NETWORKS6.1 Multi-reservoirs with Branched Pipe System
One of the important topics that the practicalengineers dealt with in real life, is the design and\oranalysis of pipeline systems that are composed of threeor more reservoirs at various elevations. This system isreferred as branching pipes since one or more pipes areseparated into two or more pipes (or combine into to asingle one) and are not coming together again at thedownstream.The point of connection of more than two pipes at asingle point is called Junction and that’s whysometimes these problems are referred as JunctionProblems as well.
In fact, at the Junction ‘J’, the mass balanceequation (Continuity) should be satisfied,
ΣQIN = ΣQOUT .
In general, if all the pipes are sufficiently long
• the minor losses and
• the velocity head just at the junction may beneglected.
Note that, the energy head at the junction ‘HJ’ hasa single common value.
The methodology for the solution depends on theavailable information related with:
• the reservoirs elevations,
• the pipes diameters,
• The pipes lengths and
• the pipes types (characteristic) etc.
If the flow directions are not known (which is the generalcase), an energy level for the junction point ‘HJ’ isassigned and hence the directions of the flows within thepipes are defined based on this assumption.
Then, by trial and error, until the equation of continuitysatisfies, the assumed junction level ‘HJ’ is reevaluated(changed).
Note that, the basic equation, which is the continuityequation within the system, is the one thatcontrols the flows direction.
Hence, the actual directions of the flow depends on:
the reservoir (or tank) pressures and/or elevations,
the diameters, lengths, and types of the pipes etc.
For the solution of this type of problems, generally a trial-and-error procedure is unavoidable.
The best procedure, as informed earlier, is the assumptionof the energy head level to the junction ‘HJ’ and thencomputing the flow rate for each pipeline and checkingthe continuity equation based on these values.
If the continuity equation is satisfied, then, thecomputed flow values are correct.
(i.e. the total flow entering equals to the total
flow leaving at the junction).
If the continuity equation is not satisfied, adifferent energy head level value at the junctionshould be reassumed.
Usually a satisfactory solution is obtained afterseveral trials.
Note 1:NEVER HJ > HIGHEST RESERVOIR WATER SUFACE LEVEL.
Under normal conditions (if no pump is installed).
Note 2:NEVER HJ < LOWEST RESERVOIR WATER SUFACE LEVEL.
Under normal conditions.
Note 3:After the first iteration assume:- HIGHER than the previously assumed value,
if at the Junction: flow entering > flow leaving.
- LOWER than the previously assumed value,
if at the Junction: flow entering < flow leaving.
Consider the possible simplest system that is consisted of1 Junction & 3 Reservoirs where the estimation of thedischarge in each pipe sections has to be determined, asshown in Fig. 6.1.
Figure 6.1: Three-reservoirs system.
J
hL AJ
hL JB
hL JC
pD
For the solution of these branch systems, the necessarynumbers of equations have to be obtained through energyand continuity concepts.
In these type of problems, basically one of these 3different parameters are unknown at the junction:1. the total energy head at the junction (HJ) is unknown.2. the flow direction of the middle reservoirs connecting
pipe (JB) is unknown.3. the flow amount of the middle reservoirs connecting
pipe (JB) is unknown.
To determine the total energy head, the flow amount and thedirection within that pipe (JB), the solution procedure iscarried out through the energy equation on the basis of theoutcome of the iterations.
First Iteration:a) Since it is difficult to incorporate the velocity head at the
junction (J), this type of problems can be solved, byassuming this velocity head to be a small quantity relativeto the other energy terms and may be ignored.
Hence, letting the total energy head (piezometric head, sincethe velocity head is neglected) at the junction (J) be equal tothe total energy head (usually the water surface elevation) ofthe reservoir surface B (middle reservoir), hence no flowwould occur within the pipe JB.
b) By writing the energy equation between A-J and J-C separately, one can obtain the values of discharges QAJ and QJC.
where the head losses are defined by using the Darcy-Weisbach equation.
AD
LD
DA hP
zz γ
CB
LCD
D hzP
z γ
zA=HJ+hLAJ=
HJ ≈
JJ
JJ
J
AJ
AJ
2 22 2
5 4
1
2 2 12.1 12.1DC
DC avDC avDC DCL DC DC DC DC
DC DC DC
L v v Lh f k f Q k Q
D g g D D
2 22 2
5 4
1
2 2 12.1 12.1AD
avAD avADAD ADL AD AD AD AD
AD AD AD
v vL Lh f k f Q k Q
D g g D D
AJ
JC
AJAJ
AJ AJ AJ
AJ
AJ
AJ
AJAJ
AJ
JC
JC
JC
JC JC
JC
JC
JC
JCJC
JC
c) Using continuity equation, compare the values of
discharges QAJ and QJC and hence, estimate the
direction of the flow along pipe J-B.
