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r
ig
er
atio
n
is
to
s
lo
w
d
o
wn
b
ac
ter
ial
m
etab
o
lis
m
,
p
r
ev
en
t b
ac
ter
ial
g
r
o
wth
,
an
d
en
s
u
r
e
th
at
th
e
f
is
h
d
o
es
n
o
t
r
o
t
o
r
d
e
ter
io
r
ate
[
9
]
.
Sto
r
in
g
f
i
s
h
with
wet
ice,
ice
b
o
x
es,
o
r
ice
b
lo
ck
s
in
a
co
o
l
b
o
x
o
r
c
o
n
v
e
n
tio
n
al
th
er
m
o
s
is
in
ef
f
ec
tiv
e
b
ec
au
s
e
th
e
ice
m
e
lts
q
u
ick
ly
.
T
r
ad
itio
n
al
f
is
h
er
m
en
o
f
ten
s
p
en
d
th
e
wh
o
le
d
ay
at
s
ea
with
a
lim
ited
s
u
p
p
ly
o
f
wet
ice.
T
h
e
weig
h
t,
co
s
t
,
an
d
d
im
en
s
io
n
s
o
f
ice
m
ak
e
it
v
er
y
d
if
f
icu
lt
to
ca
r
r
y
a
lo
t
o
f
ice
o
n
f
is
h
in
g
v
ess
els,
s
o
th
e
f
i
s
h
th
ey
ca
tch
ca
n
ex
p
er
ien
ce
a
d
ec
lin
e
in
f
r
e
s
h
n
ess
q
u
ality
[
1
0
]
.
So
m
etim
es,
tr
ad
itio
n
al
f
is
h
er
m
en
also
a
d
d
s
alt
to
t
h
e
wet
i
ce
an
d
f
is
h
t
o
p
r
eser
v
e
th
e
f
is
h
f
o
r
l
o
n
g
er
,
b
u
t
t
h
is
ca
n
ch
an
g
e
th
e
tast
e
o
f
th
e
f
is
h
,
m
ak
in
g
it salti
er
,
wh
ich
is
n
o
t a
g
o
o
d
co
n
ce
p
t [
1
1
]
.
I
n
d
o
n
esia'
s
f
is
h
in
g
in
d
u
s
tr
y
is
f
ac
in
g
a
q
u
ality
is
s
u
e
d
esp
ite
an
i
n
cr
ea
s
e
in
p
r
o
d
u
ctio
n
.
Us
u
ally
,
th
e
f
is
h
ca
u
g
h
t
ar
e
o
f
ten
s
to
r
ed
f
o
r
s
ev
er
al
h
o
u
r
s
in
th
e
f
is
h
er
m
en
'
s
b
o
at
ca
r
g
o
,
wh
ich
lead
s
t
o
a
d
ec
r
ea
s
e
in
th
e
f
r
esh
n
ess
o
f
th
e
f
is
h
.
As
a
r
esu
lt,
th
e
q
u
ality
o
f
th
e
f
is
h
ca
u
g
h
t
d
o
es
n
o
t
m
atc
h
u
p
with
th
e
in
cr
ea
s
ed
p
r
o
d
u
ctio
n
[
1
2
]
.
Fis
h
h
av
e
a
wate
r
co
n
te
n
t
th
at
is
q
u
ite
h
ig
h
,
r
ea
ch
in
g
6
0
-
7
0
%,
th
is
m
ak
es
th
e
f
is
h
q
u
ick
ly
u
n
d
er
g
o
a
r
o
ttin
g
p
r
o
ce
s
s
[
1
3
]
,
[
1
4
]
.
Fis
h
th
at
ar
e
n
o
lo
n
g
e
r
f
r
esh
h
av
e
a
lo
wer
p
r
ice
th
an
f
is
h
th
at
ar
e
s
till
f
r
esh
[
1
5
]
,
[
1
6
]
.
C
o
n
cr
ete
ev
id
en
ce
ca
n
b
e
s
ee
n
in
s
ev
er
al
ty
p
es
o
f
f
is
h
in
m
ar
k
ets
in
L
am
p
u
n
g
[
1
7
]
,
Ku
lo
n
Pro
g
o
[
1
8
]
,
an
d
Am
b
o
n
[
1
9
]
,
th
e
p
r
ice
o
f
f
is
h
th
at
is
n
o
lo
n
g
er
f
r
esh
ca
n
d
r
o
p
to
h
alf
th
e
n
o
r
m
al
p
r
ice.
T
h
e
r
ea
lity
o
f
th
is
co
n
d
itio
n
also
o
cc
u
r
s
f
o
r
f
is
h
er
m
en
i
n
Glag
ah
B
ea
ch
,
J
atim
alan
g
B
ea
ch
,
B
ar
u
B
ea
ch
,
an
d
L
o
g
en
d
i
n
g
B
ea
ch
.
Ma
n
y
o
f
th
e
f
is
h
b
r
o
u
g
h
t
b
y
f
is
h
er
m
en
f
r
o
m
th
e
s
ea
ar
e
n
o
t
y
et
f
r
esh
.
W
h
en
th
e
f
is
h
is
o
n
lan
d
f
o
r
s
ev
er
al
h
o
u
r
s
,
th
e
p
r
ice
o
f
th
e
f
is
h
d
ec
r
ea
s
es d
r
as
tically
b
ec
au
s
e
th
e
q
u
ality
d
ec
r
ea
s
es.
On
th
e
o
t
h
er
h
an
d
,
th
er
e
is
r
ef
r
ig
er
ated
s
ea
wate
r
(
R
SW
)
as
a
co
o
lin
g
tec
h
n
o
lo
g
y
th
at
u
s
es
a
m
ec
h
an
ical
r
ef
r
ig
er
ati
o
n
s
y
s
tem
to
p
r
eser
v
e
th
e
f
is
h
.
T
h
e
tech
n
o
lo
g
y
em
p
lo
y
s
lo
w
tem
p
er
atu
r
es
to
in
h
ib
it
en
zy
m
e
an
d
m
icr
o
b
ial
ac
tiv
ity
[
2
0
]
.
R
ef
r
ig
e
r
atio
n
will
ex
ten
d
th
e
s
h
elf
life
o
f
f
is
h
.
At
a
tem
p
er
atu
r
e
o
f
15
-
20
°
C
,
f
is
h
ca
n
b
e
s
to
r
ed
f
o
r
u
p
to
ab
o
u
t
two
d
a
y
s
,
at
a
te
m
p
er
atu
r
e
o
f
5
°
C
f
i
s
h
will
la
s
t
f
o
r
5
-
6
d
a
y
s
.
