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Rates and Mechanisms of Dissolution of Renal Calculi. III. Mechanisms and Rates of Dissolution of Simulated Oxalate Calculi in Acid and Edta Solutions

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Urolithiasis

Abstract

A previous communication1 showed that dissolution or urinary calculi sections did not exhibit zero-order (i. e., constant) rates under sink conditions. Since pure calcium oxalate discs did exhibit a constant dissolution rate, it was concluded that controlling processes other than the intrinsic solution properties of calcium oxalate must be operative in the dissolution behavior of real calculi. In this paper we intend to compare models described previously2 with the dissolution behavior of artificial calculi in various media.

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References

  1. J. Pawelchak, D. R. Flanagan, and A. P. Simonelli, in: “Proceedings of the Fourth International Symposium on Urolithiasis Research,” L. H. Smith, B. Finlayson, and W. G. Robertson, eds. Plenum Press, New York (in press).

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  2. J. Pawelchak, D. R. Flanagan, and A. P. Simonelli, in: “Proceedings of the Fourth International Symposium on Urolithiasis Research,” L. H. Smith, B. Finlayson, and W. G. Robertson, eds. Plenum Press, New York (in press).

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© 1981 Springer Science+Business Media New York

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Pawelchak, J., Flanagan, D.R., Simonelli, A.P. (1981). Rates and Mechanisms of Dissolution of Renal Calculi. III. Mechanisms and Rates of Dissolution of Simulated Oxalate Calculi in Acid and Edta Solutions. In: Smith, L.H., Robertson, W.G., Finlayson, B. (eds) Urolithiasis. Springer, Boston, MA. https://doi.org/10.1007/978-1-4684-8977-4_91

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  • DOI: https://doi.org/10.1007/978-1-4684-8977-4_91

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4684-8979-8

  • Online ISBN: 978-1-4684-8977-4

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