One of the below 2 equations is only correct.
AD DC DBQ Q Q
AD DC DBQ Q Q
or
AJ JC JB
AJ JC JB
Second iteration:a) Since the direction of flow along J-C is determined,suggest more reasonable (possible) total energy ‘HJ’value for that junction.
i- if QAJ > QJC → QJB is an outflow (from the junction J to reservoir B),
hence to satisfy that select: HA > HJ > HB.
(a value between zA and zB)
ii- if QAJ < QJC → QJB is an inflow (from reservoir B to the junction J),
hence to satisfy that select: HC < HJ < HB. (a value between zB and zC).
b) By writing the energy equation between A-J, B-J (or J-B) and J-C separately, obtain the values of discharges QAJ,QJD (or QJB) and QJC using the head losses defined byDarcy-Weisbach equation.
c) To check the correctness of this assumed junctionenergy level HJ, yse the properly establish correctcontinuity equation.
JBJCAJ QQQ ?
JCJBAJ QQQ?
or
d) If the continuity does not satisfy, then re-assumeanother new value for the junction head relative to theprevious assumption and the result of the continuity.
e) Repeat the above procedures from ‘a to c’ until thecontinuity at procedure ‘d’ satisfies.
Note: The head loss along a single pipe is:
hLi= = KTQi2
KT hLi = KT Qi2
ii
ii
ii
ii
Δ
Δ
Note that for any pipe headloss is:
minor5 4
L 1K f k
12.1 D 12.1 DT
if the minor loss effects are ignored, then the equation issimplified as:
5
LK f
12.1 DT
Pminor5 4 2
HL 1K f k
12.1 D 12.1 D QT
general headloss of any pipe having a pump installed over is:
ΔhL= KTQ2
Iteration Table for Branched pipes (correction for Junctions total head HJ)
Pipe
Name
Length
L
(m)
Dia.
D
(cm)
ks
(cm)
ks/D
Qi
(m3/s)
𝑅𝑒𝑖
*105
𝑓𝑖
KTi
(s2
m5)
∆hi
(m)
Qi
=∆hi
KTi
(m3/s)
𝑄𝑖
2∆ℎ𝑖
(m2/s)
𝛿h =−∑Qi
∑ Qi
2∆hi
(m)
∆hi+1= ∆hi + δh
(m)
HD(i+1)
(m)
HD(i+1)
(m)
Qi+1 =∆hi+1
KTi
(m3/s)
Iteration No: Hj=
Assume at the junction:Q (inflow) : + Q (outflow) : –
If along any pipeline portion contains a pump, than the effect of this pump should be included while calculating that portions Δh value for each iteration.
Example 6.1:For the multiple reservoir system shown, the water level elevations and
other flow parameters are detailed within the table. If the discharge of the pipe BJ,QBJ, is 100 lt/s and flows towards J and the topographic elevation of the junction atJ is zJ= 70 m; neglecting all the minor losses and assuming that the water depthswithin the reservoirs (A, B and C) remain constant; (take γ=9.8 kN/m3).
i. determine the total energy at the junction J?ii. determine the flow directions and compute the discharges of the pipes AJ and JC?
iii. determine the water elevation in the reservoir C?iv. compute the pressure head at J?v. Draw the energy grade line (EGL) of the system.
Pipe L(m) D(mm) f
AJ 1000 300 0.02
JB 1500 300 0.02
JC 2000 400 0.02
J
HJ=89.79 mQBJ=100 lt/sQAJ=87.5 lt/sQJC=187.5 lt/szC=78.44 m
Example 6.2:For the given multiple reservoir system, determine
the direction and the amount of the discharges passing ineach pipe. Water level elevations are at the reservoirs arezA=326.7 m, zB=240.2 m and zC=38.5 m. The length,diameter and type of the pipes are as tabulated. Ignore theminor losses (take γ = 9.8 kN/m3).
Pipe # Length (m) Diameter
(cm)
f
A-J: 1 3875 50 0.019
J-B: 2 2780 40 0.017
J-C: 3 1090 60 0.016
Hj ≈ 92.0 mQ1 ≈ 1.0979 m3/sQ2 ≈ 0.6233 m3/sQ3 ≈ 1.6989 m3/s
Example 6.3:
1
2
Pipe
Name
Length
L
(m)
Dia.
