Abstract

Three nitrogen species in air, HNO3, particle nitrate (pNO3−), and particle ammonium (pNH4+), have been routinely measured for estimating nitrogen dry deposition in the Canadian Air and Precipitation Monitoring Network (CAPMoN) and the U.S. Clean Air Status and Trends Network (CASNET) for several decades. To investigate the relative contributions of other nitrogen species to total nitrogen dry and dry + wet deposition, 14 short‐term field campaigns were conducted between 2001 and 2005 at eight selected rural sites across eastern Canada. Air concentrations were measured for the total oxidized nitrogen (NOy) and major species comprising NOy (NO, NO2, PAN, PPN, HNO3, pNO3−), and for the two reduced nitrogen species (NH3, pNH4+). Dry deposition fluxes of NOy and NHx (= NH3 + pNH4+) were then estimated by combining measured concentrations of individual nitrogen species with their respective dry deposition velocities estimated from big‐leaf models using on‐site meteorological measurements. Nitrogen dry deposition were estimated to be 0.8–4.0 kg N ha−1 a−1, depending on location, with 60–75% from NOy and 25–40% from NHx. HNO3 and NO2 dominated NOy dry deposition while NH3 and pNH4+ contributed equally to NHx dry deposition. The pNO3−, PAN, and unidentified NOy species also contributed appreciable amounts to NOy dry deposition. Nitrogen dry + wet deposition from NOy + NHx was estimated at 4.3–11 kg N ha−1 a−1, with dry deposition accounting for 10–50%. The routinely monitored species accounted for less than 50% of total N dry deposition; thus, total dry + wet deposition from the Canadian monitoring network had a lower bias by 5–25% at most of the sites.

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