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Book - School of Science and Technology

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Psychrometry 515whereM ˆ mass flow <strong>of</strong> entering air (kg/s)H ˆ sensible heat gains (kW)c ˆ specific heat capacity <strong>of</strong> air (kJ/kg K)t ˆ design temperature rise (K)Latent heat gainsThese do not affect the quantity <strong>of</strong> conditioned air required since they do not cause a risein temperature. The latent gains are treated quite separately from the sensible gains. Themass flow <strong>of</strong> air required to deal with the latter will usually be found to produce no morethan a small increment in humidity but in an extreme case, limitation <strong>of</strong> that increment toan acceptable figure may require that the mass be increased <strong>and</strong> the design temperaturerise reduced in consequence.PsychrometryPsychrometry is a subject concerned with the behaviour <strong>of</strong> mixtures <strong>of</strong> air <strong>and</strong> watervapour <strong>and</strong> a knowledge <strong>of</strong> it is necessary in order to perform any air-conditioningcalculations. Some <strong>of</strong> the general principles were referred to in Chapter 1 but a completestudy is outside the scope <strong>of</strong> this book <strong>and</strong> is dealt with in many textbooks on thermodynamics<strong>and</strong> several excellent specialist works.*Most <strong>of</strong> the terms which relate to mixtures <strong>of</strong> air <strong>and</strong> water vapour were defined inChapter 1 <strong>of</strong> this book but a brief list recapitulating those items which are particularlyrelevant here would include:Dry bulb temperature, DB ( C)Wet bulb temperature, WB ( C)Dew-point temperature, DP ( C)Vapour pressure (kPa)Relative humidity, RH, <strong>and</strong> percentage saturation (%)Absolute humidity or moisture content (kg/kg <strong>of</strong> dry air)Total heat, TH, or specific enthalpy (kg/kg <strong>of</strong> dry air)Specific volume (m 3 /kg <strong>of</strong> dry air)Barometric pressureThe st<strong>and</strong>ard level <strong>of</strong> atmospheric pressure is 101.325 kPa exactly, corresponding to760 mm <strong>of</strong> mercury at 0 C <strong>and</strong> st<strong>and</strong>ard gravity (9:80665 m/s 2 ). This level, equating to1.01325 bar, was the barometric pressure used in calculation <strong>of</strong> the psychrometric properties<strong>of</strong> air <strong>and</strong> water vapour presented in the Guide Section C1, <strong>and</strong> referred to later in thischapter. For practical purposes in air-conditioning design, the data so presented are* Goodman, W., Air Conditioning Analysis. Macmillan, New York, 1947. Jones, W. P., Air ConditioningEngineering. Butterworth Heinemann, 2001.

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