The ionization of hydrogen and of hydrogenic positive ions by electron impact
Ionization of hydrogen and hydrogenic positive ions by electron impact
SEARCH · Engineering Papers
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.
Ionization of hydrogen and hydrogenic positive ions by electron impact
The bonding of water to the transition metal positive ions is electrostatic in origin. The electrostatic bonding is enhanced by a variety of mechanisms: mixing in 4p character, 4s-3d hybridization, and 4s promotion into the compact 3d orbital. The importance of these effects varies between the different metal ions due to changes in the separation of the metal ion atomic states. Furthermore, the change in the metal-water repulsion when a second water is added also changes the relative importance of the different metal asymptotes. The second water binding energy varies from being 11 kcal/mol smaller than the first for Mn(+) to 3 kcal/mol larger for V(+) and Fe(+).
Positive ion density and electron temperature in ionospheric e and f regions, using ejected electrostatic probe measurements
Thermal hydrogen and helium ion distribution in magnetoionosphere - OGO-A positive ion spectrometer
Positive ion layers in E region explained by wind shear theory, obtaining steady state solutions for simple model
A, a and B functions for electron broadening of positive ions with hyperbolic path
D region positive ion composition measurements by rocket-borne quadrupole mass spectrometer, discussing downleg and upleg data
Electron and positive ion densities and their relationship to ionization sources in equatorial D region
Positive ion collection by highly negative spherical electrostatic probe in collision dominated plasma
Ionospheric characteristics from altitude variations of positive ion densities at night
Initial deceleration of solar wind positive ions upstream of earth bow shock determined from OGO 5 high time resolution plasma measurements
Daytime D region positive ion composition measurements for solar zenith angles of 53.2 and 27.8 degrees
The importance of measuring electron-ion excitation cross sections in singly and multiply charged positive ions is outlined, and recent results for Mg II and O II ions are given using the JPL's electron energy-loss merged-beams apparatus. Theoretical comparisons are given with two five-state close-coupling calculations. The energy variation of the collision strength is fitted with a semiempirical analytic function which includes approximations to polarization, resonance, and exchange contributions. In O II, first spectra anywhere of electron excitation of the optically allowed transitions are presented. In addition, excitations of two low lying, optically forbidden transitions are detected for the first time.
An instrument to measure the three-dimensional energy distribution of positive ions in order to study the interaction between the solar wind and ionized Halley cometary particles was designed. Two sensors measure the distribution from 10 eV to 20 keV once per spacecraft spin and the distribution from 90 eV to 90 keV, with coarse mass discrimination, once every 32 spins. The instrument was turned on September 8, 1985. The performance throughout all testing was nominal. The spacecraft was greater than 10 million km from the earth in the solar wind. The only population identified is the solar wind. The Fast Ion Sensor follows solar wind variations with its autoranging capability. The Implanted Ion Sensor identifies higher mass ions such as O(6+) and O(5+) in the solar wind.
Positive ion composition and density in lower E region measured by mass spectrometry
Energy fluxes of low energy protons and positive ions in earth inner radiation zone
Rocket borne mass spectrometer measurements of positive ion composition in ionosphere
Differential energy spectra of low energy protons and positive ions in earth inner radiation zone, using electrostatic analyzers aboard OGO-3 satellite