Whitlockite structures in kidney stones indicate infectious origin: a scanning electron microscopy and Synchrotron Radiation investigation
Dominique Bazin, R. Papoular, Erik Elkaı̈m, Raphaël Weil, Dominique Thiaudière, Céline Pisapia, Bénédicte Ménèz, Nathaniel S. Hwang, Frederik Tielens, Marine Livrozet, Élise Bouderlique, Jean‐Philippe Haymann, Emmanuel Letavernier, Louis Hennet, Vincent Frochot, Michel Daudon
Abstract
In this contribution dedicated to kidney stones containing Whitlockite (Wk), we addressed three questions, namely, the presence of iron in Wk, the relationship between bacterial imprints and the presence of Wk, and finally the relationship between the crystal size of Wk-bearing stones and infection. The complete dataset indicates that iron is not present in our Wk stoichiometry. We also note the presence of bacterial imprints for kidney stones with a high, but sometimes a low content, of Wk. Finally, we propose FE-SEM as a diagnostic tool for stone patients who have a negative urine culture associated with kidney stones containing less than 20% by weight Wk, a low level of carbonate in apatite, and no struvite. Such a diagnostic tool would represent a significant benefit to the clinician.