Environmental Engineering Reference
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Fig. 1.7 The magnetic Carnot refrigeration cycle in a T - s diagram (with gadolinium as the
refrigerant)
T R Z
T R Z
a
a
M
o
l 0 o
q R ¼
ds
¼
T R D
s a d ¼
dH
ð 1 : 46 Þ
T
H
d
d
The speci
c work can be de
ned with the following relation:
I
w
¼
dq
¼
T R D
s a d þ
T H D
s c b
ð 1 : 47 Þ
where
s a d =
s c b. Therefore, the COP can be de
ned as:
Δ
−Δ
q R
w
T R
T H
COP
¼
jj ¼
ð 1 : 48 Þ
T R
Magnetic Stirling Thermodynamic Cycle
Such a cycle (Fig. 1.8 ) is very dif
cult to operate in real situations. It is necessary to
keep the iso-magnetization and iso-demagnetization processes (constant magneti-
zation), which require a particular magnetic
eld variation with a simultaneous
fl
uid
fl
ow. The speci
c cooling power for this cycle can be de
ned as:
T R Z
Z
a
a
M
o
l 0 o
q R ¼
ds
¼
T R D
s a d ¼
T R
dH
ð 1 : 49 Þ
T
H
d
d
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