Reservoir sedimentation

Slides:



Advertisements
Similar presentations
9: Running Water Basins: land area that contributes water to a river system Divide: separates different drainage basins Ex. Drainage basin of Mississippi.
Advertisements

John H. Kerr Dam and Reservoir John H. Kerr Dam and Reservoir U.S. Army Corps of Engineers Wilmington District.
Department of Civil Engineering, I.T.U
Sedimentation Lesson 1: “Dirty” Water. What will we study in this unit?  Dirt (soil) in water  Soil in the water is an important nonpoint source of.
Renewable Energy II Hydroelectric power systems high initial investment, low operating cost, long life expectancy no emissions; high capacity, reliability.
Long Term Storage Long term storage means to store water during high inflows years for the benefit of low inflows years. Long term storage means to store.
Water covers 71% of Earth’s surface and is the dominant agent governing environmental processes. The rates of human usage of water outpace the natural.
Hoover Dam – Colorado River. Reasons for Dams Flood Control 39,000 dams worldwide higher than 15 m (ICOLD, 1988)
Yellowtail Dam & Bighorn Lake Billings, Montana January 2011 RECLAMATION Managing Water in the West.
Making Better Decisions in an Uncertain World Reservoir Operations Modeling.
Hydropower Dams © The GlobalEd 2 Project Photo credit: Noodle snacks, Wikimedia Gordan Dam, a dammed hydro facility in Tasmania.
HYDROPOWER DAMS By Hydro Power Group PYP 6 – Sekolah Ciputra
Erosion and Deposition
US Army Corps of Engineers Coastal and Hydraulics Laboratory Engineer Research and Development Center Lower Susquehanna River Watershed Assessment Two.
Do Now: What are the three types of turbines? What parameters determine which turbine to use at a specific site?
Sediment Issues within Transboundary Basins Presented by Paul Bireta and Fernando Salas April 12, 2012.
Climate Outlook Jayantha Obeysekera (’Obey’), Ph.D.,P.E.,D.WRE Department Director Hydrologic & Environmental Systems Modeling.
Sept 11, 2008CVEN 4838/5838Slide #1 Lecture 6 Reservoir Sedimentation.
Managing Western Water as Climate Changes Denver, CO February 20-21, 2008.
James VanShaar Riverside Technology, inc
Freshwater Resources Chapter 4, Lesson 3. Where do we get our water from?  Running water  Standing water  Reservoirs: man-made lakes used to store.
The hydrologic cycle. Running water Streamflow Two types of flow determined primarily by velocity –Laminar flow –Turbulent flow Factors that determine.
Potential Partnership UNRBA – Nicholas Institute Bill Holman & Amy Pickle August 4, 2011.
Multiple Purpose Dam & Reservoir
Rivers and Streams. What is the continental divide?
US Army Corps of Engineers BUILDING STRONG ® Reservoir Simulation Software “Westfield Sub-basin” Presenter – John Hickey, HEC August 2010.
Hydroelectric Power Steph Mecham Chris Rhoades Dylan Welch.
Chapter 13 Water: A Limited Resource. Importance of Water  Cooking & washing  Agriculture  Manufacturing  Mining  Energy production  Waste disposal.
Sediment Delivery to the Lower Neches River and the Effects of Impoundments (Town Bluff Dam-Sam Rayburn Dam)
Describe the features and characteristics of the Three Gorges Dam.
Chapter 9 Surface water Mars.
 Woodcock Creek Lake Anne Grill Vtrip Extra Credit.
How Streams Transport Material 13.2 Stream Erosion & Deposition.
Journal #5 What is a flood? Why are floods harmful? What can humans do to prevent floods?
NID Data Model based on HUC CE394K.3 Term Project by Seungwon Won December 7, 2000.
Suwannee-Satilla Drainage Basin: Flood Control Issues and Requested Action Suwannee-Satilla Regional Water Planning Council Douglas, GA December 8, 2010.
Dams Helpful or Hurtful?.
Human Modifications (historical, modern) Altered Processes that Stress Ecosystem Function (physical, biological, chemical) Indicators of Poor Ecosystem.
Defining Good Ecological Potential : Method used in the UK Niall Jones Hydro-morphology senior advisor Environment Agency.
The Work of Streams Erosion – water causes loose particles to be moved through abrasion, grinding, or by dissolving soluble material. Sediment Transport.
Residence Time. 100 gallons1 gallon/min Residence Time of Water Ice caps: 10,000 to 200,000 years Deep groundwater: ,000 years Oceans:
Guide Curve Operations Partition reservoir storage into “pools” Each pool has a separate purpose Release (or avoid releasing) water to reach the “guide.
Hydrological Information System
HYDROELECTRIC POWER Brandon Terry.
Hydrological changes resulting from dam construction
DES 606 : Watershed Modeling with HEC-HMS
Lecture Outlines PowerPoint
Management of Flood Waters through Mcphee Reservoir
03/02/2006 Flow Routing Reading: 8.1, 8.4, 9.1, 9.2.
Hydrological Information System
GANDHINAGAR INSTITUTE OF TECHNOLOGY
Chapter 9 Surface Water Runoff- water flowing downslope on Earth’s surface. Factors: Vegetation- ↓ runoff due to pore space & slows down precipitation.
EARTH SCIENCE KESSEL.
Chapter 13 Notes.
Summary In addition to the oceans, where else is water found on Earth?
Other renewable energy sources
The Work of Streams.
Stream Erosion.
Precipitation = Evaporation
Lower Susquehanna River Watershed Assessment
Dams Helpful or Hurtful?.
Flood Routing.
Running Water Earth Science Chapter 6
Prentice Hall EARTH SCIENCE
The Flow of Water.
Using Water Wisely.
River Systems Chapter 15.
Surface Water Streams, rivers, ponds, lakes and wetlands.
Part 3.
Precipitation = Evaporation
Presentation transcript:

Reservoir sedimentation

LAKE MEAD, AZ/NV

Reservoir types Flood control Hydropower Flow regulation Recreation Reservoir water volume fluctuations allow flood attenuation Hydropower Flow regulation Steady release modulates downstream stage Recreation Water supply Spillway sets water balance

Sedimentation problems Sediment reduces storage capacity of reservoir, flood attenuation Sediment loading threatens dam integrity Downstream discontinuity of sediment

Sediment pathways Coarse sediment forms delta on upstream edge Coarsest suspended material forms pro-delta wedge Wash load may settle prior to discharge depending on water residence time

Example: Yali Reservoir, Vietnam

Q: How much of modern watershed sediment yield is stored in reservoirs instead of being exported to the ocean?

Potential solutions