12
6 TH INTERNATIONAL CONFERENCE ON DAM ENGINEERING C.Pina, E.Portela, J.Gomes (ed.) Lisbon, Portugal, February 15-17, 2011 1 TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira * , Luiz Alkimin de Lacerda * , Ernesto Goldfarb Figueira , Emerson Luiz Alberti * Instituto de Tecnologia para o Desenvolvimento (LACTEC) Br-116, Km 98 – s/n° Centro Politécnico da UFPR, 81531-980 Curitiba, Brasil e-mail: [email protected], webpage: http://www.lactec.org.br/pt/ Keywords: Dams, Concrete, Ground Penetrating Radar, Non Destructive Tests. Abstract. Mapping with geophysical techniques such as the Ground Penetrating Radar (GPR) is based on the propagation of electromagnetic waves and has a wide range of applications in civil engineering. This work presents a non-destructive investigation with GPR in the conventional concrete face of a roller compacted concrete (RCC) dam. The objective is the identification of subsurface anomalies, such as niches of higher porosity in the conventional concrete, whose thickness is not greater than 50 cm. The acquisition of radargrams was carried out with a 2 GHz antenna with dual polarization, which allowed assembling a three-dimensional subsurface image from a single direction reading path. The images were treated with a specific package of filters for concrete surveys. After this post-processing, the group of images was integrated to form a block diagram. The interpretation of the whole block was performed with a controlled thickness slicing procedure for identification of anomalies within sound concrete. A general view of the investigated area is presented with the indication of anomalous regions which may require a localized repair. 1 INTRODUCTION The integrity, load capacity and service life of concrete dams is directly correlated to the quality of constituent materials and construction methods. The common practice of investigation of concrete in civil structures uses invasive methods to extract samples for laboratory tests. Besides being destructive, these methods cannot consistently reveal abnormalities within the analyzed structure. Civil engineering has recently started using non destructive geophysical techniques for the inspection of hydraulic structures. However, investigation of anomalies such as niches of higher porosity, cracks and damaged areas within concrete is not trivial. With geophysical surveys one can determine concrete conditions, detecting anomalous areas and mitigate the damage. The Ground Penetrating Radar (GPR) is a geophysical tool whose principle is based on the propagation of electromagnetic (EM) waves. It is a non destructive method of investigation used for different purposes, such as to detect the thickness of slabs 1 , the integrity of masonry structures 2 , the integrity of reinforcement in bridge decks 3 , buried Esteio Engenharia e Aerolevantamentos S.A. Elejor – Centrais Elétricas do Rio Jordão S.A.

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Page 1: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

6TH INTERNATIONAL CONFERENCE ON DAM ENGINEERING C.Pina, E.Portela, J.Gomes (ed.)

Lisbon, Portugal, February 15-17, 2011

1

TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM

Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, Ernesto Goldfarb Figueira†, Emerson Luiz Alberti‡

* Instituto de Tecnologia para o Desenvolvimento (LACTEC) Br-116, Km 98 – s/n° Centro Politécnico da UFPR, 81531-980 Curitiba, Brasil e-mail: [email protected], webpage: http://www.lactec.org.br/pt/

Keywords: Dams, Concrete, Ground Penetrating Radar, Non Destructive Tests.

Abstract. Mapping with geophysical techniques such as the Ground Penetrating Radar (GPR) is based on the propagation of electromagnetic waves and has a wide range of applications in civil engineering. This work presents a non-destructive investigation with GPR in the conventional concrete face of a roller compacted concrete (RCC) dam. The objective is the identification of subsurface anomalies, such as niches of higher porosity in the conventional concrete, whose thickness is not greater than 50 cm. The acquisition of radargrams was carried out with a 2 GHz antenna with dual polarization, which allowed assembling a three-dimensional subsurface image from a single direction reading path. The images were treated with a specific package of filters for concrete surveys. After this post-processing, the group of images was integrated to form a block diagram. The interpretation of the whole block was performed with a controlled thickness slicing procedure for identification of anomalies within sound concrete. A general view of the investigated area is presented with the indication of anomalous regions which may require a localized repair.

1 INTRODUCTION

The integrity, load capacity and service life of concrete dams is directly correlated to the quality of constituent materials and construction methods. The common practice of investigation of concrete in civil structures uses invasive methods to extract samples for laboratory tests. Besides being destructive, these methods cannot consistently reveal abnormalities within the analyzed structure.

Civil engineering has recently started using non destructive geophysical techniques for the inspection of hydraulic structures. However, investigation of anomalies such as niches of higher porosity, cracks and damaged areas within concrete is not trivial. With geophysical surveys one can determine concrete conditions, detecting anomalous areas and mitigate the damage.

The Ground Penetrating Radar (GPR) is a geophysical tool whose principle is based on the propagation of electromagnetic (EM) waves. It is a non destructive method of investigation used for different purposes, such as to detect the thickness of slabs1, the integrity of masonry structures2, the integrity of reinforcement in bridge decks3, buried

† Esteio Engenharia e Aerolevantamentos S.A. ‡ Elejor – Centrais Elétricas do Rio Jordão S.A.

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pipes4, embedd

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archaeologded objectshough the uyet a usual sent study rameters fos paper presstream faceto identify

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R – GROU

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gical surve and voids

use of GPR practice inis also an ir a better a

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UND PENE

enetrating romagneticcture. t used in thdual polarizy one direcwith limitedistance mtrigger for uisition.

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Alkimin de La

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ETRATING

Radar nonc waves and

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igure 1: GPR

acerda, Ernest

2

others. In e6 with highread in geodams or oth

vey, which in future stuhigh resoluf Santa Clnce of anos is less tha allowingth. The trida specific pformed aftefor possibl

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particular, h resolutionlogical andher hydrauwill form tudies. ution GPR ara in Para

omalies in han 50cm. T

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The mappinformation ol images wefilters for coysis of each ace anomal

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Luiz Alberti.

en used to

ical areas, te structure

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Page 3: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

2.1 Ra

One of freqpenetra

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The attenua

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Therbe greathe EM

Isabella Figu

adar wave p

of the mosquency. Thiating the ma

Figure

ee major fion, clutterteristics of tcrete is a dThe dielec

lly, concret

conductiviation is highce the radarer, it is impd target. Th

c = 0,3 mered constans argued thngth () sh

v / f, then,

refore, theoater than 1 GM pulse sh

ueira, Luiz A

propagatio

st importants definitionaterial and

e 2: Layout of

factors detring and dthe materiadielectric mctric (conste is not con

ity is directher as the frr provides tportant to he equation

m/ns is the nt. Assumihat for a g

hould be7

oretically, tGHz. To mhould be a

Alkimin de La

on in concr

t points in an is complsignal reso

f receivers (R

termine thdepth of peal as conducmaterial antant) permnductive7 a

1

tly proportirequency inhe time of know the

n of the EM

speed of lng a permitgood vertic

f > 0

to have a reminimize noat least 4

acerda, Ernest

3

rete

an investiglex and invlution for i

RX) and trans

he choice enetration.ctivity (),

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ional to frencreases. the EM wawave spee

M wave velo

v = c -0,5

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r > /4

0,0264 / r (

esolution oise in the ratimes larg

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ation with volves a "cdentifying

mitters (TX)

of frequenThese factpermittivitave as a co

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)/ mdB

equency (f)

ave propagaed in orderocity is give

adar freque8, one has vtion (r) for

(GHz)

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EM radar wchoice" becharacteris

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encies wavv = 0,106 mr a reflecte

in the imag, the domin

he characte

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waves is theetween capastic targets7

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he survey: nfluenced bheterogeneitor insulatorm about 5s is given b

ves. Theref

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e choice acity of

7.

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ulse, the

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cy must ength of e (h) of

Page 4: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

heterog

Thus,

For aspect ta surfacthe freqeffectiv

3 CO

Befoto evalu

The size for0,50 mFigure spaces ensure regular

.

Isabella Figu

geneity7,

example, fthat shouldce area forquency of thve frequenc

ONTROLLE

ore applyinuate its capconstructior the GPR

m. Eighteen3. The anfilled withits higher pmolds, as

Figu

ueira, Luiz A

for h = 1,2d not be over survey thehe transmit

cy (fr) signa

ED FIELD

ng the GPR pacity for deon plan conreadings. T

n anomaliesnomalies hah aggregateporosity. Tshown in F

ure 3: Schema

Alkimin de La

f < 0,

2 cm, the ferlooked is e pattern otted signal.al in a mate

fr =

D TEST

system in etecting anonsisted of aThe block ws were insead differenes size 1 a

The sizes ofFigure 4: Pla

atic plan of th

acerda, Ernest

4

> 4h

,0264 / h

frequency mthat when f the EM f The equati

erial such as

= f [2/(1+

Santa Claromalies of

a concrete bwas 5,20 merted in a

nt areas anand 2, whicf the anomacement of

he concrete bl

to Goldfarb a

(GHz)

must be lesthe antenn

field changion below ws concrete,

)] 0,5

ra dam, a cdifferent si

block built m long, 1 m

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lock with the

and Emerson L

ss than 2.2a is broughes considerwas sugges

controlled tizes embedin two stepm wide andc configurasses and coovered withprinted in

alies in the

anomalies la

Luiz Alberti.

2 GHz. Finht into contrably, and

sted to estim

test was perdded in concps with a md had thickation, as shonsisted ofh a plastic the concretconcrete bl

ayout.

(5)

(6)

nally, an act with reduces

mate the

(7)

rformed crete.

minimum kness of hown in f empty film to

te using lock.

Page 5: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

Aftehigh anand rec

Twoblock aindicate

Largare stillIn gene

Althconstru

F

Isabella Figu

er the GPR nd low pascovery gaino radargramat the readed by yelloger anomalil detectable

eral, thickerhough in thuction some

Figure 5: Rada

ueira, Luiz A

a

Figure 4: P

readings, tss bands ins.

ms are showding line. w arrows inies show vee, but the sr anomalieshe initial

e deviations

argram of sec

Alkimin de La

)

Placement of

the radargran the vertic

wn in FigurThe presenn each figuery strong hignals are ns show stronplan all a

s occurred,

ction A with 5

acerda, Ernest

5

f the anomalie

ams were pcal and hor

re 5 and Fignce of all

ure. hyperbolic not so evidnger signal

anomalies as indicate

5 cm thick an

to Goldfarb a

b

es in the conc

post-procesizontal dire

gure 6 alonanomalies

signals in dent, especils. were place

ed by the ra

nomalies plac

and Emerson L

)

crete block.

sed with a ections, ba

ng with a s could be

the imagesally from t

ed 10 cm adargrams.

ed at a depth

Luiz Alberti.

package ofackground r

section viewdetected

s. Small anthe less thic

in depth,

h near to 10 cm

f filters: removal

w of the and are

nomalies ck ones.

during

m.

Page 6: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

F

4 APPDAM

The the dam

Figure 7

The spacingover ea

The height normal

Isabella Figu

Figure 6: Rad

PLICATIO

GPR survem (Figure 7

7: Location in

selected arg. Once theach line, alwfirst GPR pof the conreservoir w

ueira, Luiz A

dargram of se

ON OF GP

ey in Santa ), in order t

n the upstream

rea was dise lines wereways in the profile (0,0crete pavem

water level.

Alkimin de La

ection B with

PR IN THE

Clara was pto evaluate

m face where

scretized we marked, tsame direc0 m) was rment. The .

acerda, Ernest

6

h 10 cm thick

E UPSTRE

performed the conditi

the GPR surside.

with 75 linethe GPR rection (Figurread at the l

last profile

to Goldfarb a

anomalies pl

EAM FACE

in a limitedion of the c

rvey was carri

s, 2,20 m ladings werre 8). level of thee (7,50 m)

and Emerson L

aced at a dep

E OF SANT

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long each ore done swe

crest of thewas read

Luiz Alberti.

pth near to 10

TA CLAR

he upstreamal concrete.

ding paths in

one, with aeeping the

e dam, in th2,20 m be

0 cm.

A RCC

m face of .

the right

0,10 m antenna

he same elow the

Page 7: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

4.1 Re

Almare normheterog

The of reguthe pav

It is high atmasks Figure conven

Isabella Figu

Figu

sults

most all profmally assoc

geneity. first two p

ularly spacevement leve

F

noticeablettenuation the presen10). Coin

ntional conc

ueira, Luiz A

ure 8: GPR su

files showedciated with

profiles at thed hyperbolel (Figure 9)

Figure 9: Rada

e that beyonof the 2.0

nce of reflecidently, th

crete and RC

Alkimin de La

urvey in the u

d the presensurface irr

he levels 0les. This is).

argrams at the

nd the depGHz EM

ectors, makhis depth CC.

