DESIGNING STONE TOE PROTECTION. IS STP THE RIGHT SOLUTION? IS THE CHANNEL BED STABLE? IS THE BANKFULL WIDTH IN BEND LESS THAT 130% OF BANKFULL WIDTH.

Slides:



Advertisements
Similar presentations
WinTR-20 Course February Muskingum-Cunge Flood Routing Procedure in NRCS Hydrologic Models Prepared by William Merkel USDA-NRCS National Water Quality.
Advertisements

Riparian Zone Habitat Assessment Vegetation and More.
Lower Yellowstone River Diversion Dam Project – Phase II - Physical Modeling of the Rock Ramp BRT, COE, MTAO Update Meeting November 4, 2010.
Rivers and Streams Chapter 6.1 and 6.2.
In-Stream Habitat Survey
Streambank Protection Design of Riprap Protection
CE 3205 Water and Environmental Engineering
Detention / Infiltration Structure. Figure 21–1 Point Discharge and Downstream Stability Analysis Procedure.
Rock Riffle Design Course
Design of Highway Vertical Alignment Chapter 16
Pipeline Hydraulics.
1 Time of Concentration. 2 Objectives Know how to calculate time of concentration Know how to calculate time of concentration Know why it’s important.
John M. Buffington Research Geomorphologist US Forest Service Rocky Mountain Research Station Boise, Idaho, USA PNAMP Protocol Comparison Meeting February.
Lewis Creek Reach M19 Phase 1, Phase 2, and Phase 3.
Pertemuan Open Channel 1. Bina Nusantara.
If there is no change in friction or slope as we move down stream
Design of Grass Swales Norman W. Garrick
MSU Extension Pesticide Education Turfgrass Pest Management (Category 3A) Application Calculations and Calibration Chapter 5.
Differentials, Estimating Change Section 4.5b. Recall that we sometimes use the notation dy/dx to represent the derivative of y with respect to x  this.
Proposed Novato Creek Bank Stabilization Guidelines Questa Engineering Corp.
Notes on Hydraulics of Sedimentation Tanks. A Step by Step Procedure.
“We Bring Engineering to Life” 3-D Stream Restoration Design, Monitoring and Beyond David Bidelspach, PE - Stantec Consulting Greg Jennings, PE – NCSU.
LONGITUDINAL PEAKED STONE TOE PROTECTION {LPSTP}
UNIFORM FLOW AND DESIGN OF CHANNELS
Introduction to Sine Graphs
MEASURING FLUMES By CH. VENKATARAMAIAH.
THE ENGINEERED FLOODPLAIN BENCH. Conceptually, for an incised system you can: raise the stream, lower the floodplain, or a little of both Lower either.
SACE Stage 2 Physics Motion in 2 Dimensions.
TRADITIONAL WINDROW & TRENCH-FILL REVETMENTS, & A NEW INVENTION, VEGETATED TRENCH-FILL REVETMENT {All 3 are classified as “Setback Revetments”}
Hydraulic Engineering
OSBORNE HOLLOW CREEK ROAD PROTECTION PROJECT. Gravel-Cobble Bed Stream – Rural, Pool-Riffle-Pool, Stream Slope 2-3% Goals: Halt bank erosion to protect.
CHANNEL EFFICIENCY Channel Roughness. It is often thought that the velocity of a river is greatest near its start. This is not the case, as large angular.
DESIGNING BENDWAY WEIRS
