The objective of this work is to present the first analytical and experimental results obtained with a 3D heat flux sensor for planetary regolith. The proposed structure, a sphere divided in four sectors, is sensible to heat flow magnitude and angle. Each sector includes a platinum resistor that is used both to sense its temperature and provide heating power. By operating the sectors at constant temperature, the sensor gives a response that is proportional to the heat flux vector in the regolith. The response of the sensor is therefore independent of the thermal conductivity of the regolith. A complete analytical solution of the response of the sensor is presented. The sensor may be used to provide information on the instantaneous local the...
The planetary heat flow is one of the fundamental quantities describing the thermal state of a plane...
Geothermal heat flow measurements are a high priority for the future lunar geophysical network missi...
Abstract We use the Martian surface temperature response to Phobos transits observed next to the InS...
© 2022 Elsevier. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://...
We introduce a general purpose penetrator, fitted with a heater, for measuring temperature and therm...
The thermo-mechanical properties of planetary surface and subsurface layers control to a high extent...
AbstractThe thermo-mechanical properties of planetary surface and subsurface layers control to a hig...
For determining the lunar heat flow two parameters need to be measured: The thermal gradient and the...
The thermal properties of the surface and subsurface layers of planets and planetary objects yield i...
Die Oberflächen verschiedener planetarer Körper, welche keine oder nur eine dünne Atmosphäre besitze...
abstract: Planetary surface studies across a range of spatial scales are key to interpreting modern ...
The thermal conductivity of granular planetary regolith is strongly dependent on the porosity, or pa...
A measurement of the martian planetary heat flow requires the determination of the subsurface tempe...
En vue d'applications futures dans le domaine de la récupération d'énergie à basse température à par...
The heat flow and physical properties package (HP3) of the InSight Mars mission is an instrument pac...
The planetary heat flow is one of the fundamental quantities describing the thermal state of a plane...
Geothermal heat flow measurements are a high priority for the future lunar geophysical network missi...
Abstract We use the Martian surface temperature response to Phobos transits observed next to the InS...
© 2022 Elsevier. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://...
We introduce a general purpose penetrator, fitted with a heater, for measuring temperature and therm...
The thermo-mechanical properties of planetary surface and subsurface layers control to a high extent...
AbstractThe thermo-mechanical properties of planetary surface and subsurface layers control to a hig...
For determining the lunar heat flow two parameters need to be measured: The thermal gradient and the...
The thermal properties of the surface and subsurface layers of planets and planetary objects yield i...
Die Oberflächen verschiedener planetarer Körper, welche keine oder nur eine dünne Atmosphäre besitze...
abstract: Planetary surface studies across a range of spatial scales are key to interpreting modern ...
The thermal conductivity of granular planetary regolith is strongly dependent on the porosity, or pa...
A measurement of the martian planetary heat flow requires the determination of the subsurface tempe...
En vue d'applications futures dans le domaine de la récupération d'énergie à basse température à par...
The heat flow and physical properties package (HP3) of the InSight Mars mission is an instrument pac...
The planetary heat flow is one of the fundamental quantities describing the thermal state of a plane...
Geothermal heat flow measurements are a high priority for the future lunar geophysical network missi...
Abstract We use the Martian surface temperature response to Phobos transits observed next to the InS...