T
h
e
tem
p
er
atu
r
e
co
m
m
o
n
ly
m
ain
t
ain
ed
d
u
r
in
g
th
e
f
is
h
s
to
r
ag
e
p
r
o
ce
s
s
r
an
g
es
f
r
o
m
0
-
5
°
C
b
e
ca
u
s
e
f
is
h
will
b
e
f
r
esh
f
o
r
9
-
1
4
d
ay
s
[
2
1
]
.
T
h
e
R
S
W
tech
n
o
lo
g
y
,
wh
ile
p
r
o
m
is
in
g
,
co
m
es
with
a
h
ef
ty
in
v
estme
n
t
co
s
t
f
o
r
its
in
itial
s
etu
p
,
o
p
er
atio
n
,
a
n
d
m
ain
ten
an
ce
.
Mo
r
e
o
v
er
,
u
s
in
g
n
o
n
-
en
v
ir
o
n
m
en
tally
f
r
ien
d
ly
f
o
s
s
il
f
u
els
to
o
p
er
ate
is
also
a
wea
k
n
ess
o
f
th
is
tech
n
o
lo
g
y
[
2
2
]
.
I
n
ad
d
itio
n
,
I
n
d
o
n
esia
h
as
ex
ce
llen
t
p
o
ten
tial
f
o
r
r
en
ewa
b
le
e
n
er
g
y
,
p
ar
ticu
lar
ly
s
o
lar
e
n
er
g
y
,
o
win
g
to
its
g
eo
g
r
ap
h
y
an
d
n
atu
r
al
co
n
d
itio
n
s
.
Ho
wev
e
r
,
th
e
p
o
te
n
tial
o
f
s
o
lar
en
e
r
g
y
h
as
n
o
t
b
ee
n
u
tili
ze
d
o
p
tim
ally
d
u
e
to
th
e
lim
ited
av
ailab
ilit
y
o
f
en
er
g
y
co
n
v
e
r
s
io
n
t
ec
h
n
o
lo
g
ies
[
2
3
]
,
[
2
4
]
.
T
o
ad
d
r
ess
th
is
is
s
u
e,
r
esear
ch
er
s
ar
e
p
lan
n
in
g
to
d
esig
n
an
d
m
an
u
f
ac
tu
r
e
a
s
o
lar
-
p
o
we
r
ed
f
is
h
s
to
r
ag
e
d
ev
ice.
T
h
is
r
esear
ch
d
ev
elo
p
ed
a
s
o
l
ar
-
p
o
wer
e
d
f
is
h
co
o
lin
g
s
y
s
tem
as
an
af
f
o
r
d
ab
le,
en
v
ir
o
n
m
en
tally
f
r
ien
d
ly
,
an
d
ef
f
icien
t
s
o
lu
tio
n
to
m
ain
tain
t
h
e
f
r
esh
n
ess
o
f
f
is
h
ca
u
g
h
t
b
y
tr
ad
itio
n
al
f
is
h
er
m
en
.
I
t
u
tili
ze
s
th
e
ab
u
n
d
an
t
r
en
ewa
b
le
e
n
er
g
y
in
I
n
d
o
n
esia
to
o
v
er
c
o
m
e
t
h
e
ch
allen
g
es
o
f
p
r
eser
v
in
g
f
is
h
q
u
ality
d
u
r
in
g
f
is
h
in
g
tr
ip
s
at
s
ea
.
T
h
is
s
y
s
tem
i
s
m
o
r
e
s
u
s
tain
ab
le
co
m
p
ar
ed
to
c
o
n
v
en
ti
o
n
al
co
o
lin
g
s
y
s
tem
s
th
at
u
s
e
f
o
s
s
i
l
f
u
els,
with
af
f
o
r
d
ab
le
in
v
estme
n
t a
n
d
o
p
er
atio
n
al
co
s
ts
f
o
r
tr
ad
itio
n
al
f
is
h
er
m
e
n
.
2.
P
RO
P
O
SE
D
M
E
T
H
O
D
C
o
o
l
b
o
x
es
ar
e
in
s
u
lated
b
o
x
es
u
s
ed
to
s
to
r
e
f
o
o
d
o
r
to
s
to
r
e
m
ater
ials
th
at
r
e
q
u
ir
e
o
th
er
c
o
ld
co
n
d
itio
n
s
s
u
c
h
as
f
is
h
,
ju
ice,
v
ac
cin
es,
b
lo
o
d
,
an
d
s
o
o
n
[
2
5
]
.
T
h
e
co
o
l
b
o
x
in
n
o
v
atio
n
tec
h
n
o
lo
g
y
t
h
at
will
b
e
m
ad
e
h
as
th
e
m
ain
co
m
p
o
n
en
ts
in
th
e
f
o
r
m
o
f
s
o
l
ar
p
h
o
to
v
o
ltaic
,
th
e
r
m
o
elec
tr
ic
c
o
o
ler
(
T
E
C
)
,
c
h
ar
g
e
co
n
tr
o
ller
,
Ar
d
u
in
o
UNO,
an
d
s
h
o
ck
d
ev
ice.
T
o
u
tili
ze
s
o
lar
en
er
g
y
,
in
th
is
s
tu
d
y
,
th
e
co
o
l
b
o
x
d
ev
el
o
p
ed
will
u
s
e
s
o
lar
p
h
o
to
v
o
ltaic.
T
h
is
co
m
p
o
n
en
t
u
s
es
th
e
s
u
n
d
ir
ec
tly
as
an
alter
n
ativ
e
en
er
g
y
s
o
u
r
ce
to
r
ep
lace
f
o
s
s
il
en
er
g
y
th
at
ca
n
b
e
s
to
r
ed
in
b
atter
ies
[
2
6
]
-
[
2
8
]
.
T
h
e
en
e
r
g
y
co
n
v
er
s
io
n
s
y
s
tem
co
n
v
er
ts
s
o
lar
en
er
g
y
in
to
elec
tr
icity
b
y
u
s
in
g
s
em
ico
n
d
u
cto
r
s
,
th
e
co
n
d
u
ctiv
ity
o
f
s
em
ico
n
d
u
ct
o
r
s
wid
ely
k
n
o
wn
as
PV
ce
lls
[
2
9
]
.
So
m
e
m
ater
ials
ex
h
ib
it
a
p
r
o
p
er
ty
k
n
o
wn
as
th
e
p
h
o
to
elec
tr
ic
ef
f
ec
t
th
at
ca
u
s
es
s
o
lar
p
h
o
to
v
o
ltaic
s
to
ab
s
o
r
b
p
h
o
to
n
s
o
f
lig
h
t
an
d
r
elea
s
e
elec
tr
o
n
s
.
