Determining Thermal Behavior of Dry Permafrost above Ice-Cemented Ground : In Preparation for Future Mars Missions
The purpose of this report is to investigate if thermal properties of dry permafrost can be determined by only using temperature measurements. Then see if a numerical solution to the heat conduction equation, with the assumption that the thermal properties are constant with depth and that the temper...
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ftluleatu:oai:DiVA.org:ltu-48556 2023-05-15T14:02:02+02:00 Determining Thermal Behavior of Dry Permafrost above Ice-Cemented Ground : In Preparation for Future Mars Missions Eriksson, Elin 2014 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-48556 eng eng http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-48556 Local 5ff06592-2ef6-4ff8-8670-77a634ae9e21 info:eu-repo/semantics/openAccess Technology Thermal model soil properties space Physics numerical simulation Mars Antartica Teknik Student thesis info:eu-repo/semantics/bachelorThesis text 2014 ftluleatu 2022-10-25T20:50:13Z The purpose of this report is to investigate if thermal properties of dry permafrost can be determined by only using temperature measurements. Then see if a numerical solution to the heat conduction equation, with the assumption that the thermal properties are constant with depth and that the temperatures only varies sinusoidally with time, can reasonably predict temperatures with time and depth, using those derived properties. Thus giving an understanding of the thermal behavior in it. This is done in preparation for future Mars missions, because a good understanding of the physics in dry permafrost is needed to be able to make an educated guess of where to find life. One of the parameters that is used in the numerical solution, the thermal model, is the apparent thermal diffusivity which tells how fast/slow and large/small the changes in soil temperature are. This research utilizes two well-known methods that use amplitudes and phases of temperature measurements to determine the apparent thermal diffusivity. The focus is on analyzing and comparing four different methods to calculate the amplitudes and phases of temperature measurements taken at four different depths at Linneaus Terrace, Antarctica. The first two methods use the values of the maximum and minimum temperatures at the different depths to calculate their yearly amplitudes and phases. Of those two methods, one uses the actual data when determining the maximums and minimums while the other uses the same data that has first been smoothed by a box-car algorithm. The other two methods used are Fourier transform and least square best fit. Linneaus Terrace place is located in the high elevations valleys of the Antarctic Dry Valleys which is the only place on Earth with dry permafrost above ice-cemented ground. It is therefore a good analogue for Martian soil. The Fourier transform and least square best fit gave the most reasonable values for the data. They also gave the exact same values as each other, due to the use of a data set with a period of exactly ... Bachelor Thesis Antarc* Antarctic Antarctica antartic* Ice permafrost LuleƄ University of Technology Publications (DiVA) Antarctic The Antarctic |
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Open Polar |
collection |
LuleƄ University of Technology Publications (DiVA) |
op_collection_id |
ftluleatu |
language |
English |
topic |
Technology Thermal model soil properties space Physics numerical simulation Mars Antartica Teknik |
spellingShingle |
Technology Thermal model soil properties space Physics numerical simulation Mars Antartica Teknik Eriksson, Elin Determining Thermal Behavior of Dry Permafrost above Ice-Cemented Ground : In Preparation for Future Mars Missions |
topic_facet |
Technology Thermal model soil properties space Physics numerical simulation Mars Antartica Teknik |
description |
The purpose of this report is to investigate if thermal properties of dry permafrost can be determined by only using temperature measurements. Then see if a numerical solution to the heat conduction equation, with the assumption that the thermal properties are constant with depth and that the temperatures only varies sinusoidally with time, can reasonably predict temperatures with time and depth, using those derived properties. Thus giving an understanding of the thermal behavior in it. This is done in preparation for future Mars missions, because a good understanding of the physics in dry permafrost is needed to be able to make an educated guess of where to find life. One of the parameters that is used in the numerical solution, the thermal model, is the apparent thermal diffusivity which tells how fast/slow and large/small the changes in soil temperature are. This research utilizes two well-known methods that use amplitudes and phases of temperature measurements to determine the apparent thermal diffusivity. The focus is on analyzing and comparing four different methods to calculate the amplitudes and phases of temperature measurements taken at four different depths at Linneaus Terrace, Antarctica. The first two methods use the values of the maximum and minimum temperatures at the different depths to calculate their yearly amplitudes and phases. Of those two methods, one uses the actual data when determining the maximums and minimums while the other uses the same data that has first been smoothed by a box-car algorithm. The other two methods used are Fourier transform and least square best fit. Linneaus Terrace place is located in the high elevations valleys of the Antarctic Dry Valleys which is the only place on Earth with dry permafrost above ice-cemented ground. It is therefore a good analogue for Martian soil. The Fourier transform and least square best fit gave the most reasonable values for the data. They also gave the exact same values as each other, due to the use of a data set with a period of exactly ... |
format |
Bachelor Thesis |
author |
Eriksson, Elin |
author_facet |
Eriksson, Elin |
author_sort |
Eriksson, Elin |
title |
Determining Thermal Behavior of Dry Permafrost above Ice-Cemented Ground : In Preparation for Future Mars Missions |
title_short |
Determining Thermal Behavior of Dry Permafrost above Ice-Cemented Ground : In Preparation for Future Mars Missions |
title_full |
Determining Thermal Behavior of Dry Permafrost above Ice-Cemented Ground : In Preparation for Future Mars Missions |
title_fullStr |
Determining Thermal Behavior of Dry Permafrost above Ice-Cemented Ground : In Preparation for Future Mars Missions |
title_full_unstemmed |
Determining Thermal Behavior of Dry Permafrost above Ice-Cemented Ground : In Preparation for Future Mars Missions |
title_sort |
determining thermal behavior of dry permafrost above ice-cemented ground : in preparation for future mars missions |
publishDate |
2014 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-48556 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Antarctica antartic* Ice permafrost |
genre_facet |
Antarc* Antarctic Antarctica antartic* Ice permafrost |
op_relation |
http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-48556 Local 5ff06592-2ef6-4ff8-8670-77a634ae9e21 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1766272098327592960 |