investigating thermal properties of gas-filled planetary regoliths using a thermal probe
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Abstract
Convection seems to play an important role in the transfer of heat in this case. Firstly a diffusion-convection model fits the laboratory data better than a diffusivity-only model. Also the diffusivity derived from a diffusivity-convection model was found to be in good agreement with diffusivity derived using other methods published in the literature. Thermal diffusivity measurements, inspection of the horizontal temperature profiles and visual observations suggests that limestone powder is compacted more readily than sand during entry of the penetrator into the target. For both regolith analogues the disturbance of material around the penetrator was determined to have an insignificant effect on the diffusivity measurements in this case.
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paton2012geoscientificinvestigating
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| Authors | ;M. D. Paton;A.-M. Harri;T. Mäkinen;S. F. Green |
| Journal | radiologic technology |
| Year | 2012 |
| DOI |
10.5194/gi-1-7-2012
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| URL | |
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