D
(cm)
ks
(cm)
ks/D
Qi
(m3/s)
𝑅𝑒𝑖
*105
𝑓𝑖
KTi
(s2
m5)
∆hi
(m)
Qi
=∆hi
KTi
(m3/s)
𝑄𝑖
2∆ℎ𝑖
(m2/s)
𝛿h
=−∑Qi
∑ Qi
2∆hi
(m)
∆hi+1
= ∆hi + δh
(m)
HD(i+1)
(m)
HD(i+1)
(m)
Qi+1
=∆hi+1
KTi
(m3/s)
AD 1500 30 0.026 0.00087 … … 0.019 969.360-35 =
+25+ 0.1606 0.0032
- 17.51
25 – 17.52
= +7.49
60 - 7.49
= 52.51
52.51
+ 0.0879
DB 900 25 0.09 0.0036 … … 0.0276 2102.335 – 35 =
00.0 0 0 - 17.51
= - 17.51
35 – (-17.51)
= 52.51 - 0.0912
DC 800 20 0.015 0.00075 … … 0.0183 3781.015-35=
-20- 0.0727 0.00182 -20 – 17.51
= - 37.51
15 – (-37.51)
= 52.51 - 0.0996
∑ + 0.0879 0.00502 ∑ - 0.1029 > 0.0001
(Not Ok)
First Estimate HD = HB = zB =35.0 m
Suggested total energy at D instead of 35.0 m
Pipe
Name
Len
L
(m)
Dia.
D
(cm)
ks
(cm)
ks/D
Qi
(m3
s) 𝑅𝑒𝑖
∗ 105𝑓𝑖
𝐾𝑇𝑖
(𝑠2
𝑚5)
∆ℎ𝑖
(m)
𝑄𝑖
=
∆ℎ𝑖
𝐾𝑇𝑖
(m3
s)
𝑄𝑖
2∆ℎ𝑖
(m2
s)
𝛿ℎ
=−∑𝑄𝑖
∑ 𝑄𝑖
2∆ℎ𝑖
(m)
∆ℎ𝑖+1
=
∆ℎ𝑖
+ 𝛿ℎ
(m)
𝐻𝐷(𝑖+1)
(m)
𝐻𝐷(𝑖+1)
(m)
𝑄𝑖+1
=∆ℎ𝑖+1
𝐾𝑇𝑖
(m3
s)
AD 1500 30 0.026 0.00087 + 0.0879 3.73 0.0201 1020.360-
52.51=
7.49
+0.0856 0.0057
+ 10.70
7.49
+ 10.70
= 18.19
60 -
18.19
= 41.81
41.81
+0.1335
DB 900 25 0.09 0.0036 - 0.0912 4.64 0.0279 2125.035 -
52.51=
-17.51
- 0.0907 0.0026
-17.51
+10.70
= - 6.81
35-
(-6.81)
= 41.81
- 0.0566
DC 800 20 0.015 0.00075 - 0.0996 6.35 0.0190 3925.615-
52.51=
-37.51
- 0.0977 0.0013
-37.51
+10.70
= - 26.81
15 –
(-26.81)
= 41.81
-0.0826
∑ - 0.1028 0.0096 ∑ - 0.0243 > 0.0001
(Not Ok)
Second Estimate HD = 52.51 m
At the junction:Q (inflow) : + Q (outflow) : –
Suggested total energy at D instead of 52.51 m
Pipe
Name
Len.
L
(m)
Dia.
