Hesse A, Lange P, Berg W, Bothor C, Hienzsch E
Urol Int. 1979;34(2):81-94. doi: 10.1159/000280253.
In uroliths various phosphate phases can be detected which indicate different formation conditions. Structure and topography of the respective phosphate phases are characterized by scanning electron microscopy and microprobe techniques. Trace element enrichment is investigated and illustrated; for example, sulfur is found preferentially in carbonate apatite. From the distribution of the phosphate phases, conclusions can be drawn concerning the urolith genesis.
在尿路结石中,可以检测到各种磷酸盐相,这表明了不同的形成条件。通过扫描电子显微镜和微探针技术对各个磷酸盐相的结构和形貌进行表征。研究并展示微量元素的富集情况;例如,在碳酸磷灰石中优先发现硫。根据磷酸盐相的分布,可以得出关于尿路结石成因的结论。