Figure B 11 Solute after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, reference river bed conductance, and decreased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 12 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, reference river bed conductance, and increased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 13 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, increased river bed conductance, and decreased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 14 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, increased river bed conductance, and reference porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 15 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, increased river bed conductance, and increased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 16 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Increased aquifer hydraulic conductivity, decreased river bed conductance, and decreased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit)
Figure B 11 Solute after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, reference river bed conductance, and decreased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 12 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, reference river bed conductance, and increased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 13 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, increased river bed conductance, and decreased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 14 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, increased river bed conductance, and reference porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 15 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Reference aquifer hydraulic conductivity, increased river bed conductance, and increased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit) Figure B 16 Solute plume after 1 500 years following a 30-year release from a leaking storage pond. Increased aquifer hydraulic conductivity, decreased river bed conductance, and decreased porosity. A unit input concentration at the soil-groundwater interface is assumed (i.e. C0 = 1 M/L3, where M/L3 is a user defined unit)
technical-report-number-10-human-environmental-exposure-assessment.docx