Environmental Engineering Reference
In-Depth Information
Table 4.4.2 Details of the configuration, operating conditions
and thermal properties of the thermosyphon solar-
energy water-heater used in the sample calculation.
System parameters
A c = 2.0
(m 2 )
F av = 0.9
( τα ) e = 0.72
U L = 3.5
(Wm 2 K 1 )
(WK 1 )
( UA ) s = 3
N = 8
M 2 = 297
(kg)
h 3 = 1.8
(m)
h 2 = 1.7
(m)
L r = 1
(m)
D r = 0.015
(m)
L p = 8.72
(m)
D p = 0.025
H td = 19.2
(M J m 2 )
Weather conditions
T a = 16
( C)
T m = 15
( C)
t = 59,220
(s)
Hot-water demand
M L = 208
(kg)
T L = 46
( C)
(kg m 3 )
Fluid properties
ρ w = 998
µ w = 10 3
(Ns m 2 )
v w = 1.00 × 10 6
(m 2 s)
( J kg 1 K 1 )
C w = 4190
β w = 2.1 × 10 4
(K 1 )
of the applied conditions, whereas the Bailey number, K, is a function essentially of the
system design. However, all these dimensionless groups include information available
readily to a designer who, using the nomgram, can thus determine the Brooks number
X, and thus the solar fractions.
A worked example of using the correlations to predict the daily solar fraction The
component specifications of a thermosyphon solar- energy water heater and climatic
conditions (for a typical day in June) used in the following example are given in Table
4.4.2. Evaluating the parameters K, W, I and Z gives K
=
12, W
=
0.7, Y
=
20, and
Z
0.3 respectively. Also, since the thermal performance is being determined for the
reference month of June, Z J =
=
0.3. A three-stage algorithm is used to determine
the dimensionless Brooks number, X, from which the solar fraction can be calculated.
Stage I is to determine the deviation, m J (due to circulation number effects) of the
characteristic gradient from the maximum value, m j ,max .
m =
Z
=
0.051. This stage corresponds to the first quadrant of
the nomogram shown in Figure 4.3.4. Stage two is to determine the maximum gradient,
m J , max for the system and subtract the gradient displacement, m , to give the actual
gradient, m J of the characteristic curve. m J , max ,
0.055, giving m j =
=
0.673, the actual gradient, m J ,is
then given by
m J =
m J ,max
( m J )
=
0 . 622
(4.4.21)
 
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