Ecosystem model: Difference between revisions

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'''Sol-air temperature''' (''T''<sub>sol-air</sub>) is a variable used to calculate cooling load of a building and determine the total heat gain through exterior surfaces. It is an improvement over:
 
:<math>\frac{q}{A} = h_o(T_o - T_s)</math>
 
Where:
 
* <math>q</math> = rate of heat transfer [W]
* <math>A</math> = heat transfer surface area [m²]
* <math>h_o</math> = heat transfer coefficient for radiation (long wave) and convection [W/m²K]
* <math>T_o</math> = outdoor surroundings' temperature [°C]
* <math>T_s</math> = outside surface temperature [°C]
 
The above equation only takes into account the temperature differences and ignores two important parameters, being 1) solar radiative flux; and 2) infrared exchanges from the sky. The concept of ''T''<sub>sol-air</sub> was thus introduced to enable these parameters to be included within an improved calculation. The lower formula results:
 
<math>T_\mathrm{sol-air} = T_o + \frac{ (a \cdot I - \Delta Q_{ir})}{h_o}</math>
 
Where:
 
* <math>a</math> = solar radiation absortivity (surface solar absorptance or the inverse of the solar reflectance of a material) [-]
* <math>I</math> = global solar irradiance (i.e. total solar radiation incident on the surface) [W/m²]
* <math>\Delta Q_{ir}</math> = extra infrared radiation due to difference between the external air temperature and the apparent sky temperature. This can be written as <math>\Delta Q_{ir} = F_r * h_r * \Delta T_{o-sky}</math> [W/m²]
 
The product <math> T_\mathrm{sol-air} </math> just found can now be used to calculate the amount of heat transfer per unit area, as below:
 
<math>\frac{q}{A} = h_o(T_\mathrm{sol-air} - T_s)</math>
 
An equivalent, and more useful equation for the net heat loss across the whole construction is:
 
<math>\frac{q}{A} = U_c(T_i - T_\mathrm{sol-air})</math>
 
Where:
* <math>U_c</math> = construction U-value, according to ISO 6946 [W/m²K].
* <math>T_i</math> = indoor temperature [°C]
* <math>\Delta T_{o-sky}</math> = difference between outside dry-bulb air temperature and sky mean radiant temperature [°C]
 
By expanding the above equation through substituting <math>T_\mathrm{sol-air}</math> the following heat loss equation is derived:
 
<math>\frac{q}{A}  =  U_c(T_i - T_o)  -  \frac{U_c}{h_o} {[a \cdot I - F_r  \cdot h_r \cdot \Delta T_{o-sky}]}</math>
 
The above equation is used for opaque facades in,<ref>ISO 13790, ''Energy performance of buildings — Calculation of energy use for space heating and cooling''</ref> and renders intermediate calculation of <math>T_\mathrm{sol-air}</math> unnecessary. The main advantage of this latter approach is that it avoids the need for a different outdoor temperature node for each facade. Thus, the solution scheme is kept simple, and the solar and sky radiation terms from all facades can be aggregated and distributed to internal temperature nodes as gains/losses.
 
Note to Editor: Items <math> F_r </math>  and  <math> h_r </math> require further definition to complete this article.
 
== References ==
<references/>
#Fundamentals volume of the ''ASHRAE Handbook'', ASHRAE, Inc., Atlanta, GA, USA, 2005
#''Heating and Cooling of Buildings'', 2nd ed., Kreider, Curtiss, Rabl, McGraw-Hill, New York, USA, 2002
 
==See also==
*[[HVAC]]
*[[ASHRAE]]
*[[Active solar]]
*[[Passive solar]]
 
[[Category:Heating, ventilating, and air conditioning]]
[[Category:Building engineering]]

Revision as of 00:43, 31 December 2013

Sol-air temperature (Tsol-air) is a variable used to calculate cooling load of a building and determine the total heat gain through exterior surfaces. It is an improvement over:

qA=ho(ToTs)

Where:

  • q = rate of heat transfer [W]
  • A = heat transfer surface area [m²]
  • ho = heat transfer coefficient for radiation (long wave) and convection [W/m²K]
  • To = outdoor surroundings' temperature [°C]
  • Ts = outside surface temperature [°C]

The above equation only takes into account the temperature differences and ignores two important parameters, being 1) solar radiative flux; and 2) infrared exchanges from the sky. The concept of Tsol-air was thus introduced to enable these parameters to be included within an improved calculation. The lower formula results:

Tsolair=To+(aIΔQir)ho

Where:

  • a = solar radiation absortivity (surface solar absorptance or the inverse of the solar reflectance of a material) [-]
  • I = global solar irradiance (i.e. total solar radiation incident on the surface) [W/m²]
  • ΔQir = extra infrared radiation due to difference between the external air temperature and the apparent sky temperature. This can be written as ΔQir=Fr*hr*ΔTosky [W/m²]

The product Tsolair just found can now be used to calculate the amount of heat transfer per unit area, as below:

qA=ho(TsolairTs)

An equivalent, and more useful equation for the net heat loss across the whole construction is:

qA=Uc(TiTsolair)

Where:

  • Uc = construction U-value, according to ISO 6946 [W/m²K].
  • Ti = indoor temperature [°C]
  • ΔTosky = difference between outside dry-bulb air temperature and sky mean radiant temperature [°C]

By expanding the above equation through substituting Tsolair the following heat loss equation is derived:

qA=Uc(TiTo)Ucho[aIFrhrΔTosky]

The above equation is used for opaque facades in,[1] and renders intermediate calculation of Tsolair unnecessary. The main advantage of this latter approach is that it avoids the need for a different outdoor temperature node for each facade. Thus, the solution scheme is kept simple, and the solar and sky radiation terms from all facades can be aggregated and distributed to internal temperature nodes as gains/losses.

Note to Editor: Items Fr and hr require further definition to complete this article.

References

  1. ISO 13790, Energy performance of buildings — Calculation of energy use for space heating and cooling
  1. Fundamentals volume of the ASHRAE Handbook, ASHRAE, Inc., Atlanta, GA, USA, 2005
  2. Heating and Cooling of Buildings, 2nd ed., Kreider, Curtiss, Rabl, McGraw-Hill, New York, USA, 2002

See also