The changing pattern of urinary tract stone disease.
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Biomedical subjects
Publications and source records attributed to A Hodgkinson.
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Plasma and uric acid levels were measured in 132 men with calcium-containing renal stones and in 24 healthy men of similar ages. Fasting resulted in a significant fall in the mean plasma uric acid level of normal subjects. Intermittent hyperuricaemia was observed in 7% of fasting patients. Intermittent hyperuricosuria was found in 17% of non-fasting patients but in only 2 to 6% of fasting subjects. Most of the uric acid abnormalities in patients with calcium stones therefore appear to be due to diet and may be prevented by reducing the consumption of purine-rich foods. A direct relationship was observed between uric acid excretion and urine flow at normal flow rates. It is suggested that the apparent increase in stone incidence, which occurs with rising living standards, may be due partly to increased consumption of purine-rich foods.
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An increase in the average calcium oxalate content and decrease in average calcium phosphate content of stones received for analysis has been noted in a 9-year study. These changes appear to be due to a progressive increase in the number of patients with noninfected upper urinary tract stone and to the gradual elimination of phosphatic stones as a result of improved diagnosis and treatment. Some of the conditions associated with calcium phosphate stones are examined, particularly primary hyperparathyroidism, renal tubular acidosis, and medullary sponge kidney. These results further emphasize the importance of calcium oxalate in idiopathic stone disease and the need for a fuller understanding of the factors influencing calcium oxalate crystallization.
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A better understanding of the physico-chemical principles underlying the formation of calculus has led to a need for more precise information on the chemical composition of stones. A combined qualitative and quantitative procedure for the chemical analysis of urinary calculi which is suitable for routine use is presented. The procedure involves five simple qualitative tests followed by the quantitative determination of calcium, magnesium, inorganic phosphate, and oxalate. These data are used to calculate the composition of the stone in terms of calcium oxalate, apatite, and magnesium ammonium phosphate. Analytical results and derived values for five representative types of calculi are presented.
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