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Oxygen-Bonded Carbonyls 87

Oxygen-car7ing capacity of human blood in comparison with pure perfluoro-n-octyl bromide .

Oxygen-carrying capacity of whoie blood, Hb-solution, and first-and second-generation perfiuorocarbon emulsions.

Oxygen-chelated propagating species observed during 22b-initiated ROMP.

Oxygen-conducting membranes consisting of a porous support and a dense top layer, both parts consist of the same perovskite

Oxygen-containing anion species in chloroaluminate ILs, as proposed by Osteryoung and Zawodzinsky .

Oxygen-containing groups on turbostratic carbon plane edges modified

Oxygen-containing heterocyclic compounds found in AG-secretions

Oxygen-dependent epoxidation pathways catalyzed by Mb.

Oxygen-dependent glucose enzyme sensor coupled with amperometric detection.

Oxygen-dependent stabilization of HIF-la. Western blot

Oxygen-directed, desymmetrizing Mizoroki-Heck cyclization.

Oxygen-ethyl ne interaction energies in the absence of subsurface oxy gen .

Oxygen-ethytene interaction energies in the presence of subsurface oxy gen energy unit eV, distance unit

Oxygen-evolution activity as a function of Cl- concentration in the PS-II inside-out vesicles without the 23-kOa poiypeptide present. Figure source

Oxygen-expanded chromium complexes showing proposed resonance hybrids for the expanded ligand.

Oxygen-expanded chromium dithiocarbamate complexes together with representations of possible resonance hybrids for the expanded ligand.

Oxygen-fuel mass concentrations in mixture fraction space by Equation , and at y 6,

Oxygen-functional comonomers

Oxygen-functionalized surfaces improve the attachment and culture of osteoblast-like cells in vitro. Scanning electron microscopy showing human primary osteoblast-like cells the scale bar indicates 100 pm.

Oxygen-hemoglobulin dissociation curve.

Oxygen-hydrogen distribution function in liquid water determined at 25 C by neutron diffraction .

Oxygen-hydrogen-water steam cycle

Oxygen-induced homocoupling of organoboronic acids

Oxygen-isotopic compositions of CM2 carbonaceous chondrites plotted in a three-isotope diagram. The CM2s form a linear array with a slope of 0.7, with enrichments in the heavy isotopes that show a general increase as a function of increasing alteration. Nogoya .



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