290 likes | 434 Views
Nitrate and Groundwater Flow to Springs in the Upper Floridan aquifer, Lower ACF—Chipola Basin. by Christy Crandall. Objectives of Study—2007 through 2009. 1) To quantify groundwater travel times areas contributing recharge hydrologic and geochemical processes occurring along flowpaths
E N D
Nitrate and Groundwater Flow to Springs in the Upper Floridan aquifer, Lower ACF—Chipola Basin by Christy Crandall
Objectives of Study—2007 through 2009 1) To quantify • groundwater travel times • areas contributing recharge • hydrologic and geochemical processes occurring along flowpaths 2) Test 3 nitrogen management scenarios from 2002 through 2050 in areas contributing recharge to Jackson Blue, Baltzell Group, and Sandbag Springs. • Cessation of nitrogen input after 2001 • 4 percent decline per year of nitrogen input • Maintain nitrogen input at 2001 levels
Study Area Lower ACF Basin Elevation Streams Physiographic provinves
Floridan Aquifer System Named Springs Mapped Closed-basin depressions Confinement Status
Sub-Models And Selected Groundwater sites
pART Particle Age and Area Contributing Recharge to Springs
K Uncertainties of Fertilizer Data Locations of use? Nitrate-N in mg/L Jackson County, Florida, 1945 to 2001
Estimated changes in nitrate concentrations in Jackson Blue, Baltzell Group, and Sandbag Spring from 2002 through 2050 with 3 different management scenarios • Cessation of nitrogen input after 2001 • 4 percent decline per year of nitrogen input • Maintain nitrogen input at 2001 levels
Estimated changes in nitrate concentrations in Jackson Blue Spring from 2002 through 2050 with 3 different management scenarios
Estimated changes in nitrate concentrations in Baltzell Spring Group from 2002 through 2050 with 3 different management scenarios
Estimated changes in nitrate concentrations in Sandbag Spring from 2002 through 2050 with 3 different management scenarios
Future Directions--Large Objectives • Develop linked groundwater/surface water model to calculate daily stage, stream flux, and head, as a function of pumpage, rainfall, upstream conditions, climate events, and dam releases through 2050
Future Directions—my tasks • Convert Current Model to transient flow model • Use more sophisticated unsaturated flow and streamflow routing to account for aquifer- stream interaction, evaporation and recharge in the surficial aquifer/residium. • Calibrate transient model for 1978 to 2008 recharge, stream and spring flow and pumpage conditions.