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肾单位内的结晶形成与结石形成。

Crystallization and stone formation inside the nephron.

作者信息

Kok D J

机构信息

Department of Pediatric Urology, Erasmus University Hospital Rotterdam, The Netherlands.

出版信息

Scanning Microsc. 1996;10(2):471-84; discussion 484-6.

PMID:9813625
Abstract

A model is presented visualizing the events leading to calcium-salt, crystal- and stone-formation inside the nephron. For each nephron segment, handling of urine components relevant to stone formation is considered and urine composition determined. This information was applied to nucleation experiments simulating passage of urine through a nephron. The model and in vitro experiments suggest that within normal transit times for the respective nephron segments, particles of a hydroxyapatite-like material first form near the bend in the Loop of Henle of juxtamedullary nephrons. From there on, calcium oxalate particles start to appear: first dihydrate, then monohydrate. In the collecting duct system, particle size increases primarily due to crystal agglomeration. Several conclusions with clinical and experimental relevance can be drawn. An increase in urinary volume does not decrease the chance of crystal formation in the Loop of Henle, but does decrease passage time through the collecting ducts, and thus, the time allowed for large particle formation. A calcium load does not increase the risk for nucleation up to the distal tubule, but does increase the risk of large particle formation in the collecting ducts. An oxalate load increases the chance for nucleation throughout the nephron. For experiments simulating crystallization processes occurring inside the nephron, diluted urines should be used. They should be diluted 16 to 50 times for testing nucleation, 2 to 30 times for testing crystal growth, and 2 to 20 times for testing crystal agglomeration. Undiluted urines may be used to mimic conditions in the pelvis and the bladder.

摘要

本文提出了一个模型,可视化了肾单位内导致钙盐、晶体和结石形成的过程。对于每个肾单位节段,考虑了与结石形成相关的尿液成分处理情况并确定了尿液成分。该信息被应用于模拟尿液通过肾单位的成核实验。该模型和体外实验表明,在各肾单位节段的正常转运时间内,类羟基磷灰石物质的颗粒首先在近髓肾单位的髓袢弯曲处附近形成。从那里开始,草酸钙颗粒开始出现:首先是二水合物,然后是一水合物。在集合管系统中,颗粒大小主要由于晶体团聚而增加。可以得出几个具有临床和实验相关性的结论。尿量增加不会降低髓袢中晶体形成的机会,但会减少通过集合管的时间,从而减少形成大颗粒的时间。钙负荷在远曲小管之前不会增加成核风险,但会增加集合管中形成大颗粒的风险。草酸盐负荷会增加整个肾单位成核的机会。对于模拟肾单位内发生的结晶过程的实验,应使用稀释尿液。测试成核时应稀释16至50倍,测试晶体生长时应稀释2至30倍,测试晶体团聚时应稀释2至20倍。未稀释的尿液可用于模拟肾盂和膀胱中的情况。

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