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PROCEEDINGS OF THE 7 INTERNATIONAL ... - Fizika

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M. Pučetaitė et al. / Medical Physics in the Baltic States 7 (2009) 96 - 99<br />

monohydrate to 1324 cm -1 for calcium oxalate<br />

dihydrate (Fig. 3).<br />

The second issue in this study is related to distribution<br />

of chemical components in the cross-section of the<br />

stone. FTIR microscope was used for capturing of<br />

infrared image of cross-sectioned stones. The spectra<br />

from small areas of the cross section (100×100µm)<br />

were used for constructing false-colour images.<br />

Optical density<br />

Wavenumber, cm -1<br />

600 800 1000 1200 1400 1600 1800 2000<br />

Fig. 1. Spectrum of pure uric acid stone (top) compared with<br />

spectrum of uric acid from the library (bottom).<br />

Optical density<br />

600 800 1000 1200 1400 1600 1800 2000<br />

Wavenumber cm<br />

Fig. 2. Spectrum of urinary stone (top) constituted from<br />

calcium oxalate (black curve), carbapatite (blue<br />

curve) and struvite (red curve).<br />

-1<br />

Optical density<br />

Optical density<br />

Wavenumber, cm -1 Wavenumber, cm -1<br />

600 1000 1400 1800 1200 1300 1400 1500<br />

Fig. 3. Spectra of stones containing calcium oxalate monohydrate<br />

(bottom) and calcium oxalate dihydrate (top). The band of<br />

the latter is shifted to the side of higher wavenumbers.<br />

The images were obtained by integrating area under<br />

specific spectral band. Having analyzed the data<br />

obtained, we divided the stones into two groups: the<br />

ones with some ordered distribution of chemical<br />

components and the others without any organized<br />

structure. One of the stones constituted of calcium<br />

oxalate and calcium phosphate (brushite) is shown in<br />

figure 4. Optical and false-colour images of this stone<br />

97<br />

are presented in figure 6. The false-colour image in the<br />

middle shows how calcium oxalate is distributed in the<br />

cross-section of the stone. Red colour corresponds the<br />

areas where the concentration of calcium oxalate is<br />

high and blue colour – where the concentration is low.<br />

The bottom image represents distribution of brushite.<br />

Having these images in mind, we can assume that the<br />

stone was induced by small deposit of brushite on the<br />

epithelium and the layer of calcium oxalate formed on<br />

it through time.<br />

Fig. 4. A photo of the stone constituted from calcium<br />

oxalate and calcium phosphate (brushite).<br />

A photo of another stone, constituted from calcium<br />

oxalate and calcium phosphate (carbapatite), is<br />

presented in figure 5. False-colour and optical images<br />

of this stone are shown in figure 6. Here we cannot see<br />

an organized structure, and the chemical compounds<br />

are distributed randomly in the cross-section of the<br />

stone.<br />

Fig. 5. A photo of the stone constituted of calcium<br />

oxalate and calcium phosphate (carbapatite).<br />

From this data, we can assume that both chemical<br />

components are distributed in the stone evenly what is<br />

resulted by simultaneous crystallization. In addition,<br />

there is no evidence that the stone formed on<br />

epithelium before it became loose. Most likely, the<br />

stone formed from oversaturated solution of the<br />

compounds.

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