1. Anomalous transmembrane anion transport has been observed in erythrocytes of patients with idiopathic calcium nephrolithiasis. 2. To verify whether cation transport is also abnormal, we investigated the frusemide-sensitive Na+ efflux from Na(+)-loaded erythrocytes and the natriuretic response to acute intravenous frusemide administration in calcium oxalate renal stone formers. 3. Frusemide administration induced a statistically significant smaller increase in the fractional excretion of Na+ in patients than in control subjects. Abnormal kinetic properties of erythrocyte Na(+)-K(+)-2Cl- cotransport were observed in approximately 60% of stone formers. The Km for Na+ of Na(+)-K(+)-2Cl- co-transport correlated with urinary Ca2+ excretion. 4. The abnormal kinetic properties of Na(+)-K(+)-2Cl- co-transport may be relevant for stone formation, hampering renal Ca2+ reabsorption in the distal nephron and determining critical physicochemical conditions for calcium/oxalate crystallization.

Abnormal erythrocyte and renal frusemide-sensitive sodium transport in idiopathic calcium nephrolithiasis.

Gambaro G;
1994-01-01

Abstract

1. Anomalous transmembrane anion transport has been observed in erythrocytes of patients with idiopathic calcium nephrolithiasis. 2. To verify whether cation transport is also abnormal, we investigated the frusemide-sensitive Na+ efflux from Na(+)-loaded erythrocytes and the natriuretic response to acute intravenous frusemide administration in calcium oxalate renal stone formers. 3. Frusemide administration induced a statistically significant smaller increase in the fractional excretion of Na+ in patients than in control subjects. Abnormal kinetic properties of erythrocyte Na(+)-K(+)-2Cl- cotransport were observed in approximately 60% of stone formers. The Km for Na+ of Na(+)-K(+)-2Cl- co-transport correlated with urinary Ca2+ excretion. 4. The abnormal kinetic properties of Na(+)-K(+)-2Cl- co-transport may be relevant for stone formation, hampering renal Ca2+ reabsorption in the distal nephron and determining critical physicochemical conditions for calcium/oxalate crystallization.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11562/998760
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