W
h
en
th
ese
f
r
ee
elec
tr
o
n
s
ar
e
ca
p
tu
r
ed
,
an
elec
tr
ic
cu
r
r
en
t
is
g
en
er
ated
wh
ich
ca
n
b
e
u
s
ed
as
elec
tr
icity
[
3
0
]
.
I
n
g
en
e
r
al,
en
er
g
y
-
g
en
er
atin
g
m
o
d
u
les
ar
e
co
n
n
ec
te
d
in
s
er
ies
an
d
p
ar
allel
to
o
b
tain
th
e
d
esire
d
cu
r
r
en
t,
v
o
ltag
e,
an
d
p
o
wer
v
alu
es [
3
1
]
-
[
3
3
]
.
T
h
e
o
th
er
m
ai
n
co
m
p
o
n
en
t
s
ar
e
th
er
m
o
elec
tr
ic
co
o
ler
(
T
E
C
)
also
n
am
ed
Peltier
co
o
ler
o
r
th
er
m
o
elec
tr
ic
m
o
d
u
le.
T
E
C
is
a
s
em
ico
n
d
u
cto
r
-
b
ased
elec
tr
o
n
ic
co
m
p
o
n
e
n
t
th
at
wo
r
k
s
a
s
a
h
ea
t
p
u
m
p
b
y
tr
an
s
f
er
r
in
g
h
ea
t
f
r
o
m
o
n
e
s
id
e
to
an
o
th
er
s
id
e
o
f
th
e
d
e
v
ice
an
d
p
r
o
d
u
cin
g
a
h
ea
tin
g
o
r
co
o
lin
g
ef
f
ec
t
[
3
4
]
.
T
E
C
wo
r
k
s
with
a
Pel
tier
ef
f
ec
t
th
at
tr
an
s
f
er
s
h
ea
t
f
r
o
m
o
n
e
s
id
e
o
f
th
e
d
ev
ice
to
th
e
o
th
er
s
id
e
[
3
5
]
-
[
3
6
]
.
R
esear
ch
er
s
ch
o
s
e
T
E
C
b
ec
au
s
e
T
E
C
h
as
b
ee
n
wid
ely
u
s
ed
.
Mo
r
eo
v
er
,
it
h
as
th
e
ad
v
a
n
tag
es
o
f
b
ein
g
ea
s
y
to
o
p
er
ate
an
d
lig
h
t
[
3
7
]
.
I
n
ad
d
it
io
n
,
T
E
C
h
as
n
o
m
o
v
i
n
g
p
ar
ts
,
u
s
es
n
o
wo
r
k
i
n
g
f
l
u
id
,
d
o
es
n
o
t
in
v
o
lv
e
ch
em
ical
r
ea
ctio
n
s
,
an
d
p
r
o
d
u
ce
s
n
o
e
m
is
s
io
n
s
[
3
8
]
,
[
3
9
]
.
T
E
C
h
as
s
ee
n
b
ec
k
p
r
in
ci
p
le,
th
e
s
id
e
o
f
th
e
Peltier
elem
en
t
th
at
g
ets co
ld
o
r
h
o
t
d
ep
en
d
s
o
n
th
e
d
ir
ec
tio
n
o
f
th
e
DC
cu
r
r
e
n
t f
lo
win
g
f
r
o
m
t
h
e
s
o
u
r
ce
[
4
0
]
.
Fu
r
th
er
m
o
r
e
,
th
is
s
tu
d
y
u
s
ed
a
ch
ar
g
e
co
n
tr
o
ller
as
an
elec
tr
o
n
ic
d
ev
ice
to
r
eg
u
late
th
e
d
ir
ec
t
cu
r
r
en
t
wh
ich
is
ch
ar
g
ed
t
o
th
e
b
atte
r
y
an
d
tak
e
n
f
r
o
m
th
e
b
atter
y
to
th
e
lo
ad
.
T
h
is
to
o
l
p
lay
s
a
r
o
le
i
n
r
e
g
u
latin
g
o
v
er
ch
a
r
g
in
g
(
ex
ce
s
s
ch
ar
g
in
g
b
ec
au
s
e
th
e
b
atter
y
is
f
u
lly
ch
ar
g
ed
)
an
d
e
x
ce
s
s
v
o
ltag
e
f
r
o
m
ce
r
tain
s
o
u
r
ce
s
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
t J Po
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lec
&
Dr
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s
t
I
SS
N:
2088
-
8
6
9
4
Desig
n
s
ystem
a
n
d
p
erfo
r
ma
n
ce
a
n
a
lysi
s
o
f fis
h
s
to
r
a
g
e
b
o
x
b
y
u
tili
z
in
g
…
(
R
iz
a
l J
u
s
tia
n
S
etia
w
a
n
)
2593
[
4
1
]
.
T
h
en
,
th
e
elec
tr
ical
co
n
tr
o
l
u
s
ed
in
th
is
r
esear
ch
is
Ar
d
u
in
o
UNO.
I
t
is
a
m
icr
o
co
n
tr
o
ller
b
o
ar
d
b
ased
o
n
th
e
AT
m
eg
a3
2
8
[
4
2
]
.
T
h
is
co
m
p
o
n
e
n
t
ca
n
s
u
p
p
o
r
t
au
to
m
ati
c
co
n
tr
o
l
o
f
t
h
e
d
ev
ice
an
d
ca
n
b
e
co
n
n
ec
ted
to
a
co
m
p
u
ter
u
s
in
g
a
USB
ca
b
le
[
4
3
]
.
T
h
e
AT
Me
g
a3
2
8
p
e
r
f
o
r
m
s
d
ata
p
r
o
ce
s
s
in
g
an
d
n
o
tific
ati
o
n
s
,
co
m
m
an
d
s
ar
e
d
is
p
lay
ed
o
n
th
e
L
C
D
as n
o
tif
icatio
n
s
v
ia
th
e
d
is
p
lay
lay
e
r
a
n
d
a
b
u
zz
er
as a
n
o
tific
atio
n
in
d
icato
r
[
4
4
]
.
No
t
o
n
ly
ar
e
th
e
m
a
in
co
m
p
o
n
en
t
s
f
o
r
c
o
o
l
in
g
f
i
s
h
,
b
u
t
th
e
m
ain
co
m
p
o
n
en
t
o
f
k
i
l
lin
g
b
ac
t
er
ia
in
f
i
s
h
u
s
in
g
el
ec
tr
i
c
s
h
o
ck
ca
n
al
s
o
b
e
a
f
e
atu
r
e
t
o
p
r
ev
en
t
f
is
h
f
r
o
m
d
ec
ay
.
E
lec
tr
ic
s
h
o
c
k
d
ev
i
ce
s
c
an
h
e
lp
m
ain
ta
in
f
i
s
h
f
r
e
s
h
n
e
s
s
wh
i
le
f
i
s
h
er
m
en
ar
e
o
u
t
at
s
ea
b
y
u
s
in
g
e
le
ctr
ic
s
h
o
ck
d
ev
i
ce
s
th
a
t
h
av
e
a
v
o
l
tag
e
o
f
u
p
to
2
,
5
0
0
v
o
l
t
s
[
4
5
]
.
A
n
o
n
-
th
er
m
al
f
o
o
d
p
r
e
s
e
r
v
a
tio
n
m
e
t
h
o
d
i
s
to
u
s
e
a
h
ig
h
-
v
o
l
ta
g
e
el
ec
t
r
i
c
s
h
o
ck
,
o
f
ten
ca
l
led
a
p
u
l
s
ed
el
ec
tr
i
c
f
ie
ld
(
PE
F).
U
s
in
g
el
ec
tr
i
c
s
h
o
ck
s
c
an
h
e
lp
p
r
e
s
e
r
v
e
f
i
s
h
an
d
s
u
p
p
r
e
s
s
th
e
n
u
m
b
er
o
f
m
icr
o
b
e
s
o
n
th
e
f
i
s
h
.
Fro
m
r
e
s
e
ar
ch
r
ef
er
en
c
e
s
,
i
t
i
s
p
r
o
v
e
n
th
a
t
th
e
r
e
i
s
a
s
ig
n
if
ic
an
t
d
i
f
f
er
en
ce
(
P
>
0
.
0
5
)
b
et
wee
n
u
n
tr
e
at
ed
s
a
m
p
l
e
s
a
n
d
tr
ea
ted
s
am
p
le
s
.
T
h
is
i
n
d
i
ca
te
s
th
a
t
el
ec
tr
i
c
s
h
o
ck
s
o
f
3
0
-
6
0
k
V
c
an
s
u
p
p
r
e
s
s
th
e
n
u
m
b
er
o
f
b
ac
ter
ia
.
H
ig
h
er
in
ten
s
ity
tr
e
at
m
en
t
s
ca
n
b
e
u
s
ed
f
o
r
th
e
in
ac
tiv
at
io
n
o
f
m
icr
o
o
r
g
an
i
s
m
s
b
y
ir
r
ev
er
s
ib
le
d
a
m
ag
e
t
o
th
e
ce
ll
m
em
b
r
an
e
[
4
6
]
.
Al
th
o
u
g
h
th
e
el
ec
tr
ic
s
h
o
ck
ca
n
k
i
ll
b
a
cte
r
i
a
q
u
ick
ly
an
d
ef
f
e
ct
iv
e
ly
.
Ho
wev
er
,
th
e
u
s
e
o
f
t
h
i
s
e
lec
tr
ic
s
h
o
ck
c
an
af
f
e
ct
th
e
tex
tu
r
e
o
f
f
i
s
h
m
ea
t
b
ec
au
s
e
f
i
s
h
m
e
at
t
h
a
t
is
g
iv
en
an
el
ec
tr
i
c
s
h
o
ck
tr
ea
t
m
en
t w
il
l
n
o
t
b
e
as h
ar
d
a
s
f
i
s
h
m
ea
t
w
i
th
o
u
t
tr
ea
t
m
en
t.
T
h
e
h
ig
h
er
th
e
v
o
l
ta
g
e
ap
p
l
ied
to
th
e
f
i
s
h
c
an
c
au
s
e
th
e
tex
tu
r
e
v
a
lu
e
is
g
e
t
lo
wer
,
al
th
o
u
g
h
it
d
id
n
o
t
g
iv
e
a
d
if
f
er
en
ce
in
th
e
p
H,
ta
s
t
e,
an
d
s
m
el
l
o
f
th
e
f
i
s
h
[
4
7
]
.
E
v
en
th
o
u
g
h
i
t k
i
ll
s
b
a
ct
er
i
a
q
u
i
ck
ly
an
d
k
e
ep
s
th
e
f
i
s
h
f
r
o
m
r
o
tt
in
g
q
u
ick
ly
,
th
e
t
ex
t
u
r
e
o
f
t
h
e
f
i
s
h
wi
ll
b
e
s
o
f
ter
th
an
b
e
f
o
r
e
.
T
ex
tu
r
e
i
s
an
im
p
o
r
tan
t
p
ar
am
et
er
f
o
r
f
i
s
h
m
ea
t
q
u
al
i
ty
an
d
is
v
i
ta
l
in
p
r
o
d
u
c
t a
cc
e
p
ta
n
ce
f
o
r
co
n
s
u
m
er
s
[
4
8
].
3.
RE
S
E
ARCH
M
E
T
H
O
D
T
h
is
s
tu
d
y
em
p
lo
y
s
an
ex
p
er
i
m
en
tal
m
eth
o
d
o
lo
g
y
with
a
q
u
an
titativ
e
ap
p
r
o
ac
h
to
d
em
o
n
s
tr
ate
th
e
s
cien
tific
v
alu
e
an
d
m
ea
s
u
r
em
en
t
s
tr
en
g
th
o
f
th
e
r
esear
ch
d
e
s
ig
n
an
d
an
aly
s
is
.
T
h
e
r
esear
c
h
was
co
n
d
u
cted
in
f
o
u
r
co
astal
ar
ea
s
in
th
e
R
ep
u
b
lic
o
f
I
n
d
o
n
esia
th
at
h
av
e
m
an
y
f
is
h
in
g
g
r
o
u
p
s
:
Ku
lo
n
Pro
g
o
,
Pu
r
wer
ejo
,
B
an
tu
l,
an
d
Keb
u
m
en
(
Sp
ec
ial
R
eg
io
n
o
f
Yo
g
y
ak
ar
ta
an
d
C
en
tr
al
J
av
a
Pro
v
in
ce
)
.
T
h
e
s
tag
es
th
at
h
av
e
b
ee
n
ca
r
r
ied
o
u
t
in
clu
d
e
d
ata
co
llectio
n
,
id
ea
g
en
er
atio
n
,
d
ev
ice
d
esig
n
a
n
d
ca
lcu
latio
n
,
co
llectio
n
o
f
t
o
o
ls
an
d
m
ater
ials
,
d
ev
ice
m
an
u
f
ac
tu
r
in
g
,
tr
ials
,
d
ata
an
aly
s
is
,
an
d
p
er
f
o
r
m
a
n
ce
ev
alu
atio
n
.
Du
r
in
g
th
e
r
esear
ch
,
th
e
p
r
o
b
lem
s
with
tr
ad
itio
n
al
f
is
h
co
o
lin
g
tech
n
iq
u
es
wer
e
ex
p
lo
r
ed
b
y
co
n
d
u
ctin
g
i
n
ter
v
iews
with
f
is
h
er
m
en
in
f
o
u
r
d
if
f
er
en
t
f
is
h
i
n
g
v
illag
es.
I
n
ad
d
itio
n
,
th
e
r
e
s
ea
r
ch
er
s
s
ea
r
ch
ed
f
o
r
r
elev
an
t
m
ater
ials
f
r
o
m
tr
u
s
ted
s
o
u
r
ce
s
o
n
f
is
h
c
o
o
lin
g
tech
n
iq
u
es,
p
h
o
to
v
o
ltaic
ca
lcu
lati
o
n
s
,
m
an
u
f
ac
tu
r
in
g
tech
n
iq
u
es,
a
n
d
th
e
p
o
wer
g
en
er
ated
b
y
g
alv
an
ic
c
ells
.
I
n
th
e
s
ec
o
n
d
s
tag
e,
th
e
co
llected
d
a
ta
was
an
aly
ze
d
to
f
in
d
th
e
b
est
s
o
lu
tio
n
s
to
o
v
er
co
m
e
th
e
p
r
o
b
lem
s
.
T
h
ese
id
ea
s
wer
e
th
en
tr
an
s
f
o
r
m
ed
i
n
to
an
ap
p
r
o
p
r
iate
tech
n
o
lo
g
y
.
T
h
e
th
ir
d
s
tag
e
in
v
o
lv
e
d
d
esig
n
in
g
th
e
d
ev
ice
u
s
in
g
Au
to
d
esk
I
n
v
en
t
o
r
to
o
b
tain
th
e
o
p
tim
al
s
y
s
tem
d
esig
n
f
o
r
co
o
lin
g
f
is
h
.
T
h
e
d
esig
n
in
clu
d
e
d
a
s
o
lar
p
h
o
to
v
o
ltaic
as
a
s
o
u
r
ce
o
f
elec
tr
icity
f
r
o
m
th
e
s
u
n
lig
h
t,
an
d
g
alv
an
ic
c
ells
t
h
at
u
tili
ze
s
ea
wate
r
elec
tr
o
ly
t
es.
A
ch
ar
g
e
co
n
tr
o
ller
r
eg
u
l
ates
th
e
two
en
e
r
g
y
s
o
u
r
ce
s
to
p
r
ev
e
n
t
o
v
er
lo
a
d
in
g
an
d
e
n
s
u
r
e
t
h
at
th
e
elec
tr
ic
al
en
er
g
y
p
r
o
d
u
ce
d
m
ee
ts
th
e
r
eq
u
ir
em
en
ts
.
T
h
e
r
esu
ltin
g
en
er
g
y
is
s
to
r
ed
in
a
b
atter
y
,
wh
ich
p
o
wer
s
th
e
th
e
r
m
o
elec
tr
ic
co
o
ler
t
o
co
o
l t
h
e
f
is
h
in
th
e
co
o
l
b
o
x
.
T
h
e
d
ev
ice
cr
ea
tio
n
p
r
o
ce
s
s
s
ta
r
ts
with
an
aly
zin
g
th
e
tem
p
er
at
u
r
e
d
is
tr
ib
u
tio
n
in
t
h
e
r
o
o
m
to
d
eter
m
in
e
th
e
p
lace
m
en
t
an
d
q
u
an
tity
o
f
t
h
er
m
o
elec
tr
ic
co
o
ler
s
,
as
well
as
th
e
d
im
en
s
io
n
s
o
f
th
e
co
o
lin
g
r
o
o
m
.
Fo
llo
win
g
th
is
,
th
e
r
esear
ch
er
ca
lcu
lates
th
e
r
eq
u
i
r
ed
p
h
o
t
o
v
o
ltaic
p
o
w
er
an
d
b
atter
y
ca
p
ac
ity
.
On
ce
th
e
ca
lcu
latio
n
s
ar
e
f
in
is
h
ed
,
th
e
r
esear
ch
e
r
s
elec
ts
th
e
n
ec
ess
ar
y
t
o
o
ls
an
d
m
at
er
ials
b
ased
o
n
th
eir
p
r
ice
an
d
q
u
ality
.
E
s
s
en
tial
eq
u
ip
m
en
t
in
clu
d
es
s
o
ld
er
in
g
to
o
ls
,
s
cis
s
o
r
s
,
s
a
ws,
g
lu
e,
r
u
ler
s
,
h
am
m
er
s
,
an
d
n
ails
.
T
h
e
m
ater
ials
u
s
ed
i
n
m
an
u
f
ac
tu
r
in
g
th
e
c
o
o
l
b
o
x
c
o
n
s
is
t
o
f
s
o
lar
p
h
o
to
v
o
ltaics
f
o
r
p
o
wer
s
u
p
p
ly
,
a
c
h
ar
g
e
co
n
tr
o
ller
,
a
b
atter
y
f
o
r
en
er
g
y
s
to
r
ag
e,
a
T
E
C
th
e
r
m
o
elec
tr
ic
co
o
ler
f
o
r
en
er
g
y
co
n
v
er
s
io
n
,
a
h
ea
t
s
in
k
,
ca
b
les,
a
n
d
an
L
C
D
d
is
p
lay
f
o
r
m
o
n
ito
r
in
g
b
atter
y
ca
p
ac
ity
,
tem
p
er
atu
r
e
,
an
d
h
u
m
id
i
ty
.
T
h
is
s
tag
e
is
cr
itical
f
o
r
en
s
u
r
in
g
th
at
t
h
e
ap
p
r
o
p
r
iate
co
m
p
o
n
e
n
ts
an
d
t
o
o
ls
ar
e
ass
em
b
led
b
ef
o
r
e
m
o
v
in
g
f
o
r
war
d
with
t
h
e
m
an
u
f
a
ctu
r
in
g
p
r
o
ce
s
s
.
T
h
e
r
esear
ch
was
co
n
d
u
cted
to
d
esig
n
,
ass
em
b
le,
a
n
d
test
a
s
o
lar
-
p
o
wer
ed
co
o
l
b
o
x
d
e
v
ice.
T
h
e
d
ev
ic
e
was
d
esig
n
ed
b
y
in
teg
r
atin
g
s
o
lar
p
h
o
t
o
v
o
ltaics,
a
ch
a
r
g
e
co
n
tr
o
ller
,
b
atter
y
s
to
r
ag
e,
a
n
d
a
th
er
m
o
elec
tr
ic
co
o
ler
in
t
o
a
c
o
o
l
b
o
x
u
n
it.
