What the statewide pattern says
Urban nitrogen, septic growth, and nitrate the desert stored away
Nevada's elevated systems sit in its populated basin-fill valleys — Las Vegas, Carson and Truckee — where USGS has documented shallow-aquifer nitrate from lawns, effluent, sewers and septic tanks, plus a natural reserve of desert-soil nitrate that irrigation can flush downward.
Nevada's reporting inventory is small — about 50 systems, a quarter of the state's — but one in five of those reports nitrate at or above 3.00 mg/L; whether the unreported three-quarters would hold that share, these records cannot say. The map covers Clark (Las Vegas), Douglas (Carson Valley), Washoe (Reno–Sparks), Elko and White Pine counties; the county file attributes only part of the inventory, and the coverage note beside the map says so.
Las Vegas Valley is the best-documented case. USGS found a median of 4.6 mg/L in 32 shallow monitoring wells, with 12 percent of samples above the 10 mg/L federal limit; an earlier valley study averaged 13 mg/L in wells under 100 feet deep against 3.2 mg/L in deeper ones. Sources named: lawn fertilizer, irrigation with treated effluent, leaking sewers and septic systems — and naturally occurring nitrate accumulated over thousands of years in desert soils, which excess irrigation can flush to the water table (USGS Professional Paper 1781). Deep public-supply wells in the valley mediate the risk: their median runs 0.65 mg/L.
Carson Valley in Douglas County shows the trend line. A 16-year USGS study found nitrate rising in 56 percent of long-term monitoring wells, with the highest values directly under dense septic-tank parcels — not under farmland — and groundwater ages of 30 to 40 years meaning the trend persists for decades (USGS WRIR 03-4152). Modeling projected concentrations would keep climbing toward the MCL in septic-dense subdivisions (USGS SIR 2013-5136), and a 2024 update found significant increases in 9 of 14 wells, with Johnson Lane and Gardnerville Ranchos samples having exceeded the MCL (USGS OFR 2024-1045).
The supported source reading is urban and septic nitrogen on basin-fill aquifers, with natural desert-soil nitrate contributing — not a certified source at any individual system (Nolan and Hitt, 2006).