Article ; Online: Deriving iron contents from past and future Venus surface spectra with new high-temperature laboratory emissivity data.
2021 Volume 7, Issue 3
Abstract: In situ information on the surface composition of Venus is based on measurements of a small number of landing sites. In the laboratory, we measured the emissivity of a range of igneous rocks at temperatures up to 480°C. We show that high-temperature ... ...
Abstract | In situ information on the surface composition of Venus is based on measurements of a small number of landing sites. In the laboratory, we measured the emissivity of a range of igneous rocks at temperatures up to 480°C. We show that high-temperature laboratory spectra of basalts are consistent with the only existing multispectral data from the surface of Venus obtained by the photometers on the Venera 9 and 10 landers. We derive the FeO abundances for these landing sites of 12.2 and 9.5 weight %, respectively. From orbit, Venus' surface is only observable on the nightside through small spectral windows near 1 μm where the CO |
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Language | English |
Publishing date | 2021-01-15 |
Publishing country | United States |
Document type | Journal Article |
ZDB-ID | 2810933-8 |
ISSN | 2375-2548 ; 2375-2548 |
ISSN (online) | 2375-2548 |
ISSN | 2375-2548 |
DOI | 10.1126/sciadv.aba9428 |
Database | MEDical Literature Analysis and Retrieval System OnLINE |
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