EROSION TECHNOLOGY for SITES Earth Spillway Integrity Analysis Phase 2: Inputs and Equations EROSION TECHNOLOGY for SITES Earth Spillway Integrity Analysis.

Slides:



Advertisements
Similar presentations
Process Geomorphology 9/20/2011. Pattern to Process, Process to Pattern.
Advertisements

Measuring Erodibility of Cohesive Soils By Gregory J. Hanson USDA-ARS Hydraulic Engineering Research Unit.
The effect of raindrop impacted flow on sediment composition.
PROGRESSION OF EROSION TECHNOLOGY FOR SITES and WINDAM B EROSION TESTING WORKSHOP Maricopa County, AZ October 19 & 20th.
Overland Flow n Once rainfall exceeds infiltration, water begins to flow. –Clay is hard to pick up due to cohesion. –Sand is hard to pick up due to size.
Bank-Stability and Toe-Erosion Model Andrew Simon, Robert Thomas, Andrea Curini and Natasha Bankhead USDA-ARS National Sedimentation Laboratory, Oxford,
Review of Relative Density Principles v Relative Density principles apply to compaction of relatively clean, coarse- grained soils. v Relatively clean.
Runoff Estimation, and Surface Erosion and Control Ali Fares, PhD NREM 600, Evaluation of Natural Resources Management.
Runoff Estimation, and Surface Erosion and Control Ali Fares, PhD NREM 600, Evaluation of Natural Resources Management.
SPECIALTY WORKSHOP: SITES TRAINING AND INTRODUCTION TO WINDAM ASDSO Dam Safety 2008 PART 2 – SITES EARTH SPILLWAY EVALUATION EVALUATION B. Earth Spillway.
P.I.A. Kinnell University of Canberra Rainfall Erosion Detachment and Transport Systems.
WINDAM Technology Workshop Sept 1-3, 2009 WINDAMb-e (Windows Dam Analysis Modules)
Quantifying Erodibility of Embankment Materials for the Modeling of Dam Breach Processes To HET or to JET — On Which to Bet? Tony L. Wahl – USBR Gregory.
Soil Temperature Profiles Diurnal vertical heat transmission from solar inputs  Follow downward heat pulses animation.
Soil Physical Properties Used to Assess Soil Quality Field Exercise.
CSE 221: Probabilistic Analysis of Computer Systems Topics covered: Exponential distribution Reliability and failure rate (Sec )
Classification, Engineering Properties & Consolidation Methods.
Factors that Influence Erosion
Suspended Load Above certain critical shear stress conditions, sediment particles are maintained in suspension by the exchange of momentum from the fluid.
Matt Robinson Thomas Tolman.  Describes Convective Heat Transfer  Needed for all external and internal flow situations.
Characterizing the Headcut Erodibility Index (Kh) 3) for Cohesive Soils PART 2 – SITES EARTH SPILLWAY EVALUATION B. Earth Spillway Integrity Analysis b.
Jon Fripp NDCSMC Ft. Worth, TX
Reynolds Number (Re) Re = R = A/P V = mean velocity  /  =  (which is kinematic viscosity) Re = VR(  /  ), where Driving Forces Resisting Force Re.
1 SITES INPUT using the Integrated Development Environment __________________________ SITES 2005 INTEGRATED DEVELOPMENT ENVIRONMENT for WATER RESOURCE.
EARTH EROSION THEORY SITES WORKSHOP: March 31 – April 2, 2009 Phoenix, AZ.
NC STATE UNIVERSITY DEPARTMENT of SOIL SCIENCE NC STATE UNIVERSITY DEPARTMENT of SOIL SCIENCE Capability Classes.
Level IB: Advanced Fundamentals Seminar
Harry Williams, Geomorphology1 Sediment Erosion Water flowing through a channel has the ability to transport sediment supplied to it from hillslopes and/or.
SPILLWAY RATINGS and STABILITY DESIGN PROCEDURES __________________________ SITES 2005 INTEGRATED DEVELOPMENT ENVIRONMENT for WATER RESOURCE SITE ANALYSIS.
Watershed Management Assessment Through Modeling: SALT and CEAP Dr. Claire Baffaut Water Quality Short Course Boone County Extension Office April 12, 2007.
Raindrop Impact Erosivity “Rainfall erosivity is the potential…for rainfall to cause soil loss.” (da Silva, 2003)
PART 1 - INTRODUCTION TO SITES B. History and Focus of the SITES Software and its Application SPECIALTY WORKSHOP: SITES TRAINING AND INTRODUCTION TO WINDAM.
Estimating Soil Erosion From Water Using RUSLE By: Andrea King USDA-Natural Resource Conservation Service.
By: Rick Ayers Yates County Soil & Water Conservation District
Lab 13 - Predicting Discharge and Soil Erosion Estimating Runoff Depth using the Curve Number method –Land use or cover type –Hydrologic condition –Soil.
Using GIS and the PSIAC Method to Predict Watershed Sediment Yield Rates Eric Berntsen.
Natural vs. Accelerated Soil Erosion Natural geologic erosion has occurred at a relatively slow rate since the earth was formed. Natural erosion produces.
US Army Corps of Engineers Coastal and Hydraulics Laboratory Engineer Research and Development Center Lower Susquehanna River Watershed Assessment SedFlume.
C SETTLEMENT YULVI ZAIKA. OUTCOMES OF STUDY Introduce consolidation settlement Understand 3 conditions primary consolidation based on pre consolidation.
PART 3 – USING SITES SOFTWARE C. Overview of SITES output a. Key text outputs b. Key graphical outputs SPECIALTY WORKSHOP: SITES TRAINING AND INTRODUCTION.
SITES Workshop-Phoenix, AZ
The Littoral Sedimentation and Optics Model (LSOM)
GLACIERS A glacier is: Any large mass of ice that moves slowly over land Any large mass of ice that moves slowly over land.
1 VIRGINIAWORKSHOP Feb. 28 – Mar. 3, 2006 INTRODUCTION to SITES for WATER RESOURCE SITE ANALYSIS.
Constructing student knowledge of mass transport through interpretation of field data x Jodi Ryder Central Michigan University vs x.
What is Erosion and Sedimentation ? Bill Laflamme CPESC, Office of the Commissioner MAINE DEPARTMENT OF ENVIRONMENTAL PROTECTION Protecting Maine’s Air,
Water Erosion “It is the detachment, transportation & deposition of soil particles by the force of water from one place to another.” “It is the movement.
Hydro-Thermo Dynamic Model: HTDM-1.0
Methods for Determining Streambank Critical Shear Stress: Implications for Erosion Rate Predictions The excess shear stress equation predicts the erosion.
Interill Erosion. Interill Detachment and Sediment Delivery to Rills.
Soil Section 5.2.
SITES SOFTWARE APPLICATION SEMINAR INTRODUCTION to SITES __________________________ SITES 2005 INTEGRATED DEVELOPMENT ENVIRONMENT for WATER RESOURCE SITE.
Figure 6.6. Plants growing in silt loam soil with (a) good tilth and (b) with all three types of compaction. a) good soil structure b) compacted soil porous.
4. Properties of Materials Sediment (size) Physical States of Soil Concepts of Stress and Strain Normal and Shear Stress Additional Resistance Components.
Soil Physics David Zumr room: b608 Lecture (and seminar) notes will be available: -
PART 2 – SITES EARTH SPILLWAY EVALUATION B. Earth Spillway Integrity Analysis i. Three phase model of spillway performance ii. Phase 1 and phase 2 inputs.
Chapter 4 Infiltration. Infiltration is the process by which precipitation moves downward through the surface of the earth. Infiltration replenishes soil.
Entrained-flow Gasifier Model Development Larry Baxter, Bing Liu, Humberto Garcia.
An introduction to cohesive sediment transport modelling
Soil erosion by water EROSION Detachment – particle or aggregate loosened from surface Entrainment – initiation of motion by flow TRANSPORT Rill – concentrated.
Soil Physical Properties Used to Assess Soil Quality
FE: Geotechnical Engineering
Soil Erodibility Prof. Dr. EHSANULLAH. Soil Erodibility Prof. Dr. EHSANULLAH.
Results and Discussion
Agents, Forces, and Results
Soil Section 5.2.
Stability of Slopes By: Alka Shah Civil Engineering Department
Forces That Shape the Earth’s Surface
Rainfall Erosion Detachment and Transport Systems
Presentation transcript:

EROSION TECHNOLOGY for SITES Earth Spillway Integrity Analysis Phase 2: Inputs and Equations EROSION TECHNOLOGY for SITES Earth Spillway Integrity Analysis Phase 2: Inputs and Equations EROSION MEASUREMENT TRAINING: Maricopa County, AZ October 2011

3 PHASE Spillway Erosion Model 1.SURFACE EROSION (Cover Destruction) 3. HEADCUT ADVANCE 2. CONCENTRATED FLOW EROSION

SPILLWAY EROSION PHASES 1. SURFACE EROSION 1. SURFACE EROSION (Cover Destruction) 2. CONCENTRATED FLOW EROSION (Headcut Formation) (Headcut Formation) 3. HEADCUT ADVANCE

PHASE 2 CONCENTRATED FLOW EROSION

PHASE 2 Concentrated Flow Surface Detachment.  r = k d (  e -  c )  e =  (d+  d)S Stress equation applies when eroded depth (  d) is less than approach critical flow depth (phase 2). k d = coefficient of detachment (material property)  c = critical tractive stress (material property)

SURFACE DETACHMENT

cc ee rr

DETACHMENT RATE COEFFICIENT The detachment rate coefficient may be externally determined and entered directly in SITES or estimated by SITES from soil properties.

Summary of Factors to compute Kd  Dry Density,  d  Percent finer than 2  (% clay)  Practical range is from 0.01 to 10  Number is inversely related to resistance to erosion – low value is high resistance, high value is low resistance  Note units are in ft/hr of downward erosion per unit applied stress of lb/ft 2

 Jet Erosion Test (JET)

Jet Erosion Test in NY Spillway

CRITICAL STRESS for Detachment Critical stress based on loose particle condition for all materials.

Parameters Impacting Phase 2 Erosion

SPILLWAY EROSION PHASES 1. SURFACE EROSION 1. SURFACE EROSION (Cover Destruction) 2. CONCENTRATED FLOW EROSION 3. HEADCUT ADVANCE