21
10-1 prepared by Ercan Kahya Lecture Notes 2 Lecture Notes 2 Chapter 10: Chapter 10: Channel Geometry Channel Geometry A channelized stream in poor condition A channelized stream in poor condition

Lecture Notes 2 Chapter 10: Channel Geometry

  • Upload
    pepin

  • View
    52

  • Download
    0

Embed Size (px)

DESCRIPTION

Lecture Notes 2 Chapter 10: Channel Geometry. A channelized stream in poor condition. Types of flow:. Slide from Dr. Isaac. Types of flow:. Slide from Dr. Isaac. Channel Types . Slide from Dr. Isaac. Channel Geometry . - PowerPoint PPT Presentation

Citation preview

Page 1: Lecture Notes 2 Chapter 10:  Channel Geometry

10-1prepared by Ercan Kahya

Lecture Notes 2Lecture Notes 2

Chapter 10: Chapter 10: Channel Channel GeometryGeometry

A channelized stream in poor conditionA channelized stream in poor condition

Page 2: Lecture Notes 2 Chapter 10:  Channel Geometry

10-2

Types of flow:

Slide from Dr. Isaac

Page 3: Lecture Notes 2 Chapter 10:  Channel Geometry

10-3

Types of flow:

Slide from Dr. Isaac

Page 4: Lecture Notes 2 Chapter 10:  Channel Geometry

10-4

Channel Types

Slide from Dr. Isaac

Page 5: Lecture Notes 2 Chapter 10:  Channel Geometry

10-5

Channel Geometry

A concrete trapezoidal A concrete trapezoidal channelchannel

Channel geometry encompasses all characteristics that define the channel geometry

At a point, it includes area, depth, friction, bottom width, top width, side slope, wetted perimeter.For the entire channel reach, it includes length, slope, average of each of the first 5 parameters

Page 6: Lecture Notes 2 Chapter 10:  Channel Geometry

10-6Channel Geometry

D: hydraulic depth

D = A / B

A: areaB: top width

For artificial channels

Page 7: Lecture Notes 2 Chapter 10:  Channel Geometry

10-7

Depth of flow (Depth of flow (yy) and) anddepth of flow section (depth of flow section (dd))

Geometric ElementsChannel cross-sectional shape governs the pattern of the velocity distribution, boundary shear stress & secondary circulation => DISCHARGE CAPACITY

y (depth of flow): the vertical distance of the lowest pt of a channel section to free surface

See the text book for the definition of other elements.

Page 8: Lecture Notes 2 Chapter 10:  Channel Geometry

10-8prepared by Ercan Kahya

(Chapter 11) (Chapter 11) Resistance in Open ChannelsResistance in Open Channels

Steady, uniform flow in a well-maintained channel Steady, uniform flow in a well-maintained channel

Page 9: Lecture Notes 2 Chapter 10:  Channel Geometry

10-9

Slide from Dr. Isaac

Governing Equations in Open Channel Flow

Page 10: Lecture Notes 2 Chapter 10:  Channel Geometry

10-10

Slide from Dr. Isaac

Manning Equation

Page 11: Lecture Notes 2 Chapter 10:  Channel Geometry

10-11

Channel Efficiency

- Capacity (efficiency) varies inversely with the wetted perimeter (P).

- Energy losses are less in channels with smaller P & vice versa.

- 4 options to excavate a rectangular section with an area of 20m2 :

- P: (a) 22; (b) 14; (c) 13; and (d) 14m → Choice is “c”

Page 12: Lecture Notes 2 Chapter 10:  Channel Geometry

10-12

Channel Efficiency

- For Max. Capacity Hydraulic Efficiency → Min. wetted perimeter (P).

- That section is called “most efficient” or “best hydraulic” section.

- It reduces the cost of lining.

- For a given cross-sectional area: the best hydraulic section has min P

- For a given perimeter: the best hydraulic section has max A (area).

For trapezoidal sections:

Area →

Wetted perimeter →

Page 13: Lecture Notes 2 Chapter 10:  Channel Geometry

10-13

Channel EfficiencyDetermine the relation btw b & y to minimize P for a fixed cross-sectional area and side slope

Substitute into wetted perimeter eq.:

To minimize P w.r.t. y:

yields

Note that this eq. leads to impractical design, such as very deep & narrow channel.

Page 14: Lecture Notes 2 Chapter 10:  Channel Geometry

10-14

Channel Efficiency- Alternatively “b” equation can be written as:

This implies that B (Top width) = 2L (side length)

Referring this figure

Page 15: Lecture Notes 2 Chapter 10:  Channel Geometry

10-15

Channel Efficiency- Substitute the final form of ‘b’ equation into OQ relation:

Moreover minimization w.r.t. ‘t” of side slope yields

This corresponds to a slope angle of 60 degree

But this slope is often too steep for natural channels

- Substitute this again into the final form of ‘b’ equation :

This defines the trapezoidal section of greatest possible efficiency

Page 16: Lecture Notes 2 Chapter 10:  Channel Geometry

10-16

Channel Efficiency- Even if we further substitute into R equation of trapezoidal section:

reduces to

The most efficient rectangular channel is one in which the depth is one-half of the width.

Page 17: Lecture Notes 2 Chapter 10:  Channel Geometry

10-17

Channel Efficiency

Page 18: Lecture Notes 2 Chapter 10:  Channel Geometry

10-18

Resistance in Steady Nonuniform Flow

- Manning and Chezy equations can be generalized to “nonuniform flow”

- Assumption: the stage changes only gradually w.r.t. longitudinal distance

- Then this flow is called GRADUALLY VARIED FLOW

- But acceleration is not negligible! Makes it different than uniform flow

- Channel slope, water surface, and energy gradient are not equal!

Page 19: Lecture Notes 2 Chapter 10:  Channel Geometry

10-19

Resistance in Steady Nonuniform Flow

Applying Newton`s second law:

In the case of steady flow, only convective

After math manipulations;

Shear stress at the bed;

Page 20: Lecture Notes 2 Chapter 10:  Channel Geometry

10-20

Resistance in Steady Nonuniform Flow

or

Note that

FLOW IS BEING DRIVEN BY THE HYDRAULIC GRADIENT

That is to say; the component of gravity force in the flow direction

Page 21: Lecture Notes 2 Chapter 10:  Channel Geometry

10-21

Class Exercises: