Production of water from a dynamically new comet DOI Creative Commons
Konrad J. Kossacki, S. Szutowicz

Monthly Notices of the Royal Astronomical Society, Journal Year: 2023, Volume and Issue: 526(3), P. 4484 - 4489

Published: Oct. 4, 2023

ABSTRACT In our paper, we presented the results of numerical simulations dealing with production water from nucleus a hypothetical dynamically new comet. The were performed using empirical equation based on laboratory experiments in vacuum ice agglomerates. We also obtained simple, popular approach. model is prolate ellipsoid rough surface. compared observed comet C/2012 K1 PanSTARRS. Our indicate, that can be reproduced without assuming presence highly volatile ices when dust may slide down slopes and thermal conductivity very low.

Language: Английский

Outgassing of ice agglomerates II DOI
Konrad J. Kossacki

Icarus, Journal Year: 2025, Volume and Issue: unknown, P. 116541 - 116541

Published: March 1, 2025

Language: Английский

Citations

0

Comparison of a pebbles-based model with the observed evolution of the water and carbon dioxide outgassing of comet 67P/Churyumov-Gerasimenko DOI
M. Ciarniello, M. Fulle, F. Tosi

et al.

Monthly Notices of the Royal Astronomical Society, Journal Year: 2023, Volume and Issue: 523(4), P. 5841 - 5852

Published: June 15, 2023

ABSTRACT The Rosetta mission escorted comet 67P/Churyumov-Gerasimenko for approximately two years including the perihelion passage (1.24 au, 2015 August), allowing us to monitor seasonal evolution of water and carbon dioxide loss rates. Here, we model production as measured by Rosina experiment during entire escort phase applying Water-ice-Enriched Block (WEB) model, namely a structural activity nucleus made pebbles. Furthermore, compare surface temperature distribution inferred VIRTIS-M observations in 2014 August (≈3.5 au inbound, northern summer) with expected temperatures from our simulations nucleus’ hemisphere, investigating relevance self-illumination effects ‘neck’ assessing active area extent summer. Our imply that: (1) at is mostly dehydration water-poor pebbles, continuously exposed CO2-driven erosion; (2) large heliocentric distances outbound rate dominated self-cleaning fallout deposits; (3) steep decrease curve distance results progressive reduction water-active area, predicted proposed model; (4) distributed sources, originating ‘neck’; (5) sources water-ice-rich exposures dominate up inbound equinox; (6) time CO2 consistent WEB model.

Language: Английский

Citations

7

Ejection of porous dust–ice agglomerates from the surface of the cometary nucleus DOI
Marcin Wesołowski

Icarus, Journal Year: 2023, Volume and Issue: 411, P. 115937 - 115937

Published: Dec. 30, 2023

Language: Английский

Citations

4

Production of water from a dynamically new comet DOI Creative Commons
Konrad J. Kossacki, S. Szutowicz

Monthly Notices of the Royal Astronomical Society, Journal Year: 2023, Volume and Issue: 526(3), P. 4484 - 4489

Published: Oct. 4, 2023

ABSTRACT In our paper, we presented the results of numerical simulations dealing with production water from nucleus a hypothetical dynamically new comet. The were performed using empirical equation based on laboratory experiments in vacuum ice agglomerates. We also obtained simple, popular approach. model is prolate ellipsoid rough surface. compared observed comet C/2012 K1 PanSTARRS. Our indicate, that can be reproduced without assuming presence highly volatile ices when dust may slide down slopes and thermal conductivity very low.

Language: Английский

Citations

0