acerda, Ernest

7

upstream face

nce of faintregularities

0.0 and 0.10s a clear ev

e pavement le

th of 0,50 waves in

king data is also ass

to Goldfarb a

e with a 2 GH

t irregular ain the conc

0 m show svidence of t

evel in the cr

m the signthe concreinterpretatisociated to

and Emerson L

Hz dipole ante

and truncatecrete surfac

striking reflthe concret

est of the dam

nal quality ete. Beyondion even mo the trans

Luiz Alberti.

enna.

ed reflectorsce and the

flectors in tte reinforce

m.

is poor dud this deptmore difficsition betw

s, which medium

he form ement at

ue to the th noise ult (see

ween the

Page 8: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

In sowhich aconcret

In smagnituclimbinradargr

Isabella Figu

Fig

ome profileare associate as shown

pecific radude, whichng forms duram of the c

ueira, Luiz A

gure 10: Rada

es it was noated with thn in Figure

Figure 11: P

dargrams thh are relaturing the cocorrespondi

Alkimin de La

argram showi

oticed the phe occurren11.

Presence of m

here was tted to the oncrete woring level.

acerda, Ernest

8

ing noisy data

presence of nce of met

metal fragmen

the occurrepresence

rk. The form

to Goldfarb a

a beyond the

f isolated hytallic fragm

nts in the face

ence of strof metal ems are show

and Emerson L

depth of 0,50

yperboles oments inside

e of the dam.

riking hypeelements uwn in Figur

Luiz Alberti.

0 m.

of small ame the conv

erboles of used to fasre 12 along

mplitude, entional

greater sten the gside the

Page 9: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

Figure 1

The increassurfacelevel flindicati

For specificinterpogenerat

Isabella Figu

2: Example o

GPR profed presenc

e with showuctuations ion of inter

a better vic processinlation baseted by the G

ueira, Luiz A

of striking hy

files alongce of irreguwing aggreg

(Figure 13rnal flaws.

Figure 13

isualizationng procedued on posiGPR.

Alkimin de La

yperboles (rigwhich were l

g the linesular and trgates. Wear). None of

: Normal wat

n of the proure called itive and n

acerda, Ernest

9

ht) resulting left embedded

just beloruncated rer in this arthese hiper

ter level zone

ofiles at diC-Scan w

negative p

to Goldfarb a

from metal ed in concrete

w the noreflectors, drea is particrboles dete

e showing gre

ifferent depwas perforeaks of th

and Emerson L

lements used.

rmal reservdue to the cularly highcted in the

eater wear.

pths from tmed8, con

he electrom

Luiz Alberti.

d to fix the for

voir level irregular c

h due to thradargram

the mappednsisting of magnetic re

rms (left)

showed concrete he water

ms are an

d area a a data

eflectors

Page 10: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

The identifiareas in

The defined

Figu

Voidwith reto 35 cm

Lookpresencthe damFigure

A clranges

Isabella Figu

product ofication of hn blue (Figumetal elem

d and equid

ure 14: 5 cm C

ds or niched colors. Inm, slightly king at thece of a contm can be ob16 detail).

Figure 15: R

oser look afrom depth

ueira, Luiz A

f this interhighly condure 14). ments used istant spots

C-Scan of the

es of highern the surveabove the 5

e radargramtinuous plabserved. Th

Radargrams a

at the C-scah 15 cm to 3

Alkimin de La

rpolation isductive are

for fastenis of high co

e mapped area

r porosity eyed volum5,00 m levems betweenane anomalyhe anomaly

at levels 4,60

an shows th35 cm.

acerda, Ernest

10

s a block, eas, depicte

ing the climonductivity

a. The circled

with high me the circle

el, is an evin levels 4y in a diagy goes from

m, 4,70 m an

he anomaly

to Goldfarb a

which afteed in warm

mbing formbetween 4

d areas indica

water quaned red spotidence of o,60 m andonal positio

m 15 cm to

nd 4,80 m wit

y in detail, w

and Emerson L

r a 5 cm sm colors, an

ms are clea0 cm and 4

ate anomalies

ntity wouldts detected ne or more

d 4,80 m, on with res35 cm dep

th the anomal

which is ov

Luiz Alberti.

slicing, allond highly r

arly shown 45 cm depth

at various de

d also be infrom depth

e anomaliesin Figure

spect to thepth (Figure

ly indicated.

ver 80 cm l

ows the resistive

at well h.

epths.

ndicated h 20 cm . 15, the

e face of e 14 and

ong and

Page 11: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

5 CO

The investiganomal

It is or for in

In threvealeabove correcti

The convenwere us

6 AC

The for the (LI 10/

7 REF

[1] PERResExa200

[2] HAG.;InvDe

[3] MABriEng

[4] POGeGe

[5] COValDis

Isabella Figu

ONCLUSIO

GPR has gation of thlies with higa relatively

nvestigatiohe examineed the presethe normaive interven

GPR radntional concsed for fast

KNOWLE

authors wofinancial su1233240-8)

FERENCE

REZ-GRACsolution in amples. ND09.

