Sediment Transport Through Lake Clarke and Lake Aldred

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Sediment Transport Through Lake Clarke and Lake Aldred Jon Viducich, EI Martin J. Teal,

Sediment Transport Through Lake Clarke and Lake Aldred Jon Viducich, EI Martin J. Teal, PE, PH, D. WRE April 5, 2017 Preliminary Data – Subject to Revision

Topics • Introduction and Background • Study Goals • Model Development • Model Calibration

Topics • Introduction and Background • Study Goals • Model Development • Model Calibration and Verification • Summary of Results and Limitations • Conclusion 1 Preliminary Data – Subject to revision

Introduction and Background • Recent Interest in the Lower Susquehanna River Reservoirs ü Dynamic

Introduction and Background • Recent Interest in the Lower Susquehanna River Reservoirs ü Dynamic equilibrium ü Potential impacts on Chesapeake Bay water quality ü Past studies Lake Clarke Lake Aldred Conowingo Reservoir Figure 1 -2 from Lower Susquehanna River Watershed Assessment (2015) 2 Preliminary Data – Subject to revision

Introduction and Background • Safe Harbor Dam ü Constructed 1931 ü 75 feet tall,

Introduction and Background • Safe Harbor Dam ü Constructed 1931 ü 75 feet tall, impounds Lake Clarke (7, 360 acres) • Holtwood Dam ü Constructed 1910 ü 55 feet tall, impounds Lake Aldred (2, 400 acres) Safe Harbor Dam, October 24, 2010 (U. S. C. G. Aux 5 DNR on Flickr) 3 Preliminary Data – Subject to revision Holtwood Dam, December 2015 (http: //suereno. blogspot. com)

Study Goals • Develop unsteady, 1 D sediment transport model ü Marietta, PA to

Study Goals • Develop unsteady, 1 D sediment transport model ü Marietta, PA to Holtwood Dam (20. 4 miles) • Aid in parameterization of Chesapeake Bay Watershed Model • Input for HDR model of Conowingo Pond 4 Preliminary Data – Subject to revision

Study Goals – Model Improvements • Improve upon past studies using U. S. Army

Study Goals – Model Improvements • Improve upon past studies using U. S. Army Corps of Engineers HEC-RAS 5. 0 Model (unsteady) ü Solves the unsteady flow equation, routing flow and explicitly accounting for storage and travel time ü Conserves volume, important in reservoir systems ü Cohesive and non-cohesive sediments Figure 17 -1 HEC-RAS Version 5. 0 User’s Manual (2016) 5 Preliminary Data – Subject to revision

Model Boundary Conditions and Setup • Geometric Data • Flow & Temperature Data •

Model Boundary Conditions and Setup • Geometric Data • Flow & Temperature Data • Sediment Data Safe Harbor Dam ü Bed sediment (12 size classes) ü Inflow loads • Transport Function • Sediment Parameters • Dam Operations ü Rating curves 6 Preliminary Data – Subject to revision Holtwood Dam

Model Calibration and Verification • Hydraulic Calibration at Marietta, PA • Sediment Volume Change

Model Calibration and Verification • Hydraulic Calibration at Marietta, PA • Sediment Volume Change ü 2008 -2013 (calibration) ü 2013 -2015 (verification) 7 Preliminary Data – Subject to revision

Model Calibration and Verification (2) • Sediment Transport Calibration ü January 2008 – August

Model Calibration and Verification (2) • Sediment Transport Calibration ü January 2008 – August 2013 ü Several large events, including Tropical Storm Lee • Sediment Transport Verification ü August 2013 October 2015 ü Unusually low flows 8 Preliminary Data – Subject to revision Observed vs. Modeled Cumulative Volume Change: Lake Clarke Sub-Areas 1 -5, January 2008 – October 2015 Observed vs. Modeled Cumulative Volume Change: Lake Aldred Sub-Areas 3 -6, January 2008 – October 2015

Summary of Results and Limitations • Additional Runs ü Historical flow events applied to

Summary of Results and Limitations • Additional Runs ü Historical flow events applied to end of simulation • Results Increased transport on rising limb Decreased transport on falling limb 9 Preliminary Data – Subject to revision

Summary of Results and Limitations (2) • Model Limitations ü One-dimensional model cannot replicate

Summary of Results and Limitations (2) • Model Limitations ü One-dimensional model cannot replicate two-dimensional processes ü Uncertainties in input data (geometry, flow, sediment) and calibration data (measurements) ü Lack of actual dam operation data ü Lack of extreme (>700, 000 cfs) events during simulation/measurement periods Sediment Loading (tons/d) Marietta, PA Sediment Loading 10, 000 1, 000 100, 000 10, 000 Obs Data 1, 000 HEC-RAS Initial Values 100 10 1, 000 100, 000 Discharge (cfs) 10 Preliminary Data – Subject to revision

Summary of Results and Limitations (3) • Rating Curve Limitations ü Hysteresis and variance

Summary of Results and Limitations (3) • Rating Curve Limitations ü Hysteresis and variance at large discharges limits rating curves’ usefulness during extreme events ü Mass balance suggests better representation for Lake Clarke than Lake Aldred 11 Preliminary Data – Subject to revision

Conclusion • 1 D HEC-RAS 5. 0 sediment transport model as part of multi-model

Conclusion • 1 D HEC-RAS 5. 0 sediment transport model as part of multi-model study • Applied inputs to model sediment change 2008 -2015 • Calibrated model successfully simulated bed changes • Results used to develop sediment rating curves for other researchers 12 Preliminary Data – Subject to revision

Questions? Holtwood Dam, September 10, 2011 (The. Gates 1210 on You. Tube) 13

Questions? Holtwood Dam, September 10, 2011 (The. Gates 1210 on You. Tube) 13