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O C Zafiriou

Publications and source records attributed to O C Zafiriou.

4 recordsLinked to original sources
PubMed2001

A simple automated continuous-flow-equilibration method for measuring carbon monoxide in seawater.

A simple, robust, low-maintenance method using air-segmented continuous-flow equilibration was developed and automated to measure carbon monoxide (CO) in natural waters precisely and accurately. Finely regulated flows of CO-free air and of seawater or standard water were pumped into a glass coil, forming discrete gas/liquid segments. The partially CO-equilibrated gas effluent was injected into a Trace Analytical reduction analyzer for CO detection. A semiempirical mass-balance model was established for predicting and optimizing the performance of the CO extractor. The optimized gas and water flow rates were approximately 1.2 and approximately 14 mL min(-1), respectively, giving a response time of less than 15 min and a CO-extraction yield of approximately 80%. The analytical blank, precision, and accuracy were, respectively, 0.02 nM, +/-2.5% (at the approximately 1 nM level), and better than 5%. Two extractors can be interfaced to one detector at 4-6 samples per hour for each extractor. Coupled with a continuous surface-water sampler, the system was successfully applied to monitoring the diurnal variation of CO concentration in Sargasso Sea surface waters.

Automation↗
PubMed1990

Steady-state nitric oxide concentrations during denitrification.

Three species of denitrifying bacteria, Paracoccus denitrificans, Pseudomonas stutzeri strain JM300, and Achromobacter cycloclastes, were allowed to reduce nitrate or nitrite in anaerobic, closed vials while the equilibration of gases between aqueous and gas phases was facilitated by vigorous stirring. The gas phase was sampled and analyzed for NO with use of a chemiluminescence detector calibrated against bottled NO standards or against NO produced by the nitrite-iodide reaction. [NOaq] was inferred from [NOg] and the solubility of NO. NO was detected only during denitrification in amounts that, once established, did not change with time, were independent of the initial concentration of nitrate or nitrite, and were largely independent of cell concentration, at least when nitrate was the oxidant. The usual level of NO was promptly re-established following the addition of exogenous NO or following the loss of NO by sparging. The aforementioned properties are expected for a steady-state intermediate in denitrification. Steady-state [NOaq] ranged between 1 and 65 nM depending on species and conditions. Similar results were also obtained in a related experiment in which P. stutzeri strain ZoBell respired nitrite under growth conditions. The very low steady-state [NOaq] observed during denitrification imply that the maximum activity of nitric oxide reductase in vivo, if it could be realized, would be large relative to that for nitrite reductase. This circumstance allows NO to be an intermediate without reaching toxic steady-state levels.

Alcaligenes↗
PubMed1989

Nitric oxide and nitrous oxide production and cycling during dissimilatory nitrite reduction by Pseudomonas perfectomarina.

The denitrifier Pseudomonas perfectomarina reduced nitrite under conditions of kinetic competition between cells and gas sparging for extracellular dissolved nitric and nitrous oxides, NOaq and N2Oaq, in a chemically defined marine medium. Time courses of nitrite reduction and NOg and N2Og alpha removal were integrated to give NOg and N2Og yields. At high sparging rates, the NOg yield was greater than 50% of nitrite-N reduced, and the yield of NOg + N2Og was approximately 75%. Hence interrupted denitrification yields NOaq and N2Oaq as major products. The yields varied with sparging rates in agreement with a quantitative model of denitrification (Betlach, M. P., and Tiedje, J.M. (1981) Appl. Environ. Microbiol. 42, 1074-1084) that applies simplified Michaelis-Menten kinetics to NO2-----NOaq----N2Oaq----N2. The fit gave an estimate of the maximum scavengeable NOaq yield of 73 +/- 8% of nitrite-N. Thus a minor path independent of NOaq is also required. The fit of the model to data at lower sparging rates, where normal denitrification products predominate, implies that the extracellular NOaq pool yield is independent of gas sparging rate. Thus in P. perfectomarina NOaq and N2Oaq are intermediates, or facilely equilibrate with true intermediates, during complete denitrification. The recovery of most nitrite-N as NO and/or N2O under perturbed conditions is not an artifact of irreversible product removal, but an attribute of denitrification in this species, and most probably it is characteristic of denitrification in other species as well.

Kinetics↗