“…Long water residence time may facilitate N removal capacity through denitrification while denitrification effectiveness may decline in hyper-N rich rivers (Chen et al, 2014;Mulholland et al, 2008;Seitzinger et al, 2006;Seitzinger et al, 2002). Direct measurement of excess dissolved N 2 (ΔN 2 , denitrification product) and estimation of area-weighted N 2 emission flux in the Jiulong River network during 2010-2011 suggest that gaseous N removal accounts for 25% (North River) and 21% (West River) of riverine N export (Chen et al, 2014). However, considering the short water residence time and shallow water depth compared to larger rivers, we set L N to 0.25 in the North River and 0.…”