Formation and stability of calcium oxalates, the main crystalline phases of kidney stones

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Abstract

Wide spread of oxalate mineralization in living organisms is a strong reason for its intense worldwide study during recent decades. Calcium oxalates can be found in human body (stones of urinary system, calcifications in lungs, crystals in a bone marrow etc.) (Socol et al. 2003; Zuzuk2005; Korago1992), in body of animals (stones of cats urinary system), and in plants (Korago 1992). Most often calcium oxalates occur as a part of pathogenic formations of the human urinary system (Korago 1992). The part of oxalate kidney stones ranges from50%to 75%depending of the geographical region. Our collection of kidney stones that were removed in Saint-Petersburg hospitals includes 263 samples, 81% of which consists of calcium oxalate minerals fully or as a part.

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Izatulina, A. R., Punin, Y. O., Shtukenberg, A. G., Frank-Kamenetskaya, O. V., & Gurzhiy, V. V. (2012). Formation and stability of calcium oxalates, the main crystalline phases of kidney stones. In Minerals as Advanced Materials II (Vol. 9783642200182, pp. 415–424). Springer-Verlag Berlin Heidelberg. https://doi.org/10.1007/978-3-642-20018-2_38

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