hitt, 2006).