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The (alpha) value was determined so that the calculated temperature at BSR depths best agreed with the temperature estimated based on the phase boundary.
The temperatures at the BSR depths were used for the boundary condition (b) to restrict the calculated thermal structure by choosing the best coherency between the temperature at the BSRs and the calculated temperature at the same depth of the shallow thermal structure.
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These values are thereafter used to calculate temperatures at any point in the gas and solid phases under reaction.
Equation (4) has then been applied to calculate temperatures at 1000 m depth intervals between 3500 and 9500 m.
The second step is to calculate temperatures at the mid-point of each 1000 m depth interval from 3000 m to the base of the model, i.e. at depths X (m) equal to 3500, 4500, 5500, 6500, 7500, 8500 and 9500 m.
Temperature values were used to calculate temperature rate at various concentrations of SA. (A-F).
Temperature values from Figure 1 were used to calculate temperature rate at various concentrations of ASA (A-F).
The calculated melting temperature at αc of the samples was also almost the same regardless of their ν.
It provides the TD of more than 1 K at room temperature, which can be compared with the previous study [8, 10, 11]. Figure 3 The influence of the irradiation on the TDs. a assuming the heating temperature of 623 K at one end of the CNW and particle radius of 65 nm, we calculated the temperature at the other end.
For each city, they calculated the temperature at which deaths were least likely to occur.
A soil temperature calculation equation usually employed in civil engineering was used to calculate soil temperature at various depths in a cemetery located in Brisbane, Australia, in order to explain the extensive degradation of human remains and funerary objects observed at exhumation.
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