Theoretical studies of the mid-latitude ionosphere

Following a brief description of the atmosphere and ionosphere in Chapter I we describe how the equations of continuity and momentum for 0+, H+, He+, 0++ are derived from the formulations of St-Maurice and Schunk(1977) and Quegan et al.(1981) in Chapter II. In Chapter III we investigate the nature of the downward flow of protons in a collapsing post-sunset ionosphere. We derive an analytical form for the limiting temperature, we also note the importance of the polarization field term and concluded that the flow will remain subsonic for realistic conditions. The time-dependent behaviour of He+ under sunspot minimum conditions is investigated in Chapter IV. This is achieved by numerical solution of the 0+, H+ and,He+ continuity and momentum equations, treating He+ as a minor ion with 0+ , H+ as major ions. We found that He+ flows upwards during the day-time and downwards during the nighttime. He+ flux tube content reached a maximum on the 8th day of the integration period and started to decreasing. This is due to the large amount of H+ present at the late stages of the integration period which makes He+ unable to diffuse through the H+ layer away from the loss region. In Chapter V we investigate the behaviour of 0++ using sunspot maximum parameters. Although our results support the findings of Geis and Young (1981) that the large amounts of 0++ at the equator are caused mainly by thermal diffusion, the model used by Geis and Young overemphesizes the effect of thermal diffusion. The importance of 0++ - 0+ collision frequency is also noted. In Chapter VI we extend the work of Chapter IV, presenting a comparative study of H and He at sunspot minimum and sunspot maximum.In this last Chapter all three ions, O+ ,H+ and He+ , are treated theoretically as major ions and we concentrate mainly on light ion contents and fluxes. The results of this Chapter indicate that by assuming He+ as a minor ion we under-estimate He+ and over-estimate. H+. Some interesting features concerning the day to day behaviour of the light ion fluxes arise. In particular the day-time H+ fluxes decrease from day to day in contrast to the work of Murphy et al.(1976). In appendix.A we derive some analytical forms for the optical depth so that the models can include a realistic description of photoionization.

The control of mitosis in mammalian tissues

The question of which factors are central in determining whether a cell will undertake a new round of mitosis or will decycle has been examined in the isolated thymic lymphocyte model. Such cell populations possess both in vivo and in vitro a subpopulation of quiescent lymphoblasts which may be induced to reinitiate their mitotic programme. In the intact animal the major determinant of proliferative activity is the plasma ionised calcium concentration. However it has been established in culture that a variety of hormones, ions, cyclic nucleotides, plant lectins and ionophores may like calcium elicit a mitogenic response. These agents do not appear however to initiate DNA synthesis in an identical fashion. Rather there are two distinct intracellular mitogenic axes. The first axis includes a number of adenylate cyclase stimulants, cyclic AMP, phosphodiesterase inhibitors and magnesium ions. It was found that all these mitogens required extracellular magnesium ions to exhibit their stimulatory capacity. This dichotomy in mitogenic activity was further emphasised by the observation that these mitogens are all inhibited by testosterone, whilst the magnesium-independent mitogens were insensitive to this androgen. Indeed this second group of stimulatory factors required the presence of calcium ions in the extracellular milieu for activity, and were, in contrast to the magnesium-dependent mitogens inhibited by the presence of oestradiol in the culture. By examining the interrelationships between these various mitogens and inhibitors it has been possible to propose a mechanism to describe the activation process in the thymocyte. Studies of the metabolism of cyclic nucleotides, membrane potential and transmembrane ion fluxes indicate that there may be a complex relationship between membrane fluidity, ion balance and cyclic nucleotide levels which may individually or in concert promote the initiation of DNA synthesis. A number of possible mechanisms are discussed to account for these observations.