Homework Help is Here – Start Your Trial Now!
Science
Earth Science
5. Use the manning's equation above to find the streamflow rate (Q) under the following conditions: a. Rectangular canal b. Gravel beds plus large boulders (n) c. River top width (B) = 500 m River depth (Y) = 2 m d. e. River bed slope (S) = 0.03 m/m f. Conversion constant (k) = 1

5. Use the manning's equation above to find the streamflow rate (Q) under the following conditions: a. Rectangular canal b. Gravel beds plus large boulders (n) c. River top width (B) = 500 m River depth (Y) = 2 m d. e. River bed slope (S) = 0.03 m/m f. Conversion constant (k) = 1

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
See similar textbooks
icon
Related questions
Question

Please type your response. Not handwritten.

Manning's Equation O=VA == k R2/3 S 0 Values of Manning n Cement plaster Untreated gunite n Lined Canals Wood, planed Wood, unplaned Concrete, trowled Concrete, wood forms, unfinished Rubble in cement Asphalt, smooth Asphalt, rough Natural Channels 1/2 Gravel beds, straight Gravel beds plus large boulders Earth, straight, with some grass Earth, winding, no vegetation Earth, winding with vegetation A Chow, V. T. 1959. Open-Channel Hydraulics. McGraw-Hill, Inc. n 0.011 0.016 0.012 0.013 0.012 0.015 0.020 0.013 0.016 0.025 0.040 0.026 0.030 0.050
Transcribed Image Text:Manning's Equation O=VA == k R2/3 S 0 Values of Manning n Cement plaster Untreated gunite n Lined Canals Wood, planed Wood, unplaned Concrete, trowled Concrete, wood forms, unfinished Rubble in cement Asphalt, smooth Asphalt, rough Natural Channels 1/2 Gravel beds, straight Gravel beds plus large boulders Earth, straight, with some grass Earth, winding, no vegetation Earth, winding with vegetation A Chow, V. T. 1959. Open-Channel Hydraulics. McGraw-Hill, Inc. n 0.011 0.016 0.012 0.013 0.012 0.015 0.020 0.013 0.016 0.025 0.040 0.026 0.030 0.050
5. Use the manning's equation above to find the streamflow rate (Q) under the following conditions: a. Rectangular canal b. Gravel beds plus large boulders (n) c. River top width (B) = 500 m d. River depth (Y) = 2 m e. River bed slope (S) = 0.03 m/m f. Conversion constant (k) = 1
Transcribed Image Text:5. Use the manning's equation above to find the streamflow rate (Q) under the following conditions: a. Rectangular canal b. Gravel beds plus large boulders (n) c. River top width (B) = 500 m d. River depth (Y) = 2 m e. River bed slope (S) = 0.03 m/m f. Conversion constant (k) = 1
Expert Solution
trending now

Trending now

This is a popular solution!

steps

Step by step

Solved in 3 steps with 1 images

SEE SOLUTIONCheck out a sample Q&A here
Blurred answer
Recommended textbooks for you
Applications and Investigations in Earth Science …
Applications and Investigations in Earth Science …
Earth Science
ISBN:
9780134746241
Author:
Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:
PEARSON
Exercises for Weather & Climate (9th Edition)
Exercises for Weather & Climate (9th Edition)
Earth Science
ISBN:
9780134041360
Author:
Greg Carbone
Publisher:
PEARSON
Environmental Science
Environmental Science
Earth Science
ISBN:
9781260153125
Author:
William P Cunningham Prof., Mary Ann Cunningham Professor
Publisher:
McGraw-Hill Education
Earth Science (15th Edition)
Earth Science (15th Edition)
Earth Science
ISBN:
9780134543536
Author:
Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:
PEARSON
Environmental Science (MindTap Course List)
Environmental Science (MindTap Course List)
Earth Science
ISBN:
9781337569613
Author:
G. Tyler Miller, Scott Spoolman
Publisher:
Cengage Learning
Physical Geology
Physical Geology
Earth Science
ISBN:
9781259916823
Author:
Plummer, Charles C., CARLSON, Diane H., Hammersley, Lisa
Publisher:
Mcgraw-hill Education,
SEE MORE TEXTBOOKS