Abstract

Objectives: The aim of this study was to investigate frequencies of kidney stone constituents in a Norwegian population and examine trends over time by comparing with an earlier study of this population.Materials and methods: Upper urinary tract calculi consecutively collected from patients who underwent stone surgery at Akershus University Hospital from July 2014 to December 2017, in total 1252 calculi, were analysed by infrared spectroscopy. The results were compared with a study of 500 calculi collected from June 1975 to September 1980 at the same hospital.Results: The male:female ratio was 1.83:1. Single-component stones constituted 39%, 35% were binary, and 25% ternary. Main stone component frequencies were oxalate 71.3%, calcium oxalate monohydrate 53.7% with higher occurrence in males, calcium oxalate dihydrate 17.6%, carbonate apatite 10.8% and struvite 5.7%, both with higher occurrence in females, uric acid 8.9% with a non-significant male predominance, brushite 1.6% and cystine about 1%. Over four decades the frequency of UA stones increased by 4.6-times, whereas struvite and pure carbonate apatite stones decreased and no change was observed for brushite stones.Conclusion: Frequencies of kidney stone types in this Norwegian population are mainly in accordance with other studies, except a large increase in UA stones over four decades, partly caused by a particularly low frequency of UA stones in the old study, a decreased carbonate apatite frequency over four decades, and an unaltered brushite frequency. Also, in contrast to other studies, a relatively small and non-significant male UA stone predominance was found.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.