Sharp JX-9400 Informacje Techniczne Strona 101

  • Pobierz
  • Dodaj do moich podręczników
  • Drukuj
  • Strona
    / 211
  • Spis treści
  • BOOKMARKI
  • Oceniono. / 5. Na podstawie oceny klientów
Przeglądanie stron 100
Figure 5.1, a psychrometric chart for air, shows several characteristics of
humid air. The curves show the water content of air as a function of its
temperature for various relative humidities. The water content cannot be
greater than that shown by the saturation curve. Air with a relative humidity
0 <’<1 has a water content times that of the saturated air.
Energy is needed for heating or cooling the air as well as for evaporating
water in it or condensing water for drying it. Taking as a reference dry air at
08C, the specific enthalpy or energy needed to hea t and humidify 1 kg of air
to reach the temperature and humidity ratio x is:
h ¼ c
da
þðL þ c
w
Þx ð5:1Þ
where:
c
da
is the specific heat capacity of dry air, about 1006 J/(kgK);
c
w
is the specific heat capacity of water vapour, about 1805 J/(kgK);
L is the latent heat of evaporation, i.e. the heat required to evaporate 1 kg of
water, about 2,501,000 J/kg;
x is the humidity ratio, i.e. the mass of water vapour per kilogram of dry
air.
This humidity ratio, x, is related to the water content, !, which is the mass
concentration of water vapour in moist air of Figure 5.1, by:
x ¼
!
1 !
and ! ¼
x
1 þ x
ð5:2Þ
0
5
10
15
20
25
30
Water content [g/kg]
Sat.
90%
80%
70%
60%
50%
40%
30%
20%
10%
0 10 20 30 ºC
10
20
30
40
50
60
70
80
90 kJ/kg
Figure 5.1 Psychrometric chart with constant relative humidity curves
and constant enthalpy lines
Note: It is shown that air at 208C and 50 per cent relative humidity contains about
7.5 g of water vapour per kilogram. Its enthalpy is 39 kJ/kg and its dew point is close
to 108C.
80 Ventilation and Airflow in Buildings
Przeglądanie stron 100
1 2 ... 96 97 98 99 100 101 102 103 104 105 106 ... 210 211

Komentarze do niniejszej Instrukcji

Brak uwag