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Urolithiasis pp 309–313Cite as

The Role of Affluence in Recurrent Stone Formation

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Abstract

The formation of urinary calculi is a multifactorial disorder and is the end-product of a number of pathogenetic mechanisms. It has been suggested that stone-formation in the upper urinary tract is a disease of the industrialized countries1. Recently, Robertson2, among others, has drawn attention to a possible relationship between urinary stone-formation and environmental factors. The purpose of the present study is to investigate the relationship between aspects of social infra-structure and the incidence of recurrent stone-formation.

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References

  1. D. A. Andersen, in: “Proceedings of the Renal Stone Research Symposium,” B. E. C. Nordin and A. Hodgkinson, eds., J. & A. Churchill, Ltd., London (1969).

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  2. W. G. Robertson, M. Peacock, and P. J. Heyburn, in: “Pathogeneseund Klinik der Harnsteine VI,” W. Vahlensieck and G. Gasser, eds., Dr. D. Steinkopff, Darmstadt (1978).

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  3. W. G. Robertson, M. Peacock, and P. J. Heyburn in: “Statistische Nachrichten,” 35:12 (1980).

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  4. W. G. Robertson, P. J. Heyburn, and M. Peacock, Clin. Sei.57:285 (1979).

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  5. F. L. Coe, in: “Uric Acid,” W. N. Kelley and J. M. Weiner, eds., Springer, Berlin-Heidelberg-New York (1978).

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© 1981 Springer Science+Business Media New York

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Zechner, O., Scheiber, V. (1981). The Role of Affluence in Recurrent Stone Formation. In: Smith, L.H., Robertson, W.G., Finlayson, B. (eds) Urolithiasis. Springer, Boston, MA. https://doi.org/10.1007/978-1-4684-8977-4_51

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  • DOI: https://doi.org/10.1007/978-1-4684-8977-4_51

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4684-8979-8

  • Online ISBN: 978-1-4684-8977-4

  • eBook Packages: Springer Book Archive

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