Thermal Environment for the Lunar Volatile Prospector Mission

Matthias Killian, Technical University of Munich, Germany Richard Fisackerly, European Space Agency (ESA), Netherlands ICES102: Thermal Control for Planetary and Small Body Surface Missions The 47th International Conference on Environmental Systems was held in South Carolina, USA on 16 July 2017 thr...

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Main Authors: Killian, Matthias, Fisackerly, Richard
Format: Other/Unknown Material
Language:English
Published: 47th International Conference on Environmental Systems 2017
Subjects:
LVP
Online Access:http://hdl.handle.net/2346/72970
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spelling fttexastechuniv:oai:ttu-ir.tdl.org:2346/72970 2023-05-15T18:23:10+02:00 Thermal Environment for the Lunar Volatile Prospector Mission Killian, Matthias Fisackerly, Richard 2017-07-16 application/pdf http://hdl.handle.net/2346/72970 eng eng 47th International Conference on Environmental Systems ICES_2017_156 http://hdl.handle.net/2346/72970 Thermal Lunar Moon Traverse Rover LVP Presentations 2017 fttexastechuniv 2023-01-04T07:16:52Z Matthias Killian, Technical University of Munich, Germany Richard Fisackerly, European Space Agency (ESA), Netherlands ICES102: Thermal Control for Planetary and Small Body Surface Missions The 47th International Conference on Environmental Systems was held in South Carolina, USA on 16 July 2017 through 20 July 2017. The ESA mission concept Lunar Volatiles Prospector intends to send a rover to the south pole of the Moon for scientific exploration. Investigation of permanently shadowed regions (PSR) is one of the main objectives of the mission in the search for and analysis of volatiles. An instrument onboard a rover with a mobile range of about 50 km shall determine the distribution of water and other volatiles on a local scale. Previous analyses, which considered additional requirements on waypoints and scientific return, revealed a preference for the Shoemaker and Faustini crater region. On addition to mission constraints such as visibility to earth for communication purposes, available light for recharging batteries etc., the thermal environment plays a significant role for the success of a mission to this region. Lunar surface temperatures in the polar region vary between 25 K and 300 K for the targeted period in the year 2022. In this paper, a traverse is characterized regarding the thermal environment and corresponding heat fluxes of the rover. ESATAN-TMS was used in order to calculate radiative heat transfer and to solve the model. With analyses from this paper, dynamic thermal requirements can be established for a potential rover. In addition, thermal calculations from this paper shall be the baseline for future optimization of the traverse together with scientific requirements for a best scientific return as well as mitigating requirements for the design of the rover. Other/Unknown Material South pole Texas Tech University: TTU DSpace Repository South Pole
institution Open Polar
collection Texas Tech University: TTU DSpace Repository
op_collection_id fttexastechuniv
language English
topic Thermal
Lunar
Moon
Traverse
Rover
LVP
spellingShingle Thermal
Lunar
Moon
Traverse
Rover
LVP
Killian, Matthias
Fisackerly, Richard
Thermal Environment for the Lunar Volatile Prospector Mission
topic_facet Thermal
Lunar
Moon
Traverse
Rover
LVP
description Matthias Killian, Technical University of Munich, Germany Richard Fisackerly, European Space Agency (ESA), Netherlands ICES102: Thermal Control for Planetary and Small Body Surface Missions The 47th International Conference on Environmental Systems was held in South Carolina, USA on 16 July 2017 through 20 July 2017. The ESA mission concept Lunar Volatiles Prospector intends to send a rover to the south pole of the Moon for scientific exploration. Investigation of permanently shadowed regions (PSR) is one of the main objectives of the mission in the search for and analysis of volatiles. An instrument onboard a rover with a mobile range of about 50 km shall determine the distribution of water and other volatiles on a local scale. Previous analyses, which considered additional requirements on waypoints and scientific return, revealed a preference for the Shoemaker and Faustini crater region. On addition to mission constraints such as visibility to earth for communication purposes, available light for recharging batteries etc., the thermal environment plays a significant role for the success of a mission to this region. Lunar surface temperatures in the polar region vary between 25 K and 300 K for the targeted period in the year 2022. In this paper, a traverse is characterized regarding the thermal environment and corresponding heat fluxes of the rover. ESATAN-TMS was used in order to calculate radiative heat transfer and to solve the model. With analyses from this paper, dynamic thermal requirements can be established for a potential rover. In addition, thermal calculations from this paper shall be the baseline for future optimization of the traverse together with scientific requirements for a best scientific return as well as mitigating requirements for the design of the rover.
format Other/Unknown Material
author Killian, Matthias
Fisackerly, Richard
author_facet Killian, Matthias
Fisackerly, Richard
author_sort Killian, Matthias
title Thermal Environment for the Lunar Volatile Prospector Mission
title_short Thermal Environment for the Lunar Volatile Prospector Mission
title_full Thermal Environment for the Lunar Volatile Prospector Mission
title_fullStr Thermal Environment for the Lunar Volatile Prospector Mission
title_full_unstemmed Thermal Environment for the Lunar Volatile Prospector Mission
title_sort thermal environment for the lunar volatile prospector mission
publisher 47th International Conference on Environmental Systems
publishDate 2017
url http://hdl.handle.net/2346/72970
geographic South Pole
geographic_facet South Pole
genre South pole
genre_facet South pole
op_relation ICES_2017_156
http://hdl.handle.net/2346/72970
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