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Flow structure in front of the broad-crested weir

Abstract

The paper deals with research focused on description of flow structure in front of broad-crested weir. Based on experimental measurement, the flow structure in front of the weir (the recirculation zone of flow and tornado vortices) and flow structure on the weir crest has been described. The determined flow character has been simulated using numerical model and based on comparing results the suitable model of turbulence has been recommended.

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Flow structure in front of the broad-crested weir

Author: Zachoval, Zbyněk; Roušar, Ladislav
Publisher: EDP Sciences
Year: 2014
DOI: 10.1051/epjconf/20159202117
Source: https://dspace.vut.cz/bitstreams/f10483c8-9cb2-43d2-8d9c-45306b3415ff/download
a Co esponding au ho : [email p o ec ed]
Flow s uc u e in on o he b oad-c es ed wei
Zbynk Zacho al1,a and Ladisla Rouša 2
1BUT, FCE, IWS, LWMR, 602 00 B no, Czech Republic
2BUT, FCE, IWS, 602 00 B no, Czech Republic
Abs ac . The pape deals wi h esea ch ocused on desc ip ion o low s uc u e in on o b oad-c es ed
wei . Based on expe imen al measu emen , he low s uc u e in on o he wei ( he eci cula ion zone o
low and o nado o ices) and low s uc u e on he wei c es has been desc ibed. The de e mined low
cha ac e has been simula ed using nume ical model and based on compa ing esul s he sui able model o
u bulence has been ecommended.
1 In oduc ion
Rec angula b oad-c es ed wei s a e equen ly used o
he de e mina ion o discha ge [1]. Wei s a e moun ed in
a p isma ic ec angula channel usually he same wid h B
as wid h o wei b o su icien ly inc ease wa e su ace,
ne e hless, do no in luence on maximum capaci y o
channel. The wei c es is ho izon al wi h he wei
hickness , he ups eam and downs eam aces a e
e ical, he wei su ace is smoo h, he ups eam and
downs eam wei edges a e sha p and he wei heigh is P
(Figu e 1). The e o o moun ing hem is o ensu e a
ee o e low in whole a ange o measu ing discha ges
[2].
Rec angula b oad-c es ed wei s o m h ee
eci cula ion zones o low [3]: ups eam [4], c es [5]
and downs eam eci cula ion zones [3] (Figu e 1). The
ups eam and c es eci cula ion zones ha e an in luence
on a wei capaci y, he downs eam eci cula ion zone
does no because he pa allel supe c i ical low is c ea ed
on he wei c es [6].
2 Flow s uc u e in on o he b oad-
c es ed wei
A di e en ela i e wei heigh s h/P, a di e en low
s uc u e o ms in on o ups eam ace [7]. In a case o
high wei s, he ups eam eci cula ion zone is no o med;
in medium-high wei s, only he ups eam eci cula ion
zone is o med; and in low wei s, he ups eam
eci cula ion zone is o med and is supplemen ed by
o nado o ices [8-11]. The c i e ia o he o ma ion o
indi idual low s uc u es ha e been de e mined by
Zacho al and Rouša [12].
Lu z
P
hu z ups eam
eci cula ion
zone
c es eci cula ion
zone
L
h
poin o low s agna ion
line o low s agna ion
ups eam
eci cula ion
zone
a ea o
low
s agna ion
line o
low
s agna ion
a ea o
de eloping
o eces
bed
s eamline
a e age posi ion o
o nado o ex axis
Lc z
hc z
c es
eci cula ion
zone
Figu e 1. Scheme o wei , low and no a ion o a iables.
3 Re iew o nume ical models o low
o e b oad-c es ed wei
The nume ical modelling o po en ial low o e b oad-
c es ed wei was in es iga ed by, e.g., Moos [13],
S ee ha an [14], Dias e al. [15]. Howe e , he po en ial
low does no desc ibe eci cula ion zones o low, hence
he esul s we e di e en . To achie e eliable esul s o
DOI: 10.1051/
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A icle a ailable a h p://www.epj-con e ences.o g o h p://dx.doi.o g/10.1051/epjcon /20159202117
ansi low, hey mus ha e been composed by special
ways [13].
The simula ion o o ical low o e ec angula wei
was s udied by Bomba deli e al. [16]. They used 2D
model o u bulen low o incomp essible iscous
liquid. The low was desc ibed by Reynolds-a e aged
Na ie –S okes equa ions (RANS). Tu bulence was
sol ed by Reno malized G oup (RNG) k-
ε
model [17].