AMROUCH ARLIGUI

vestigation structive Te

ASER K. Ridge Deck gineering N

RSANI J.Lofísica Rasaofísica 24(1

OLLA C.. Dlutazione e struttive Mo

ueira, Luiz A

Figure 1

ONS

proved tohe upstreamgh precisioy quick men of specifi

ed area of thence of a plal reservoirntion was n

dargrams acrete zone, ening the c

EDGEMEN

ould like toupport for ) through la

ES

CIA V., DI NDT Stud

DTCE’09 N

HE R.; KLYIE G.. Numof Jointing

esting in Civ

R.. IntegratioCondition

Nantes, Fran

L.; BORGESa do IAG/U1): 49-61 20

Diagnosi dConservazi

onitoraggio

Alkimin de La

6: Detail of th

o be a usem face of coon and resolethod of dafic areas withe upstreamlane anomar level andnot justifiedlso revealregularly s

climbing for

NTS

o thank ELEcarrying ouaw 8010/90

CAPUA Ddies of Str

Non-Destruc

YSZ1 G.; BAmerical Modg Defects vel Enginee

on of GrounEvaluation

nce 2009.

S W.R.; ROUSP: Instala006.

di Muraturaione di CosDiagnostica

acerda, Ernest

11

he C-scan wi

eful compleoncrete damlution.

ata acquisitith single orm face of Saly inside thd the impld. ed the prspaced in vrms during

EJOR – Ceut this resea0.

D., GONZAructural Elective Testin

ALAYSSACdeling of Gin Brick

ering Nante

nd Penetratin. NDTCE

ODRIGUES ação e Resu

a, Calcestrustruzioni e Ia, Itália 200

to Goldfarb a

ith identified

ementary nms, allowing

ion, whichr periodic aSanta Clarahe conventementation

esence of vertical and the dam co

entrais Hidrarch, and C

ALEZ-DRIGements: Exng in Civel

C J.; AUREGround-penMasonry Ss, France 20

ing Radar aE’09 Non-D

S.I.; HIODultados GPR

uzzo e LegInfrastruttur09.

and Emerson L

anomaly.

non destrucg the identif

can be appassessmentsa RCC damional concr

n of a refi

metal eled horizontalonstruction

relétricas dCNPq for th

GO R., PUJxperimental l Engineerin

ENS S.; RHnetrating RaStructures. 009.

nd InfraredDestructive

DO F.Y.. O SR 2D-3D. R

gno Tramitere. II Giorna

Luiz Alberti.

uctive tool fication of

plied to largs.

m, the GPR rete. Its locined inspec

ements insl directions

n.

do Rio Jordhe research

JADES L. GMethodolo

ng Nantes,

HAZI J.; BAadar (GPR)

NDTCE’0

d ThermograTesting i

Sítio ControRevista Bras

te Georadarale delle Pr

for the internal

ge areas

profiles cation is ction or

side the s, which

dão S.A. support

G.. GPR ogy and France,

ALLIVY for the

09 Non-

aphy for n Civel

olado de ileira de

r per la rove non

Page 12: TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF … · TRIDIMENSIONAL GPR MAPPING IN THE UPSTREAM FACE OF AN RCC DAM Isabella F. R. Figueira*, Luiz Alkimin de Lacerda*, ... act

Isabella Figueira, Luiz Alkimin de Lacerda, Ernesto Goldfarb and Emerson Luiz Alberti.

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[6] SPORER A.. Inspeção não Destrutiva de Estruturas de Concreto por Georadar (GPR).

Revista Abendi nº 32. Artigo Técnico, Brasil 2009.

[7] PADARATZ, I.J.; FORDE, M.C.. Influence of antenna frequency on impulse radar surveys of concrete structures. 6th Int. Conf. on Structural Faults and Repair, London, 2, 331-336. 1995.

[8] GRED 3D Copyright© 2008