T
h
e
m
an
u
f
ac
tu
r
in
g
p
r
o
ce
s
s
in
cl
u
d
ed
ass
em
b
lin
g
th
e
s
o
lar
p
a
n
els
an
d
c
o
n
tr
o
ller
,
co
n
s
tr
u
ctin
g
th
e
co
o
lin
g
ch
a
m
b
er
with
th
e
th
er
m
o
elec
tr
i
c
co
o
ler
a
n
d
h
ea
t
s
in
k
,
b
e
f
o
r
e
ass
em
b
lin
g
all
co
m
p
o
n
en
ts
.
T
h
e
d
e
v
ice
u
n
d
e
r
wen
t
two
tr
ials
-
a
lim
ited
la
b
tr
ial,
f
o
llo
wed
b
y
f
ield
tr
ials
wi
th
f
is
h
er
m
en
at
Glag
ah
,
J
atim
alan
g
,
B
ar
u
,
an
d
L
o
g
en
d
in
g
b
ea
ch
es
to
en
s
u
r
e
o
p
tim
al
f
u
n
ctio
n
in
g
o
f
th
e
c
o
m
p
o
n
en
ts
in
r
ea
l
-
wo
r
ld
co
n
d
itio
n
s
f
o
r
co
o
lin
g
t
h
e
ca
tch
.
Af
ter
war
d
,
a
d
etaile
d
p
er
f
o
r
m
an
ce
an
al
y
s
is
was
c
o
n
d
u
cte
d
,
in
clu
d
in
g
th
e
wo
r
k
in
g
s
y
s
tem
,
s
tab
ilit
y
,
tem
p
er
atu
r
e
r
ed
u
ctio
n
,
co
o
li
n
g
tim
e,
a
n
d
im
p
ac
t
o
n
f
is
h
q
u
ality
,
with
r
esu
lts
d
o
cu
m
e
n
ted
.
T
h
e
p
er
f
o
r
m
an
c
e
was
th
en
e
v
alu
ated
t
o
d
ete
r
m
in
e
if
t
h
e
d
e
v
ice
m
et
t
h
e
r
es
ea
r
ch
o
b
jectiv
es
f
o
r
cr
ea
tin
g
a
s
cien
tific
jo
u
r
n
al.
B
ased
o
n
th
e
e
v
alu
atio
n
,
th
e
r
esear
ch
e
r
w
o
u
ld
eith
er
p
r
o
ce
e
d
t
o
m
ak
e
a
s
cien
tific
r
ep
o
r
t
an
d
ar
ticle
if
d
ee
m
e
d
f
ea
s
ib
le
o
r
r
ep
air
an
d
r
ev
is
e
th
e
d
ev
ice
if
n
o
t,
a
f
ter
r
e
-
v
er
i
f
y
in
g
th
e
d
esig
n
an
d
ca
lcu
latio
n
s
.
Fin
ally
,
a
s
cien
tific
ar
ticle
was
cr
ea
ted
to
r
ep
o
r
t
th
e
d
etailed
r
esu
lts
f
r
o
m
im
p
lem
en
tin
g
th
e
d
ev
ice
,
with
all
ac
tiv
ities
d
o
cu
m
en
ted
th
r
o
u
g
h
p
h
o
to
s
an
d
v
id
eo
s
f
o
r
ar
ch
iv
in
g
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2088
-
8
6
9
4
I
n
t J Po
w
E
lec
&
Dr
i Sy
s
t
,
Vo
l.
1
5
,
No
.
4
,
Dec
em
b
er
20
2
4
:
2591
-
2
6
0
2
2594
4.
RE
SU
L
T
S AN
D
D
I
SCU
SS
I
O
N
4
.
1
.
Dev
ice
wo
rk
ing
princip
le
T
h
e
s
o
lar
p
h
o
to
v
o
ltaic
co
o
l
b
o
x
f
o
r
f
is
h
is
a
h
y
b
r
i
d
d
ev
ice
p
o
wer
ed
b
y
s
o
lar
en
er
g
y
,
u
tili
zin
g
th
e
Peltier
ef
f
ec
t
o
n
a
th
er
m
o
elec
tr
ic
co
o
ler
to
ch
ill
th
e
ca
u
g
h
t
f
is
h
.
T
h
e
d
esig
n
in
cl
u
d
es
a
f
is
h
s
to
r
ag
e
a
r
ea
(
co
o
lin
g
ch
am
b
er
)
with
a
th
er
m
o
elec
tr
ic
co
o
ler
elem
en
t,
a
b
atter
y
as t
h
e
DC
s
o
u
r
c
e,
an
d
a
c
h
ar
g
e
co
n
tr
o
ller
f
o
r
v
o
ltag
e
r
eg
u
latio
n
.
T
h
e
co
o
l
b
o
x
is
p
lace
d
o
n
a
wate
r
-
f
illed
b
lo
c
k
,
wh
er
e
s
ea
wate
r
g
u
ar
d
s
th
e
tem
p
er
atu
r
e
d
if
f
er
en
ce
ac
r
o
s
s
th
e
th
er
m
o
elec
tr
ic
co
o
ler
elem
en
ts
.
I
t
f
ea
tu
r
es
tem
p
er
atu
r
e,
h
u
m
id
ity
,
an
d
w
eig
h
t
s
en
s
o
r
s
f
o
r
tech
n
o
lo
g
ical
s
o
p
h
is
ticatio
n
.
An
elec
tr
ic
s
h
o
ck
s
y
s
tem
p
r
o
t
ec
ts
f
is
h
f
r
o
m
b
ac
ter
ia
lo
n
g
er
th
an
o
th
er
c
o
o
lin
g
d
ev
ices.
W
ith
a
r
ec
tan
g
u
lar
d
im
en
s
io
n
,
th
is
m
o
b
ile
c
o
o
l
b
o
x
allo
ws
f
is
h
er
m
en
a
n
d
f
is
h
v
en
d
o
r
s
to
r
ed
u
ce
p
r
eser
v
atio
n
c
o
s
ts
wh
ile
m
ain
tain
in
g
f
r
esh
n
ess
as sh
o
wn
in
Fig
u
r
e
1
.
T
h
e
co
o
l
b
o
x
is
im
p
lem
e
n
ted
o
n
a
t
r
ad
itio
n
al
f
is
h
in
g
b
o
at
as
s
h
o
wn
in
Fig
u
r
e
2
th
e
d
im
e
n
s
io
n
s
o
f
t
h
is
d
ev
ice
ar
e
9
2
×
50
×
2
8
ce
n
tim
eter
s
b
ec
au
s
e
it
ad
ju
s
ts
th
e
wid
th
an
d
h
eig
h
t
o
f
t
h
e
h
u
ll
o
f
tr
a
d
itio
n
al
f
is
h
in
g
b
o
ats
in
g
en
er
al.
