Fluvial Hydraulics CH-3

Slides:



Advertisements
Similar presentations
Lecture 8: Design of Erodible Channels
Advertisements

School of Civil Engineering/Linton School of Computing, Information Technology & Engineering Lecture 10: Threshold Motion of Sediments CEM001 Hydraulic.
SEMINAR IN ADVANCED STRUCTURE analysis and design of box culvert
Total & Specific Energy
Basic Governing Differential Equations
Example: Uniform Flow at Known Q and y
SHEAR IN BEAMS. SHEAR IN BEAMS Example (4.1): A rectangular beam has the dimensions shown in Figure 4.12.a and is loaded with a 40 ton concentrated.
Types of flow: Slide from Dr. Isaac.
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.
Hydraulics Engineering
HYDRAULIC 1 CVE 303.
CHAPTER 6: Water Flow in Open Channels
CE 230-Engineering Fluid Mechanics Lecture # Noncircular conduits Uniform flow in open channels.
Basic Governing Differential Equations
Pertemuan Open Channel 1. Bina Nusantara.
CM 197 Mechanics of Materials Chap 14: Stresses in Beams
Modeling River Ice and River Ice Jams with HEC-RAS
Copyright © 2011 Pearson Education South Asia Pte Ltd
Open channel hydraulics
UNIFORM FLOW AND DESIGN OF CHANNELS
CH 7 - Open Channel Flow Brays Bayou Concrete Channel Uniform & Steady
Hydraulic Routing in Rivers
Force on Floating bodies:
Reynolds Number (Re) Re = R = A/P V = mean velocity  /  =  (which is kinematic viscosity) Re = VR(  /  ), where Driving Forces Resisting Force Re.
Hydraulic Engineering
FOOTINGS. FOOTINGS Introduction Footings are structural elements that transmit column or wall loads to the underlying soil below the structure. Footings.
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.
The Islamic University of Gaza Faculty of Engineering Civil Engineering Department Hydraulics - ECIV 3322 Chapter 6 Open Channel.
Module 3d: Flow in Pipes Manning’s Equation
Flow Energy PE + KE = constant between any two points  PE (loss) =  KE (gain) Rivers are non-conservative; some energy is lost from the system and can.
Uniform Open Channel Flow
ERT 349 SOIL AND WATER ENGINEERING
Lecture 13 Design of erodible and non-erodible, alluvial channels- Kennedy’s and Lacey’s theories.
Basic Hydraulics: Channels Analysis and design – I
Basic Hydraulics: Open Channel Flow – I
Chapter 8 Table of Contents Section 1 Fluids and Buoyant Force
OC FLOW: ENERGY CONCEPTS, CHANNEL ANALYSIS
ONE-DIMENSIONAL ANALYSIS ON BEDEVOLUTION ACCOMPANING BANK EROSION Satoru Nakanishi Hokkaido University Graduate School Kazuyoshi Hasegawa Hokkaido University.
8. 1 Mixer Sizing Methods Four different sizing criteria - Velocity - Shear Stress - Yield Stress - Mixing Time.
RIVER CHANNEL CALCULATIONS
Sanitary Engineering Lecture 7
Manning’s Equation Gauckler(1867)–Manning–Strickler (1923)
Norman W. Garrick Design of Grass Swales.
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
Shear in Straight Members Shear Formula Shear Stresses in Beams
Shearing Stresses in Beams and Thin-Walled Members
ERT 349 SOIL AND WATER ENGINEERING
4 channel types defined at reach scale, based on 3 features
Fluvial Geomorphology
Uniform Open Channel Flow
4 channel types defined at reach scale, based on 3 features
Fluid flow in an open channel
Uniform Open Channel Flow – Ch 7
Soil Mechanics-II Soil Stabilization and Improvement
Open Channel Storm water Irrigation Waste water collection and treatment.
Time of Concentration.
The Islamic University of Gaza Faculty of Engineering Civil Engineering Department Hydraulics - ECIV 3322 Chapter 6 Open Channel.
Discharge, stream flow & channel shape
The shapes of stream channels
Introduction/Open-Channel Flow
Hydrodynamic Concepts
Fluvial Hydraulics CH-3
Fluvial Hydraulics CH-3
Design of Stable Channels CH-4
Design of Stable Channels CH-4
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.
Heat Transfer Correlations for Internal Flow
Tractive Force Design with SewerGEMS
Presentation transcript:

Fluvial Hydraulics CH-3 Uniform Flow – Stable Channels

Shear Stress on Bed Shear stress defined earlier as… How does this equation simplify for channels with a large width? Assume a trapezoidal channel… Will shear stress on bed be larger or smaller than the shear stress on the sides of the channel?

