Stream Velocity Tutorial Start These are readings from station 1. End.
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Transcript of Stream Velocity Tutorial Start These are readings from station 1. End.
![Page 1: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/1.jpg)
Stream Velocity
Tutorial
StartStart
![Page 2: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/2.jpg)
These are readings from station 1.
These are readings from station 1.
End
![Page 3: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/3.jpg)
The rates of change can be adjusted.
The rates of change can be adjusted.
End
![Page 4: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/4.jpg)
Now, let’s change the channel gradient from 0.55 to 0.70.
Now, let’s change the channel gradient from 0.55 to 0.70.
End
![Page 5: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/5.jpg)
Notice that the gradient of station 1 is the same as the value of channel gradient above.
Notice that the gradient of station 1 is the same as the value of channel gradient above.
End
![Page 6: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/6.jpg)
Now, let’s change the rate of change.
Now, let’s change the rate of change.
End
![Page 7: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/7.jpg)
From station 1 onwards, there is a constant decrease of gradient by 0.030 for stations 2 to 10.
From station 1 onwards, there is a constant decrease of gradient by 0.030 for stations 2 to 10.
End
![Page 8: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/8.jpg)
Let’s change the hydraulic radius of station 1 to 0.7 and the rate of change to 0.01.
Let’s change the hydraulic radius of station 1 to 0.7 and the rate of change to 0.01.
End
![Page 9: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/9.jpg)
Notice the corresponding changes here.
Notice the corresponding changes here.
End
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End
From station 1 onwards, there is a constant decrease of hydraulic radius by 0.010 for stations 2 to 10.
From station 1 onwards, there is a constant decrease of hydraulic radius by 0.010 for stations 2 to 10. End
![Page 11: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/11.jpg)
Now, let’s change the channel roughness of station 1 and rate of change to 0.07 and 0.002 respectively.
Now, let’s change the channel roughness of station 1 and rate of change to 0.07 and 0.002 respectively.
End
![Page 12: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/12.jpg)
Here we have a new set of channel roughness readings.
Here we have a new set of channel roughness readings.
End
![Page 13: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/13.jpg)
With Gradient With Gradient With Gradient, Hydraulic RadiusWith Gradient, Hydraulic RadiusWith Gradient, Hydraulic Radius and Channel Roughness
With Gradient, Hydraulic Radius and Channel RoughnessWith gradient, hydraulic radius and channel roughness, a set of velocities are calculated according to the formula
With gradient, hydraulic radius and channel roughness, a set of velocities are calculated according to the formula
EndnSR
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![Page 14: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/14.jpg)
These values show the percentage change of Gradient, Hydraulic Radius , Channel Roughness and Velocity.
These values show the percentage change of Gradient, Hydraulic Radius , Channel Roughness and Velocity.
These values show the percentage change of Gradient, Hydraulic Radius , Channel Roughness and Velocity.
These values show the percentage change of Gradient, Hydraulic Radius , Channel Roughness and Velocity.
These values show the percentage change of Gradient, Hydraulic Radius , Channel Roughness and Velocity.
These values show the percentage change of Gradient, Hydraulic Radius , Channel Roughness and Velocity.
These readings show the percentage changes of gradient, hydraulic radius, channel roughness and velocity.
These readings show the percentage changes of gradient, hydraulic radius, channel roughness and velocity.End
![Page 15: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/15.jpg)
Click on the Velocity graph tab, a plotted graph will be shown.
Click on the Velocity graph tab, a plotted graph will be shown.
End
![Page 16: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/16.jpg)
This graph adjusts in accordance to the readings in channel gradient, hydraulic radius and channel roughness.
This graph adjusts in accordance to the readings in channel gradient, hydraulic radius and channel roughness.
End
![Page 17: Stream Velocity Tutorial Start These are readings from station 1. End.](https://reader035.fdocuments.in/reader035/viewer/2022062720/56649f055503460f94c1aae6/html5/thumbnails/17.jpg)
Click on the Velocity tab to go back to the previous screen.
Click on the Velocity tab to go back to the previous screen.
End
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That’s the end of this tutorial.
That’s the end of this tutorial.
End