Geschreven door studenten die geslaagd zijn Direct beschikbaar na je betaling Online lezen of als PDF Verkeerd document? Gratis ruilen 4,6 TrustPilot
logo-home
Tentamen (uitwerkingen)

Solutions Manual for Fundamentals of Open Channel Flow (2nd Edition, by Glenn E. Moglen) Chapter 1 to 7

Beoordeling
-
Verkocht
-
Pagina's
113
Cijfer
A+
Geüpload op
04-06-2025
Geschreven in
2024/2025

Solutions Manual for Fundamentals of Open Channel Flow (2nd Edition, by Glenn E. Moglen) Chapter 1 to 7

Instelling
Fundamentals Of Open Channel Flow 2nd Edition
Vak
Fundamentals of Open Channel Flow 2nd Edition

Voorbeeld van de inhoud

JHGFD




SOLUTION MANUAL

Fundamentals of Open Channel Flow

by Glenn E. Moglen
N
2nd Edition
U
R
SE
D
O
C
S


KJHGFDS

, JHGFD

Chapter 1: Introductory Material - Solutions

1.1. What slope would lead to a 1% difference between depth in the vertical plane rather than
depth measured perpendicular to the channel bottom? Compare this slope to the
observation that a channel slope of S0 = 0.01 m/m is generally considered quite steep for
open channel flow.

Solution:

If  is the angle between the horizontal plane andx the plane of the channel then,
 = cos  
1.01x
N
 
Thus,
U
 = 8.1o
or, in terms of rise/run,
S = tan(8.1o) = 0.14 m/m
R
Comparing this number to a channel slope of S0=0.01 m/m we see that the slope
SE
corresponding to a 1.0 percent difference between depths is more than an order of
magnitude larger.

1.2. Using Bernoulli’s equation, write the energy balance in general terms for flow in an open
channel from location 1 to 2 where hL is the head loss between these two locations.
Simplify the equation by taking the perspective of a point on the water surface at both
D
locations. Note: your solution should show that the pressure term from Bernoulli’s
equation is not relevant for open channel flow.
O
Solution:
p v2 p2 v22
+ z1 = + +z +h
C
1
+ 1

 2g  2g 2 L

If we take a point on the water surface at both locations, the p1 equals p2 equals
S
atmospheric pressure, and thus these terms may be cancelled from both sides of the
equality,
v12 v22 + z + h
+ z1 = 2 L
2g 2g
The remaining equation if y is substituted for z and if hL is set to zero, forms the basis for
the specific energy equation which is the focus for Chapter 2.




KJHGFDS

, JHGFD

-1-
N
U
R
SE
D
O
C
S


KJHGFDS

, Chapter 1: Introductory Material


1.3. Parts (a), (b), and (c) require simple multiplication/division and/or addition/subtraction to
solve. The reader is cautioned to pay special attention to significant digits when reporting
the final answer.
a. If the density of water is 1000 kg/m3 and gravitational acceleration is 9.81 m/s2, what
is the unit weight of water?
b. If the density of water is 1.0  103 kg/m3 and gravitational acceleration is 9.81 m/s2,
what is the unit weight of water?
c. The cross-sectional area of a channel is broken into three separate subareas with the
following sizes: 1.3 m2, 0.92 m2, and 15 m2. What is the total cross-sectional area of
the channel?
N
Solution:

a) The unit weight of water is the product of density and gravitational acceleration so,
U
 = g = (1000) (9.81) = 9810N
Since density is given with one significant figure. The answer has one significant figure
R
resulting in: 10,000 N.
b) The new statement gives density with two significant figures, so the answer becomes:
9800 N.
SE
c) The calculator-based sum of the three provided numbers is 17.22. However, the number
“15” indicates uncertainty in the “ones” place of the number. This same uncertainty
needs to be conveyed in the answer, so the correct answer is 17 m2.
D
1.4. The mean or bulk velocity of flow in a stream is observed to be 1.1 m/s. A rock tossed
into this same flow sets up ripples that radiate outward in all directions. It is noted that
the ripples propagating directly upstream travel at a velocity of 0.67 m/s in the opposite
direction to the direction of the flowing stream.
O
a. What is the Froude number for this flow?
b. Estimate the depth of flow in this stream.
C
Solution:

a) The wave velocity (velocity of ripple propagation) provided is the net velocity, equal
to the velocity of wave propagation in a still pool of water minus the bulk velocity
S
downstream. The wave velocity is 1.1 + 0.67 = 1.8 m/s. Using the definition of the
Froude number:
v = 1.1 = 0.61
Fr =
gy 1.8
b) The depth of flow in the stream can be estimated based on the wave velocity, vw = 1.8
m/s.


-2-

Geschreven voor

Instelling
Fundamentals of Open Channel Flow 2nd Edition
Vak
Fundamentals of Open Channel Flow 2nd Edition

Documentinformatie

Geüpload op
4 juni 2025
Aantal pagina's
113
Geschreven in
2024/2025
Type
Tentamen (uitwerkingen)
Bevat
Vragen en antwoorden

Onderwerpen

$18.49
Krijg toegang tot het volledige document:

Verkeerd document? Gratis ruilen Binnen 14 dagen na aankoop en voor het downloaden kun je een ander document kiezen. Je kunt het bedrag gewoon opnieuw besteden.
Geschreven door studenten die geslaagd zijn
Direct beschikbaar na je betaling
Online lezen of als PDF

Maak kennis met de verkoper

Seller avatar
De reputatie van een verkoper is gebaseerd op het aantal documenten dat iemand tegen betaling verkocht heeft en de beoordelingen die voor die items ontvangen zijn. Er zijn drie niveau’s te onderscheiden: brons, zilver en goud. Hoe beter de reputatie, hoe meer de kwaliteit van zijn of haar werk te vertrouwen is.
ScoreGuides Chamberlain College Of Nursing
Volgen Je moet ingelogd zijn om studenten of vakken te kunnen volgen
Verkocht
1468
Lid sinds
3 jaar
Aantal volgers
782
Documenten
2448
Laatst verkocht
1 dag geleden
ScoreGuides – Study Smarter, Score Higher

ScoreGuides provides high-quality study guides, test banks, and solutions manuals across a wide range of subjects. Each document is carefully created and structured to help students master key concepts, practice effectively, and excel in exams. Trusted by thousands of learners worldwide — study smarter, score higher!

4.1

132 beoordelingen

5
79
4
22
3
11
2
8
1
12

Recent door jou bekeken

Waarom studenten kiezen voor Stuvia

Gemaakt door medestudenten, geverifieerd door reviews

Kwaliteit die je kunt vertrouwen: geschreven door studenten die slaagden en beoordeeld door anderen die dit document gebruikten.

Niet tevreden? Kies een ander document

Geen zorgen! Je kunt voor hetzelfde geld direct een ander document kiezen dat beter past bij wat je zoekt.

Betaal zoals je wilt, start meteen met leren

Geen abonnement, geen verplichtingen. Betaal zoals je gewend bent via iDeal of creditcard en download je PDF-document meteen.

Student with book image

“Gekocht, gedownload en geslaagd. Zo makkelijk kan het dus zijn.”

Alisha Student

Bezig met je bronvermelding?

Maak nauwkeurige citaten in APA, MLA en Harvard met onze gratis bronnengenerator.

Bezig met je bronvermelding?

Veelgestelde vragen