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Book - School of Science and Technology

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74 The building in summertime <strong>of</strong> peak gain may not be released from the inner surfaces until after rooms therehave ceased to be occupied.As will be appreciated therefore, the temperature difference between outside air (t ao )<strong>and</strong> inside air (t ai ), does not represent the situation properly since the outside surfacetemperature <strong>of</strong> the material will have been raised by the heat absorbed, as noted above. Aconvenient but approximate method <strong>of</strong> dealing with this situation is to make use <strong>of</strong> theconcept <strong>of</strong> sol±air temperature (t so ), a hypothetical scale which takes into account not onlythe outside air temperature but also increments to it which represent the increase due tothe effects <strong>of</strong> solar radiation. Tables <strong>of</strong> sol±air temperature, hour by hour during thecritical months <strong>of</strong> insolation, are given in the Guide Section A2 for a number <strong>of</strong> orientations<strong>and</strong> with respect to both `light' <strong>and</strong> `dark' coloured building surfaces.The subject <strong>of</strong> dynamic response, including the influence <strong>of</strong> time lag () <strong>and</strong> decrementfactors ( f ) was discussed briefly at the end <strong>of</strong> the previous chapter. In summer, when heatgain is a penalty rather than a bonus, some attempt must be made in calculationsperformed manually to take these factors into consideration. The application <strong>of</strong> sol±airtemperature tables to the problem takes account <strong>of</strong> the average <strong>of</strong> such temperatures over24 hours as well as that relevant to the duration <strong>of</strong> the time lag, making use <strong>of</strong> thefollowing equation to determine heat gain at the time taken for peak loading, hours:Q/AU ˆ (t som t ai ) ‡ f (t so t som )which may be transposed to:Q/AU ˆ (t s t ai )whereQ/AU ˆ heat flow into the space at the time, , which has been taken for peakloading (W/m 2 ):t som ˆ mean sol air temperature over 24 hours ( C):t so ˆ sol air temperature at time, , i:e: prior to the appropriate time lag, hours ( C):t s ˆ t som (1 f ) ‡ f (t so )( C):Selected values <strong>of</strong> this notional temperature (t s ) for a medium coloured building surface(i.e. one between `light' <strong>and</strong> `dark' <strong>and</strong> which absorbs 70% <strong>of</strong> total radiation) <strong>and</strong> for anumber <strong>of</strong> combinations <strong>of</strong> time lag <strong>and</strong> decrement factors are listed in Table 3.1. Thesevalues apply strictly to south-east Engl<strong>and</strong> in the month <strong>of</strong> July, but may be used for suchlatitudes over the months <strong>of</strong> May to September without too much loss <strong>of</strong> accuracy.Further, the temperatures listed may be applied, within the relevant margin <strong>of</strong> error, inconjunction with most published figures for time lag <strong>and</strong> decrement factor, includingthose given in Table 3.2 which represent these characteristics for a range <strong>of</strong> typicalconstruction elements. Routine calculations are simple, as illustrated by the followingexample:A wall facing south-east is constructed <strong>of</strong> 220 mm solid brick, with lightweight plasterinternally. The internal air temperature is to be maintained at 21 C, the peak cooling loadfor the space concerned being taken at 16.00 hours BST in July.

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