What the statewide pattern says
Fractured rock, sprawl, and septic
North Carolina's signal is suburban rather than agricultural: Piedmont fractured-rock aquifers under dense development and on-site wastewater, with small community systems carrying the readings.
Wake County is the best-measured case. Reviewing 5,899 public-system samples, the county’s comprehensive groundwater investigation found nitrate at or above 3 mg/L — the level its analysts treat as indicating human impact — in 19.5 percent of samples, and identified septic-tank effluent as the impact source in affected areas, with fertilizer and land-applied wastewater solids as contributors (Wake County Comprehensive Groundwater Investigation).
The plumbing explains the pattern. The Piedmont’s fractured crystalline bedrock stores and moves water in cracks, so a contaminant can be confined to shallow fractures at one lot and, a few hundred feet away, ride connected fractures hundreds of feet down. USGS’s geochemistry work across the North Carolina Piedmont and Mountains documents exactly that behavior, with oxic shallow water carrying nitrate until depth and reducing conditions allow denitrification (USGS Scientific Investigations Report 2009-5149).
That is why the highlighted counties — Wake, Gaston, Iredell, Catawba, Guilford — are growth counties rather than row-crop counties: the readings come from subdivisions, mobile-home parks and small community wells sitting on fractured rock amid dense septic. Gaston’s strong showing has no county-specific published study this page can cite; the Piedmont-wide mechanism is what the literature supports.
The supported source reading is mixed suburban nitrogen — on-site wastewater first, lawn and legacy agricultural fertilizer behind it — on fractured-rock aquifers — not a certified source at any individual system. The setting fits the national vulnerability picture of nitrogen input on fast-pathway ground (Nolan and Hitt, 2006).