Quantitative analysis of H2O+ coma images using a multiscale MHD model with detailed ion chemistry

被引:30
作者
Haberli, RM
Combi, MR
Gombosi, TI
De Zeeuw, DL
Powell, KG
机构
[1] Univ Michigan, Space Phys Res Lab, Ann Arbor, MI 48109 USA
[2] Univ Michigan, Dept Aerosp Engn, Ann Arbor, MI 48109 USA
基金
美国国家航空航天局; 美国国家科学基金会;
关键词
comets; composition ionospheres; spectroscopy;
D O I
10.1006/icar.1997.5835
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The observation of ions created by ionization of cometary gas, either by ground-based observations or by in situ measurements can give us useful information about the gas production and composition of comets. However, due to the interaction of ions with the magnetized solar wind and their high chemical reactivity, it is not possible to relate measured ion densities (or column densities) directly to the parent gas densities. In order to quantitatively analyze measured ion abundances in cometary comae it is necessary to understand their dynamics and chemistry. We have developed a detailed ion-chemical network of cometary atmospheres. We include production of ions by photo- and electron impact-ionization of a background neutral atmosphere, charge exchange of solar wind ions with cometary atoms/molecules, reactions between ions and molecules, and dissociative recombination of molecular ions with thermal electrons. By combining the ion-chemical network with the three-dimensional plasma flow as computed by a new fully three-dimensional MHD model of cometary plasma environments (Gombosi et al. 1996) we are able to compute the density of the major cometary ions everywhere in the coma. The input parameters for our model are the solar wind conditions (density, speed, temperature, magnetic field) and the composition and production rate of the gas. We applied our model to Comet P/Halley in early March 1986, for which the input parameters are reasonably well known. We compare the resulting column density of H2O+ with ground-based observations of H2O+ from DiSanti et al. (1990). The results of our model are in good agreement with both the spatial distribution and the absolute abundance of H2O+ and with their variations with the changing overall water production rate between two days. The results are encouraging that it will be possible to obtain production rates of neutral cometary constituents from observations of their ion products. (C) 1997 Academic Press.
引用
收藏
页码:373 / 386
页数:14
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