From: N2O emission and its influencing factors in subtropical streams, China
Sampling season | River | Sampling area | Temp (°C) | w-NO3− (mg L− 1) | w-NH4+ (mg L− 1) | DOC (mg L− 1) | DOC/NO3− |
---|---|---|---|---|---|---|---|
High flow season | Jinshui River | Downstream | 28.72 ± 0.51a | 0.94 ± 0.30 | 0.78 ± 0.19 | 7.67 ± 1.06b | 9.10 ± 4.49 |
Midstream | 25.23 ± 4.71a | 1.03 ± 0.23 | 0.71 ± 0.11 | 8.63 ± 0.59a | 10.45 ± 2.21 | ||
Upstream | 16.04 ± 0.53b | 1.15 ± 0.07 | 0.56 ± 0.03 | 10.61 ± 2.17a | 11.32 ± 1.57 | ||
Qi River | Downstream | 32.07 ± 0.97a | 1.44 ± 0.33 | 0.67 ± 0.19 | 7.12 ± 1.58 | 8.69 ± 2.55 | |
Midstream | 29.78 ± 1.05ab | 1.09 ± 0.12 | 0.49 ± 0.05 | 7.45 ± 0.60 | 8.57 ± 1.18 | ||
Upstream | 23.92 ± 5.58b | 1.68 ± 0.52 | 0.67 ± 0.42 | 8.84 ± 0.76 | 7.66 ± 1.57 | ||
Normal flow season | Jinshui River | Downstream | 8.73 ± 0.32a | 1.23 ± 1.12 | 0.04 ± 0.00 | 7.49 ± 2.28a | 10.08 ± 7.30 |
Midstream | 7.58 ± 0.78b | 0.60 ± 0.11 | 0.04 ± 0.01 | 5.02 ± 0.20ab | 12.83 ± 1.91 | ||
Upstream | 4.77 ± 0.42c | 0.91 ± 0.08 | 0.04 ± 0.00 | 4.60 ± 0.48b | 11.88 ± 0.54 | ||
Qi River | Downstream | 12.13 ± 1.37a | 0.86 ± 0.38 | 0.04 ± 0.01 | 14.04 ± 4.34a | 8.55 ± 16.95 | |
Midstream | 10.73 ± 0.50ab | 1.28 ± 0.32 | 0.04 ± 0.01 | 9.84 ± 1.39ab | 6.86 ± 2.77 | ||
Upstream | 8.47 ± 1.99b | 1.29 ± 0.72 | 0.04 ± 0.01 | 6.57 ± 0.55b | 5.69 ± 2.38 | ||
Low flow season | Jinshui River | Downstream | 10.43 ± 0.64a | 0.50 ± 0.01c | 0.38 ± 0.02 | 12.35 ± 0.54a | 24.63 ± 0.84a |
Midstream | 7.66 ± 1.23b | 0.59 ± 0.02b | 0.32 ± 0.03 | 8.08 ± 0.62b | 21.47 ± 1.61b | ||
Upstream | 4.34 ± 0.08c | 0.91 ± 0.04a | 0.47 ± 0.14 | 6.44 ± 0.07c | 17.52 ± 0.29c | ||
Qi River | Downstream | 9.87 ± 0.38 | 0.56 ± 0.26b | 0.39 ± 0.09 | 26.28 ± 4.15a | 13.76 ± 46.82 | |
Midstream | 9.79 ± 2.18 | 1.13 ± 0.18a | 0.39 ± 0.02 | 20.81 ± 2.41ab | 10.92 ± 1.51 | ||
Upstream | 8.87 ± 1.88 | 0.84 ± 0.23a | 0.42 ± 0.01 | 15.77 ± 1.17b | 8.94 ± 5.35 |