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By Thomas ( Ed. ) Abbondi

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30 The Physical Environment 3-5. A radiation thermometer measures surface temperature by assuming the surface viewed is a black body, then converting the radiant energy flux it senses to a mean surface temperature by means of the Stephan-Boltzmann equation. (a) If the two walls in Problem 3-2 are actually at a temperature of 180°F, and the radiation thermometer is pointed at Wall 2, what temperature will it register? (b) If Wall 1 is actually at 40°F and Wall 2 actually at 180°F, but the radiation thermometer registers a temperature of 150°F for Wall 2, what is the emissivity of Wall 2?

In other words, other things being equal, the soil temperature will change most rapidly at those levels where the temperature profile is the least linear. Figure 4-13 Temperature Fig. 4-13. Schematic representation (hypothetical) of the equilibration of temperature in a soil profile. 54 The Physical Environment shows this relationship graphically. If we begin with a curved temperature profile, constrain the temperature at the upper and lower faces of the soil slab to remain constant with time, and allow the soil temperatures within the slab to come to equilibrium, the result will be a linear profile.

In what follows, the expression "air temperature" will be used to refer to a measure only of the true air temperature. Most of the examples cited, which include many measurements taken very close to the ground surface, are from research results obtained with the very small probes mentioned above. Environmental Temperature 33 Air Temperature near the Ground: Time Variations Figure 4-1 shows a typical plot of air temperature near the ground through the course of a clear, sunny day. Temperature values are omitted in order to concentrate on the time relationships involved.

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Advanced Techniques: Painting and Weathering Military Vehicles by Thomas ( Ed. ) Abbondi

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