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Characterization of the scour cavity evolution around a complex bridge pier

Abstract

A study on the time development of local scour around a complex pier was developed using a small-scale model embedded in a sediment bed. A total of 15 laboratorial tests were performed at the Hydraulics Laboratory of the Faculty of Engineering of the University of Porto. The duration of each experiment was previously established to progressively characterize the scour cavity. After each experiment, the flume was gradually emptied to facilitate the application of close-range photogrammetry. The scour depth values resulting from the application of photogrammetry at the pile cap front agree well with the values obtained experimentally. The temporal development of the scour cavity is presented and discussed. Empirical formulas for the scour cavity time development and for the relation of scour depths to scour cavity volumes were obtained. The obtained three-dimensional models can also be used for calibration and validation of numerical models.

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Characterization of the scour cavity evolution around a complex bridge pier

Author: Pedro Ramos,Ana Bento,Rodrigo Maia,João Pedro Pêgo
Year: 2015
DOI: 10.1080/23249676.2015.1090353
Source: https://repositorio-aberto.up.pt/bitstream/10216/81114/2/104950.pdf
Cha ac e iza ion o he scou ca i y e olu ion a ound a complex
b idge pie
Ped o Xa ie Ramos1, Ana Ma ga ida Ben o1, Rod igo Maia1 e João Ped o
Pêgo1
1Ci il Enginee ing Depa men , Uni e si y o Po o – Facul y o Enginee ing, Po o,
Po ugal and CIIMAR - In e disciplina y Cen e o Ma ine and En i onmen al
Resea ch
E-mail: jppego@ e.up.p
Abs ac
A s udy on he ime de elopmen o local scou a ound a complex pie was
de eloped using a small-scale model embedded in a sedimen bed. A o al o 15
labo a o ial es s we e pe o med a he Hyd aulics Labo a o y o he Facul y o
Enginee ing o he Uni e si y o Po o. The du a ion o each expe imen was
p e iously es ablished o p og essi ely cha ac e ize he scou ca i y. A e each
expe imen , he lume was g adually emp ied o acili a e he applica ion o close-
ange pho og amme y. The scou dep h alues esul ing om he applica ion o
pho og amme y a he pile cap on ag ee well wi h he alues ob ained
expe imen ally. The empo al de elopmen o he scou ca i y is p esen ed and
discussed. Empi ical o mulas o he scou ca i y ime de elopmen and o he
ela ion o scou dep hs o scou ca i y olumes we e ob ained. The ob ained h ee-
dimensional models can also be used o calib a ion and alida ion o nume ical
models.
Keywo ds: Complex b idge pie ; Local scou ; Scou ca i y; Pho og amme y,
Sedimen anspo
In oduc ion
Local scou a ound pie s is he main cause o s uc u al collapse o b idges, due o
ailu e o piles ounda ions in i e beds. In he ecen decades, many esea che s ha e
in es iga ed he low and he scou pa e ns a ound b idge pie s.
A la ge numbe o s udies ocused essen ially in he p edic ion o he scou
dep h in he base o pie s (B euse s e al. 1977; B euse s and Raudki i 1991; Mel ille
and Coleman, 2000). These s udies we e mos ly done by expe imen al means, esul ing
in semi-empi ical equa ions o he e alua ion o he maximum scou dep h (Da gahi,
1990). Fo a be e unde s anding o he low ield a ound pie s, se e al esea che s
ha e s udied he low ield a ound cylinde s and pie s (Da gahi, 1989; G a and
Yulis iyan o, 1998; E ema e al. 2006; Dey and Rayka , 2007). Mos o he men ioned
s udies ha e only analysed he local scou a ound single pie s. Howe e , b idge design
commonly leads o he conside a ion o complex pie ounda ions, mos usually
in eg a ing a bo om pile on he op o a pile g oup, in which he di ec applica ion o
he esul s de i ed om single pie s is mos o en un eliable (Lande s and Muelle ,
1996). Resea che s as Coleman (2005), A aie-Ash iani e al. (2010) and Mo eno e al.
(2012) ha e ocused hei s udies on he p edic ion o he maximum scou dep h a ound
pile g oups and complex pie s.
