TY - JOUR
T1 - Spatial and Temporal Chemical Variability in the Hillsborough River System
AU - Pillsbury, Lori A.
AU - Byrne, Robert H.
PY - 2007/1/1
Y1 - 2007/1/1
N2 - The Hillsborough River originates in the Green Swamp, a principal recharge area of the Floridan Aquifer system. As the river flows to Tampa Bay, its chemistry is influenced by a variety of natural and anthropogenic inputs. Spatial and temporal variations in the river's major ion concentrations, CO 2 -system chemistry, and nutrients were examined in a two-year study between 1999 and 2001. At thirteen sampling stations along approximately 87 km of the river, water samples were collected in surroundings that ranged from pristine to urban. Concentrations of major ions were lowest in the river's headwaters, showed only minor spatial variations mid-river, and sharply increased in tidally influenced waters below the dam on the lower river. The mid-river major ion composition is relatively constant in large part because two of the river's most compositionally distinctive inputs, Blackwater Creek and Crystal Springs, are located well upstream. Below the confluence of Blackwater Creek and river water that is largely derived from Crystal Springs, concentrations of Na + , K + , Mg 2+ , Ca 2+ , HCO 3 − , F − , Cl − and PO 4 3− showed spatial variations that were smaller than +/− 30%. Only SO 4 2− and NO 3 − exhibited strong downstream variations. Sulfate concentrations increased by more than a factor of two, and NO 3 − decreased by more than an order of magnitude. In contrast to spatial variations in the river's chemistry, temporal variations were quite large. Concentrations of major ions decreased during the rainy season (June–September) by as much as a factor of 3–5, and phosphate concentrations increased by approximately an order of magnitude. The river's CO 2 -system also showed strong seasonal variations. River pH and CaCO 3 saturation state decreased sharply during periods of high precipitation. CaCO 3 supersaturation was observed during the exceptionally dry periods of the study, and undersaturation was observed during periods of high rainfall. Overall, the Hillsborough River's delivery of solutes to Tampa Bay is greatly influenced by temporal variations in river hydrology, and distinct chemical signatures from the river's tributaries, groundwater sources, and anthropogenic inputs. The river's output of phosphate to the bay, which is exceptionally high during periods of high river-flow, is especially notable.
AB - The Hillsborough River originates in the Green Swamp, a principal recharge area of the Floridan Aquifer system. As the river flows to Tampa Bay, its chemistry is influenced by a variety of natural and anthropogenic inputs. Spatial and temporal variations in the river's major ion concentrations, CO 2 -system chemistry, and nutrients were examined in a two-year study between 1999 and 2001. At thirteen sampling stations along approximately 87 km of the river, water samples were collected in surroundings that ranged from pristine to urban. Concentrations of major ions were lowest in the river's headwaters, showed only minor spatial variations mid-river, and sharply increased in tidally influenced waters below the dam on the lower river. The mid-river major ion composition is relatively constant in large part because two of the river's most compositionally distinctive inputs, Blackwater Creek and Crystal Springs, are located well upstream. Below the confluence of Blackwater Creek and river water that is largely derived from Crystal Springs, concentrations of Na + , K + , Mg 2+ , Ca 2+ , HCO 3 − , F − , Cl − and PO 4 3− showed spatial variations that were smaller than +/− 30%. Only SO 4 2− and NO 3 − exhibited strong downstream variations. Sulfate concentrations increased by more than a factor of two, and NO 3 − decreased by more than an order of magnitude. In contrast to spatial variations in the river's chemistry, temporal variations were quite large. Concentrations of major ions decreased during the rainy season (June–September) by as much as a factor of 3–5, and phosphate concentrations increased by approximately an order of magnitude. The river's CO 2 -system also showed strong seasonal variations. River pH and CaCO 3 saturation state decreased sharply during periods of high precipitation. CaCO 3 supersaturation was observed during the exceptionally dry periods of the study, and undersaturation was observed during periods of high rainfall. Overall, the Hillsborough River's delivery of solutes to Tampa Bay is greatly influenced by temporal variations in river hydrology, and distinct chemical signatures from the river's tributaries, groundwater sources, and anthropogenic inputs. The river's output of phosphate to the bay, which is exceptionally high during periods of high river-flow, is especially notable.
KW - Florida
KW - Major ions
KW - pH
KW - Carbonate
KW - Phosphate
KW - Nitrate
KW - Hillsborough River
UR - https://digitalcommons.usf.edu/msc_facpub/1751
UR - https://doi.org/10.1016/j.marchem.2006.12.005
U2 - 10.1016/j.marchem.2006.12.005
DO - 10.1016/j.marchem.2006.12.005
M3 - Article
VL - 104
JO - Marine Chemistry
JF - Marine Chemistry
ER -