D
(cm)
ks
(cm)ks/D
𝑄𝑖
(m3
s)
𝑅𝑒𝑖
105𝑓𝑖
𝐾𝑇𝑖
(s2
m5)
∆ℎ𝑖
(m)
𝑄𝑖
=∆ℎ𝑖
𝐾𝑇𝑖
(m3
s)
𝑄𝑖
2∆ℎ𝑖
(m2
s)
𝛿ℎ
=−∑𝑄𝑖
∑ 𝑄𝑖
2∆ℎ𝑖
(m)
∆ℎ𝑖+1
= ∆ℎ𝑖
+ 𝛿ℎ
(m)
𝐻𝐷(𝑖+1)
(m)
𝐻𝐷(𝑖+1)
(m)
𝑄𝑖+1
=∆ℎ𝑖+1
𝐾𝑇𝑖
(m3
s)
AD 1500 30 0.026 0.00087 +
0.13355.66 0.0197 1005.0 + 18.19 + 0.1345 0.0037 0.42
18.19 +
0.42 =
18.61
60 -
18.61 =
41.39
41.39
+0.13608
DB 900 25 0.09 0.0036 -
0.05662.88 0.0281 2140.2 - 6.81 - 0.0563 0.0041 0.42
- 6.81 +
0.42 =
- 6.39
35 –
(-6.39)
= 41.39
-0.05464
DC 800 20 0.015 0.00075 -
0.08265.25 0.0192 3967.0 - 26.81 - 0.0821 0.0015 0.42
-26.81 +
0.42 =
-26.39
15 –
(-26.39)
= 41.39
-0.08156
∑ - 0.0039 0.0093 ∑ - 0.00012 > 0.0001
(Not OK)
Third Estimate HD = 41.81 m
At the junction:Q (inflow) : + Q (outflow) : –
Suggested total energy at D instead of 41.80 m
Pipe
Name
Len.
L
(m)
Dia.
D
(cm)
ks
(cm)ks/D
𝑄𝑖
(m3
s)
𝑅𝑒𝑖
105𝑓𝑖
𝐾𝑇𝑖
(s2
m5)
∆ℎ𝑖
(m)
𝑄𝑖
=∆ℎ𝑖
𝐾𝑇𝑖
(m3
s)
𝑄𝑖
2∆ℎ𝑖
(m2
s)
𝛿ℎ =
−∑𝑄𝑖
∑ 𝑄𝑖
2∆ℎ𝑖
(m)
∆ℎ𝑖+1
= ∆ℎ𝑖
+ 𝛿ℎ
(m)
𝐻𝐷(𝑖+1)
(m)
𝐻𝐷(𝑖+1)
(m)
𝑄𝑖+1
=∆ℎ𝑖+1
𝐾𝑇𝑖
(m3
s)
AD 1500 30 0.026 0.00087 +
0.136085.66 0.0197 1005.0 +
18.61
+
0.13608
0.00366 0.0118.61 +
0.01 =
18.62
60 -
18.62 =
41.38
41.38
+0.1361
DB 900 25 0.09 0.0036 -
0.054642.88 0.0281 2140.2 -
6.39
- 0.05464 0.00428 0.01- 6.39 +
0.01 =
- 6.38
35 –
(-6.38)
= 41.38
-0.0546
DC 800 20 0.015 0.00075 -
0.081565.25 0.0192 3967.0 -
26.39
- 0.08156 0.00155 0.01-26.39 +
0.01 =
-26.38
15 –
(-26.38)
= 41.38
-0.08155
∑ - 0.00012 0.00949 ∑ - 0.00005 < 0.0001
(OK)
Fourth Estimate HD = 41.39 m
At the junction:Q (inflow) : + Q (outflow) : –
Suggested total energy at D instead of 41.39 m
HD=41.38 m,
AB
C
75 m20 m
50 mJ
P
D1=8 cmL1=300 mcast iron
12
3
D2=10 cmL2=500 mgalvanized iron
D3=12 cmL3=400 masphalted cast iron
Hp = 12 - 550 Q2
(Q is in m3/s)
Example T:Water at 200 C flows between three reservoirs (A, B and C). Ignore minor lossesDetermine the discharge and the flow directions in each pipe for:a) No pump along pipe 3b) 1-pump along pipe 3 that pumps water from reservoir C,c) 2-pumps in series along pipe 3 that pumps water from reservoir C.
Example T: SolutionWater at 200 C flows between three reservoirs (A, B and C). Ignore minor lossesDetermine the discharge and the flow directions in each pipe for:a) No pump along pipe 3,b) 1-pump along pipe 3 that pumps water from reservoir C,c) 2-pumps in series along pipe 3 that pumps water from reservoir C.