The p edic ion o in si u scou a b idge pie s using empi ical o mulas should be
done wi h cau ion since hey we e de i ed mainly om small-scale labo a o y
expe imen s. This led o he de elopmen o ma hema ical models capable o simula ing
he scou ing p ocess a b idge pie s, known in he li e a u e as Compu a ional Fluid
Dynamics (CFD) ools. Olsen and Melaaen (1993) de eloped a 3D model o scou
a ound a ci cula single pie . A compa ison wi h expe imen ally measu ed scou
pa e ns e ealed good ag eemen . Tseng e al. (2000) pe o med 3D calcula ions o he
low a ound a e ical wall-moun ed cylinde using la ge-eddy simula ion (LES),
alida ing he esul s agains Da gahi’s (1989) expe imen al da a. Abdelaziz (2011)
simula ed he low and he sedimen anspo a ound a ci cula pie o compa e wi h he
eloci y ields and he opog aphic da a expe imen ally ob ained by Unge and Hage
(2006).
Fo a well-calib a ed nume ical model, good expe imen al da a is essen ial. To
he au ho s’ knowledge, he e a e no de ailed ime measu emen s o he scou ca i y
geome y de elopmen in he icini y o a complex pie (see Figu e 1).
The main goal o he p esen s udy is he h ee-dimensional cha ac e iza ion o
he scou e olu ion a ound a complex pie by close- ange pho og amme ic means. The
applica ion o pho og amme y in his ield is s ill in he beginning (Rapp and Ede ,
2012), bu i has p o ed o p o ide eliable insigh s in o he whole scou ca i y
geome y, leading o a deepe unde s anding o such phenomena. I has mos ly been
used o measu e he scou ca i y a ound single pie s (P lege e al. 2010; Ede e al.
2011, Rapp e al. 2012). The p oposed me hodology will lead o an o iginal
expe imen al da ase as well as a se o empi ical ela ions o he scou pa e ns o be
la e used as a use ul inpu o nume ical simula ions.
Expe imen al Se up
Expe imen al appa a us
The expe imen s we e pe o med in a 32.2 m long and 1 m wide eci cula ion lume,
loca ed in he Hyd aulics Labo a o y o he Facul y o Enginee ing o he Uni e si y o
Po o (FEUP). Figu e 2 illus a es a gene al longi udinal iew o he expe imen al se up.
The side-walls a e made o glass o enable he isualiza ion o he low. The wa e is
eci cula ed om a ese oi by means o a cen i ugal pump g oup. The in low
discha ge was manually egula ed and con olled by means o wo elec omagne ic
lowme e s a he channel en ance. In he ups eam each o he lume, some channel
bed mac o ugosi ies we e designed o ensu e a u bulen low de elopmen . The low
dep h was adjus ed by means o an elec ic ga e a he downs eam end o he lume.
The app oach low eloci y (u = 0.327 ms-1) was se o be 97% o he c i ical low
eloci y calcula ed by Neil’s o mula (Neil, 1967). The e o e, a low dep h o 0.18 m
and a low discha ge o 0.059 m3s-1 we e imposed, gua an eeing clea -wa e low
condi ions o he expe imen s pe o med. The lume bo om was buil upon he o iginal
conc e e lume bo om in o de o ob ain wo sedimen boxes: one, o c ea e a sand pi
whe e he complex pie was ins alled and, he o he one o c ea e a sand ap whe e he
e oded sedimen s we e e ained (bo h sedimen boxes 0.35 m deep and 3.40 m long).
The sand ma e ial was cha ac e ized by a median diame e , D50, o 0.86 mm, a
g ada ion coe icien o he sedimen size dis ibu ion, σd, o 1.4 and a densi y, ρ, o
2650 kgm-3.
The geome ic cha ac e is ics and he posi ion ela i e o he ini ial i e bed o
he complex pie used in he pe o med expe imen s is depic ed in Figu e 3. The model
was buil o his pu pose wi h he column and he pile cap made o ac ylic glass and he
ou ounda ion piles o Poly inyl chlo ide (PVC). The column and he pile cap ha e
ounded edges. The s udied pie was placed in he sand pi on he channel midplane and
posi ioned in o de o expose hal o he pile cap heigh (0.029 m) o he low cu en
( he posi i e x-axis indica es he di ec ion o he low). In ag eemen wi h Teixei a
(2013) he highes scou dep hs occu ed o his con igu a ion o he complex pie .
