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Initially, a linear temperature increase of 20 550 °C from the surface to the Moho depth (36 km), with a further linear temperature increase to 1,350 °C at the base of the lithosphere.
The surface is maintained at linear temperature and concentration variations.
Linear temperature profile and non-linear temperature profile obtained by solving heat conduction problem are taken into account.
The activation energy for total reaction increases substantially with temperature and exhibits almost linear temperature dependence.
Finally, the static equilibrium equations are solved considering the linear temperature field.
The linear temperature and quadratic WHSV terms gave significant effect on both responses.
Similar(10)
Linear temperature-dependent laws exist for many inorganic fibrous materials that exhibit a decreased thermal conductivity at lower temperatures.
A linear, temperature-independent isotherm and constant diffusion coefficient are assumed.
The linear temperature-dependent integrated PL intensity and spectral position paves the way for the application of this kind of colloidal solutions as temperature-sensitive media.
The graph reveals linear temperature-mortality relationships over lags.
The tube simulations show a non-linear temperature profile along the tube with the maximum temperature in the outer pipe.
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