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Biomedical subjects

R S Moore

Publications and source records attributed to R S Moore.

At least 37 records · Page 2Linked to original sources
PubMed1992

Renal and metabolic effects of glucagon in the fetus.

The effects of pharmacological doses of glucagon (0.5 micrograms/kg/min) were studied in 8 chronically-catheterised fetal sheep. These doses of glucagon raised fetal blood glucose, and caused a small fall in fetal arterial PO2 (P less than 0.05). Arterial PCO2 rose (P less than 0.05) and pH fell (P less than 0.05) while plasma osmolality increased (P less than 0.01). There were no effects of glucagon on fetal renal function but in the fetus, like the adult, i.v. glucagon caused increases in heart rate (P less than 0.01) which were not associated with changes in arterial pressure.

Animals↗
PubMed1991

Changes in fetal and maternal plasma protein concentration and colloid osmotic pressure with gestation.

In pregnant ewes, plasma protein levels over the gestation age range of 58-141 days fell progressively (r = -0.332, P less than 0.05, n = 36) but colloid osmotic pressure (COP, mmHg) did not change significantly. In fetal sheep carried by these ewes, plasma protein levels increased with age (r = 0.85, P less than 0.00001, n = 32). COP also rose (r = 0.8, P less than 0.00001, n = 23). Since maternal COP did not change and fetal COP increased, the net transplacental COP gradient between mother and fetus decreased with increasing age (r = -0.589, P less than 0.004, n = 22). Fetal plasma protein levels can be used to calculate fetal COP while maternal plasma protein levels cannot be used to calculate maternal COP.

Animals↗
PubMed1988

Second-degree heart block associated with envenomation by Vipera berus.

Evenomation by the common European adder (Vipera berus) is well known for its significant morbidity but low mortality. Cardiac complications tend to take second place to the systemic upset and usually only comprise non-specific ECG changes. This case illustrates many of the classical features of adder bite but it is also the first account of heart block as a complication.

Aged↗
PubMed1982

Adsorption of reovirus by minerals and soils.

Adsorption of [35S]methionine-labeled reovirus by 30 dry soils, minerals, and finely ground rocks suspended in synthetic freshwater at pH 7 was investigated to determine the conditions necessary for optimum virus removal during land application of wastewaters. All of the minerals and soils studied were excellent adsorbents of reovirus, with greater than 99% of the virus adsorbed after 1 h at 4 degrees C. Thereafter, virus remaining in suspension was significantly inactivated, and within 24 h a three to five log10 reduction in titer occurred. The presence of divalent cations, i.e., Ca2+ and Mg2+, in synthetic freshwater enhanced removal, whereas soluble organic matter decreased the amount of virus adsorbed in secondary effluent. The amount of virus adsorbed by these substrates was inversely correlated with the amount of organic matter, capacity to adsorb cationic polyelectrolyte, and electrophoretic mobility. Adsorption increased with increasing available surface area, as suspended infectivity was reduced further by the more finely divided substrates. However, the organic content of the soils reduced the level of infectious virus adsorbed below that expected from surface area measurements alone. The inverse correlation between virus adsorption and substrate capacity for cationic polyelectrolyte indicates that the adsorption of infectious reovirus particles is predominately a charged colloidal particle-charged surface interaction. Thus, adsorption of polyelectrolyte may be useful in predicting the fate of viruses during land application of sewage effluents and sludges.

Adsorption↗
PubMed1981

Poliovirus adsorption by 34 minerals and soils.

The adsorption of radiolabeled infectious poliovirus type 2 by 34 well-defined soils and mineral substrates was analyzed in a synthetic freshwater medium containing 1 mM CaCl(2) and 1.25 mM NaHCO(3) at pH 7. In a model system, adsorption of poliovirus by Ottawa sand was rapid and reached equilibrium within 1 h at 4 degrees C. Near saturation, the adsorption could be described by the Langmuir equation; the apparent surface saturation was 2.5 x 10(6) plaque-forming units of poliovirus per mg of Ottawa sand. At low surface coverage, adsorption was described by the Freundlich equation. The soils and minerals used ranged from acidic to basic and from high in organic content to organic free. The available negative surface charge on each substrate was measured by the adsorption of a cationic polyelectrolyte, polydiallyldimethylammonium chloride. Most of the substrates adsorbed more than 95% of the virus. In general, soils, in comparison with minerals, were weak adsorbents. Among the soils, muck and Genesee silt loam were the poorest adsorbents; among the minerals, montmorillonite, glauconite, and bituminous shale were the least effective. The most effective adsorbents were magnetite sand and hematite, which are predominantly oxides of iron. Correlation coefficients for substrate properties and virus adsorption revealed that the elemental composition of the adsorbents had little effect on poliovirus uptake. Substrate surface area and pH, by themselves, were not significantly correlated with poliovirus uptake. A strong negative correlation was found between poliovirus adsorption and both the contents of organic matter and the available negative surface charge on the substrates as determined by their capacities for adsorbing the cationic polyelectrolyte, polydiallyldimethylammonium chloride.

Adsorption↗
PubMed1981

Influence of pH and electrolyte composition on adsorption of poliovirus by soils and minerals.

The pH and the nature an concentration of simple electrolytes influenced the interaction of poliovirus type 2 with three soils, a sand, and a clay mineral. In electrolytes above pH 9 the virus was not adsorbed extensively to the substrates, but below pH 7 almost all virus was bound. For each adsorbent there was a characteristic pH region of transition from strong to weak uptake. Differences between the soils in virus uptake were shown to parallel their pH-dependent mineral. In electrolytes above pH 9 the virus was not adsorbed extensively to the substrates, but below pH 7 almost all virus was bound. For each adsorbent there was a characteristic pH region of transition from strong to weak uptake. Differences between the soils in virus uptake were shown to parallel their pH-dependent mineral. In electrolytes above pH 9 the virus was not adsorbed extensively to the substrates, but below pH 7 almost all virus was bound. For each adsorbent there was a characteristic pH region of transition from strong to weak uptake. Differences between the soils in virus uptake were shown to parallel their pH-dependent charge properties, as determined by whole-particle microelectrophoresis. Only when the pH was close to or above the critical region was uptake increased with electrolyte concentration. The transition region for all substrates was above pH 7.5 the isoelectric point of the virus. Thus, it appears that when both the virus and substrate are highly negative charged, repulsive electrostatic effects may exceed inherent attractive interactions, thereby inhibiting adsorption.

Adsorption↗