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the late dry season and higher concentrations and variability during the wet season |
peaking in September or October (Fig 3.12). Also, there is a noticeable increase in |
June, which is the first rainy month after the dry season. |
0 |
.01 |
.02 |
.03 |
.04 |
.05 |
.06 |
.07 |
.08 NO3 |
1 2 3 4 5 6 7 8 9 10 11 12 |
0 |
.02 |
.04 |
.06 |
.08 |
.1 |
.12 |
.14 NO3 |
1 2 3 4 5 6 7 8 9 10 11 12 |
0 |
.01 |
.02 |
.03 |
.04 |
.05 |
.06 NO3 |
1 2 3 4 5 6 7 8 9 10 11 12 |
0 |
.02 |
.04 |
.06 |
.08 |
.1 |
.12 NO3 |
1 2 3 4 5 6 7 8 9 10 11 12 |
0 |
.1 |
.2 |
.3 |
.4 |
.5 |
.6 NO3 |
1 2 3 4 5 6 7 8 9 10 11 12 |
0 |
.05 |
.1 |
.15 |
.2 |
.25 |
.3 |
.35 NO3 |
1 2 3 4 5 6 7 8 9 10 11 12 |
0 |
.005 |
.01 |
.015 |
.02 |
.025 |
.03 |
.035 NO3 |
1 2 3 4 5 6 7 8 9 10 11 12 |
0 |
.01 |
.02 |
.03 |
.04 |
.05 |
.06 |
.07 NO3 |
1 2 3 4 5 6 7 8 9 10 11 12 |
0 |
.02 |
.04 |
.06 |
.08 |
.1 |
.12 NO3 |
1 2 3 4 5 6 7 8 9 10 11 12 |
CS MBS NCI |
NCO NNB SCI |
SCM SCO SNB |
43 |
Figure 3.12: Seasonal variability of Ammonium (NH4) in Biscayne Bay |
Total Nitrogen (TN) and Total Organic Nitrogen (TON) |
Most of the TN (about 75%) is in organic form (TON). The TN spatial distribution |
varies across the bay, with the southern portion having higher values and the northern |
one lower values. The highest mean TN concentrations are observed at MBS (0.468 |
mg/l) and SCI (0.433 mg/l) and the lowest at SCO (0.216 mg/l). Although TN displays |
slightly higher values in the wet season, a clear seasonality (Fig 3.13) is not well |
defined. However, a persistent high occurs in August. The exceptions are CS and |
MBS, both of which display a seasonal pattern with higher values in the wet season. |
TON, on the other hand, has no defined seasonal pattern (Fig 3.14).The high TN values |
observed at MBS are difficult to explain considering that TN loads from the C-111 canal |
into Manatee Bay are less than 50 Ton/yr, nearly 1/10th from that of canals discharging |
into SCI. Hence, the significantly higher median TN and TON concentrations in MBS |
and SCI may be due to contributions from wetlands, either as overland flow or from |
groundwater. |
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