a) No pump Hj≈ 48.80 m where Q1 + Q3 = Q2
Q1 = 0.01107 m3/s, Q2 = 0.01725 m3/s, Q3 = 0.00618 m3/s
b) 1-pump Hj≈ 58.27 m where Q1 + Q3 = Q2
Q1 = 0.00882 m3/s, Q2 = 0.01993 m3/s, Q3 = 0.01111 m3/s
c) 2-pumps series Hj≈ 66.53 m where Q1 + Q3 = Q2
Q1 = 0.00624 m3/s, Q2 = 0.02201 m3/s, Q3 = 0.01577 m3/s
AB
C
75 m20 m
50 mJ P
D1=8 cmL1=300 mcast iron
12
3
D2=10 cmL2=500 mgalvanized iron
D3=12 cmL3=400 masphalted cast iron
Hp = 12 - 550Q2
(Q is in m3/s)
Example T:Water at 200 C flows between three reservoirs (A, B and C). Ignore minor losses.Determine the discharge and the flow directions in each pipe for: a) 1 pump along pipe 3 that pumps water to reservoir C,b) 2-pumps in series along pipe 3 that pumps water to reservoir C,c) 3-pumps in series along pipe 3 that pumps water to reservoir C,d) 4-pumps in series along pipe 3 that pumps water to reservoir C.
Example T: SolutionWater at 200 C flows between three reservoirs (A, B and C). Ignore minor losses.Determine the discharge and the flow directions in each pipe for: a) 1 pump along pipe 3 that pumps water to reservoir C,b) 2-pumps in series along pipe 3 that pumps water to reservoir C,c) 3-pumps in series along pipe 3 that pumps water to reservoir C,d) 4-pumps in series along pipe 3 that pumps water to reservoir C.
a) Not possible since Hj > 38.0 m does not satisfy Q1 = Q2 + Q3
b) 2-pumps in series Hj ≈ 27.33 m where Q1 = Q2 + Q3
Q1 = 0.01498 m3/s, Q2 = 0.00856 m3/s, Q3 = 0.00642 m3/sc) 3-pumps in series Hj ≈ 20.34 m where Q1 = Q2 + Q3
Q1 = 0.01605 m3/s, Q2 = 0.00169 m3/s, Q3 = 0.01436 m3/s d) 4-pumps in series Hj ≈ 16.89 m where Q1 + Q2 = Q3 (continuity equation changed!)
Q1 = 0.01655 m3/s, Q2 = 0.00549 m3/s, Q3 = 0.02204 m3/s
Example T:
For the given multi-reservoir system, determine the amount of flow passing from each pipeline with their directions.
QAJ = 516 lt/s , QBJ = 267 lt/s , QJM = 248 lt/s , QCM = 454 lt/s, QDM = 205 lt/s HJ = 82.24 m HM = 89.70 m
M
Question 4: (35 points)
Find the flow distribution of water at 23°C in the branching system (QA=?, QB=?, QC=? and QD=?).
For simplicity take f=0.02 for all the pipes. The pump manufacturer suggested that Hp=120-0.5Q2. (Hp (m),
Q(m3/s)). Note that water surface elevations at the reservoirs are kept as constant: zA=20 m, zB=52 m, zC=105
m, zD=40 m. Use at least 3 trials.
ANSWER: From QA = 0.9032 m3/s
To QB = 0.4070 m3/s, QC = 0.1003 m3/s QC = 0.3963 m3/s.
Pipe Length ‘L’ (m) Diameter ‘ϕ’ (mm) Total Minor Loss ‘Σk’ [-]
1 263.2 500 7.82
2 789.3 320 2.6
3 2106.8 300 3.8
4 1551.8 350 3.6
Below given reservoir-pipeline-pumping system plan, water @ 13 °C is discharging from pipe 4 to the atmosphere at
a rate of Q4=63.50 lt/s. The system is functioning under the absolute atmospheric pressure Patm=101.17 kPa (abs).
a) Determine the discharges flowing within other pipes? (20 p)
b) The topographic water surface elevation of reservoir C? (5 p)
c) The required power ‘P’ for this pumping system. (8 p)
d) What should be the maximum topographic elevation at junction B ‘zB’ for no cavitation. (7 p)
Single pump ‘Hp – Q’ characteristic is:
Q (lt/s) 0 10 20 30 40 50 53
Hp (m) 10.75 10.37 9.23 7.33 4.67 1.25 0
η (%) 57.8 71.5 83.6 75.2 51.8 38.9 0
Equation of a Single pump: Hp = 10.75 - 3800Q2 (where Q in [m3/s] and Hp in [m])
Previous Exam Question:
If in a water distribution system all the pipes coming outfrom one reservoir and get increased by branches wherenone of them ever get reconnected or interconnectedagain so as to form loops are called BRANCHED (OPEN)NETWORK.This distribution network mainly used for municipalitiessince requires less number of pipes but having lots ofweaknesses, hence not recommended nowadays.Nowadays, the most popular system in municipalities isthe LOOP (CLOSED) NETWORK where all the pipes areinterconnected with each other by forming junctions andloops. This system having more advantages than branchednetworks.
