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Query: UMLS:C0085580 (essential hypertension)
 14,686 document(s) hit in 31,850,051 MEDLINE articles (0.00 seconds)

To evaluate the antihypertensive and hormonal effects of oral magnesium supplementation, 17 inpatients with untreated, uncomplicated mild-to-moderate essential hypertension (EH) and 8 age-matched normotensive controls (controls) were given MgO orally 3 times a day at a daily dose of 1.0 g (0.6 g per day as Mg) for a period of 2 weeks. Supplementation of MgO elicited a significant fall in averaged mean blood pressure calculated with a 24-h ambulatory blood pressure monitoring system (MBP) in EH from a baseline value of 104.3 +/- 12.2 to 99.5 +/- 11.6 mmHg (p < 0.05), while controls remained unaltered from a baseline value of 85.1 +/- 11.5 to 84.5 +/- 13.3 mmHg. The percentage reductions in systolic and diastolic blood pressures were similar during daytime and nighttime in EH. According to the extent of reduction in MBP with magnesium supplementation, EH patients were divided into 2 groups, responder and nonresponder. The level of plasma renin activity (PRA) in the responder group was significantly higher than that of the nonresponder group (p < 0.05). After 2 weeks of magnesium supplementation, the plasma level of Na+, K(+)-ATPase inhibitory activity (PATPI), defined as equivalency to ouabain, was reduced significantly from 0.75 +/- 0.54 to 0.40 +/- 0.30 mumol ouabain/ml (p < 0.05) in the responder group, while it remained unaltered in controls and the nonresponder group. PRA, plasma aldosterone concentration, urinary epinephrine and norepinephrine excretion, and urinary sodium excretion did not change significantly in either control subjects or EH (responder and nonresponder groups). A significant negative correlation existed between the pretreatment PRA and changes in MBP after magnesium supplementation in EH (r = -0.65, p < 0.01), and there was a significant positive correlation between changes in PATPI and changes in MBP as a whole (r = 0.41, p < 0.05). These results support the view that oral magnesium supplementation is a useful approach to treatment of patients with uncomplicated essential hypertension, especially those with high plasmas renin activity. It appears that magnesium suppresses circulating Na+,K(+)-ATPase inhibitory activity to attenuate vascular tone, and thereby reduces blood pressure in EH.
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PMID:Effects of dietary magnesium supplementation on diurnal variations of blood pressure and plasma Na+, K(+)-ATPase activity in essential hypertension. 133 97

To elucidate the effects of magnesium on high blood pressure, a 4-week study of oral magnesium supplementation (MgO 1 g/day) was conducted in 21 outpatients with uncomplicated essential hypertension. During the study, blood pressure and intraerythrocyte sodium concentration decreased significantly, and the erythrocyte ouabain-sensitive 22Na efflux rate constant (Kos) and intraerythrocyte magnesium concentration both increased. Serum triglyceride and free fatty acid concentrations were reduced. Furthermore, the elevation in Kos significantly and positively correlated with both the increase in intraerythrocyte magnesium concentration and the decrease in mean blood pressure. There was a significant inverse correlation between the prestudy Kos and the decrease in mean blood pressure. In addition, when patients were divided according to their overall decrease in mean blood pressure, the prestudy intraerythrocyte sodium concentration was significantly higher in patients with a mean blood pressure decrease of more than 7 mm Hg than that of patients whose mean blood pressure decrease was less than 7 mm Hg. These results suggest that oral magnesium supplementation may lower blood pressure through the activation of a cell membrane sodium pump and may reduce serum lipid concentration. It also suggests that the lower the prestudy Kos or the higher the prestudy intraerythrocyte sodium concentration, the more effective the oral magnesium treatment is in lowering blood pressure. Therefore, we concluded that appropriate oral magnesium intake might be effective as a nonpharmacological treatment for essential hypertension.
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PMID:Oral magnesium supplementation in patients with essential hypertension. 253 96

The effects of magnesium supplementation were tested in 20 patients with essential hypertension receiving long-term thiazide diuretic treatment (Th group) and 21 age-matched untreated patients (EHT group). Intra-erythrocyte cations, water content and the ouabain-sensitive sodium efflux rate constant were measured. The Th group received magnesium supplementations as MgO (600 mg Mg/day) for 4 weeks. In the Th group intra-erythrocyte magnesium and the sodium efflux rate constant were lower and red cell sodium was higher than in the EHT group. During magnesium supplementation, there were significant decreases (p less than 0.01) in intra-erythrocyte sodium content and mean blood pressure, and increases (p less than 0.005) in red cell magnesium content and the sodium efflux rate constant. These effects of magnesium were more evident in 9 patients who were unresponsive to diuretic therapy, a definite reduction in mean blood pressure, from 104.8 +/- 2.7 mmHg to 94.4 +/- 2.2 mmHg (p less than 0.001), being observed. In the remaining 11 patients, however, blood pressure remained unchanged. The sodium efflux rate constant was positively correlated with red cell magnesium content and negatively correlated with sodium content (r = 0.61, p less than 0.005 and r = -0.57, p less than 0.01, respectively). These results indicate that long-term diuretic treatment may give rise to intracellular magnesium deficiency and a suppression of cell membrane active sodium transport. The results also suggest that oral magnesium may decrease intracellular sodium, possibly through the activation of Na-K-ATPase, which in turn may contribute to the reduction in blood pressure. Therefore, magnesium supplementation may be a worthwhile additional therapy for diuretics.
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PMID:Intracellular magnesium deficiency and effect of oral magnesium on blood pressure and red cell sodium transport in diuretic-treated hypertensive patients. 322 92

