2018
DOI: 10.1093/mnras/sty2926
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The refractory-to-ice mass ratio in comets

Abstract: We review the complex relationship between the dust-togas mass ratio usually estimated in the material lost by comets, and the Refractory-to-Ice mass ratio inside the nucleus, which constrains the origin of comets. Such a relationship is dominated by the mass transfer from the perihelion erosion to fallout over most of the nucleus surface. This makes the Refractory-to-Ice mass ratio inside the nucleus up to ten times larger than the dust-togas mass ratio in the lost material, because the lost material is missi… Show more

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Cited by 76 publications
(84 citation statements)
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“…Landslides on 67P reveal a clear rocky‐type behavior for cometary material that, once collapsed, assumes a rock avalanche mobilization associated to relatively high friction coefficients. This behavior agrees with the refractory to ice ratio estimated from grains ejected from 67P (Fulle et al, ). In addition, the considerable variability of H/L values among the different landslides suggests that different volatile contents of the detached mass play a fundamental role on the gravitational process and final runout, hence being a general indicator for the subsurface cometary heterogeneities.…”
Section: Resultssupporting
confidence: 90%
“…Landslides on 67P reveal a clear rocky‐type behavior for cometary material that, once collapsed, assumes a rock avalanche mobilization associated to relatively high friction coefficients. This behavior agrees with the refractory to ice ratio estimated from grains ejected from 67P (Fulle et al, ). In addition, the considerable variability of H/L values among the different landslides suggests that different volatile contents of the detached mass play a fundamental role on the gravitational process and final runout, hence being a general indicator for the subsurface cometary heterogeneities.…”
Section: Resultssupporting
confidence: 90%
“…Ma'at), are almost entirely cleaned-up in consolidated regions, exposing the underlying consolidated material. This is consistent with the idea of "self-cleaning" of the Northern hemisphere proposed by Fulle et al (2019). (c) and (d) could quench dust activity in fallback regions, but do not play a role in consolidated areas.…”
Section: Discussionsupporting
confidence: 91%
“…Even higher D/I ratios (cf. Fulle et al (2018)), which would be associated with a higher percentage of backfall of dry dust, can easily be derived from the numbers given in Table 4. The most prominent differences when changing the D/I ratio are expected in the H/Si and O/Si ratios, given that water is the main component in the cometary ices.…”
Section: Discussionmentioning
confidence: 99%