Micrometer-sized Water Ice Particles for Planetary Science Experiments: Influence of Surface Structure on Collisional Properties.

Gärtner, S., Gundlach, B., Headen, T. F., Ratte, J., Oesert, J., Gorb, S. N., Youngs, T. G. A., Bowron, D. T., Blum, J. and Fraser, H. J. (2017) Micrometer-sized Water Ice Particles for Planetary Science Experiments: Influence of Surface Structure on Collisional Properties. The Astrophysical Journal, 848 (2). DOI 10.3847/1538-4357/aa8c7f.

Full text not available from this repository.

Supplementary data:

Abstract

Models and observations suggest that ice-particle aggregation at and beyond the snowline dominates the earliest stages of planet formation, which therefore is subject to many laboratory studies. However, the pressure–temperature gradients in protoplanetary disks mean that the ices are constantly processed, undergoing phase changes between different solid phases and the gas phase. Open questions remain as to whether the properties of the icy particles themselves dictate collision outcomes and therefore how effectively collision experiments reproduce conditions in protoplanetary environments. Previous experiments often yielded apparently contradictory results on collision outcomes, only agreeing in a temperature dependence setting in above ≈210 K. By exploiting the unique capabilities of the NIMROD neutron scattering instrument, we characterized the bulk and surface structure of icy particles used in collision experiments, and studied how these structures alter as a function of temperature at a constant pressure of around 30 mbar. Our icy grains, formed under liquid nitrogen, undergo changes in the crystalline ice-phase, sublimation, sintering and surface pre-melting as they are heated from 103 to 247 K. An increase in the thickness of the diffuse surface layer from ≈10 to ≈30 Å (≈2.5 to 12 bilayers) proves increased molecular mobility at temperatures above ≈210 K. Because none of the other changes tie-in with the temperature trends in collisional outcomes, we conclude that the surface pre-melting phenomenon plays a key role in collision experiments at these temperatures. Consequently, the pressure–temperature environment, may have a larger influence on collision outcomes than previously thought.

Document Type: Article
Keywords: accretion, accretion disks; methods: laboratory: solid state; planets and satellites: formation
Research affiliation: Kiel University > Kiel Marine Science
OceanRep > The Future Ocean - Cluster of Excellence
Kiel University
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.3847/1538-4357/aa8c7f
ISSN: 1538-4357
Projects: Future Ocean
Date Deposited: 18 Dec 2017 09:53
Last Modified: 25 Apr 2019 09:37
URI: http://oceanrep.geomar.de/id/eprint/40690

Actions (login required)

View Item View Item