6.2 Interconnected Pipeline Systems
6.2 Interconnected Pipeline Systems
This type of water distribution network analysis, providesthe basis for the design of new systems and the extensionof the existing systems.
In fact, an extension of pipes in parallel is a casefrequently encountered in municipal distribution systems,in which the pipes are interconnected, so that the flow tothe given outlet may come by several different paths.
Indeed, it is frequently impossible to tell by inspection,which direction the flow occurs. Nevertheless, the flow inany network, however is complicated and must satisfy thebasic relations: the continuity and the energy equations.
Design criteria are those specified as minimum flow ratesand pressure heads that must be attained at the outletpoints of the network.
It should be remembered that, the flow and pressuredistribution across a network are affected by thearrangement and the size of the pipes and thedistribution of the outflows.
Since a change of diameter in one pipe length will affectthe flow and pressure distribution everywhere, networkdesign is not an explicit process.
Hence, designing any section between any twojunctions can not be done by isolating thatportion! The whole network should beconsidered.
For the analysis, the determination of the pipe flowrates and pressure heads which satisfies thecontinuity and energy conservation equationsshould be used.
In literature the common solution techniques for this typeof connections are:I. The Head Balance Method (‘LOOP METHOD’)
[HARDY-CROSS METHOD]II. The Quantity Balance Method (‘NODAL METHOD’)III. The Newton – Raphson MethodIV. The Linear Theory Method.
Closed Network Sistems
SOLUTIONOF
INTERCONNECTED PIPELINE SYSTEMBY
HARDY-CROSS METHOD
It is the earliest (1936) systematic method used for network analysis
Solution procedure of Hardy-Cross method:1. Check the continuity of the whole system,
2. Name and/or label each and every node and pipe within the system,
3. Determine and give different names for each loop and also assign+ve flow direction for each loop. For the sign convection selectingthe clockwise flow as positive is a usual procedure.
1. Assign an arbitrary direction and a discharge value for one of thepipes in each loop and hence distribute the flow at each node byconsidering the continuity equation. It is a good practice NOT toassume a zero flow to any pipe. Note that: for problems of 2 loopsonly 2 (1 for each loop) arbitrary discharge values and directionswill be assinged.
+ Q
5. For each loop, obtain the energy equation by considering thesuggested directions and discharges. It is definite that, for thecommon pipe of two loops, if the error obtained from the previousloop is applied after correction to the other loop, then the number ofiteration needed to reach to the required solution will be reduced!
6. For the second trial, use the previously calculated discharge values ineach pipe of that Loop,
7. Until the required acceptable limit is reached for the whole system,the number iterations should be continued.
To determine the required correction, thebasic assumption comes from the headbalance criterion where the algebraic sumof the losses around any closed loop shouldbe zero; Δh=0.
KT (i)
But if the minor loss effects are ignored, then theequation is simplified as:
D 12.1
LfK
5
i
iiT(i)
2
minor5 4 2
L 1f k Q
12.1 D 12.1 D
PH
Q
The head loss along a single pipe is:
hL=2
minor5 4
L 1f k Q
12.1 D 12.1 D
= KT(i)Q(i)
2(i)
Δ
KT(i)
The head loss along a single pipe with a pump installed is:
hL(i)=Δ
For the estimation of flow error ΔQ:
2
(i)(i)(i)
2
(i)T(i)
2
(i)(i)T(i)L(i) QQQ2QKQQKh
Neglecting ΔQ(i)2, by assuming ΔQ(i) is a small value,
then:
(i)(i)
2
(i)T(i)L(i) QQ2QKh
So within a close loop since ΣhL= 0 from the continuity,
Neglecting the minor losses in the pipes, for the given data, using Hardy-Cross Method, determine the flow
in each pipe. Note that for simplicity, let f=0.0193 for pipes constant, do for ΔQ < 0.5 lt/s.
Pipe AB BC CD BD DE AE
Length (m) 600 580 215 480 810 335
Diameter (mm) 250 150 200 220 100 150
Example 6.4:Neglecting the minor losses in the pipes, for the given data, using Hardy-Cross Method, determine the flow
in each pipe. Note that for simplicity, let f=0.0193 for pipes constant, do for ΔQ < 0.5 lt/s.
