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Abstract: Radon-222 (222Rn) and ammonium (NH4 +) were measured in interstitial water of the Neuse River Estuary (NRE), North Carolina, USA to determine the advective flux of NH4 + from sediments to the overlying water column. Porewater samples were collected over an annual cycle from multi-level piezometers installed in nearshore sites. NH4 + concentrations in sandy environments of the NRE were 10-fold higher than concentrations in the overlying water column. Shallow porewaters exhibited seasonal variations in NH4 + concentrations, which resulted in temporal changes in NH4 + flux from the sediment. Submarine groundwater discharge (SGD) was measured indirectly by using 222Rn as a tracer and directly via seepage meters. Discharge rates were variable depending upon the sampling location and season. The mean SGD was 9.1±1.5cmd−1 with a maximum SGD during spring at a rate of 13.6cmd−1 based on 222Rn porewater distribution. High porewater NH4 + concentrations in sandy nearshore sediments contributed NH4 + to the overlying water via groundwater discharge as an advective process. The overall mean NH4 + flux was 11.2±2.0mmolNH4 + m−2 d−1. Seasonal trends in groundwater seepage rates and NH4 + concentration suggest that groundwater is an important mechanism advecting nutrients from porewaters to surface waters, which is comparable to riverine NH4 + discharge. SGD N:P ratios (NH4 + as N) were >16:1, indicating that SGD is an important contributor of inorganic N for phytoplankton growth and may influence the NRE toward a less N-limited system. The data from this study will advance current understanding about the role of NH4 + in the progressive eutrophication of shallow estuarine ecosystems. [Copyright &y& Elsevier]