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A very short electrical current impulse applied to the substrate leads to the surface heating.
The heat transfer model is shown to correctly approach the dry growth limit, based on mass conservation alone, under appropriate thermal conditions when the surface heating rate is diminished sufficiently.
We examine the efficiency and accuracy of the IMC and SIMC methods for test problems involving the evolution of a collisionally pumped trapping problem to its steady-state, the surface heating of a cold medium by a beam, and the diffusion of energy from a localized region that is collisionally pumped.
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Geothermal power stations use water pumped down to hot rocks under the earth that returns to the surface heated, fuelling electricity generation or to be used for space heating.
The surface heat flow values are normally >50 mW/m2 (Ravi Shankar, 1988).
The surface heat flow was calculated from the crustal and mantle heat flows (Eq. 5).
The surface heat flux gradually decreases with time because of the thickening of the surface TBL.
The surface heat flow may not come from the mantle but from the crust.
Six intervals (black bar) were chosen to calculate the surface heat flow (Table 3).
Xiong et al. [29] used it to consider the surface heat flux for the sideways heat equation.
The surface heat-transfer coefficient distribution law on the surfaces of rotor exciting winding was studied.
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