Pipe AB BC CD BD DE AE
Length (m) 600 580 215 480 810 335
Diameter (mm) 250 150 200 220 100 150
Example 6.4:
115.696 lt/s
5.643 lt/s
54
.35
7 lt
/s
49.422 lt/s
34.076 lt/s
Example 6.5:
++
Iteration 1
Loop
I
pipe ks(cm) D(cm) ks/D L(m) Q(L/s) Re*105 f K KQ 𝑄 2K 𝑄 ∆Q(m
3/s)
AB 0.006 25 0.00024 500 120 5.408 0.0158 668.562 9.627 160.455
-0.00579
BE 0.006 15 0.0004 200 10 0.751 0.0207 4505.663 0.451 90.113
EF 0.006 20 0.0003 600 -40 2.254 0.0175 2711.777 -4.339 216.942
FA 0.006 25 0.00024 300 -80 3.606 0.0163 413.831 -2.649 66.213
∑ 3.09 533.723
Loop
2
pipe
-0.0117
BC 0.006 15 0.0004 400 50 3.756 0.0176 9294.290 23.24 929.429
CD 0.006 10 0.0006 200 10 1.127 0.0206 34049.59 3.405 680.992
DE 0.006 15 0.0004 400 -20 1.502 0.019 8271.265 -3.309 330.851
EB 0.006 15 0.0004 200 -4.21 0.316 0.0243 5289.256 -0.094 44.536
∑ 23.24 1985.808
ΔQ < 0.5 lt/s NOT OK
This pipe is a common pipe for loop 1 and 2. So the discharge of this common Pipe is corrected based on the previous loops discharge error.
T
Iteration 2
Loop
1
pipe ks(cm) D(cm) ks/D L(m) Q(L/s) Re*105 f K KQ 𝑄 2K 𝑄 ∆Q(m
3/s)
AB 0.006 25 0.00024 500 114.21 5.147 0.0159 672.793 8.776 153.679
-0.00199
BE 0.006 15 0.0004 200 15.91 1.195 0.0195 4244.465 1.074 135.059
EF 0.006 20 0.0003 600 -45.79 2.58 0.0173 2680.785 -5.621 245.506
FA 0.006 25 0.00024 300 -85.79 3.867 0.0162 411.293 -3.027 70.57
∑ 1.202 604.814
Loop
2
pipe
-0.00327
BC 0.006 15 0.0004 400 38.3 2.877 0.0179 9424.889 13.83 721.946
CD 0.006 10 0.0006 200 -1.7 0.192 0.0275 45454.55 -0.131 154.545
DE 0.006 15 0.0004 400 -31.7 2.381 0.0182 7923.001 -7.962 502.318
EB 0.006 15 0.0004 200 -13.92 1.046 0.0198 4309.764 -0.835 119.984
∑ 4.902 1498.793
ΔQ < 0.5 lt/s NOT OK
This pipe is a common pipe for loop 1 and 2. So the discharge of this common Pipe is corrected based on the previous loops discharge error.
T
Iteration 3
Loop
1
pipe ks(cm) D(cm) ks/D L(m) Q(L/s) Re*105 f K KQ 𝑄 2K 𝑄 ∆Q(m
3/s)
-0.00074
AB 0.006 25 0.00024 500 112.22 5.058 0.0159 672.793 8.473 151.002
BE 0.006 15 0.0004 200 17.19 1.291 0.0193 4200.932 1.241 144.428
EF 0.006 20 0.0003 600 -47.78 2.692 0.0172 2665.289 -6.085 254.695
FA 0.006 25 0.00024 300 -87.78 3.956 0.0162 411.293 -3.169 72.207
∑ 0.46 622.332
Loop
2
pipe
1.68E-05
BC 0.006 15 0.0004 400 35.03 2.631 0.018 9468.422 11.62 663.358
CD 0.006 10 0.0006 200 -4.97 0.56 0.0226 37355.37 -0.923 371.312
DE 0.006 15 0.0004 400 -34.97 2.627 0.018 7835.935 -9.583 548.045
EB 0.006 15 0.0004 200 -16.45 1.236 0.0194 4222.698 -1.143 138.927
∑ -0.029 1721.642
V
ΔQ < 0.5 lt/s NOT OK FOR LOOP 1 SO NEEDS CORRECTION ALTHOUGH LOOP 2 SATISFIES
This pipe is a common pipe for loop 1 and 2. So the discharge of this common Pipe is corrected based on the previous loops discharge error.