Acco ding o Mo eno e al. (2012), he con ac ion and wall e ec s we e negligible o
he scou ing p ocess, since a ios o B/Dpc ≥10 and B/h≥5 we e gua an eed (B being he
lume wid h, Dpc he pile cap diame e and h he low dep h).
Expe imen al p ocedu e
The expe imen al es s equi ed he ollowing p e ious s eps: (i) ins alla ion o he
complex pie ; (ii) illing o he box pi wi h sand un il he adjacen conc e e bed le el
was eached; (iii) co e age o he complex pie icini y ini ial bed le el a ea wi h hin
geo ex ile, coupled o a me allic g id, o p eclude undesi able scou a he beginning o
he expe imen ; (i ) g adual opening o he al es un il he desi ed wa e dep h and
in low discha ge was eached; and, ( ) emo al o he geo ex ile plaques wi h he aid o
wo la e al wi es. Hence, he expe imen was immedia ely ini ia ed. In o al, 15
expe imen s we e pe o med o cha ac e ize he scou ca i y e olu ion. Each es
co esponded o a p e iously designa ed ime du a ion, in acco dance o p e-de ined
ime s eps o he scou ing p ocess. Be o e each expe imen un, he sand bed was
adjus ed and le elled a 0.029 m abo e he pile cap bo om. In e e y expe imen , he
idimensional econs uc ion o he scou hole was pe o med a e he low was
s opped and he lume was slowly made emp y.
Expe imen al me hodology
The objec i es o his in es iga ion included he measu emen o he scou dep hs a
di e en posi ions and he cha ac e iza ion o he scou ca i y geome y. The o me
was pe o med by means o a limnime e , enabling o measu e he scou dep h a he
pile cap on (c oss in Figu e 4), and by eading o he scale a ached o each
indi idual ounda ion pile; he la e was possible by close- ange pho og amme ic
means, enabling he quan i ica ion o he spa ial dis ibu ion o scou a ound he
complex pie componen s.
Fo he applica ion o pho og amme y, he scou hole and he su ounding
a ec ed a ea we e pho og aphed wi h a single digi al came a (Canon Powe Sho SX
160 IS), successi ely posi ioned in di e en spo s o co e he whole a ea o in e es . To
enable he spa ial e e ence accomplishmen , a se o g ound con ol poin s (ci cles in
Figu e 4) was conside ed.

The came a cap u es we e aken om a ho izon al pla o m, ela i ely close o
he sedimen bed (a a dis ance o app oxima ely 0.60 m), a e each expe imen . Due o
he di e en du a ion o he expe imen s, he numbe o pho os and he loca ion o he
g ound con ol poin s we e adjus ed acco ding o he a eal ex en and dep h o he scou
hole. The g ound con ol poin s consis ed in speci ic (and symme ical) poin s on wo
la e al ule s (see Figu e 4). The pho og amme ic p ocessing so wa e, used in his
esea ch was Agiso Pho oScan P o essional, Ve sion 1.0.4 (Agiso 2014b).Unlike o
adi ional pho og amme y, his so wa e nei he equi es he idimensional loca ion
and o ien a ion o he came a a image cap u e, no he idimensional loca ion o he
con ol poin s p io o he scene econs uc ion. Howe e , he con ol poin coo dina es
a e s ill equi ed in pos -p ocessing o ans o m he model om ela i e o absolu e
coo dina es (Wes oby e al. 2012).
The digi al ele a ion models (DEMs) we e ex ac ed and impo ed in o Global
Mappe (Ve sion 15.0), a GIS Da a p ocessing so wa e. The Global Mappe so wa e
allowed o pe o m he calcula ion o he bed ele a ion and he measu emen o he
scou ca i y olume as well as o pe o m a compa ison wi h he scou dep hs di ec ly
ead in he labo a o y.
Resul s and Discussion
Figu e 5 illus a es he de elopmen o he bed le el con igu a ion p o iles along he
cen eline o he complex pie a e 60 min., 8 hou s, 24 hou s, 72 hou s, 8 days and 11
days., no malized by he low dep h (cons an , h=0.18 m). These p o iles we e ob ained
by pho og amme y; he c oss do s e e o he scou dep h measu ed by he limnime e
(a he pile cap on , o each o he expe imen s) and he ci cle do s deno e he scou
dep hs ob ained by means o eading he ule scales a he ounda ion piles (when
possible). Signi ican conclusions can be d awn om he analysis o he ups eam
s e ch o he bed p o ile ime e olu ion (Figu e 5) such as i s maximum slope o
compa e wi h he angle o epose o he sand bed. The maximum slope o he ups eam
s e ch eached a alue o 74%, co esponding o an angle o 36.5°. This angle is abou
20% highe han he ypical alue o 30° o we sand. Resea che s as Roulund e al.
