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Proceedings e report - Firenze University Press

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CHARACTERIZATION OF WATERLOGGED WOOD BY INFRARED SPECTROSCOPY<br />

Fig. 4. Linear regression plot of estimated vs. laboratory-evaluated holocellulose content for the analysed<br />

samples. The regression model refers only to the model obtained with open black circles, corresponding only to<br />

elm samples from Pisa and Comacchio with low ash content (below 6.9% for all of them). The other circles are<br />

samples with ash content above 10%, including elm, cypress and oak.<br />

3.3. Influence of sample inhomogeneity<br />

Fig. 5 shows two normalized spectra obtained in two different portions of the same fine powder and<br />

apparently homogenised meal of the sample np_A07 (Naples, ship A). As can be observed the two<br />

spectra show differences most noticeable at 1454, 1420, and 1024 cm -1 .<br />

Fig. 5. Min-Max normalized (1800-1480 cm -1 ) ATR-FTIR spectra obtained in two different portions of the<br />

extracted meal of the same sample, np_A07, from ship A of Naples. Main differences can be seen at 1454, 1420<br />

and 1024 cm -1 .<br />

If the two spectra are included in the regression line (Fig. 4), two different values of holocellulose<br />

(41% and 55%) are obtained. This addresses the question of the representativeness of the aliquot used<br />

to obtain the spectra that could be handled with a careful homogenisation of the samples<br />

complemented with an increased number of spectra per sample.<br />

4. Conclusions<br />

The results obtained suggest that it would be possible to build models to assess the holocellulose<br />

content of waterlogged archaeological wood by means of ATR-FTIR analysis using simple linear<br />

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