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MEDICAL PHYSICS IN <strong>THE</strong> BALTIC STATES 7 (2009)<br />

Proceedings of International Conference “Medical Physics 2009”<br />

8 - 10 October 2009, Kaunas, Lithuania<br />

INFRARED SPECTROSCOPICAL STUDIES <strong>OF</strong> DISTRIBUTION <strong>OF</strong> CHEMICAL<br />

COMPONENTS IN URINARY STONES<br />

Milda PUČETAITĖ*, Valdas ŠABLINSKAS*, Vaiva HEDRIXSON**, Zita KUČINSKIENĖ**, Arūnas ŽELVYS***,<br />

Feliksas JANKEVIČIUS***<br />

*Dept. of General Physics and Spectroscopy, Faculty of Physics, Vilnius University; ** Dept. of Physiology,<br />

Biochemistry and Laboratory Medicine, Faculty of Medicine, Vilnius University; ***Centre of Urology, Vilniaus<br />

University Hospital Santariskių klinikos, Faculty of Medicine, Vilnius University<br />

Abstract: Kidney diseases which cause the occurrence of urinary stones are frequent in human pathology. The<br />

formation process of the stones is not fully understood therefore the studies of chemical composition and structure are<br />

of great importance. The means of Fourier transform infrared spectroscopy (FTIR) were used to determine the<br />

composition of the stones while FTIR microscopy was used to create chemical maps of cross-sectioned stones. The<br />

data from the study were used to analyze the formation process of the stones.<br />

Keywords: urinary stones, FTIR, microspectroscopic surface reflectance imaging<br />

1. Introduction<br />

The composition and structure of urinary stones is<br />

complex and depend on a variety of factors which<br />

include diet, sex, environment, metabolism, etc. The<br />

identification of the components and structure of the<br />

stone enables to find out the underlying cause of the<br />

disease, prescribe treatment and prevent recurrences<br />

[1].<br />

The qualitative and quantitative analysis of urinary<br />

calculi is challenging because of their usually small<br />

size, fragility, heterogeneous composition. Fourier<br />

transform infrared spectroscopy (FTIR) is easy and<br />

rapid method to obtain quantitative and qualitative<br />

information about chemical composition of the calculi<br />

even from small amount of the substance. In addition,<br />

this method enables to distinguish such similar<br />

components in the stones as calcium oxalate mono-<br />

and dihydrate. Microspectroscopic surface reflectance<br />

imaging is an informative method for analyzing<br />

morphology of cross-sectioned stones [2].<br />

2. Experimental<br />

Urinary stones for this study were surgically removed<br />

from patients in Vilnius University hospital Santariskiu<br />

klinikos. 2 mg of homogenized sample was finely<br />

grounded with potassium bromide (KBr) powder of<br />

spectroscopic purity and converted into a pellet using<br />

manually operated hydraulic press “Specac” exerting a<br />

pressure of 10 tons. The pellet was placed in the<br />

sample compartment of “Vertex 70” spectrometer from<br />

“Bruker” in the path of infrared radiation emitted by<br />

96<br />

“glowbar” light source. The spectrum was obtained<br />

using liquid nitrogen cooled MCT (mercury cadmium<br />

telluride) detector with 4 cm -1 spectral resolution. The<br />

spectrum was then matched against library spectra to<br />

identify various stone components.<br />

The cross-sectioned stones were fixed on glass<br />

microscope slides using two-component epoxidic glue<br />

and polished. Spectra were obtained using FTIR<br />

microscope “Hyperion 3000” from “Bruker” with<br />

single element MCT detector. The resolution of the<br />

spectrometer was set to 2 cm -1 . False-colour images<br />

representing the distribution of different chemical<br />

components in the urinary stones were obtained by<br />

integrating the area under the spectral band of specific<br />

chemical component. OPUS software was used for this<br />

purpose.<br />

3. Results and discussions<br />

In this study, the components found in the stones were:<br />

calcium oxalate (mono- and dihydrate), phosphates<br />

(carbapatite and brushite), uric acid and struvite. The<br />

majority of stones (~78%) are constituted from calcium<br />

oxalate with phosphate deposits. Some of the stones<br />

(~17%) are constituted from pure uric acid (Fig. 1) and<br />

the others (~5%) – from three components: calcium<br />

oxalate, phosphate and struvite (Fig. 2).<br />

FTIR spectroscopy allows distinguish two very similar<br />

substances: calcium oxalate monohydrate and calcium<br />

oxalate dihydrate [3]. Such analysis in this work was<br />

based on the position of C-O stretching spectral band.<br />

This band shifts from 1317 cm -1 for calcium oxalate

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