Energy Deposition in Planetary Atmospheres by Charged Particles and Solar Photons

We discuss here the energy deposition of solar FUV, EUV and X-ray photons, energetic auroral particles, and pickup ions. Photons and the photoelectrons that they produce may interact with thermospheric neutral species producing dissociation, ionization, excitation, and heating. The interaction of X-rays or keV electrons with atmospheric neutrals may produce core-ionized species, which may decay by the production of characteristic X-rays or Auger electrons. Energetic particles may precipitate into the atmosphere, and their collisions with atmospheric particles also produce ionization, excitation, and heating, and auroral emissions. Auroral energetic particles, like photoelectrons, interact with the atmospheric species through discrete collisions that produce ionization, excitation, and heating of the ambient electron population. Auroral particles are, however, not restricted to the sunlit regions. They originate outside the atmosphere and are more energetic than photoelectrons, especially at magnetized planets. The spectroscopic analysis of auroral emissions is discussed here, along with its relevance to precipitating particle diagnostics. Atmospheres can also be modified by the energy deposited by the incident pickup ions with energies of eV’s to MeV’s; these particles may be of solar wind origin, or from a magnetospheric plasma. When the modeling of the energy deposition of the plasma is calculated, the subsequent modeling of the atmospheric processes, such as chemistry, emission, and the fate of hot recoil particles produced is roughly independent of the exciting radiation. However, calculating the spatial distribution of the energy deposition versus depth into the atmosphere produced by an incident plasma is much more complex than is the calculation of the solar excitation profile. Here, the nature of the energy deposition processes by the incident plasma are described as is the fate of the hot recoil particles produced by exothermic chemistry and by knock-on collisions by the incident ions.     

The effect of simulated microgravity on hybridoma cells

The effect of clinostat-simulated microgravity on SP-2/0 and 1D6 hybridoma cells was studied. Clinorotation during 4-5 days at 1.5 rounds per minute decreased dramatically their proliferating capacity: the rotated cells divided less than once while control cells performed 4-5 divisions. They decreased the non-specific adhesion to tissue culture plastic, but increased the number of cell-to-cell contacts. Such phenomenological changes were accompanied with the alterations in pericellular glycosaminoglycans: decreased accumulation of hyaluronic acid and increased accumulation of chondroitin/dermatan-sulfate, as well as with the increase of cytoplasmic Ca2+ concentration. Clinorotation resulted in hybridoma nicotinic receptor desensitization but not down-regulation. In contrast, both the quantity and quality (molecular isoforms, affinity and specificity) of the antibody produced by 1D6 hybridoma cells were not altered by clinorotation. It is concluded that simulated microgravity affected the proliferating and adhesive, but not biosynthetic properties of hybridoma cells.