Engineering topics
Publications and source records attributed to Huebner, Walter F..
We have included gravity in our fluid dynamic model with chemical kinetics of dusty comet comae and applied it with two dust sizes to 2060 Chiron. A progress report on the model and preliminary results concerning gas/dust dynamics and chemistry is given.
Potential interpretations are presented for observations of four comets: Brorsen-Metcalf (1989o), Okazaki-Levy-Rudenko (1989r), Aarseth-Brewington (1989a1), and Austin (1989o1). The relationship of minor species with each other and possible parents as well as with dust are being pursued in a number of investigations. Of particular interest are the abundance ratios of CH4 to CO and NH3 to N2. The need for closer collaboration betwen observing teams and modelers is examined. The need for dust size distribution as a function of cometocentric distance to be analyzed in closer collaboration between observers and modelers is discussed.
The spacecraft flybys of Comets Giacobini-Zinner and Halley were highly successful. Many untested theories were confirmed and additional clues provided to decide between competing models, but without leading to a clear preference. New questions were also raised. Based on the improved knowledge, research efforts will now be much better focused than was possible before the encounters. Moreover, interpretation of the Earth-based (ground-based, airborne, rocket-borne, and Earth satellite) observations should be improved. The goals of the workshop are defined in terms of the results from spacecraft measurements and Earth-based observations of Comets Giacobini-Zinner and Halley. A summary is presented of the new knowledge about the nucleus, the coma gas and dust, and the plasma. It is realized that extreme caution must be used when generalizing results from the Comet Giacobini-Zinner and Halley investigations to comets universally. The many surprises of the successful missions, the dangers inherent in generalizations to other comets, and the many still open and new questions are the reasons for the need of further spacecraft investigations. However, an unquestionably successful start was made in expanding the knowledge about the physics and chemistry of comets and all the related implications, and the question about the similarities of and differences between comets can now be explored further.
A hydrodynamic model was developed of a spherically symmetric dusty gas flow in a cometary atmosphere assuming a single fluid, inviscid, perfect gas. The hydrodynamics for gas and dust, which involves the gas drag force (momentum transfer), heat exchange between gas and dust, photodissociation energy for H2O gas, and radiative heating and cooling terms for dust particles, are solved using the Gear method for stiff, coupled differential equations. Calculations were done with a dust size distribution for radii alpha = 0.01 micron to 10 cm with densities variable with the size. A nucleus size of 4.0 km radius with a density of 0.5 g/cu cm and a total dust-to-gas mass ratio chi = 1 was adopted. There are indications from in situ observations that dust particle fragment into smaller ones. Fragmentation of dust particles was incorporated into the model. This is done by adding source and sink terms in the continuity equations for the dust. Lifetimes for the decay of dust particles were assumed as a function of particle size. It is also assumed that dust particles always fragment only into the next smaller size.