Twenty patients receiving long-term (1.0 to 10.3 years) thiazide diuretic treatment for essential hypertension (Th group) received magnesium supplementation as MgO (600 mg Mg/day) for 4 weeks and placebo for another 4 weeks. Before and at the end of each period, we measured blood pressure; intraerythrocyte magnesium, sodium, and potassium (R-Mg, R-Na, and R-K); and erythrocyte ouabain (10-4 M) sensitive sodium efflux rate constant (Kos). The same measurements were also performed in 21 untreated age-matched essential hypertensives (EHT group). In the Th group, R-Mg was lower, R-Na was higher, and Kos was lower than in the EHT group before magnesium supplementation. Oral magnesium resulted in a significant increase in R-Mg (p less than 0.005) and a decrease in R-Na (p less than 0.01), together with an increase in Kos (p less than 0.005) in the Th group. During magnesium supplementation, the increased Kos was correlated negatively with the lowered R-Na (r = -0.57, p less than 0.01) and positively with the increased R-Mg (r = 0.61, p less than 0.005). Systolic, diastolic, and mean blood pressures were reduced significantly during magnesium administration by a mean of 7.5, 3.0, and 4.5 mm Hg. The results indicate that long-term diuretic treatment may give rise to an intracellular magnesium deficiency and a suppression in cell membrane active transport for sodium, with a resultant increase in intracellular sodium content.(ABSTRACT TRUNCATED AT 250 WORDS)
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PMID:Effects of oral magnesium on blood pressure and red cell sodium transport in patients receiving long-term thiazide diuretics for hypertension. 341 12

Fifteen patients with uncomplicated mild to moderate primary hypertension (7 males, 8 females, age range 36-65 years) were submitted to a double blind randomized crossover study, receiving MgO 3 times a day at a daily dose of 1.0 g (600 mg/day of magnesium) and placebo for a period of 6 weeks. This was to test the effects of oral magnesium supplementation on blood pressure and sodium, potassium, calcium and magnesium intraerythrocyte concentrations. Concomitantly, plasma renin activity and serum aldosterone was also measured. Oral magnesium reduced significantly the systolic (delta = -7.6 mmHg, P < 0.05); diastolic (delta = -3.8 mmHg, P < 0.01) and mean blood pressure (delta = -5.9 mmHg, P < 0.01). After magnesium supplementation intraerythrocyte sodium concentration was reduced (delta = -0.55 mEq/l per cell, P < 0.01) and intraerythrocyte magnesium concentration was increased (delta = 1.20 mg/dl per cell, P < 0.01). The diminution of the blood pressure correlated positively with the reduction in intraerythrocyte sodium (r = 0.66, P < 0.01) after magnesium. However, our results have shown that the blood pressure response to oral magnesium was not homogeneous. Forty percent of our patients had their blood pressure effectively controlled (more than 10 mmHg reduction in mean blood pressure), being the hypotensive effect more evident in patients with recent hypertension and in those where the reduction in intraerythrocyte sodium was significantly greater than in the non-responder individuals. Intraerythrocyte potassium and calcium, serum aldosterone, plasma renin activity and urinary sodium excretion were maintained unchanged after magnesium supplementation. These data showed that oral magnesium supplementation may reduce the blood pressure, which can be partially explained by the decrease in intracellular sodium and augment in intracellular magnesium.
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PMID:Effects of magnesium on blood pressure and intracellular ion levels of Brazilian hypertensive patients. 889 90

The hydration rates of 12 obsidian samples of different chemical compositions were measured at temperatures from 95 degrees to 245 degrees C. An expression relating hydration rate to temperature was derived for each sample. The SiO(2) content and refractive index are related to the hydration rate, as are the CaO, MgO, and original water contents. With this information it is possible to calculate the hydration rate of a sample from its silica content, refractive index, or chemical index and a knowledge of the effective temperature at which the hydration occurred. The effective hydration temperature can be either measured or approximated from weather records. Rates have been calculated by both methods, and the results show that weather records can give a good approximation to the true EHT, particularly in tropical and subtropical climates. If one determines the EHT by any of the methods suggested, and also measures or knows the rate of hydration of the particular obsidian used, it should be possible to carry out absolute dating to +/- 10 percent of the true age over periods as short as several years and as long as millions of years.
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PMID:Hydration rate of obsidian. 1778 1