Titlebook: Urolithiasis; Clinical and Basic R Lynwood H. Smith,William G. Robertson,Birdwell Fin Book 1981 Springer Science+Business Media New York 19

vocation

Book 1981 five participants from continental Europe, Great Britain, and the United States met to review their work and exchange ideas regarding the formation of urinary calculi. This meeting achieved several important goals. It pulled together a nidus of workers in the many scientific disciplines that relate

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Hypophosphatemia in Recurrent Renal Stone Formers — Consequence of Arterial Hypertension?uals.. Hypophosphatemia is of interest in view of some recent proposals which try to link plasma phosphate and intestinal hyperabsorption of calcium in the pathogenesis of the hypercalciuria of recurrent renal stone formers via increased circulating levels of 1,25(OH). vitamin D..

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Urinary Excretion of Citrate in Normal Subjects and Patients with UrolithiasisIn previous investigations it has been demonstrated that citrate has two different roles in urine with respect to calcium-oxalate stone formation: (a) a complex formation between calcium and citrate resulting in a decreased ion activity product for calcium-oxalate, and (b) a direct inhibitory influence on the crystallization of calcium-oxalate.

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猛擊

Experience with the Short Ammonium Chloride TestSince renal tubular acidosis is often complicated by stone formation, it seemed justified to investigate a stone forming population in order to study the incidence of renal acidification defects. For this purpose it was necessary to develop a clinically useful method and to standardize the ammonium chloride test.

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Prediction of Stone Recurrence developed recurrent stones. This occurred more often in males than in females and particularly in individuals with a high urinary calcium. However, the overlap between the two groups was large and in the individual patient determinations of serum and urinary electrolytes could not predict the risk of recurrence.

Substance

Study of Calcium Crystals in Patients with Kidney Stonesble to find any difference in the saturation of calcium oxalate between stone-formers and normals, whereas the saturation of octocalcium phosphate was indeed higher in the stone formers although there was a considerable overlap..

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