| Literature DB >> 7158089 |
E Schulz, M Hackeschmidt, G Stadie.
Abstract
The formation of urinary calculi is usually interpreted chemico-crystallographically. However, hydrodynamic examinations, both theoretical and experimental, show that unfavourable flow conditions in the pelvi-calyceal system may allow pathogens to remain in the appropriate zones for the length of time necessary for growth. Some light is shed on a new factor which has so far been ignored. Part I deals with theoretical considerations, while part II gives information on preliminary experiments using statistical models.Mesh:
Year: 1982 PMID: 7158089
Source DB: PubMed Journal: Z Urol Nephrol ISSN: 0044-3611