Home Page > Programs > Biscayne Bay Alliance > Biscayne Bay Alliance Data 2004

Thanks to all of our volunteers for their hard work! In 2004, Volunteers took water samples from six sites in Miami-Dade County. The samples were analyzed by scientists in Florida International University's Our Rivers and Coastal Oceans (ORCO) Lab for parameters that would give insight into the quality of the water passing through the waterway. FIU analyzed the samples for the following parameters:

  • TN:Total Nitrogen

  • N+N: Nitrate + Nitrite

  • TDN: Total Dissolved Nitrogen

  • TP: Total Phosphorous

  • PO4: Phosphate

  • TDP:Total Dissolved Phosphorous

  • DOC: Dissolved Organic Carbon

  • NH4: Ammonia
Beakers
Ammonia (NH4)

Ammonia Nitrogen in our waterways has been measured by the County since 1979. The State limits the concentration of Ammonia in freshwater to 0.02mg/L, while the County permits up to 0.05 mg/L (0.02mg/L to 0.05mg/L, depending on the sampling method). Many monitoring stations exceed this standard on a regular basis, with the most consistent offenders located on or near the Miami River, or in south Miami-Dade near agricultural areas.

High concentrations of Ammonia usually results from polluted stormwater runoff from urbanized areas, sewage contamination, or from leachate (water that has percolated through and is leaking from a location) from landfills or old dumps that have not been properly closed. High levels of ammonia can be toxic to invertebrates and fish, and contribute to nutrient loading by supplying excess available nitrogen.

Ammonia Graph

In the above graph, the only sampling site that appears to consistently fall within standards is Bill Sadwoski Park. Matheson Hammock appears consistenly to fall out of range, while the Coral Gables Waterway spikes at the the highest level of 0.74mg/L. This spike could be a result of an event such as a major rainfall, the opening of flood gates, etc., or be due to sampling inconsistencies. The levels of NH4 in the canals are considerably higher than those observed in Biscayne Bay. Fortunately for the Bay, the concentrations of NH4 drop to more acceptable upon mixing with Bay waters. However, more research is needed to define acceptable levels of nutrients concentrations for a near shore estuarine mixing zone.

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Nitrate + Nitrite

Nitrate cannot be measured directly; a chemical reaction is performed to convert the nitrate to nitrite. However, to avoid confusion test results are expressed as combined nitrate + nitrite nitrogen, which is often abbreviated as (NOx-N). Phew, that's a mouthful.

The Biscayne Bay ecosystem naturally exists on very low levels of nitrogen and phosphorous and is vulnerable to excess nutrient loading. In order to prevent degradation of water quality in Biscayne Bay, concentrations of nitrate-nitrite should not exceed 0.01mg/L. Unfortunately, nitrate-nitrite levels found in tributaries feeding the Bay frequently exceed this standard, particularly in the south Miami-Dade, where canals (such as the Mowry and Princeton canals, whose averages are hundreds of times greater) receive runoff from the agricultural lands typical in this area. Fortunately for the Bay, the concentrations of nitrate-nitrite drop to more acceptable upon mixing with Bay waters. However, more research is needed to define acceptable levels of nutrients concentrations for a near shore estuarine mixing zone

Sources of nitrates include wastewater treatment plants, runoff from fertilized lawns and cropland, failing septic systems, runoff from animal manure storage areas, and industrial discharges that contain corrosion inhibitors.

N+N Graph

With this data set, the only waterway that consistently fell within desired limits was Matheson Hammock. Matheson Hammock may have high ammonia rates due to the large amount of decomposing plant material around the site, but low nitrate-nitrite levels due to it's proximity to Biscayne Bay (perhaps the salinity of the water at this site prevents bacterial decomposition in nitrate, in addition to high levels of flushing). Four different sites show a spike in N+N levels in the sampling event on 8/14/2004, while Mahi canal consistently showed nutrient levels higher than the other sampling sites.. Additionally, there appears to be a trend towards rising nutrient levels for nearly all sites over this sampling period, however statistical analysis needs to be done to determine whether these observations are significant.

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Dissolved Organic Carbon

Dissolved Organic Carbon (DOC) is a measure of the amount of dissolved organic material (carbon that passes through a 0.45 micron filter) present in a waterbody. DOC is produced from the decay of plankton, grazing by zooplankton, the decomposition of leaf litter, precipitation, and leaching from soils. DOC is of interest to ecologists as it can help chacterize the physical, chemical, and biological properties of water. For instance, high DOC can protect microorganisms from UVB radiation and depress primary productivity by afffecting the depth light penetrates through the water column (euphotic zone).

DOC may even affect the amount of toxic metals in an ecosystem. In the Everglades, current research indicates high levels of DOC (typically found in a wetland ecosystem due) may reduce levels of mercury in the ecosystem that can enter the bodies of wildlife, by binding with mercury and reducing its reactivity and availability. Read more about mercury and DOC in the Everglades from the USGS...

DOC can be influenced by human activities on a local and global scale. Activities such as deforestation, development, or land use can alter the amount of DOC entering into a waterbody by changing leaf litter decomposition or erosion rates, while pollutants entering the atmosphere can affect the amount of DOC entering the waterbody through precipitation and chemically reacting with DOC. While research is ongoing in this subject, current research indicates that these activities reduce the amount of DOC remaining in the waterbody.

DOC graph