The structure of di-valent and tri-valent metals
Pseudopotential and second order perturbation theory applied to divalent and trivalent metal structures
SEARCH · Search NASA
Search indexed NASA NTRS and DOE OSTI research on propulsion, heat transfer, battery materials and energy systems. Follow report and document links to the original sources.
Quote a phrase for an exact phrase match. Source license links do not imply unrestricted reuse.
Pseudopotential and second order perturbation theory applied to divalent and trivalent metal structures
Partial wave calculation of diatomic divalent molecular /HeH/ ion
Absorption spectra of divalent iron in transition group elements and gallium phosphide
Structures of divalent and trivalent metals in terms of pseudopotentials and second order perturbation theory
Magnetic field induced hyperfine structure in mono- and divalent iron ions in magnesium and calcium oxide, showing evidence of paramagnetic resonance
Divalent Eu ion ground state splitting in C3h symmetry sites and associated color centers in EPR spectrum study of Eu ion doped lanthanum trichloride
Free ion and rare earth crystal energy levels spectra compared to divalent and trivalent spectra
EPR observation of Eu ion transformation from trivalent to divalent charge states under illumination in cadmium fluoride-Eu crystal
Hyperfine coupling constants of positive divalent Mn ion in calcium and barium fluorides, measuring temperature dependence by analyzing electron spin resonance spectrum
Nuclear magnetic resonance measurements determine which metallochlorophylls, besides magnesium-containing chlorophylls, possess coordination aggregation properties. Infrared spectroscopy reveals that only zinc pheophytin and zinc methyl pheophorbide showed significant coordination aggregation, whereas divalent nickel and copper did not.
Ground state energies of HeH divalent ion, comparing perturbation calculation values with variation-perturbation technique
Electron transport chain of monovalent and divalent cations and of polyamines, studying effects on menadione reductase activity to determine salt dependence
Divalent Mg-Fe ion order-disorder and thermodynamics of orthopyroxene /Mg,Fe/SiO3 crystalline solution
Chemical synthesis of thermally stable organometallic polymers with divalent metal ion and tetraphenylphosphonitrilic units
Elimination of two step voltage discharge property of silver zinc batteries by using divalent silver oxide capacity of cell to charge anodes to monovalent silver state
The electrochemical oxidation of p-type boron in 0.2 N NaNO3 solutions of pH 0.4 to 13.1 was studied by galvanostatic techniques. The capacitance of the electrode, Tafel slopes, and a limited analysis of reaction mechanisms are reported. The anodic dissolution in acid solution is a charge-transfer-limited one-electron reaction to form a monovalent species in the over-potential region of 0.25 to 0.70 V. The dissolution in basic solution is most probably a one-electron charge-transfer reaction from a monovalent to divalent species involving three hydroxyl ions. Open circuit potentials were mixed potentials, probably due to hydrogen formation at open circuit but not contributing to the electrochemical reaction at the applied overpotential. Exchange current, estimated by extrapolation of the Tafel line to the standard oxidation potential for the boron reaction, were of the order of 10 to the minus 6th power A/cm2 in acid solution and 10 to the minus 12th power A/cm2 in basic solution. The reaction order of the rate determining acidic and basic reactions was determined with regard to (H+) and (OH-). The level of illumination had no effect on the electrochemical behavior of the electrode.
The subsolidus cooling history of basaltic rocks can be deduced from the distribution of divalent Mg and Fe ions over the two nonequivalent positions M1 and M2 in pyroxene. The ion exchange reaction between M1 and M2 is generally characterized by rapid kinetics. It is found that the normal cooling process of basalt 14053 was interrupted at a temperature below 840 C and that the rock was then quenched extremely rapidly.
Analyses for porphyrins in the lunar samples were carried out by extracting the lunar soils as received by organic solvents followed by analytical demetallation using methanesulfonic acid after which free-base porphyrins, if present, were recovered and demonstrably recomplexed with divalent cations. Samples from Apollo 11 showed the presence of fluorescent substances attributed to exhaust from the descent engine. One sample from Apollo 12 showed pigments resembling porphyrins. The Apollo 14 results were negative.