Table 2. Field observations of inorganic nitrogen, N2O and estimates of air-water fluxes in six pristine Australian mangrove creeks.
|
NOx Concentration (μM) |
NH4 concentration (μM) |
N2O concentration (nM) |
N2O saturation (%) |
Average atmospheric N2O fluxa (μmol m−2 d−1) | Weighted atmospheric N2O fluxb (μmol m−2 d−1) | N2O mass balancec (μmol m−2 d−1) | |||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Site | Latitude | Mean | Range | Mean | Range | Mean | Range | Mean | Range | Mean | Daily integrated | Daily integrated |
Darwin | −12.45 | 0.59 | <0.1–1.07 | 0.53 | <0.1–0.79 | 6.3 | 6.0–6.8 | 98.9 | 94.7–104.3 | −0.12 ± 0.01d> | −0.07d | −0.11 |
Hinchinbrook | −18.25 | 0.75 | 0.29–1.14 | 1.56 | <0.1–5.93 | 6.1 | 5.6–6.9 | 83.3 | 75.4–90.5 | −3.43 ± 0.06d | −3.26d | −3.20 |
Seventeen Seventy | −24.17 | 0.56 | <0.1–1.07 | 0.75 | 0.29–1.86 | 7.7 | 7.1–8.9 | 94.3 | 87.6–106.2 | −1.75 ± 0.11d | −0.48d | −0.35 |
Moreton Bay | −27.78 | ND | ND | ND | ND | 5.1 | 3.4–6.6 | 77.4 | 50.3–104.7 | −3.19 ± 0.08d | −1.52d | −2.61 |
Newcastle | −32.85 | 0.11 | <0.1–0.50 | 12.69 | 0.5–40.14 | 7.5 | 6.4–8.9 | 106.4 | 92.1–123.4 | 0.71 ± 0.03d | 0.69d | 0.03 |
Melbourne | −38.26 | 0.11 | <0.1–0.42 | 25.50 | <0.1–142.86 | 7.9 | 6.9–9.1 | 96.6 | 85.9–114.8 | −1.33 ± 0.07d | −0.12d | −0.08 |
Average | 0.42 | <0.1–1.14 | 8.20 | <0.1–142.86 | 6.8 | 3.4–9.1 | 92.9 | 50.3–123.4 | −1.52 ± 0.17 | −0.79 ± 0.57 | −1.05 ± 0.59 |
aPer m2 water area, ±95% confidence interval bweighted for changes in water area and flux rates over the study period and normalised to total catchment area, ccalculated as a function of discharge and dissolved N2O concentration integrated at 1 minute intervals, normalised to catchment area, dFlux rates determined using empirical transfer velocity equation of Ho et al.33.