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Biomedical subjects

T Briellmann

Publications and source records attributed to T Briellmann.

3 recordsLinked to original sources

Stone formation in human kidney.

Microscopic crystals were found by SEM analysis in kidneys of stone forming patients as well as in kidneys of non-stone formers. In most samples calcifications were intratubular in the collecting ducts near the papillary tip. 1-2 micron sized particles lay in a gelatinous substance on the epithelium. The only difference in crystal composition is the higher phosphate content in the kidneys of the non-stone forming group. A correlation between the element concentration of the tissue and the occurrence of microliths is given by the cadmium content of the kidney samples. Both groups showed higher cadmium values in the cortex or medulla when crystals were found in the corresponding papillary samples. Urine supersaturation with respect to calcium oxalate was higher in the stone forming group caused by a higher calcium and oxalate but a lower magnesium excretion.

Calcinosis↗

Fluoridation of drinking water: effects on kidney stone formation.

The influence of fluoride in drinking water on stone formation was studied in animals and in "in vitro" crystallization experiments. In male Wistar rats fluoride inhibits ethylenglycol induced calcification of the kidneys and stone formation. The in vitro results performed in synthetic urine exhibited a dose-dependent delay of crystal growth.

Animals↗

The oxalate-tolerance-value: a whole urine method to discriminate between calcium oxalate-stoneformers and others.

In undiluted urine portions the oxalate-concentration required for precipitation (= oxalate-tolerance) can be obtained by titration with sodium-oxalate and turbidimetric detection. The corresponding urinary calcium-concentration was measured and the two values plotted against each other. With regard to a standard-curve (measurements in synthetic urine) different behaviour between urines of stone forming patients and others can be observed.

Calcium Oxalate↗