T
h
e
s
o
lar
co
o
l
b
o
x
h
as
two
wo
r
k
in
g
s
y
s
tem
s
:
an
elec
tr
ic
s
h
o
ck
s
y
s
tem
an
d
a
s
o
lar
p
h
o
to
v
o
ltaic
+
th
er
m
o
elec
tr
ic
co
o
ler
s
y
s
tem
.
T
h
e
elec
tr
ic
s
h
o
ck
s
y
s
tem
f
ea
tu
r
es
a
f
is
h
s
h
o
ck
in
g
p
r
o
ce
s
s
u
s
in
g
a
2
0
0
0
V
elec
tr
ical
v
o
ltag
e
f
r
o
m
a
s
tep
-
u
p
tr
an
s
f
o
r
m
e
r
to
k
ill
g
e
r
m
s
an
d
in
h
ib
it
s
p
o
ilag
e,
as
s
h
o
wn
in
F
ig
u
r
e
3
.
Fo
llo
win
g
a
1
0
-
s
ec
o
n
d
s
h
o
ck
in
g
p
r
o
ce
s
s
,
th
e
f
is
h
u
n
d
er
g
o
es
co
o
lin
g
wi
th
in
a
s
o
lar
-
p
o
wer
ed
r
ef
r
ig
e
r
a
t
io
n
u
n
it
eq
u
ip
p
ed
with
a
Peltier
co
o
lin
g
s
y
s
tem
,
ef
f
ec
tiv
ely
p
r
e
v
en
tin
g
b
ac
ter
ia
l c
o
n
tam
in
atio
n
.
T
h
e
co
o
l
b
o
x
h
as
a
s
o
la
r
p
h
o
t
o
v
o
ltai
c
an
d
t
h
e
r
m
o
e
le
ct
r
ic
c
o
o
le
r
w
o
r
k
in
g
s
y
s
te
m
.
As
s
h
o
wn
i
n
Fig
u
r
e
4
,
i
t
a
b
s
o
r
b
s
s
u
n
l
ig
h
t
t
h
r
o
u
g
h
a
3
0
0
W
p
m
o
n
o
c
r
y
s
tal
li
n
e
s
o
la
r
p
h
o
t
o
v
o
l
tai
c
p
a
n
e
l,
c
o
n
v
e
r
ti
n
g
s
o
l
ar
e
n
e
r
g
y
in
t
o
el
ec
t
r
i
ca
l
e
n
e
r
g
y
t
o
p
o
w
e
r
th
e
c
o
o
l
b
o
x
.
A
c
h
a
r
g
e
c
o
n
t
r
o
ll
er
r
eg
u
l
at
es
t
h
e
p
o
we
r
g
en
er
ate
d
b
y
th
e
s
o
l
ar
c
ells
,
wh
i
ch
is
s
t
o
r
e
d
in
a
1
2
V
5
0
Ah
b
a
tte
r
y
.
T
h
is
s
to
r
e
d
p
o
w
er
ac
t
iv
at
es
t
h
e
T
E
C
1
-
1
2
7
1
0
t
h
er
m
o
el
ec
t
r
i
c
c
o
o
le
r
,
cr
ea
ti
n
g
a
t
em
p
e
r
a
tu
r
e
d
i
f
f
e
r
e
n
ce
b
etw
ee
n
t
h
e
tw
o
p
lat
es.
T
h
e
i
n
n
e
r
p
l
ate
f
a
ce
s
t
h
e
s
t
o
r
a
g
e
c
h
a
m
b
e
r
,
p
r
o
d
u
ci
n
g
d
is
t
r
i
b
u
te
d
c
o
l
d
t
em
p
er
at
u
r
e,
wh
i
le
th
e
o
u
te
r
p
l
ate
f
ac
es
a
h
ea
ts
i
n
k
.
Pa
r
t
o
f
th
e
h
e
atsi
n
k
is
s
u
b
m
e
r
g
ed
i
n
w
at
er
o
n
a
l
ar
g
e
b
lo
c
k
,
in
cr
ea
s
i
n
g
t
h
e
te
m
p
e
r
at
u
r
e
d
e
lta
b
etw
ee
n
t
h
e
th
er
m
o
el
ec
tr
i
c
c
o
o
l
er
'
s
o
u
t
e
r
a
n
d
i
n
n
e
r
s
i
d
es
.
I
f
th
e
o
u
ts
i
d
e
m
e
d
i
a
te
m
p
e
r
at
u
r
e
is
v
e
r
y
c
o
l
d
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at
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u
r
e
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o
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l
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ar
ts
Fig
u
r
e
2
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o
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lem
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atio
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Fig
u
r
e
3
.
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lectr
ic
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ck
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y
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tem
Fig
u
r
e
4
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So
lar
p
h
o
t
o
v
o
ltaic
a
n
d
th
er
m
o
elec
tr
ic
co
o
le
r
s
y
s
tem
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
t J Po
w
E
lec
&
Dr
i Sy
s
t
I
SS
N:
2088
-
8
6
9
4
Desig
n
s
ystem
a
n
d
p
erfo
r
ma
n
ce
a
n
a
lysi
s
o
f fis
h
s
to
r
a
g
e
b
o
x
b
y
u
tili
z
in
g
…
(
R
iz
a
l J
u
s
tia
n
S
etia
w
a
n
)
2595
4
.
2
.
Ca
lcula
t
io
ns
o
n dev
ice
m
a
nu
f
a
ct
uring
T
h
e
av
er
a
g
e
ca
tch
o
f
Glag
ah
,
J
atim
alan
g
,
B
ar
u
,
a
n
d
L
o
g
en
d
in
g
B
ea
ch
es
f
is
h
er
m
en
is
2
3
-
3
0
k
ilo
g
r
am
s
o
f
f
is
h
p
er
d
a
y
.
Usu
ally
,
th
e
f
i
s
h
ca
u
g
h
t
ar
e
s
k
ip
jack
tu
n
a,
b
an
y
ar
f
is
h
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m
ilk
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,
y
ello
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is
h
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o
m
f
r
et,
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d
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n
a
m
ac
k
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r
el.
