What the statewide pattern says
Reservoirs for the cities, wells for the rest
Connecticut's modest nitrate signal sits in its stratified-drift river valleys — the setting its small groundwater systems and its large private-well population share.
Connecticut's big cities drink from upland reservoirs; that accounts for part of the small inventory here — about 60 public systems reporting groundwater nitrate, the smallest in this series — and the reach of the source records accounts for the rest. The mid-band systems that appear — Hartford, New Haven and Tolland counties — sit on stratified-drift valley aquifers under dense development.
The regional science sets the baseline: Connecticut lies inside the northern glacial aquifer system, whose private-well nitrate median runs about 0.11 mg/L — among the lowest measured nationally — but whose rare high wells concentrate where oxidizing shallow sand meets nitrogen sources (USGS SIR 2010-5100). USGS estimated high nitrate in about 4 percent of the glacial system's area (Erickson and others, 2019).
Connecticut has no county-level nitrate study this page can cite, so the reading stops at the setting: valley-fill sand and gravel under suburbs and legacy septic, with the state's several hundred thousand private bedrock and valley wells carrying the untested share.
The supported source reading is mixed suburban nitrogen on stratified-drift valley aquifers — not a certified source at any individual system (Nolan and Hitt, 2006).