SPILLWAY RATINGS and STABILITY DESIGN PROCEDURES __________________________ SITES 2005 INTEGRATED DEVELOPMENT ENVIRONMENT for WATER RESOURCE SITE ANALYSIS.
2.2 What are the major fluvial processes?
Kinematics in One Dimension We will focus today on problem- solving. Note: some problems are hard, some are not so hard. Part of the learning is recognizing.
Sulphur Dunnigan Burn Dump, Yolo County, CA. (30 miles north of Sacramento, CA.) BUILT 1998.
March 2009WinTR-20 Course1 Muskingum-Cunge Flood Routing Procedure in NRCS Hydrologic Models Prepared by William Merkel USDA-NRCS National Water Quality.
GUTTERS and INLETS Gutter : A gutter is a triangle open channel along the curb stone of streets which carry the storm water along streets to inlets. Inlets.
Hydrologic Hazards at the Earth’s Surface
A stream is a body of water that carries rock particles and dissolved ions and flows down slope along a clearly defined path, called a channel. Thus, streams.
CTC 261 Culvert Basics.
HAW CREEK, PIKE COUNTY, MISSOURI-TRIB TO SALT RIVER ERODING STREAM THREATHENING COUNTY ROAD #107, FOURTEEN FT TALL ERODING BANK WITHIN 4 FT OF THE ROAD,
Basic Hydraulics: Channels Analysis and design – I
Bradshaw Model. Upstream Downstream Discharge Occupied channel width Channel depth Average velocity Load quantity Load particle size Channel bed roughness.
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
 It is the type of V. F. in which the width of throat is decreased to such an extent that the depth of water in throat is equal to critical depth. 
© Awad S. Hanna, PhD, P.E.1 Estimating and Scheduling CEE 492 Lecture 5 ESTIMATING EARTHWORK.
Riprap Installation Construction Inspection for Field Office Activities Will use Riprap Gradation and Riprap Subgrade Problems from Class Problem Section.
Manning’s Equation Gauckler(1867)–Manning–Strickler (1923)
EXAMPLE Water flows uniformly in a 2m wide rectangular channel at a depth of 45cm. The channel slope is and n= Find the flow rate in cumecs.
UNIFORM FLOW AND DESIGN OF CHANNELS
Expression Session Summarise “stream discharge” and “river load” using diagrams to assist your answer.
Profile Leveling.
GUTTERS and INLETS (m3/s(
4 channel types defined at reach scale, based on 3 features
Uniform Open Channel Flow
4 channel types defined at reach scale, based on 3 features
CLASS PLAN RIVER BEHAVIOR FLOW GAUGING MANNING’S EQUATION
Floods and Flood Routing
Module # 17 Overview of Geomorphic Channel Design Practice
ESTIMATING EARTHWORK Prof Awad S. Hanna.
Anthony Keene Kristin LaForge CIVE 717 Spring 2018
Kastanis- Existing Conditions
Design of Stable Channels CH-4
ESTIMATING EARTHWORK Prof Awad S. Hanna.
Longitudinal Profile Survey for Successful Culvert Replacement
Scour Analysis on the west fork of the Duchesne River
Example 3.E - Graf Assume a channel with uniform flow at a depth of 5.03 m. Channel is rectangular with a width of 9 m and average velocity of 12 m/s.
In-Stream Structures & Grade Control
Presentation transcript:

DESIGNING STONE TOE PROTECTION

IS STP THE RIGHT SOLUTION? IS THE CHANNEL BED STABLE? IS THE BANKFULL WIDTH IN BEND LESS THAT 130% OF BANKFULL WIDTH AT RIFFLE IS UNVEGETATED POINT BAR LESS THAN 30% OF BANKFULL WIDTH AT RIFFLE

Lanes Balance

IS STP THE RIGHT SOLUTION? IS THE CEM STAGE IV OR V? IS THE RADIUS OF CURVATURE/BANKFULL WIDTH RATIO GREATER THAN 1.8?

CONSIDER GRADE CONTROL!! A REALLY GOOD INSURANCE IS TO ADD A SMALL ROCK RIFFLE GRADE CONTROL TO YOUR STP PROJECT!!

IF RADIUS IS TOO SMALL FOR RADIUS/Wbkf IS LESS THAN 1.8--CONSIDER USING “TRADITIONAL BANK PROTECTION”!!

Scour Depth Assume Scour Depth will equal Max. Bankfull Flow Depth Assumes bed material allows full Sine Wave Flow to develop over time

STP DESIGN START AND STOP AT STABLE POINT DESIGN HEIGHT SHOULD BE A MINIMUM OF 1.5 FT. ABOVE DOWNSTREAM RIFFLE ELEVATION DESIGN HEIGHT SHOULD INCREASE AS “BANKFULL DEPTHS” INCREASE AND/OR Rc/Wbkf DECREASES

STP DESIGN GOAL IS TO PROTECT TOE IN AREA BELOW POINT WHERE VEGETATION CAN BE ESTABLISHED--- THEREFORE USE VEGETATION IN A “STABLE” AREA AS A GUIDE FOR REQUIRED HEIGHT OF STP

STP DESIGN CREST ELEVATION SHOULD BE UNIFORM THROUGH OUT ENTIRE BEND ALIGNMENT SHOULD BE AS SMOOTH AS POSSIBLE “KEYS” SHOULD ALWAYS BE LOCATED AT U.S AND D.S ENDS

STP DESIGN ADDITIONAL “KEYS” SHOULD BE PLACED AT REGULAR INTERVALS THROUGH THE ENTIRE REACH AT A MAXIMUM OF 100 FT. SPACING MAY BE SPACED CLOSER IN SMALL RADIUS BENDS (50-75 FT)

STP DESIGN PLACE STP IN “WINDROW” WITH SMALL DEPRESSIONAL AREA BEHIND PEAK TO CAPTURE SILT AND CREATE A “BENCH” FOR VEGETATIVE GROWTH.

QUANTITIES WILL VARY ALONG REACH DEPENDING ON WATER DEPTH USUALLY BEST TO FIGURE AVERAGE DEPTH THROUGH REACH TO CALCULATE QUANTITIES 1 TON/FT DESIGN WILL NOT BE 1 TON/FT FOR ENTIRE LENGTH TREATED

QUANTITIES RIFFLE ELEVATION - MAX. BANKFULL DEPTH = MAXIMUM SCOUR DEPTH ELEVATION EXAMPLE RIFFLE = MAX. Dbkf= 4.0 FT. MAX. SCOUR DEPTH = 96.0

QUANTITIES POOL DEPTH IS 3 FT. BELOW RIFFLE ELEVATION ANTICIPATE ADDITIONAL 1 FT. OF SCOUR--ADD ROCK TO LAUNCH INTO DEEPENED POOL WITHOUT LOSING CREST BY WIDENING CREST WIDTH.

QUANTITIES CALCULATE AVE. HT. OF STP AS HT. ABOVE WATER + AVERAGE WATER DEPTH + ANTICIPATED SCOUR DEPTH END AREA IS APPROX. = 3H X H /2 = SQ. FT (1.5:1 SIDESLOPES) MULTILPLY BY 105 LBS/ CU. FT. AND CONVERT TO TONS/FT OF STP

QUANTITIES EXAMPLE 1.5 FT. ABOVE WATER FT AVE. WATER DEPTH + 1 FT. ANTICIPATED SCOUR = 3.5 FT. OF STP 3(3.5) X 3.5)/ 2 = 18.4 CU. FT CU. FT. X 105 LBS/CU. FT. = 1932 LBS. = TONS/ FT

SIZING MATERIAL 1. CHECK VELOCITY FROM I&E FORM 2. MULTIPLY MEAN VELOCITY BY 2 3. CHECK TABLE OF VELOCITIES TO MOVE DIFFERENT DIAMETER STONES 4. SELECT STONE SIZE WHERE MAXIMUM STONE WILL NOT BE MOVED

STONE CLASSES

SUMMARY CHECK BED STABILITY & Rc CHECK WIDTH OF CHANNEL AND POINT BAR CHECK ELEV. OF VEGETATION IN STABLE AREA ABOVE RIFFLE ELEV. CHECK POOL DEPTH

SUMMARY (cont.) ADD---HT. OF VEG. ABOVE WATER AVE. WATER DEPTH IN REACH ANTICIPATED SCOUR DEPTH TOTAL = HEIGHT OF STP END AREA = 3H X H/2 VOLUME = END AREA X 105 LBS/CU. FT. (DIVIDE BY 2000 TO GET TON/FT)

SUMMARY (cont.) MAKE CREST UNIFORM KEEP IT PEAKED KEEP IT SMOOTH BE SURE TO “KEY” IT IN SIZE STONE TO RESIST 2 X MEAN VELOCITY