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25th International Meeting on Organic Geochemistry IMOG 2011

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P-388<br />

ESR spectroscopic study of humic acid-like materials obtained<br />

by the autoxidati<strong>on</strong> of caffeic and chlorogenic acid<br />

Ruņica Nikoliš 1 , Tatjana AnŤelkoviš 1 , Goran Nikoliš 2<br />

1 University of Niš, Faculty of Sciences, Department of Chemistry, Niš, Serbia, 2 University of Niš, Faculty of<br />

Medicine, Department of Chemistry, Niš, Serbia (corresp<strong>on</strong>ding author:ruzicanf@yahoo.com)<br />

Electr<strong>on</strong> spin res<strong>on</strong>ance (ESR) spectroscopy is<br />

widely used technique for the investigati<strong>on</strong> of both<br />

natural humic acids and humic acid-like materials<br />

obtained from various phenolic compounds [1,2].<br />

Beside the characterizati<strong>on</strong> of organic radicals it is<br />

also possible by using ESR to study interacti<strong>on</strong>s of<br />

such samples with paramagnetic metal i<strong>on</strong>s some of<br />

which (eg. Fe 3+ , Cu 2+ , Mn 2+ ) are ubiquitous in natural<br />

samples [3].<br />

As far as organic radicals in humic acids and humic<br />

acid-like materials are c<strong>on</strong>cerned the researchers<br />

mainly reported ESR spectra c<strong>on</strong>sisting of <strong>on</strong>e broad<br />

symmetrical line with no hyperfine structure for both<br />

solid samples and samples in soluti<strong>on</strong>s. These<br />

organic radicals thus were characterized by the<br />

linewidth of ESR signal and its g-value, and it was<br />

possible to determine the free radical c<strong>on</strong>centrati<strong>on</strong> in<br />

solid samples. Only in few cases ESR spectra with<br />

some hyperfine structure were obtained [1], but the<br />

reas<strong>on</strong> for that might be that modulati<strong>on</strong> amplitudes<br />

used for recording most of the ESR spectra reported<br />

in the literature were to high (usually values between<br />

0.1 and 0.2 mT were reported).<br />

In this work we recorded ESR spectra of humic<br />

acid-like materials obtained by the prol<strong>on</strong>ged<br />

autoxidati<strong>on</strong> of 20 mM soluti<strong>on</strong>s of caffeic or<br />

chlorogenic acid at pH 8.4 (Tris buffer) in the<br />

presence of an excess of Mg i<strong>on</strong>s. ESR<br />

measurements were carried out in a quartz flat cell<br />

using an X-band Bruker ESP-300 spectrometer by<br />

employing microwave power of 2.0 mW and<br />

modulati<strong>on</strong> amplitude of 0.01 mT. The spectra<br />

obtained immediately after starting the autoxidati<strong>on</strong><br />

reacti<strong>on</strong> displayed well resolved hyperfine structure<br />

which enabled characterizati<strong>on</strong> of initially formed spinstabilized<br />

ortho semiquin<strong>on</strong>e radicals. After prol<strong>on</strong>ged<br />

autoxidati<strong>on</strong> soluti<strong>on</strong>s became turbid and<br />

corresp<strong>on</strong>ding ESR spectra lost some, but not all, of<br />

its hyperfine structure. The ESR spectrum of system<br />

based <strong>on</strong> caffeic acid is shown in Fig. 1. and its<br />

appearance is very similar to the ESR spectrum of the<br />

unfracti<strong>on</strong>ated Tsubame humic acid in soluti<strong>on</strong> [1].<br />

For the chlorogenic acid system under the same<br />

c<strong>on</strong>diti<strong>on</strong>s we obtained similar ESR spectrum, but<br />

with much more noise and less resolved hyperfine<br />

structure. In some earlier experiments after prol<strong>on</strong>ged<br />

autoxidati<strong>on</strong> of rutin under the same c<strong>on</strong>diti<strong>on</strong>s we<br />

obtained ESR spectra c<strong>on</strong>sisting of <strong>on</strong>e<br />

unsymmetrical line but without hyperfine structure [4].<br />

Fig. 1. ESR spectrum of humic acid-like material<br />

obtained by the 7 day autooxidati<strong>on</strong> of caffeic acid in<br />

the presence of Mg i<strong>on</strong>s at pH 8.4 in aqueous<br />

soluti<strong>on</strong>.<br />

Our results suggest that ESR spectra of humic<br />

acids and humic acid-like materials should be<br />

recorded with the use of small enough values of<br />

modulati<strong>on</strong> amplitude in order to see whether some<br />

hyperfine structure is present. This may help better<br />

characterizati<strong>on</strong> of such samples.<br />

References<br />

[1] Watanabe, A., McPhail, D.B., Maie, N.,<br />

Kawasaki, S., Anders<strong>on</strong>, H.A., Cheshire, M.V.<br />

(2005) Org. Geochem. 36, 981-990.<br />

[2] Giannakopoulos, E., Drosos, M., Deligiannakis,<br />

Y. (2009) J. Coll. Int. Sci. 336, 59-66.<br />

[3] Barriquello, M.F., da Costa Saab, S., Filho,<br />

N.C.,Martin-Neto, L. (2010) J. Braz. Chem. Soc.<br />

21, 2302-2307.<br />

[4] Nikoliš, G.M., Nikoliš, R.S., Miliš, B.Lj.,<br />

Ţanadanoviš-Brunet, J.M. (2000) Proceedings of<br />

the 5th <str<strong>on</strong>g>Internati<strong>on</strong>al</str<strong>on</strong>g> C<strong>on</strong>ference <strong>on</strong> Fundamental<br />

and Applied Aspects of Physical Chemistry,<br />

Belgrade, Yugoslavia, 123-125.<br />

517

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