They compa ed esul s wi h measu emen s Hage and
Schwal [18] and s a ed good ag eemen wi h a pa e n o
wa e su ace e en in ange o he c es eci cula ion
zone. Shake and Rhodes [19] simula ed wo phase low
in 3D desc ibed by RANS equa ions supplemen ed wi h
k-
ε
u bulence model [20] and wall unc ion. To
de e mine wa e su ace hey used Volume o luid
(VOF) me hod [21]. They ound good ag eemen wi h
low and wa e su ace le el, only hey no ed di e ences
in posi ion o he c es eci cula ion zone and in pos i ion
o a nappe. Ha gea es e al. [22] simula ed wo phase 2D
low (one case 3D) and es ed h ee di e en u bulence
models k-
ε
, RNG k-
ε
and Reynolds S ess Model (RSM)
[23]. RNG k-
ε
and RSM u bulence models simula ed
low mo e eliable han k-
ε
. They de e mined ha 3D
model does no p o ide in compa ison wi h 2D model a
imp o emen in pa e n o wa e su ace. The g ea es
di icul ies hey saw in simula ion o hyd aulic jump and
a ea ion o low. Hsu and Ozdemi [24] modeled he
same low as Ha g ea es and concen a ed on
compa ison wi h RNG k-
ε
and RSM u bulence models.
They s a ed ha model RSM yields be e esul s o
wa e su ace le el. Ki kgoz e al. [11] deal wi h 2D
modelling. They compa ed nume ically sol ed po en ial
low ield, nume ically sol ed low ield wi h he use o
RANS equa ions and k-
ω
[25] and k-
ε
ubulence models
wi h measu ed by me hod Pa icle Image Velocime y
(PIV) [26]. They ecommended RANS app oach wi h k-
ω
u bulence model. Adegbulugbe [27] ca ied ou a s udy o
he ela ed e i ica ion as Ha g ea es e al. [22]. He
claimed ha he mos accu a e esul s we e ob ained
using wi h RNG k-
ε
u bulence model.
4 Expe imen
Fo compa ing was chosen he wei desc ibed by
Zacho al e al. [29]. The wei was made o o ganic glass,
was moun ed in o a ec angula lume, wi h wei heigh
P = 0.250 m, wid h b = 1.003 m and hickness
= 0.500 m. The eloci y ield measu emen s was
conduc ed wi h a combina ion o Ul asonic Veloci y
P o ile (UVP) Moni o and PIV. The eloci y ield was
measu ed a inle channel by UVP Moni o [29] and in
on o he wei and on he wei c es by PIV [5]. The
shape o eci cula ion zones was isualiza ed by dye and
by pa icles added in o low. The ea e , he low
s uc u e was displayed by pa icles mo ing on he
bo om. The le el o wa e su ace was measu ed by a
poin gauge and he discha ge was de e mined by
calib a ed iangula sha p-c es ed wei .
5 Nume ical model
5.1 Selec ed app oach
The a ie y o app oaches may be used o sol ing low
s uc u e in on o he ec angula b oad-c es ed wei .
E e y app oach b ings wi h i a ce ain deg ee o
simpli ica ion and, he eby e o desc ip ion compa ed
wi h eali y. The equi emen s o he esul s de e mine
he choice o empo al and spa ial schema iza ion.
Fo sol ing s eady o e low om a mac oscopic iew
desc ibed by pa e n o wa e su ace and by ime-
a e aged eloci y ield he models we e used based on
RANS equa ions and La ge eddy simula ion (LES) model
wi h Smago insky subg id-scale (SGS) model. The
modelling o eci cula ion zones no a ec ed side walls
was pe o med by 2D and o nado o ex by 3D due o
hei spa ial cha ac e . Fo modelling u bulence wi h
RANS app oach he i s o de models we e selec ed
based on u bulence iscosi y: one laye models S anda d
k-
ε
, RNG k-
ε
, S anda d k-
ω
models and wo laye Shea
S ess T anspo (SST) model [28]. Fu he , he second
o de models we e used based on Reynolds s ess
anspo equa ion [23]: Baseline (BSL) Reynolds S ess
(RS) and Speziale-Sa ka -Ga ski (SSG) RS [30]. Fo
sol ing he so wa e we e used ANSYS-CFX (3D, 2D)
(Figu e 2) – wo phase low, ANSYS-Flo an (2D)
(Figu e 3) – one phase low and Flow-3D (2D) (Figu e 4)
– one phase low.
5.2 Calcula ion
Fluid domain geome y included he inle channel, he
wei and a pa o ou le channel wi h ee nappe. The
inle channel leng h was so long o de elop eloci y
p o ile.
A inle bounda y he hyd os a ic p essu e
dis ibu ion was se o a dep h es ablished om he
measu emen s and a cons an eloci y. A ou le bounda y
he ee ou low was se . The walls we e hyd aulically
smoo h. The hal domain was sol ed because longi udinal
symme y. The e e ence p essu e was ze o.
The numbe o elemen s depended on used so wa e
and dimension, o 2D model i was app oxima ely om
1·105 (Flow-3D, ANSYS-Flo an) o 5·105 (ANSYS-
CFX) and o 3D model 5·106. The calcula ions we e
pe o med in ange o discha ges 0.040 m3/s, 0.070 m3/s
and 0.130 m3/s. Ma e ial p ope ies o wa e we e:
densi y 998 kg/m3 and iscosi y 1·10-6 m2/s. All
coe icien s o u bulence models we e le unchanged.
The mesh was s uc u ed wi h ec angula elemen s.
