731 |
Analysis of olgimetric and subunit sizes of membrane receptorsLai, Francis Anthony Chi Choi January 1986 (has links)
No description available.
|
732 |
Neuropeptide receptors on cultured astrocytes from rodent central nervous systemCholewinski, Andrzej Josef January 1987 (has links)
No description available.
|
733 |
Structure and expression of the singed locus in Drosophila melanogasterPaterson, J. January 1990 (has links)
No description available.
|
734 |
Aspects of the production of alkaloids in Penicillium and ClavicepsBoyes-Korkis, Jane Marina January 1990 (has links)
No description available.
|
735 |
A study of the secreted acetylcholinesterases of Nippostrongylus basiliensisBlackburn, Catherine Clare January 1991 (has links)
No description available.
|
736 |
The motion of a thermal in a stratified environmentHall, William Shield January 1963 (has links)
A historical survey is made of the development of the idea of an isolated bubble of buoyant fluid i.e. a thermal, including previous attempts to apply similar theories to the motion of cumulus clouds and to buoyant bubbles in stratified environments. In the present work, when motion of a thermal in a velocity stratification (i.e. a wind shear) is considered, attention first of all, is restricted to situations in which the wind shear is such as to maintain the thermal's axis at a constant angle to the horizontal. In this case analytical relationships are found for the radius, buoyancy, time taken and track of the thermal against height. When the angle of inclination of the thermal's axis can vary,these quantities are computed numerically for particular combinations of values of the initial parameters. The ratio of the coefficients of momentum and heat transfer is calculated as a corollary of the above theory and found to be small in a typical atmospheric situation. Equations are presented, but not solved, which would give the motion of a cloud tower in uniform shear. The motion of a thermal in a density stratification is first considered for three assumed types of motion i.e. where the thermal's size (i) increases linearly, (ii) remains constant and (iii) decreases linearly with height. In types (ii) and (iii) erosion of material is assumed. In all types the density and velocity distributions are assumed similar throughout the motion and formulae for the exterior density gradients are calculated. Finally, an experimentally produced formula, giving the effect on a thermal of a density discontinuity in the exterior fluid, is generalised to continuous density gradients and formulae produced for the radius of a thermal against height or time. The latter is found to compare well with the observed radius of a cumulus tower as a function of time.
|
737 |
Physical and kinetic studies of the acetylcholine receptor from vertebrate muscle and fishLo, M. M. S. January 1981 (has links)
No description available.
|
738 |
Immunological characterisation of nicotinic acetylcholine receptorsMehraban, F. January 1983 (has links)
No description available.
|
739 |
Quantitation of peptidoleukotrienes : methodology and applicationsBeaubien, B. C. January 1984 (has links)
No description available.
|
740 |
Molecular studies on the gaba-benzodiazepine receptorBilbe, Graeme January 1985 (has links)
No description available.
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