IEA Solar Heating and Cooling Programm - NachhaltigWirtschaften.at

IEA Solar Heating and Cooling Programm - NachhaltigWirtschaften.at IEA Solar Heating and Cooling Programm - NachhaltigWirtschaften.at

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IEA SHC Task 38 Solar Air Conditioning and Refrigeration Subtask C2-A, November 9, 2009 Exhaust humid air Regeneration hot air Outside moist air Dry air Figure 3: Desiccant wheel The desiccant wheel model used below is that proposed first by Banks [8] and also by Maclaine-cross and Banks [7]. The following assumptions are made [3]: • The state properties of the air streams are spatially uniform at the desiccant wheel inlet • The interstices of the porous medium are straight and parallel • There is no leakage or carry-over of streams • The interstitial air velocity and pressure are constant • Heat and mass transfer between the air and the porous desiccant matrix is considered using lumped transfer coefficients • Diffusion and dispersion in the fluid flow direction are neglected • No radial variation of the fluid or matrix states • The sorption isotherm does not represent a hysteresis • Air reaches equilibrium with the porous medium Heat and mass conservation equations: ∂ha ∂ha ∂H d + u + µ ∂t ∂z ∂t = 0 (7) ∂wa ∂wa ∂Wd + u + µ ∂t ∂z ∂t = 0 (8) Heat and mass transfer equations: ∂H d ∂ha ∂ha µ + J m ( Le( Ta, eq − Ta ) ) + ( wa, eq − wa ) = 0 (9) ∂t ∂T ∂w a w ∂Wd µ + J m ( wa, eq − wa ) = 0 (10) ∂t a T page 28

IEA SHC Task 38 Solar Air Conditioning and Refrigeration Subtask C2-A, November 9, 2009 Equations (7), (8), (9) and (10) are coupled, hyperbolic and non-linear. With the assumption of the Lewis number (Le), equal unity and the desiccant matrix in equilibrium with air means that (T d = T eq and w eq = w a ). Banks [8] used matrix algebra and demonstrated that these equations (7 to 10) can be reduced by applying the potential function Fi(T,w) to the following system: ∂Fi , eq ∂F , a ∂F , a γ iµ + u + = 0 i=1;2 ∂t ∂t ∂z (11) ∂Fi , d γ iµ + J m ( Fi , eq − Fi , a ) = 0 i=1;2 ∂t (12) These equations are similar to those for the sensible regenerator (Equations 1 and 2), with the potential function F i replacing the temperature and the parameters γ i replacing the specific heat ratio, and they can be solved using analogy with heat transfer alone as suggested by Maclaine-cross and Banks [7] and Close and Banks [9]. There are many expressions for the potential functions of moist air-silica gel; we chose those proposed by Jurinak [10] and Stabat [11]. F = h 1 (13) 1.5 ( 273.15 + T ) 0. 8 2 1. 1 F = + w (14) 6360 The solution sequence for the desiccant wheel is then: . j i C j = m a C C M = * d i( moy) ri . min j * i = m C C a i min i max N γ NUT 0 1 = C min ⎛ ⎜ ⎝ 1 + 1 ( h A) ( h A) m s m r ⎞ ⎟ ⎠ −1 ⎡ ( ) ( ) ⎥ ⎥ ⎤ = m 1 ⎢ − * ε i ε cc NUT0 , Ci 1 or ε * 1. 93 i = C ri ( C * ri ≤ 0. 4 ) for very low rotation speed ⎢⎣ 9 Cri ⎦ page 29

<strong>IEA</strong> SHC Task 38 <strong>Solar</strong> Air Conditioning <strong>and</strong> Refriger<strong>at</strong>ion Subtask C2-A, November 9, 2009<br />

Exhaust<br />

humid air<br />

Regener<strong>at</strong>ion hot<br />

air<br />

Outside<br />

moist air<br />

Dry air<br />

Figure 3: Desiccant wheel<br />

The desiccant wheel model used below is th<strong>at</strong> proposed first by Banks [8] <strong>and</strong> also by<br />

Maclaine-cross <strong>and</strong> Banks [7]. The following assumptions are made [3]:<br />

• The st<strong>at</strong>e properties of the air streams are sp<strong>at</strong>ially uniform <strong>at</strong> the desiccant wheel<br />

inlet<br />

• The interstices of the porous medium are straight <strong>and</strong> parallel<br />

• There is no leakage or carry-over of streams<br />

• The interstitial air velocity <strong>and</strong> pressure are constant<br />

• He<strong>at</strong> <strong>and</strong> mass transfer between the air <strong>and</strong> the porous desiccant m<strong>at</strong>rix is<br />

considered using lumped transfer coefficients<br />

• Diffusion <strong>and</strong> dispersion in the fluid flow direction are neglected<br />

• No radial vari<strong>at</strong>ion of the fluid or m<strong>at</strong>rix st<strong>at</strong>es<br />

• The sorption isotherm does not represent a hysteresis<br />

• Air reaches equilibrium with the porous medium<br />

He<strong>at</strong> <strong>and</strong> mass conserv<strong>at</strong>ion equ<strong>at</strong>ions:<br />

∂ha ∂ha<br />

∂H<br />

d<br />

+ u + µ<br />

∂t<br />

∂z<br />

∂t<br />

= 0<br />

(7)<br />

∂wa ∂wa<br />

∂Wd<br />

+ u + µ<br />

∂t<br />

∂z<br />

∂t<br />

= 0<br />

(8)<br />

He<strong>at</strong> <strong>and</strong> mass transfer equ<strong>at</strong>ions:<br />

∂H<br />

d<br />

∂ha<br />

∂ha<br />

µ + J<br />

m<br />

( Le(<br />

Ta, eq<br />

− Ta<br />

) ) + ( wa,<br />

eq<br />

− wa<br />

) = 0<br />

(9)<br />

∂t<br />

∂T<br />

∂w<br />

a<br />

w<br />

∂Wd<br />

µ + J<br />

m<br />

( wa, eq<br />

− wa<br />

) = 0<br />

(10)<br />

∂t<br />

a<br />

T<br />

page 28

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