5.3 E alua ed pa ame e s
The e alua ed pa ame e s we e he o e low head h a a
gi en discha ge, he leng h o c es eci cula ion zone
Lc z, he heigh o c es eci cula ion zone hc z, he leng h
o ups eam eci cula ion zone Lu z, he heigh o
ups eam eci cula ion zone hu z and he a e age posi ion
o o nado o ex axis L .
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6 Resul s
The measu ed alues o e alua ed pa ame e s calcula ed
o he discha ge 0.070 m3/s a e shown in Table 1.
The esul s 2D calcula ions a e p esen ed in he o m
o eloci y ields o all e alua ed discha ges sol ed by
all so wa e.
Table 1. E alua ed pa ame e s [uni s in m], 2D, Q = 0.070 m3/s.
Model h Lc z h
c z L
u z h
u z
Measu ed 0.131 0.108 0.022 0.140 0.140
S anda d k-
ε
ANSYS-Flo an
ANSYS-CFX
Flow-3D
0.132
0.129
0.129
0.050
0.100
0.087
0.006
0.019
0.013
0.087
0.142
0.198
0.067
0.075
0.103
RNG k-
ε
ANSYS-Flo an
ANSYS-CFX
Flow-3D
0.130
0.130
0.127
0.068
0.130
0.081
0.008
0.020
0.012
0.072
0.148
0.144
0.060
0.106
0.084
S anda d k-
ω
ANSYS-Flo an
ANSYS-CFX
0.129
0.132
0.057
0.069
0.006
0.011
0.139
0.165
0.061
0.111
SST
ANSYS-Flo an
ANSYS-CFX
0.128
0.130
0.074
0.114
0.015
0.020
0.360
0.162
0.113
0.111
BSL RS
ANSYS-CFX 0.129 0.123 0.020 0.197 0.128
SSG RS
ANSYS-CFX 0.129 0.143 0.021 0.230 0.114
LES
(Smago insky SGS)
Flow-3D
0.128 0.092 0.015 0.317 0.116
Figu e 2. ANSYS-CFX, 2D, k-
ε
, 0.070 m3/s, eloci y ield.
Figu e 3. ANSYS-Flo an, 2D, k-
ε
, 0.040 m3/s, eloci y ield
Figu e 4. Flow-3D, 2D, k-
ε
, 0.130 m3/s, eloci y ield.
Figu e 5. To nado o ex.
Figu e 6. ANSYS-CFX, 2D, SST, 0.070 m3/s, s eamlines.
Figu e 7. ANSYS-CFX, 3D, SST, 0.070 m3/s.
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.
7 Conclusions
F om he esul s in Table 1 is e iden ha alues o
e alua ed pa ame e s change wi h used so wa e and
u bulence model.
P ac ically, all one laye models based on u bulen
iscosi y unde es ima e a size o eci cula ion zones. The
mos eliable esul s o hem RNG k-
ε
u bulence model
p o ide. The models based on Reynolds s ess anspo
equa ion o e es ima e he leng h o eci cula ion zones in
di ec ion o low. Two laye s model SST p o ides he
mos eliable esul s om all used models (Figu e 6).
LES model o e es ima es he leng h o ups eam
eci cula ion zone. O e es ima ion o he leng h o
ups eam eci cula ion zone may be caused by a ac ha
he nume ical model due o small numbe o elemen s
does no simula e o ices a ising nea he bed in on o
he ups eam eci cula ion zone [12].
The alues o esul s in Table 1 a e signi ican ly
dependen on he elemen size which i is mainly
e lec ed a he heigh o c es eci cula ion zone. The
bes esul s a e achie ed wi h he la ges numbe o
elemen s which explains he di e ences in esul s wi h
used so wa e.
The sol ed o e low head was p ac ically o all
models sligh ly smalle han measu ed. E o o i s
de e mina ion is in all cases up o 3 %. The co ec
modelling o he heigh o he c es eci cula ion zone is
essen ial o de e mina e he o e low head. The e o e, i
is ecommended o use a leas 8 elemen s along i s
heigh . In he case o using a smalle numbe o elemen s
he modelled c es eci cula ion zone is smalle . In he
case o using a la ge numbe o elemen s ha ing no
signi ican e inemen i s heigh . The co ec modelling o
he ups eam eci cula ion zone has signi ican ly less an
in luence on he o e low head han he c es
eci cula ion zone.
To nado o ex (Figu e 5) was able o simula e
(Figu e 7), i s posi ion is in a ange o measu ed alues
[12]. The low in a ea o o nado o ex is de eloped
du ing he simula ion p ocess as he las . The e o e, he
su icien numbe o simula ion is necessa y o pe o m.
Fo de e mining o he o e low head has negligible
e ec .
Fo p ac ical use in de e mining o he o e low head
a known discha ge and ice e sa is possible due o he
ela i ely small demands on mesh and high accu acy
de e mina ion o low cha ac e o ecommend RANS
app oach and a wo laye SST u bulence model.
Acknowledgmen s
Acknowledgmen s a e due o p ojec s FAST-S-14-2203 -
Cha ac e is ics o subme gence o low ec angula b oad-
c es ed wei s and FAST-S-13-2010 T anspo o pa icles
o e he ec angula b oad-c es ed wei .
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