“…Although DIN is expected to constitute a greater proportion of TDN in areas with long-term high atmospheric inorganic N deposition (Allott et al, 1995), the relative importance of organic N accumulation in peat-dominated ecosystems may vary along a deposition gradient, depending on direct biomass uptake of atmospheric N, and the rate of litter decomposition (Yesmin et al, 1995). Over a period of time, high atmospheric inorganic N deposition may alter the soil microbial processing of organic matter (OM) and/or the availability of organic substrates that lead to DON/dissolved organic carbon (DOC) formation, resulting in marked losses of DON/DOC to the fluvial environment (Pregitzer et al, 2004), especially under storm conditions (Clark et al, 2007;Inamdar and Mitchell, 2007).…”