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IGCAR : Annual Report - Indira Gandhi Centre for Atomic Research

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IGC<br />

<strong>Annual</strong> <strong>Report</strong> 2007<br />

Absorbance<br />

(a)<br />

ν 4<br />

712<br />

*<br />

ν 2<br />

876<br />

Raman<br />

1070<br />

1425<br />

ν 3<br />

*<br />

Reference<br />

10 mm<br />

20 mm<br />

Absorbance<br />

2ν 2 +ν 4<br />

500 1000 1500 2000 2500 3000 3500 4000<br />

Wavenumber (cm -1 )<br />

convenient method to estimate<br />

the Ca(OH) 2 content through its<br />

characteristic decomposition.<br />

The content of Ca(OH) 2 as<br />

obtained from the peak area at<br />

753 K from DTA, is plotted as a<br />

function of depth <strong>for</strong> the<br />

samples from one of the blocks<br />

in Fig.1. From the figure it is<br />

clear that the concentration is<br />

increasing linearly up to about<br />

40 mm depth of interacted<br />

concrete. Thus it is clear that<br />

DTA is a sensitive means to<br />

obtain the Ca(OH) 2 content,<br />

which in turn is an indicator of<br />

the concrete damage.<br />

Fourier trans<strong>for</strong>m infrared<br />

(FTIR) studies<br />

Alternatively, the quality of<br />

concrete can also be<br />

determined from their<br />

characteristic stretching<br />

frequencies from the mid<br />

infrared region absorption<br />

spectrum. Control runs have<br />

also been carried out to<br />

delineate the thermal effects of<br />

sodium fire from that of the<br />

chemical interaction effects.<br />

Definite signatures of<br />

3110<br />

3240<br />

2ν 3<br />

10 mm<br />

3643<br />

20 mm<br />

Reference<br />

3000 3250 3500 3750<br />

Wavenumber (cm -1 )<br />

Fig.2a Room temperature infrared<br />

spectra of reference sample along<br />

with sodium exposed samples<br />

removed from 10 and 20 mm from<br />

the affected surface of concrete<br />

thermochemical degradation<br />

indicating dehydration and<br />

structural modification of the<br />

limestone concrete have been<br />

obtained <strong>for</strong> the first time using<br />

this technique.<br />

Fig.2a shows the room<br />

temperature mid infrared<br />

spectrum of the limestone<br />

aggregate reference concrete<br />

along with the spectra of<br />

sodium exposed samples as a<br />

function of depth. The spectrum<br />

revealed the broad absorption<br />

feature centered around 3500<br />

cm -1<br />

attributed to stretching<br />

mode of bound water in<br />

concrete. In particular the<br />

sharp feature at 3643 cm -1<br />

riding on the broad water<br />

background is said to arise due<br />

to the O-H stretching of<br />

Ca(OH) 2 - the major hydration<br />

product of Portland Cement.<br />

Estimating the area under this<br />

peak at 3643 cm -1 could follow<br />

the extent of degradation of<br />

concrete. It is clearly evident<br />

from the figure that the<br />

spectrum of the sodium<br />

exposed sample removed from<br />

10 mm from the affected<br />

surface shows appreciable<br />

changes as compared to that of<br />

the reference sample. The<br />

stretching modes of water in the<br />

affected sample reveals a<br />

significant softening associated<br />

with a dramatic increase in the<br />

intensity of the low frequency<br />

components as compared to<br />

that of the reference sample<br />

(inset in Fig. 2a). The intensity<br />

of the 3643 cm -1 peak is also<br />

seen to significantly decrease.<br />

These changes indicate the loss<br />

of both free and bound water<br />

from the concrete on account<br />

of sodium exposure, thus<br />

degrading the concrete. The<br />

appearance of a new mode at<br />

1070 cm -1 and the splitting of<br />

the doubly degenerate<br />

ν 3 and ν 4 modes indicate a<br />

structural trans<strong>for</strong>mation of the<br />

limestone aggregates.<br />

Fig.2b shows the changes in<br />

the vibrational frequencies of<br />

the stretching modes of water<br />

as a function of depth from the<br />

affected surface. It is evident<br />

from the figure that the<br />

conversion of bound water into<br />

free water is confined to depths<br />

of 30 mm from affected<br />

surface. Thus infrared<br />

spectroscopy helps to provide<br />

an insight into the changes<br />

occurring at the molecular<br />

level.<br />

Frequency (cm -1 )<br />

3260<br />

3235<br />

3210<br />

3185<br />

3450<br />

3425<br />

3400<br />

3375<br />

3615<br />

3590<br />

3565<br />

(b)<br />

A<br />

B<br />

C<br />

D<br />

Ref<br />

3540<br />

0 25 50 100<br />

Distance from surface (mm)<br />

Fig.2b Variation of stretching<br />

frequencies of water as a function of<br />

depth from the affected surface of<br />

concrete. Half shaded circles<br />

correspond to the unexposed<br />

reference samples. A, B, C and D<br />

Correspond to various location on<br />

the sodium interacted surface<br />

R&D FOR FBRs 77

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