1990
DOI: 10.1016/0019-1035(90)90143-w
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Finite lifetime fragment model for synchronic band formation in dust tails of Comets

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Cited by 15 publications
(7 citation statements)
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“…Dust tail striae are thought to form through the fragmentation of dust agglomerates [Sekanina andFarrell, 1980, 1982;Hill and Mendis, 1980;Notni and Thaenert, 1988;Nishioka and Watanabe, 1990;Pittichová et al, 1997]. The escaping gases drag ice-mixed dust forming a strongly coupled ensemble in the vicinity of the nucleus, which then decouple as they expand farther out leaving the several hundreds of m s −1 fast icy conglomerates exposed to the solar conditions (solar heat, electrostatic charging, collisions, etc.)…”
mentioning
confidence: 99%
“…Dust tail striae are thought to form through the fragmentation of dust agglomerates [Sekanina andFarrell, 1980, 1982;Hill and Mendis, 1980;Notni and Thaenert, 1988;Nishioka and Watanabe, 1990;Pittichová et al, 1997]. The escaping gases drag ice-mixed dust forming a strongly coupled ensemble in the vicinity of the nucleus, which then decouple as they expand farther out leaving the several hundreds of m s −1 fast icy conglomerates exposed to the solar conditions (solar heat, electrostatic charging, collisions, etc.)…”
mentioning
confidence: 99%
“…This provides a good match to observational data (Pittichová et al, 1997), but the required physical properties of dust are difficult to explain. Nishioka and Watanabe (1990), Nishioka (1998) and Nishioka (2021) instead suggest a continuous cascade of striae formation, which relaxes the constraints on dust properties, but has alleged problems explaining stria shapes (Sekenina and Pittichová, 1997). Other potential mechanisms include optically thick dust clouds (Froehlich and Notni, 1988;Notni and Thaenert, 1988), or the destruction of macroscopic sized (10-100 m) boulders by rotational stresses (Steckloff and Jacobson, 2016).…”
Section: Striae Formation Theoriesmentioning
confidence: 99%
“…Пiзнiше всi батькiвськi частки фрагментують в один i той же час на вiдстанях аж до декiлькох мiльйонiв кiлометрiв. Пiзнiше ця модель була застосована до комет C/1957 P1 (Mrkos) [19], C/1962 C1 (Seki-Lines) [10] та C/1910 A1 (Great January Comet) [18]. Необхiднiсть раптового одночасного розпаду батькiвських частинок є головним вразливим мiсцем даної моделi.…”
Section: вступunclassified