(2005) also epo ed ha du ing he de elopmen o a scou ca i y, some a eas a he
ups eam side show highe local bed slopes han he angle o epose. Two main easons
we e iden i ied o explain his phenomenon: he backwa d low a he base o he pile
e oding he oo o he ups eam slope o he scou ca i y, and he con inuous sedimen
supply o sedimen s in o he scou ca i y.
Rega ding he ime du a ion equi ed o he se ies’ end expe imen , he c i e ion
o Mel ille and Chiew (1999) was used. I co esponds o he ime a which he a e o
inc ease o scou does no exceed 5% o he ounda ion pile leng h and he low dep h in
a 24 hou s pe iod (in he p esen case, 0.05 m and 0.18 m, espec i ely). In he p esen
case, he end scou s age was eached a e 264 hou s (11 days) wi h a maximum scou
dep h o 19.8 cm a he on o he i s ounda ion pile (Figu e 6). I should be e e ed
ha he ounda ion piles we e numbe ed om ups eam (pile 1) o downs eam (pile 4).
As s a ed be o e, only he scou measu emen s a he pile cap on could (and we e)
pe o med a he beginning o each expe imen . The scou measu emen s a he
ounda ion piles we e only egis e ed as soon as he p ocess o he scou ca i y
de elopmen eached he on o each o he piles, whe e a ule was glued. A educ ion
o he scou dep h a e a e app oxima ely 50 hou s (pile 1 in Figu e 6) may be
explained by a po en ial sliding o he ups eam slope o he scou ca i y. On he p esen
s udy, he scou dep hs measu ed a e ele en days we e: 19.48 cm along he pile cap
on alignmen , 19.8 cm a he i s ounda ion pile on , 13.1 cm
a he second and 7.5 cm and 6.2 cm a he hi d and ou h, espec i ely. This same
complex pie con igu a ion had been s udied by Teixei a (2013). This au ho compu ed
he alues sugges ed o his con igu a ion by wo scou dep h p edic ion me hods
e e enced in he li e a u e, Richa dson and Da is (2001) and FDT (2010). The o me
sugges s a maximum scou dep h o a ound 19.8 cm while he la e gi es a alue o
20.5 cm. These alues a e e y close o he expe imen al ones ob ained in his wo k.
Figu e 7 compa es he scou dep h empo al de elopmen o he end o he
se ies expe imen (du a ion = 11 days) wi h he scou dep h achie ed o each o he
o he (14) expe imen s ( e e ed o as “o he es s”), ob ained by limnime e
measu emen s and by means o pho og amme y a he pile cap on .
The g aph sugges s ha he in e up ion o he expe imen al es s and he
emp ying o he lume ( o he pho og amme y applica ion) do no in e e e wi h he
scou ing p ocess since i yielded a good ag eemen be ween he h ee se o poin s
ep esen ed in Figu e 7.
In o de o s udy he gene a ion and ime e olu ion o he scou ca i y, digi al
ele a ion models we e p oduced a e each expe imen al un and adequa ely ea ed.
The co esponding g aphs o he ins an s conside ed in Figu e 5 a e p esen ed in Figu e
8 as a unc ion o bed ele a ion- o- low dep h a io. The bed ele a ion wi h espec o
he x-y-plane appea s in a g ey-scale ange depending on he le el o each poin
(no malized wi h he low dep h – h=0.18 m).
Al hough many s udies we e dedica ed o in es iga e he empo al e olu ion o
he scou dep h in he icini y o a complex pie , e y ew s udies ha e add essed he
h ee-dimensional cha ac e iza ion o he scou ca i y. To achie e his goal, he digi al
ele a ion model esul s we e used o compu e he olume o he scou ca i y. Figu e 9
shows he ca i y’s scou a e olume empo al e olu ion wi h espec o he ime
du a ion o he end o he se ies expe imen ( e=11 days).
