Bond strength of chlorine peroxide.

The bond strength of chlorine peroxide (ClOOCl) is studied by photoionization mass spectrometry. The experimental results are obtained from the fragmentation threshold yielding ClO+, which is observed at 11.52 +/- 0.025 eV. The O-O bond strength D(o) is derived from this value in comparison to the first ionization energy of ClO, yielding D(o)298 = 72.39 +/- 2.8 kJ mol(-1). The present work provides a new and independent method to examine the equilibrium constant K(eq) for chlorine peroxide formation via dimerization of ClO in the stratosphere. This yields an approximation for the equilibrium constant in the stratospheric temperature regime between 190 and 230 K of the form K(eq) = 1.92 x 10(-27) cm3 molecules(-1) x exp(8430 K/T). This value of K(eq) is lower than current reference data and agrees well with high altitude aircraft measurements within their scattering range. Considering the error limits of the present experimental results and the resulting equilibrium constant, there is agreement with previous works, but the upper limit of current reference values appears to be too high. This result is discussed along with possible atmospheric implications.

Cryogenic trapping of carbonyl sulfide without using expendable cryogens

We report on a cryogenic trapping procedure that functions without the use of liquid cryogens at a trapping temperature of -150 degrees C. A heat-transfer device was designed that links a commercially available closed-cycle refrigerator to a cryotrap made of a glass-coated steel tube filled with Chromosorb W adsorbent material. This forms part of an analytical system incorporating GC separation with subsequent FPD detection, used for the analysis of carbonyl sulfide. The recovery is greater than 95% for trapping times up to 30 min. The analytical performance is excellent with both accuracy and precision better than 2%. Equipped with the new cryogenic trapping device, the measurement system is capable of continuous operation over a period of several weeks.

Dissimilatory Fe(III) reduction by Clostridium beijerinckii isolated from freshwater sediment using Fe(III) maltol enrichment.

A microorganism which reduces Fe(III) during the fermentation of glucose was isolated from freshwater sediment. The Fe(III) was supplied to enrichment cultures as a soluble complex with the bidentate ligand maltol (3-hydroxy-2-methyl-4-pyrone). Advantages that were afforded by the use of Fe(III)(maltol)3 over previously published methods included negation of the requirement for assays of Fe(II) formation. Because Fe(III)(maltol)3 has a characteristic deep red colour, Fe(III) reduction could be quantified spectrophotometrically by monitoring the disappearance of the complex in liquid cultures. Furthermore, Fe(III) reduction on agar plates containing the complex was apparent by zones of decolourisation around the bacterial colonies. 16S rRNA gene sequencing indicated the isolate to be a strain of Clostridium beijerinckii. Growth experiments were performed on the isolate in batch cultures with varying concentrations of Fe(III) citrate and 50 mM glucose. Increasing the level of Fe(III) citrate present was found to alter the fermentation balance, with less acidic products being formed. The presence of Fe(III) led to increases in the growth rate and growth yield, which were both approximately doubled when the supply of the cation reached 25 mM. A NAD(P)H-dependent Fe(III) reductase activity was localised to the bacterial membrane and found not to be sensitive to respiratory inhibitors. Taken together, these data suggest that dissimilatory Fe(III) reduction by the isolate provides a means of utilising the cation as an electron sink, thus facilitating pyridine nucleotide to be recycled during fermentative metabolism.