T
V
Iteration 4
Loop
1
pipe ks(cm) D(cm) ks/D L(m) Q(L/s) Re*105 f K KQ 𝑄 2K 𝑄 ∆Q(m
3/s)
AB 0.006 25 0.00024 500 111.48 5.024 0.0159 672.793 8.361 150.006
-4.8E-06
BE 0.006 15 0.0004 200 16.43 1.234 0.0194 4222.698 1.14 138.758
EF 0.006 20 0.0003 600 -48.52 2.734 0.0172 2665.289 -6.275 258.64
FA 0.006 25 0.00024 300 -88.52 3.99 0.0162 411.293 -3.223 72.815
∑ 0.003 620.219
ΔQ < 0.5 lt/s OK
T
BA C
E D
200 lt/s60 lt/s
30 lt/s
30 lt/s40 lt/s
F
40 lt/s
111.48111.48112.22114.21120
16.4316.43 16.4316.45 17.1913.92 15.9110 4.21
48.5248.5247.7845.7940
88.5288.5287.7885.7980
35.05
35.03
38.3
50
- 4.95
- 4.97
- 1.710
34.95
34.97
31.720
BA C
F E D
120 lt/s 45 lt/s
10 lt/s
50 lt/s75 lt/s60 lt/s
Example 6.6:
+
Example 6.6:
BA C
F E D
120 lt/s45 lt/s
10 lt/s
50 lt/s
75 lt/s60 lt/s
69.48
24
.63
9.48
50
.52
0.159
.85
59.85
EA+=𝑃𝐴+
𝛾+
𝑣𝐴+2
2𝑔+ 𝑧𝐴+= 68.6 m
EB−= 68.6 – 3.854 = 64.746 m
EA+=EB- + ∑ ℎ𝑙𝑜𝑠𝑠 𝐴−𝐵 EB−=𝑃𝐵−
𝛾+
𝑣𝐵−2
2𝑔+ 𝑧𝐵−
∴PB−
γ+ 0.102 +26.8 = 64.746 PB−
γ= 37.844 m
For the given flow network system, determine the discharge passing in each pipe.Take υ =1.004x10-6 m2/s. Solve until ΔQ < 0.50 lt/s.The pump characteristic in pipe 1 : Hp = 18.0 – 0.009Q2 (put Q as lt/s to this equation)
or : Hp = 18.0 – 9000Q2 (put Q as m3/s to this equation).
Example 6.7 T:
43.811
14.189
24.811
41.189
36.358
68.358
25.642
Answer 6.7 T:
ITERATION TABLE FOR MULTI-RESERVOIRS (BRANCHED-PIPES)
(CORRECTION BASED ON JUNCTION POINT TOTAL ENERGY HEAD ‘HJUNCTION’)
Iteration No:
Pipe
Name
Pipe
Length L
(m)
Diameter D
(cm)
k
s
(cm)
ks/D Q
i
(m3/s)
𝐑𝐞
*105 𝐟
KTi
(𝐬𝟐
𝐦𝟓)
∆𝐡𝐢
(m)
𝐐𝐢
= ∆𝐡𝐢
𝐊𝐓𝐢
(m3/s)
𝐐𝐢
𝟐∆𝐡𝐢
(m2/s)
𝛅𝐡
=−∑𝐐𝐢
∑ 𝐐𝐢
𝟐∆𝐡𝐢
(m)
∆𝐡𝐢+𝟏
= ∆𝐡𝐢 + 𝛅𝐡
(m)
𝐇𝐃(𝐢+𝟏)
(m)
𝐇𝐃(𝐢+𝟏)
(m)
𝐐𝐢+𝟏
= ∆𝐡𝐢+𝟏
𝐊𝐓𝐢
(m3/s)
Iteration No:
LOOP Diameter Material
# (φ) (ks)
Σ
KT KTQ│Q│ 2KT│Q│Re Length (L)Pipe Name Q
f
)
)(
(
Hardy-Cross Method Correction Table
EPANET• EPANET is a program for analyzing the hydraulic and
water quality behavior of pressurized pipe networks(both JUNCTION & LOOP problems).
• It was developed by the U.S. Environmental ProtectionAgency's National Risk Management ResearchLaboratory.
• It is public domain software that may be FREELYCOPIED and DISTRIBUTED.
• A complete Users Manual as well as full source codeand other updates can be downloaded from:www.epa.gov/ORD/NRMRL/wswrd/epanet.html.
• You can download this software through the following like:
https://www.epa.gov/sites/production/files/2014-06/en2setup_0.exe