Field
Investigations of Florida Bay Water Quality
Several
cruises have been completed in 1997 to survey the water quality in Florida
Bay. During these cruises, our group has measured carbonate system parameters
(including total alkalinity (TA), pH, total carbon dioxide (TCO2), and
partial pressure of carbon dioxide (pCO2), as well as salinity and nutrients.
In addition, our group has measured samples collected by other groups.
TA, pH, TCO2, and pCO2 have been used in an effort
to characterize the carbonate system in Florida Bay. The carbonate system
data collected have been used to evaluate the saturation state of calcite
and aragonite particles that can absorb phosphate, as well as to examine
the uptake of inorganic carbon by phytoplankton. A flowing multi-parameter
nutrient system, developed in our lab, has been used on several of the
cruises to continuously monitor nutrient concentrations. Nutrient data
(nitrate, nitrite, phosphate, and silicate) have also been combined with
the carbonate parameters to examine the relationship between the carbonate
system and nutrient elements in Florida Bay water. Chlorophyll-a data were
also collected during a cruise to evaluate primary production of Florida
Bay water. The results of the carbonate, nutrient, and chlorophyll-a data
are summarized in
The
lower values were found offshore and along the coastal line of Key West,
the higher values were found in Shark River. Fig.and shows the
results of nutrient concentrations for our November 1997 cruise onboard
the R/V Calanus. shows the nutrients and carbonate parameters in the Shark
River. Fig. and
shows the carbonate parameter measurements made in Shark River. The alkalinity
increases from 2300 mM outside of the river to 7000 mM while the pCO2 increases
from around 600 ppm to 2700 ppm. The high CO2 measurements are related
to the biological and perhaps photochemical degradation of plant materials
in the river. We plan to continue to participate on cruises in Florida
Bay over the next year with others working in the program.