Lower Susquehanna River Watershed Assessment

Slides:



Advertisements
Similar presentations
1B Clastic Sediments Lecture 27 SEDIMENT TRANSPORT Onset of motion
Advertisements

CLASTIC TRANSPORT AND FLUID FLOW
Irene Seco Manuel Gómez Alma Schellart Simon Tait Erosion resistance and behaviour of highly organic in-sewer sediment 7th International Conference on.
Digital Imaging and Remote Sensing Laboratory ALGE Modeling and Data Needs Dr. Anthony Vodacek Nina Raqueno Yan Li Center for Imaging Science Rochester.
JSSBIO1Huttula Lecture Set Sediment transport models.
Warm – Up 9/9 What are the four conditions that influence the amount of runoff an area would have? Get out your surface water notes from Friday to prepare.
Streamflow and Runoff The character, amount, and timing of discharge from a basin tells a lot about flow paths within the basin Therefore, important to.
Geomorphic Impacts of Dam Removal Rollin H. Hotchkiss Director, Albrook Hydraulics Laboratory Washington State University, Pullman, WA
Objectives Describe how surface water can move weathered materials.
15. Physics of Sediment Transport William Wilcock (based in part on lectures by Jeff Parsons) OCEAN/ESS
Part 3 RECURRENCE FREQUENCY OF FLOODING. River flow data can be shown in a variety of formats on probability plots like that shown here, which relates.
Lecture 3 Sediment transport. Processes of transport (And a few examples)
Suspended Load Above certain critical shear stress conditions, sediment particles are maintained in suspension by the exchange of momentum from the fluid.
HYDRAULICS AND SEDIMENT TRANSPORT: RIVERS AND TURBIDITY CURRENTS
Lower Susquehanna River Dam Sediment and Solutions Conowingo Relicensing; LSRWA; MD County Resistance; Solutions; CAC Involvement Thursday November 29.
US Army Corps of Engineers Coastal and Hydraulics Laboratory Engineer Research and Development Center Lower Susquehanna River Watershed Assessment Two.
Chapter 13 Surface Water.
Update on the HEC-RAS Reservoir Transport Simulation Mike Langland and Ed Koerkle 03/30/2012.
Reynolds Number (Re) Re = R = A/P V = mean velocity  /  =  (which is kinematic viscosity) Re = VR(  /  ), where Driving Forces Resisting Force Re.
Intro to Geomorphology (Geos 450/550) Lecture 5: watershed analyses field trip #3 – Walnut Gulch watersheds estimating flood discharges.
Lower Susquehanna River Watershed Assessment Citizens Advisory Committee November 29, 2012 Anna Compton USACE 1.
RIVER PROCESSES Introduction to Watershed Science Merritt College Marc Epstein, Instructor.
Emily Shimada, Environmental Science, University of Idaho Research Team B: Watershed Management in the Andean Paramo Faculty Advisors: Dr. Alex Fremier,
Natural Riparian Resources Water Landscape & SoilVegetation.
LECTURE 8 LAYER-AVERAGED GOVERNING EQUATIONS FOR TURBIDITY CURRENTS
Basic Hydraulics: Solids Transport. What is sediment? Matter that settles to the bottom of a liquid Matter transported by water or wind May be particles.
US Army Corps of Engineers Coastal and Hydraulics Laboratory Engineer Research and Development Center Lower Susquehanna River Watershed Assessment SedFlume.
Section 13.1 Streams and Rivers
Modellierung von Sedimenttransporten im Wattenmeer - Gerold Brink-Spalink - Forschergruppe BioGeoChemie des Watts TP 4 Gerold Brink-Spalink Jörg-Olaf Wolff.
 These two agents: erosion and deposition are the most important agents that affect weathered materials.  Erosion involves the physical removal of weathered.
15. Physics of Sediment Transport William Wilcock (based in part on lectures by Jeff Parsons) OCEAN/ESS 410.
Development, Testing and Application of the Multi-Block LTFATE Hydrodynamic and Sediment Transport Model Earl J. Hayter See instructions for customizing.
Transpiration Similar to evaporation, this is the loss of water through plants. – Pores in leaves (stomata) are opened to release oxygen and water vapor.
Running Water. Hydrologic Cycle The hydrologic cycle is a summary of the circulation of Earth’s water supply ► Processes involved in the hydrologic cycle.
Sediment Transport Stream Capacity - The capacity of a stream or river is the total amount of sediment a stream is able to transport comprised of three.
Erosion and Transportation
Fine sediment transport. Fines Till derived soils (e.g., Clarion) ~ 45-70% fines Alluvial soils (e.g., Coland) 65-80% fines Loess-derived soils ~ > 80%
Journal #4 Why are river system constantly changing? The narrow depression that a stream follows downhill is called its _________. What causes the formation.
Channel Processes and Hjulstrom’s Curve
Running Water Day 2. Objective By the end of today, I will be able to: – Evaluate how materials are _____________in a stream and how they are _______________.
CONTENTS 1. Intakes for Collecting Surface Water Page no. (1) (3) (5)
Surface Water Movement
Hydrological changes resulting from dam construction
Presentation to Roanoke River Basin Bi-State Commission March 31, 2010
Basic Hydraulics: Solids Transport
4 channel types defined at reach scale, based on 3 features
Warm-up What are four things that impact INFILTRATION? (the answer is in your notes) After you finish the warm-up put your river basin project in the inbox.
Uniform Open Channel Flow
by Maddie, Ty, McKinley, and Garrett
4 channel types defined at reach scale, based on 3 features
Chapter 9 Surface Water Runoff- water flowing downslope on Earth’s surface. Factors: Vegetation- ↓ runoff due to pore space & slows down precipitation.
Erosional/Depositional Systems
Water Testing Project for the North Fork River
Summary In addition to the oceans, where else is water found on Earth?
Chapter 5 Sediment Yield
Hydrology The study of water.
Modelling tools - MIKE11 Part1-Introduction
The Work of Streams.
Exercise 1: Fenton River Floodplain Exercise
Stream Erosion.
Reservoir sedimentation
OCEAN/ESS Physics of Sediment Transport William Wilcock (based in part on lectures by Jeff Parsons)
Lower Susquehanna River Watershed Assessment
하구및 연안생태Coastal management
하구및 연안생태Coastal management
The Flow of Water.
하구및 연안생태Coastal management
하구및 연안생태Coastal management
River Systems Chapter 15.
Living with Earth 1st Edition
Presentation transcript:

Lower Susquehanna River Watershed Assessment Two Dimensional Modeling Studies Conowingo Pond Conowingo Dam Susquehanna Flats

Lower Susquehanna River Watershed Assessment Progress to Date: Task 1 – Evaluated Reservoir Sedimentation 3D Effects Task 2 – Built a 2D model of Conowingo Pond Including Hydrodynamic Simulations Task 3 – Built a 2D model of Susquehanna Flats Including

Lower Susquehanna River Watershed Assessment TASK 1 – Investigate Impacts of 3D Phenomena What are the 3D Effects in Reservoirs? Currents Generated by Density Gradients due to Temperature Stratification Currents Generated by Winds Reservoir Discharge at Depth

Lower Susquehanna River Watershed Assessment TASK 1 – Investigate Impacts of 3D Phenomena When are These Effects Important? Low River Discharge into Reservoir Advection (Flow Velocity) is low; Turbulence and Mixing at a Minimum High Water Residence Time in Reservoir

Lower Susquehanna River Watershed Assessment TASK 1 – Investigate Impacts of 3D Phenomena The Concern: Will 3D Effects Significantly Impact 2D Sediment Transport and Fate Simulations? The Approach: Evaluate Sediment Availability to Reservoir When 3D Impacts May be Significant

Lower Susquehanna River Watershed Assessment Water Retention Time In Conowingo Pond * Flows > 30,000 cfs have a retention time of 5 days or less * ASSUME all Flows < 30,000 cfs Have Dominant 3D Effects * ASSUME all Flows > 30,000 cfs Have Sufficient Mixing

Lower Susquehanna River Watershed Assessment Rouse Number Calculation to Predict Mixing / Stratification Medium Silt at 30,000 cfs R = Up / k(tB / r)0.5 Ratio of particle fall velocity To Bed Shear Stress Ratio of Gravitational Force that encourages settling to bed shear forces that encourage re-suspension Transport Mode Rouse Number Bed Load > 2.5 50% Suspended 1.2 – 2.5 100% Suspended 0.8 – 1.2 Wash Load < 0.8

Lower Susquehanna River Watershed Assessment Flow Duration Curve for Susquehanna River Median Flow is about 26,000 cfs 56% of Flows are Less Than 30,000 cfs

Lower Susquehanna River Watershed Assessment Sediment Rating Curve for Susquehanna River Sediment Load Entering the Reservoir in Tons / Day for a Given Discharge

Lower Susquehanna River Watershed Assessment Integration of the Flow Duration Curve and Sediment Rating Curve Total Load / Year: 4,283,166 Tons Total Load < 30,000 cfs: 224,869 Tons BOTTOM LINE: Reservoir is Exposed to only 5% of Total Yearly Load During Low Flow Conditions Although 3D Effects do Occur, They Are Negligible

Lower Susquehanna River Watershed Assessment 2D Model Development – Conowingo Pond AdH Numerical Mesh Info 21,893 Elements 11,432 Nodes Power plant and Flood Gate Discharge Capability

Lower Susquehanna River Watershed Assessment 2D Model Development – 2008 Bathymetry

Lower Susquehanna River Watershed Assessment 2D Model Development – Power Plant and Gates Floodgates Power Plant

Lower Susquehanna River Watershed Assessment Susquehanna River Return Flood Flows Simulated 700,000 cfs Flood ~ 40 Year Return Event

Lower Susquehanna River Watershed Assessment Water Depth at 700,000 cfs

Lower Susquehanna River Watershed Assessment Velocity at 700,000 cfs

Lower Susquehanna River Watershed Assessment Discharge Through Power Plant < 86,000 cfs

Lower Susquehanna River Watershed Assessment Discharge Through Flood Gates > 400,000 cfs

Lower Susquehanna River Watershed Assessment Post-Spill Site Overview

Lower Susquehanna River Watershed Assessment 2D Model Development – Susquehanna River Through Susquehanna Flats AdH Numerical Mesh Info 16,357 Elements 8,587 Nodes

Lower Susquehanna River Watershed Assessment 2D Model Development – Model Bathymetry

Lower Susquehanna River Watershed Assessment Water Depth at 100,000 cfs Mean Low Lower Water Tail Water Elevation

Lower Susquehanna River Watershed Assessment Velocity at 100,000 cfs Mean Low Lower Water Tail Water Elevation

Lower Susquehanna River Watershed Assessment Velocity at 100,000 cfs Flow Patterns with Submerged Vegetation Roughness Assignment