| Literature DB >> 732883 |
Abstract
Oxalate, uric acid, and phosphate stones have been analyzed for their carbon isotope composition. The oxalate stones show delta13C values between -17.0 and -19.5%, the uric acid stones between -14.9 and -19.4%, and the phosphate stones between -13.0 and -23.9%. It is proposed that endogenic rather than exogenic sources are responsible for the 13C/12C ratios of the stones. The isotopic composition of the phosphate stones seems to be influenced primarily by bacterial activity.Entities:
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Year: 1978 PMID: 732883 DOI: 10.1007/bf00364908
Source DB: PubMed Journal: Naturwissenschaften ISSN: 0028-1042