As expec ed, conside able anspo o sedimen s occu ed du ing he i s ime
s eps o he scou ing p ocess (wi h scou a es o 63.4 and 54.4 cm3min-1, o he i s
wo poin s on he a le in Figu e 9). Then, he scou a e dec eased asymp o ically o a
alue o 4 cm3min-1 a he inal scou s age. The ca i y’s olume scou a e (S) ime
de elopmen da a, ep esen ed in Figu e 9, could i wi h a high co ela ion coe icien
( 2=0.9668) o an exponen ial unc ion (Equa ion 1):
𝑆 =𝜆(𝑡
𝑡𝑒)−0.336 (1)
whe e λ assumes he alue o 3.43 in he p esen s udy. Figu e 10 shows he
ela ion o he scou ed ca i y olume, V, wi h he maximum scou ed dep h, ds, a any
scou ing s age. These a iables we e no malized wi h espec o he co esponding end
s age, Ve and dse. The cu e, exp essed by equa ion (2), con i ms ha he scou ed
olume is p opo ional o he powe o 3 o he scou dep h, as e i ied by many
expe imen s.
𝑉
𝑉𝑒=(𝑑𝑠
𝑑𝑠𝑒)3
(2)
F om Figu e 10, i is clea ha he maximum scou dep h app oaches much
as e he co esponding end s age han he ca i y olume. The same pa ame e s a e
plo ed in Figu e 11 wi h espec o he ime no malized wi h he du a ion o he inal
se ies expe imen ( / e); he co esponding g aphs enhance he p e ious
conclusion.Besides he scou ca i y olume conside a ions ano he impo an analysis
pe o med conce ns he geome ic cha ac e iza ion o he scou ca i y. By he end o
each expe imen , o he scou ca i y ob ained, h ee di e en leng h and wid h
measu emen s we e conduc ed: ou o hem in speci ic loca ions (l1, l2, w1 and w2)
and he o he wo a he loca ions whe e he maximum wid h and leng h occu ed (lmax
and wmax). These a iables a e schema ically ep esen ed in Figu e 12 in acco dance
Figu e 3: Geome ic cha ac e is ics and posi ion ela i e o he ini ial i e bed o he complex pie (dimensions in
me e s).
Figu e 4: Scheme o he expe imen al da a collec ion. Came a posi ions (squa e boxes), g ound con ol poin s
(ci cles) and limnime e measu ing poin (c oss).
0.029
0.050
0.475
0.506
0.120
0.058
0.080
column
pile cap
pile ounda ion
z
y
x
0.180
z
yx
0.354

Figu e 5: Bed p o ile con igu a ion ime e olu ion along he complex pie cen eline.
13
24 5 6
-0.2
0
0.2
-0.4 =60 min.
13
245 6
-0.2
0
0.2
-0.4 =8 hou s
-0.6
13
24 5 6
-0.2
0
0.2
-0.4
=24 hou s
-0.6
13
2456
-0.2
0
0.2
-0.4
=72 hou s
-0.6
-0.8
1 32 4 5 6
-0.2
0
0.2
-0.4
=8 days
-0.6
-0.8
-1.0
-1.2
13
24 5 6
-0.2
0
0.2
-0.4
=11 days
-0.6
-0.8
-1.0
-1.2
x/h
z/h
Figu e 6: End expe imen (11 days): Scou dep h e olu ion a he pile cap on and a he piles on .
Figu e 7: Compa ison o he expe imen al app oaches: scou dep hs a he pile cap.
0
5
10
15
20
25
0.01 0.1 1 10 100 1000
Scou dep h (cm)
Time (h)
pile cap pile 1 pile 2 pile 3 pile 4
0
5
10
15
20
25
0.01 0.1 1 10 100 1000
Scou dep h (cm)
Time (h)
se ies' end expe imen
o he se ies o es s, by means o limnime e measu emen s
o he se ies o es s, by means o pho og amme y
Figu e 8: Digi al ele a ion models.
Figu e 9: Ca i y’s olume scou a e ime e olu ion.
Figu e 10: Rela ion be ween he scou dep h and olume a es o each expe imen .
Figu e 11: Rela ion be ween maximum scou dep h and olume a es o he end expe imen .
Figu e 12: Scheme o he ypical scou ca i y and cha ac e is ic geome ic dimensions.
0
0.2
0.4
0.6
0.8
1
1.2
0.0001 0.001 0.01 0.1 1
/ e
ds/dse V/Ve
lmax
wmax
Dpc (12 cm)
w1 w2
l2
l1