An isotope dilution method to measure nitrification rates in the northern Gulf of Mexico and other eutrophic waters

An isotope dilution method is described to determine nitrification rates in the northern Gulf of Mexico (NGOMEX) and other eutrophic waters using high performance liquid chromatography (HPLC). A N 15 H 4 + isotope tracer method was not successful for NGOMEX waters due to excessive levels of unlabeled nitrogen (N) captured on sample filters. Nitrification rates were estimated by measuring the dilution of added N 15 O 3 − by N 14 O 2 − + N 14 O 3 − (= 14NO X ) generated from in situ N 14 H 4 + during sample incubations. NO X in pre- and post-incubation samples was reduced to NH 4 + with zinc (Zn) dust following sample acidification. Samples were analyzed by HPLC for NH 4 + concentration and atom% 15N composition. Results were corrected for background natural abundance NH 4 + concentrations measured in sub-samples collected before the reduction step. Nitrification rates were calculated using the difference between initial and final corrected NO X isotopic ratios and concentrations before and after the incubations. Laboratory experiments demonstrated that Zn reduction of NO X to NH 4 + averaged 102% (±0.2–0.8%) within 30 min. Different levels of N 14 O 3 − were added to sub-samples of coastal sea water containing a pool of added N 15 O 3 − to simulate a range of nitrification rates. Analysis of the resulting solutions produced a linear relationship ( R 2=0.9895; p