Reflectance study of ice and Mars soil simulant associations - I. H2O ice

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Reflectance study of ice and Mars soil simulant associations - I. H2O ice. / Yoldi, Zurine; Pommerol, Antoine; Poch, Olivier; Thomas, Nicolas.

In: Icarus, Vol. 358, 114169, 01.04.2021.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Yoldi, Z, Pommerol, A, Poch, O & Thomas, N 2021, 'Reflectance study of ice and Mars soil simulant associations - I. H2O ice', Icarus, vol. 358, 114169. https://doi.org/10.1016/j.icarus.2020.114169

APA

Yoldi, Z., Pommerol, A., Poch, O., & Thomas, N. (2021). Reflectance study of ice and Mars soil simulant associations - I. H2O ice. Icarus, 358, [114169]. https://doi.org/10.1016/j.icarus.2020.114169

Vancouver

Yoldi Z, Pommerol A, Poch O, Thomas N. Reflectance study of ice and Mars soil simulant associations - I. H2O ice. Icarus. 2021 Apr 1;358. 114169. https://doi.org/10.1016/j.icarus.2020.114169

Author

Yoldi, Zurine ; Pommerol, Antoine ; Poch, Olivier ; Thomas, Nicolas. / Reflectance study of ice and Mars soil simulant associations - I. H2O ice. In: Icarus. 2021 ; Vol. 358.

Bibtex

@article{11cb17bc33ba4bfe8e9ade680c574496,
title = "Reflectance study of ice and Mars soil simulant associations - I. H2O ice",
abstract = "The reflectance of water ice and dust mixtures depends, amongst other parameters, on how the components are mixed (e.g. intimate mixture, areal mixture or coating). Therefore, when inverting the reflectance spectra measured from planetary surfaces to derive the amount of water ice present at the surface, it is critical to distinguish between different mixing modes of ice and dust. However, the distinction between mixing modes from reflectance spectra remains ambiguous. Here we show how to identify some water ice/soil mixing modes from the study of defined spectral criteria and colour analysis of laboratory mixtures. We have recreated ice and dust mixtures and found that the appearance of frost on a surface increases its reflectance and flattens its spectral slopes, whereas the increasing presence of water ice in intimate mixtures mainly impacts the absorption bands. In particular, we provide laboratory data and a spectral analysis to help interpret ice and soil reflectance spectra from the Martian surface.",
keywords = "Reflectance, Water-ice, Mixture, Mars, Frost",
author = "Zurine Yoldi and Antoine Pommerol and Olivier Poch and Nicolas Thomas",
year = "2021",
month = apr,
day = "1",
doi = "10.1016/j.icarus.2020.114169",
language = "English",
volume = "358",
journal = "Icarus",
issn = "0019-1035",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Reflectance study of ice and Mars soil simulant associations - I. H2O ice

AU - Yoldi, Zurine

AU - Pommerol, Antoine

AU - Poch, Olivier

AU - Thomas, Nicolas

PY - 2021/4/1

Y1 - 2021/4/1

N2 - The reflectance of water ice and dust mixtures depends, amongst other parameters, on how the components are mixed (e.g. intimate mixture, areal mixture or coating). Therefore, when inverting the reflectance spectra measured from planetary surfaces to derive the amount of water ice present at the surface, it is critical to distinguish between different mixing modes of ice and dust. However, the distinction between mixing modes from reflectance spectra remains ambiguous. Here we show how to identify some water ice/soil mixing modes from the study of defined spectral criteria and colour analysis of laboratory mixtures. We have recreated ice and dust mixtures and found that the appearance of frost on a surface increases its reflectance and flattens its spectral slopes, whereas the increasing presence of water ice in intimate mixtures mainly impacts the absorption bands. In particular, we provide laboratory data and a spectral analysis to help interpret ice and soil reflectance spectra from the Martian surface.

AB - The reflectance of water ice and dust mixtures depends, amongst other parameters, on how the components are mixed (e.g. intimate mixture, areal mixture or coating). Therefore, when inverting the reflectance spectra measured from planetary surfaces to derive the amount of water ice present at the surface, it is critical to distinguish between different mixing modes of ice and dust. However, the distinction between mixing modes from reflectance spectra remains ambiguous. Here we show how to identify some water ice/soil mixing modes from the study of defined spectral criteria and colour analysis of laboratory mixtures. We have recreated ice and dust mixtures and found that the appearance of frost on a surface increases its reflectance and flattens its spectral slopes, whereas the increasing presence of water ice in intimate mixtures mainly impacts the absorption bands. In particular, we provide laboratory data and a spectral analysis to help interpret ice and soil reflectance spectra from the Martian surface.

KW - Reflectance

KW - Water-ice

KW - Mixture

KW - Mars

KW - Frost

U2 - 10.1016/j.icarus.2020.114169

DO - 10.1016/j.icarus.2020.114169

M3 - Journal article

VL - 358

JO - Icarus

JF - Icarus

SN - 0019-1035

M1 - 114169

ER -

ID: 258081734