What the statewide pattern says
Deep aquifers protect; shallow farm ground shows
Alabama's higher nitrate is a shallow-aquifer story — the farmed limestone plateaus of the north and the sandy coastal aquifers of Baldwin County — while deep public-supply aquifers run clean.
The statewide baseline is protective. USGS sampling of the deep Coastal Plain aquifers that serve public supply — wells 250 to 2,000 feet deep — found nutrients were not present at high or even moderate concentrations anywhere in the study area (Barlow, 2016 — USGS Fact Sheet 2016-3076). Depth and confining clay do the work.
The shallow settings tell the other half. In the Interior Low Plateaus of north Alabama, where row crops have grown on limestone since the early 1800s, the Paleozoic carbonate aquifer carries a median nitrate of 1.3 mg/L — higher than every other Alabama aquifer's median — attributed to crop fertilization (USGS National Water Summary, Alabama). And in southern Baldwin County, study of the sandy coastal aquifers found the highest nitrate in the central and northeastern parts of the county, sourced primarily to agricultural inputs (Murgulet and Tick; see also KarimiDermani and others, 2025).
That split is the Alabama map: Baldwin County on the coast and a thin scatter through the northern farm counties — St. Clair, Madison, Monroe — mark the shallow, farmed, or karst-influenced ground, while the deep-aquifer cities stay quiet.
The supported source reading is agricultural nitrogen on shallow or karst ground — not a certified source at any individual system (Nolan and Hitt, 2006).