Distribution of Shear Stress Shear stress is distributed over the wetted perimeter, P Graf gives the typical distribution for a trapezoidal channel (Chow, 1959) – derived from analytical and finite-difference methods Pattern of distribution varies with shape of the section but unaffected by size of the section

Forces - Bottom of the Channel Particles at bottom of channel resist shear stress of moving fluid… Write a force balance equation at the moment of motion (incipient motion): David Chin, Water Resources Engineering

Forces on the Side of the Channel Particles at side of channel resist shear stress of moving fluid and particle weight that acts down the side of the channel… Total force tending to move particle: Total force resisting motion:

Forces on the Side of the Channel When motion is incipient: Based on this equation, what is the requirement for stable side walls?

Example 3.C A channel excavated in earth should convey a water discharge of Q = 57 m3/s at an average temperature of 14oC. The bed slope is 0.001; the banks have side slopes of 1.5:1 (H:V). A grain size analysis yielded d50 = 37 mm, the angle of repose is 37o, ss = 2.65, and n = 0.02. What should be the dimensions of this channel, if no erosion is allowed either at the bottom or on the banks?

Solution Methodology Stability of banks requires q < j Check using m… q = 33.7o Calculate critical bed-shear stress on walls: Need the critical shear stress – How?

Solution Methodology Calculate a flow depth not to exceed these critical values: Use minimum value of h based on shear stress on side walls Actually should use an h smaller than this critical value

Solution Methodology Last step is to solve for b: Use Manning’s Equation with given Q Use Table 1.1 for A, Rh

Stable Section Stable cross section – section in a channel with a mobile bed where there is no erosion over the entire wetted perimeter Ideal stable cross section – stable cross section with a maximum discharge and a minimal wetted perimeter Minimum water area, minimum top width, and maximum mean velocity  minimum excavation

Stable Section Assume a channel with a side wall angle at the water surface equal to the angle of repose: To design a stable hydraulic section for maximum efficiency, it is necessary to create a condition of impending motion everywhere on channel bed

Stable Section (US Bureau of Reclamation) Tractive force acting on a particle on the sloping wall:

Stable Section (US Bureau of Reclamation) Condition of impending motion everywhere on bed: Note the difference between h and h’

Stable Section (US Bureau of Reclamation) The following differential equation is derived:

Stable Section (US Bureau of Reclamation)

Stable Section (US Bureau of Reclamation) Other hydraulic parameters of the ideal cross section:

Stable Section (US Bureau of Reclamation) If Q which must be conveyed through the channel is different than Qi=UA: Q < Qi : Replace B with reduced B’ Q > Qi : Replace B with increased B”

Example 3.C A channel excavated in earth should convey a water discharge of Q = 57 m3/s at an average temperature of 14oC. The bed slope is 0.001; the banks have side slopes of 1.5:1 (H:V). A grain size analysis yielded d50 = 37 mm, the angle of repose is 37o, ss = 2.65, and n = 0.02. What should be the dimensions of this channel, if no erosion is allowed either at the bottom or on the banks?

Example 3.D An artificial channel is constructed in a mountainous region and should convey 30 m3/s at T=14oC without causing erosion. The slope of the channel will be 0.01 and n = 0.025. The grain size analysis has shown that the granular material is non-cohesive with d50=50 mm, j = 37o, and ss = 2.65. (a) Determine dimensions of a rectangular channel with sides of wooden boards. (b) Determine the dimensions of an ideal stable cross section with the channel constructed of its bed material.

Solution Methodology Use critical shear stress criteria: Use Fig. 3.13 (Shields diagram) to determine t*cr Use t*cr to solve for tocr Use the bed shear stress equation to solve for the hydraulic radius: Use Manning’s equation to calculate U Solve for A, P, b and h

Solution Methodology We need to first solve for h (maximum depth in the middle of the ideal cross-section): Use critical shear stress from before to solve for tocr Solve for h using:

Solution Methodology Use equations for ideal cross-section to solve for h’, A, B, and U Check the ideal discharge versus the actual discharge and adjust B if necessary

Example 3.D An artificial channel is constructed in a mountainous region and should convey 30 m3/s at T=14oC without causing erosion. The slope of the channel will be 0.01 and n = 0.025. The grain size analysis has shown that the granular material is non-cohesive with d50=50 mm, j = 37o, and ss = 2.65. (a) Determine dimensions of a rectangular channel with sides of wooden boards. (b) Determine the dimensions of an ideal stable cross section with the channel constructed of its bed material.