Takeuchi H, Arai Y, Konishi T, Tomoyoshi T
Department of Urology, Shiga University of Medical Science.
Hinyokika Kiyo. 1988 Sep;34(9):1529-35.
The architecture of mixed uric acid and calcium oxalate stones was studied by polarized light microscopy. Some uric acid stones contained calcium oxalate stones (whewellite or weddellite) as a nucleus. Other uric acid stones contained calcium oxalate crystals in the nucleus or inner portion. A uric acid stone covered with layers of calcium oxalate was also found. In the mixed stones, nuclei of randomly mixed fine grained whewellite and uric acid were seen and both crystals appeared in alternating sequence in the outer layers. Weddellite crystals dissolved layers of uric acid and invaded into them in the nuclear or peripheral zones. Whewellite may precipitate in the same or a similar condition as uric acid precipitates, whereas weddellite may precipitate in a different condition. We discussed the pathogenesis of mixed uric acid and calcium oxalate stones, heterogeneous nucleation and epitaxial growth based on a morphologic study of the mixed stones.
通过偏光显微镜研究了尿酸和草酸钙混合结石的结构。一些尿酸结石含有草酸钙结石(水草酸钙或二水草酸钙)作为核心。其他尿酸结石在核心或内部含有草酸钙晶体。还发现了一层覆盖着草酸钙的尿酸结石。在混合结石中,可见随机混合的细粒水草酸钙和尿酸的核心,并且两种晶体在外层以交替顺序出现。二水草酸钙晶体溶解尿酸层并在核区或周边区域侵入其中。水草酸钙可能在与尿酸沉淀相同或相似的条件下沉淀,而二水草酸钙可能在不同条件下沉淀。我们基于对混合结石的形态学研究,讨论了尿酸和草酸钙混合结石的发病机制、异质成核和外延生长。