PHYSICOCHEMICAL ASPECTS OF UROLITHIASIS
PHYSICOCHEMICAL ASPECTS OF UROLITHIASIS
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DOI：
10.1038/ki.1978.53
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发表时间：
1978-01-01
影响因子：
19.6
通讯作者：
FINLAYSON, B
中科院分区：
文献类型：
--
作者：
FINLAYSON, B
以下讨论集中于草酸钙和磷酸钙结石，但也可以推广到其他形式的结石。尽管它构成了该主题的入门读物，但它确实试图解决我们目前对尿石症物理特征的贫乏知识中的不一致问题。此外，它还描述了似乎有用且应纳入尿石症研究的概念和方法，以使该领域的未来工作易于通过传统物理理论进行分析。尿石症的已知物理化学特征很容易分为四个相互关联的主题：驱动力（过饱和）、成核、晶体和颗粒的生长以及聚集。
The following discussion centers on calcium oxalate and calcium phosphate stones, but permits generalization to other forms of stone. Although it constitutes a primer on the subject, it does attempt to deal with inconsistencies in our current meager knowledge of the physical characteristics of urolithiasis. In addition, it describes concepts and approaches that appear to be useful and that should be incorporated into urolithiasis research, to make future work in the field susceptible to analysis by conventional physical theory.The known physicochemical features of urolithiasis are readily divided into four interrelated subjects: the driving force (supersaturation), nucleation, the growth of crystals and particles, and aggregation.