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Query: UMLS:C0020500 (hyperoxaluria)
 912 document(s) hit in 31,850,051 MEDLINE articles (0.00 seconds)

Nephrolithiasis is one of the most frequent pathologies of the urinary tract. Its prevalence in the city of Buenos Aires is 4%. Different biochemical and physiological disturbances may create an environment conductive to renal stone formation. We present the results of an ambulatory evaluation in 2612 patients for the purpose of updating the classification of nephrolithiasis. An abnormal urinary biochemistry was observed in 2423 patients (92.8%) that could be classified in 15 categories. A single diagnosis was documented in 61.5% of the patients, and the remaining 31.2% had more than one diagnosis (concurrent abnormalities). No abnormality was found in 189 stone formers (7.2%). Idiopathic hypercalciuria was the most frequent abnormality, it was encountered in 31.2%; hyperuricosuria and gouty diathesis (presence of urine pH < 5.5, with normal or high uricemia) accounted for 9.4% and 5.4% of patients, respectively. On the other hand, hypomagnesuria affected 6.7% of the stone formers and hypocitraturia was observed in 4.5%. Primary hyperparathiriodism, hyperoxaluria and cystinuria were seen less frequently in 2.6%, 1.3 and 0.45% of patients. Low urine volume was found in 12% of the patients. Among those patients with more than one abnormality, we found that hypercalciuria together with hyperuricosuria and hypocitraturia (12%) was the prevalent association followed by hypercalciuria with hyperuricosuria (9.1%). Our results show the importance of studying nephrolithiasis patients from a biochemical point of view, since this is the only way to achieve a diagnosis of the metabolic abnormality and introduce a specific therapy to prevent recurrence.
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PMID:[Metabolic changes in 2612 patients with nephrolithiasis]. 1068 59

Idiopathic hypercalciuria is the most important predisposing risk factor for calcium oxalate (CaOx) renal stone formation. We assessed the associations between spontaneous CaOx crystallization based on the Bonn Risk Index (BRI), urinary pH, calciuria, oxaluria, and citraturia in 140 Caucasian patients with hypercalciuria, aged 4-17 years, and compared the findings with those in 210 normocalciuric controls. Of the 140 hypercalciuric patients, 58 had renal stones, and 82 had recurrent erythrocyturia, renal colic, or urinary obstructive symptoms-but without stones. Urinary ionized calcium ([Ca(2+)]) levels were measured using a selective electrode, while the onset of crystallization was determined using a photometer and titration with 40 mmol/L ammonium oxalate (Ox(2-)). The calculation of the BRI was based on the [Ca(2+)]:Ox(2-) ratio. The BRI values were 12-fold higher in hypercalciuric children than in healthy controls, but no differences were found in the BRI between subjects with urinary stones and those with urolithiasis-like symptoms. An increased BRI suggested an association with hypercalciuria, lower urinary pH, hypocitraturia, and hypooxaluria. These data indicate that hypercalciuria is an important factor associated with increased urinary CaOx crystallization, although the causal pathways need further investigation. Determination of the BRI in children with hypercalciuria may improve the risk assessment of kidney stones.
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PMID:Spontaneous urinary calcium oxalate crystallization in hypercalciuric children. 1935 Feb 80