Abstract
The goal of this study was to investigate the role of MgSO4 in aglomerular kidney function, independent of changes in NaCl. The renal handling of MgSO4 was manipulated by intravenous infusion of an isoosmotic solution containing 80 mmol/L MgSO4 or through exposure to an environment that was reduced in MgSO4 concentration by 90%. Intravenous infusion resulted in a transient increase in circulating Mg2+ and SO4 (2-) levels; however, the concentration of both divalent ions in the urine remained elevated throughout the entire infusion period. Infusion also resulted in a transient increase in urine flow rate and apparent glomerular filtration rate, measured using the glomerular filtration rate marker, [3H] PEG 4000. Exposure to MgSO4-depleted conditions resulted in a significant decrease in plasma and urine concentrations of Mg2+ and in the urine concentrations of SO4 (2-); correspondingly, urine flow rate was significantly depressed. The urinary excretion of both Mg2+ and SO4 (2-) demonstrated nonlinear saturation kinetics. The urinary excretion of Mg2+ was significantly correlated with plasma Mg2+ concentration (r=0.75, P=0.04) and yielded a Michealis constant (Km) of 1.67+/-1.43 mmol/L; P=0.26 and a maximal velocity (Vmax) of 117.4+/-47.0 micromol/kg/hr; P=0.046. The urinary excretion of SO4 (2-) was significantly correlated with plasma SO4 (2-) concentration (r=0.94, P<0.02) with a Km of 0.76+/-0.54; P=0.26 and a Vmax of 59.3+/-13.1; P=0.02.
