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We will now move on to study rating curves for natural channels Section Control Channel Control Overbank Gh - e Discharge

We will now move on to study rating curves for natural channels

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We will now move on to study rating curves for natural channels. Overbank. Gh - e. Channel Control. Section Control. Discharge. The relation between stage and discharge in a natural channel can also be assumed to be a power function. - PowerPoint PPT Presentation

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Page 1: We will now move on to study rating curves for  natural channels

We will now move on to study rating curves for natural channels

SectionControl

ChannelControl

Overbank

Gh

- e

Discharge

Page 2: We will now move on to study rating curves for  natural channels

The relation between stage and discharge in a natural channel can also be assumed to be a power function

Page 3: We will now move on to study rating curves for  natural channels

Here is the power function that is often used to relate discharge and head under section control

Q = a(GH-e)b

where:a = coefficientb = slope of the relation(b is almost always greater than 2)

Page 4: We will now move on to study rating curves for  natural channels

Here is the equation that is often used to relate discharge and head under channel control

Manning’s equation:Q = 1.486 A R 2/3 S 1/2 n

Where:A = cross section areaR = hydraulic radius (area/wetted perimeter)S = energy slopen = Manning’s “n” (roughness coefficient)

Page 5: We will now move on to study rating curves for  natural channels

Manning equation can be reduced to a simple power function

Q = 1.486 A R 2/3 S 1/2 n Can be reduced to:

Q = C d1.67 = C (GH-e)1.67

Click here if you want to see how this is done.

Page 6: We will now move on to study rating curves for  natural channels

Just to be sure we all know how to use exponents and how to compute basic hydraulic parameters we will go through a brief math primer

Q = 2.5 x 20 x 2 1.50 =

Weir equation: Q = CBH 3/2

whereC = 2.5, B = Top width = 20 ftH = Average depth of flow = 2 ft

141 ft3/s

Page 7: We will now move on to study rating curves for  natural channels

Math Primer (cont)

Manning equation:Q = 1.486 AR 2/3 S 1/2

nwhere:

n = roughness coefficient = 0.05A = cross sectional area = 500 ft2

R = Hydraulic Radius (area / wetted perimeter) = 4.5 ftS = Energy slope (assume to be same as water surface

slope = 0.002 ft/ft

Q = 1.486 x 500 x 4.5 .667 x 0.0021/2 = 0.05

1812 ft3/s

Page 8: We will now move on to study rating curves for  natural channels

Math Primer (cont).

Compute area for gh = 10 ft

Area for main channel =

0 ft

10 ft

5 ft

(10 x 100) – ((5 x 100)/2) = 750 ft2

Area for overflow = (5 x 100) = 500 ft2

TOTAL AREA = 1250 ft2

100 ft0 ft 200 ft

Sand bar

Overflow

Page 9: We will now move on to study rating curves for  natural channels

Math Primer (cont.)

Compute WP, and R for gh = 12 ft

WP for main channel =

2 ft

12 ft

7 ft

10 + 100 + 5 = 115 ftWP for overflow = 100 + 5 = 105 ft

TOTAL WP = 220 ft

R = A / WP = (1000 + 500) / 220 = 6.82 ft

100 ft0 ft 200 ft

Overflow

Note: WP does not increase on main channel left bank above gh of 5 ft. There is no boundary friction there.

1000 ft2500 ft2

Main Channel

Page 10: We will now move on to study rating curves for  natural channels

Rating curve slopes can provide insights to control conditions

<21

>21

SectionControl

ChannelControl

Overbank

Gh

- e

Page 11: We will now move on to study rating curves for  natural channels

1

10

1 10 100Discharge

Gag

e H

eigh

tHere is how to measure rating curve slopes

<2 (usually 1.3 to 1.8)

>2

1

1

Measure down one unit then measure horizontal distance to rating using same unit of measure slope. Rating mustbe straight line and scales cannot be distorted!

Page 12: We will now move on to study rating curves for  natural channels

San Francisquito Creek

0.01

0.1

1

10

100

0.1 1 10 100 1000 10000Discharge, in cfs

Gag

e H

eigh

t - o

ffset

An example of a rating and controls

PZF = 0.07

G.H. = 5.4

G.H. = 6.25

Click here to see video of control at high flow (1.2 MB file)

Page 13: We will now move on to study rating curves for  natural channels

Artificial controls can also have compound shapes

Artificial section control

Page 14: We will now move on to study rating curves for  natural channels

Multiple offsets can be used to straighten different parts of ratings

• Use of multiple offsets makes sense for many ratings• GRSAT making working with multiple offsets easy!

Offset = 3

Offset = 1

Page 15: We will now move on to study rating curves for  natural channels

You must smooth the transition between rating segments when multiple offsets are used!

Click on the photo below to view an animation of changing controls

Page 16: We will now move on to study rating curves for  natural channels

It is often necessary to extend ratings to stages above or below where measurements have been made

??

?

?

Page 17: We will now move on to study rating curves for  natural channels

Ratings can be extended to low stages by:

1. Using arithmetic-scale graph and the PZF as a guide.

2. Using knowledge of the control

3. Using hydraulic equations

Point of zero flow

Page 18: We will now move on to study rating curves for  natural channels

Ratings can be extended to high stages by:

1. Plotting techniques• Use straight line, knowledge of

control.2. Slope-conveyance3. Step-backwater model4. Areal comparison of peak runoff rates5. Flood routing

Page 19: We will now move on to study rating curves for  natural channels

• Rule of Thumb -- Do NOT extend beyond twice the highest measured discharge (this may be a direct or indirect measurement)

Here is a rule of thumb to keep in mind when extending ratings

Page 20: We will now move on to study rating curves for  natural channels

1

10

100

10 100 1000

Discharge

Stag

e

?

?

The wrong offset can increase uncertainty when extending ratings

Page 21: We will now move on to study rating curves for  natural channels

10 100 1000

Discharge

Stag

e 2015

6

Straight lineextension

You can be much more certain of how to extending the rating when the correct offset is used!

Page 22: We will now move on to study rating curves for  natural channels

ChannelControl

Overbank

Gag

e he

ight

Rating extensions must consider channel geometry

Page 23: We will now move on to study rating curves for  natural channels

When to Draw a New Rating?

• When measurements indicate a significant, consistent, and permanent departure from the current rating, especially on the upper end.

• When the shape of the shift diagrams departs significantly from the shape of the rating.