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Based on these release profiles, we classified seven MMs into three types: least heated, moderately heated, and severely heated MMs (Table 1).
The other least heated MM, D03IB067, is composed of anhydrous minerals.
The other least heated MM, D03IB068, contains a small numbers of pores in the cross section (Fig. 5b).
Based on the release patterns of SW 4He, which should reflect the degree of heating during atmospheric entry, the seven MMs were classified into three types including two least heated, three moderately heated, and two severely heated MMs.
For the least heated MMs, the release patterns of 4He (Fig. 1) indicate peak temperatures of 400 to 650 °C because ~50%% of 4He is released by 650 °C, including 71 and 43 % for D03IB067 and D03IB068, respectively, as calculated from Table 2 (Nier and Schlutter 1992 , 1993.
The rest of the tents are at least heated.
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In the middle of the summer, one can "check" with the other to operate at the time of the day that creates the least heat.
You can see the results above: blue areas show the least heat loss and red and yellow areas show the worst.
Why do you think that is? WILLIAM LEAST HEAT-MOON: My theory is it comes from the historic fact we are all from the other side of the planet.
The least heat exchanger area required at constant power rating is found when the working fluid is n-pentane.
The question is for the least heat capacity flow rates of the heat carrier required for 1 MW net power output.
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