THERMODYNAMIC WET BULB TEMPERATURE OR ADIABATIC SATURATION TEMPERATURE (AST)

The thermodynamic wet bulb temperature or AST is the temperature at which the air can be brought to saturation state adiabatically by the evaporation of water in the flowing air. A schematic representation of this process, called the adiabatic saturation process, is shown in Fig. 20.3. It consists of an adiabatic enclosure containing adequate quantity of water. There is also an arrangement for feed water from the top.

The unsaturated air enters the enclosure at section 1. As the air flows through the enclosure water evaporates which is carried by the flowing stream of air. Thus the specific humidity of air increases. The water level in the enclosure is maintained by the feed water. Both the air and water are cooled as the evaporation takes place. The process continues until the energy transferred from the air to water is equal to the energy required to vaporise water. When steady conditions are reached, the air flowing at section 2 becomes saturated with water vapour. The temperature of the saturated air at section 2 is known as thermodynamic wet bulb temperature or adiabatic saturation temperature. The adiabatic saturation process is represented on T-s diagram as shown by the curve 1-2 in Fig. 20.4. The adiabatic saturation temperature is taken equal to the wet bulb temperature.

Let   td1 = DBT of initial unsaturated air

td2 = DBT of saturated air

     = adiabatic saturation temperature, tw

h1h2 = enthalpy of unsaturated and saturated air respectively

w1w2 = specific humidity of air at sections 1 and 2 respectively

hfw = sensible heat of water at adiabatic saturation temperature

For energy balance of air at inlet and outlet, we have

h1 + (w2 − w1)hfw = h2

or   h1 + whfw1 = h2 + whfw1

Now   h1 = ha1 + w1 hs1

and  h2 = ha2 + w2 hs2

where  ha1 = enthalpy of 1 kg dry air at DBT = td1 = cpa td1

hs1 = enthalpy of superheated vapour at tdper kg of vapour

ha2 = enthalpy of 1 kg dry air at WBT = tw = cpa td2

hs2 = enthalpy of saturated vapour at WBT = tw per kg of vapour

Thus, we get

(ha1 + w1hs1) − w1hfw = (ha2 + w2hs2) − w2hfw

w1(hs1 + hfw) = w2 (hs2 + hfw) + (ha2 − ha1)

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Also  h1 = cpatd1 + w1hs1

h2 = cpatd2 + w2hs2

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Figure 20.3 Adiabatic saturator

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Figure 20.4 T-s diagram for adiabatic saturation process

where  hs2 = hf2 + hfg2

hs1 = hs2 + cpv (td1 − td2) = hf2 + hfg2 + cpv (td1 − td2)

From the energy balance, we get

cpatd1 + w1[hf2 + hfg2 + cpv (td1 − td2)]+ (w2 − w1hf2

cpatd2 + w2 (hf2 + hfg2)

or  (cpa + w1 cpv)td1 − (cpa + w2 cpv)td2 = hfg2 (w2 − w1)

images

where cp1 and cp2 are humid specific heats

If cp1 = cp2 = cp, then

cp (td1 − td2) = hfg2 (w2 − w1)

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Example 20.4

Atmospheric air at 1 bar enters the adiabatic saturator. The dry bulb temperature is 30°C and wet bulb temperature 20°C during adiabatic saturation process. Calculate the following:

  1. Humidity ratio of entering air,
  2. Vapour pressure and relative humidity at 30°C, and
  3. Dew point temperature.

Solution

Given: pb = 1 bar, td = 30°C, tw = 20°C

  1. Saturation pressure of vapour at 20°C, from steam tables is,pv2 = 2.34 kPa or 0.0234 barEnthalpy of saturated vapour at 20°C, hs2 = hg2 = 2538.2 kJ/kgSensible heat of water at 20°C, hfw = 83.9 kJ/kgEnthalpy of saturated vapour at 30°C, hs1 = hg1 = 2556.4 kJ/kgEnthalpy of 1 kg unsaturated air at td = 30°C,ha1 =mcpatd =1×1.005×30 = 30.15kJ/kgEnthalpy of 1 kg saturated air at tw = 20°C,ha2 =mcpatw =1×1.005× 20 = 20.10 kJ/kgimages
  2. Now images images0.0107 − 0.0107 pv1 = 0.622 pv1pv1 = 0.0169 barSaturation pressure corresponding to 30°C from steam tables is,ps = 4.246 kPa or 0.04246 barRelative humidity,images
  3. Dew point temperature is the saturation temperature corresponding to the partial pressure of water vapour, pv1 = 0.0169 bar or 1.69 kPaFrom steam tables, we havetdp = 14.85°C

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