The thermal properties of porous andesite

  title={The thermal properties of porous andesite},
  author={Michael J. Heap and Alexandra R. L. Kushnir and J{\'e}r{\'e}mie Vasseur and Fabian B. Wadsworth and Pauline Harl{\'e} and Patrick Baud and Ben M. Kennedy and Valentin R. Troll and Frances M Deegan},
  journal={Journal of Volcanology and Geothermal Research},
Dynamic Properties of Thermal Shock Treated Sandstone Subjected to Coupled Dynamic and Static Loads
In deep rock engineering, the rock mass can be subjected to thermal stress caused by sudden changes in temperature, which is referred to as thermal shock (TS). To study the effect of TS on heated
Petrophysical characterization of the Los Humeros geothermal field (Mexico): from outcrop to parametrization of a 3D geological model
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Particularly in the presence of a hydrothermal system, many volcanoes output large quantities of heat through the transport of water from deep within the edifice to the surface. Thus, heat flux is a
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Geothermal exploration concepts can be improved at an early stage of exploration by assessing the petrophysical rock properties of samples from surface outcrops. The results can be used to better
The fire resistance of high-strength concrete containing natural zeolites


Thermal properties of Central Aare granite for temperatures up to 500°C: Irreversible changes due to thermal crack formation
Thermal diffusivity, heat capacity, and thermal conductivity of Central Aare granite are reported in the temperature range from 25°C to 500°C. Each rock sample underwent three consecutive heating and
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The Upper Rhine Graben (URG) has been extensively studied for geothermal exploitation over the past decades. Yet, the thermal conductivity of the sedimentary cover is still poorly constrained,
Interrelations Between Thermal Conductivity and Other Physical Properties of Rocks: Experimental Data
Abstract — A new non-contact and non-destructive optical scanning instrument provided a large number of high-precision measurements of thermal conductivity tensor components in samples of sedimentary