Ho
wev
e
r
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th
e
m
ajo
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ity
o
f
th
e
f
is
h
ca
u
g
h
t
we
r
e
u
s
u
ally
d
o
m
in
ated
b
y
s
k
ip
j
ac
k
tu
n
a
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C
a
ka
la
n
g
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wh
ich
h
ad
a
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g
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h
o
f
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0
cm
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th
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m
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ick
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e
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s
o
f
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cm
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d
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a
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er
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t
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er
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h
o
f
600
-
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r
am
s
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Ass
u
m
in
g
t
h
e
f
is
h
ca
u
g
h
t
ar
e
o
f
th
e
s
am
e
s
ize,
it
ca
n
b
e
esti
m
ated
th
a
t
th
e
n
u
m
b
er
o
f
f
is
h
ca
u
g
h
t is ar
o
u
n
d
5
0
f
is
h
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Sk
ip
j
ac
k
tu
n
a
h
as
a
d
en
s
ity
o
f
ab
o
u
t 9
2
0
k
g
/m
3
,
s
o
th
e
v
o
lu
m
e
o
f
th
e
b
o
x
r
eq
u
ir
ed
is
0
.
0
3
2
6
1
m
3
.
B
ased
o
n
th
e
s
p
ec
if
icatio
n
s
o
f
th
e
co
o
l
b
o
x
es
s
o
ld
in
th
e
m
ar
k
et,
th
e
s
ize
o
f
a
f
is
h
b
o
x
th
at
is
s
u
f
f
icien
t
is
1
2
5
cm
l
o
n
g
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9
0
c
m
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d
6
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cm
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ig
h
o
r
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o
th
er
wo
r
d
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as
a
ca
p
ac
ity
o
f
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g
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h
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ased
o
n
ASHR
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p
r
o
d
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ct
lo
a
d
ca
lcu
latio
n
is
th
e
lo
a
d
r
eq
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ir
e
d
to
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ed
u
ce
th
e
tem
p
er
at
u
r
e
o
f
t
h
e
p
r
o
d
u
ct
(
f
is
h
)
,
th
e
n
th
at
it c
an
b
e
p
r
eser
v
ed
[
49
]
,
[
5
0
]
.
T
h
is
p
r
o
d
u
ct
lo
ad
ca
lcu
latio
n
u
s
es th
e
(
1
)
.
Q
fish
=
m
fish
. C
p
fish
.
▲
T
fish
Q
fish
=
(
3
0
)
×
(
3
,
5
5
0
)
×
(
2
7
.
8
7
-
0)
Q
fish
=
2
,
9
6
8
.
1
k
J
Q
product
=
ℎ
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product
=
2
,
96
8
.
1
5
×
3600
=
0
.
1
6
4
8
9
4
4
k
W
Q
product
=
1
6
4
.
8
9
4
4
W
/h
o
u
r
(
1
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Av
er
ag
e
ca
tch
o
f
f
is
h
p
er
d
ay
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3
0
k
g
,
av
e
r
ag
e
f
is
h
in
g
tim
e
p
er
d
a
y
is
5
h
o
u
r
s
.
T
h
en
,
th
e
C
p
f
is
h
s
k
ip
jack
tu
n
a
(
c
a
k
a
la
n
g
)
is
3
5
5
0
J
/Kg
°
K.
Av
er
ag
e
Sea
tem
p
e
r
atu
r
e
in
Yo
g
y
ak
ar
ta
is
2
7
.
8
7
°
C
.
B
ef
o
r
e
cr
ea
t
in
g
th
e
d
ev
ice,
r
eq
u
ir
e
d
to
ca
lcu
late
tr
an
s
m
is
s
io
n
lo
ad
.
T
r
an
s
m
is
s
io
n
lo
ad
is
a
lo
ad
ca
u
s
ed
b
y
h
ea
t
lo
s
s
e
s
th
at
o
cc
u
r
in
co
o
l
b
o
x
walls.
C
o
o
l
B
o
x
h
as
d
im
en
s
io
n
s
o
f
1
2
5
cm
lo
n
g
,
9
0
cm
wid
e,
an
d
6
0
cm
h
ig
h
.
T
h
e
wall
o
f
th
e
co
o
l
b
o
x
is
m
ad
e
f
r
o
m
a
co
m
b
in
ati
o
n
o
f
p
o
l
y
s
ty
r
en
e
(
p
s
)
lay
er
s
,
alu
m
in
u
m
f
o
il
(
af
)
,
p
last
ic
in
s
u
lato
r
(
p
i)
,
an
d
wo
o
d
(
w)
.
T
h
e
h
ea
t
lo
s
s
co
n
s
is
ts
o
f
t
h
e
b
o
tto
m
s
id
e,
to
p
s
id
e,
r
ig
h
t
s
id
e,
lef
t
s
id
e,
f
r
o
n
t
s
id
e,
an
d
b
ac
k
s
id
e.
R
eg
ar
d
in
g
th
e
o
u
ter
wall
o
f
c
o
o
l
b
o
x
,
t
h
e
b
o
tto
m
,
r
ig
h
t,
lef
t,
f
r
o
n
t,
an
d
b
ac
k
s
id
e
ar
e
co
v
e
r
ed
wi
th
p
o
ly
s
ty
r
e
n
e
(
p
s
)
,
alu
m
in
u
m
f
o
il
(
af
)
,
p
last
ic
in
s
u
lato
r
(
p
i)
,
an
d
wo
o
d
(
w)
.
Me
an
wh
ile,
th
e
to
p
is
co
v
er
e
d
b
y
p
o
ly
s
ty
r
e
n
e
(
p
s
)
,
alu
m
in
u
m
f
o
il
(
af
)
,
a
n
d
p
last
ic
in
s
u
lato
r
(
p
i)
.
Hea
t
tr
a
n
s
f
er
b
y
co
n
v
ec
tio
n
is
n
eg
lig
i
b
le
b
e
ca
u
s
e
th
er
e
is
n
o
air
m
o
v
in
g
o
n
th
e
wall
s
id
e
o
f
th
i
s
co
o
l
b
o
x
.
Fu
r
th
e
r
m
o
r
e
,
th
e
v
alu
e
o
f
h
ea
t
lo
s
s
f
r
o
m
ea
c
h
w
all
ca
n
b
e
ass
u
m
ed
b
y
th
e
ca
lcu
latio
n
s
in
(
2
)
an
d
(
3
)
.
-
T
o
p
s
id
e
h
ea
t lo
s
s
1
1
=
+
+
1
1
=
2
,
1
10
−
2
3
,
3
10
−
2
+
2
10
−
4
180
+
3
10
−
4
0
,
15
1
1
=
1
.
5
6
6
m
2
K/W
U
=
0
.
6
3
8
5
w/(
m
2
K)
(
2
)
-
B
o
tto
m
,
r
ig
h
t,
lef
t,
f
r
o
n
t,
an
d
b
eh
in
d
h
ea
t lo
s
s
1
1
=
+
+
+
1
1
=
2
,
1
10
−
2
3
,
3
10
−
2
+
2
10
−
4
180
+
3
10
−
4
0
,
15
+
4
10
−
3
0
,
16
1
1
=
1
.
5
0
7
4
m
2
K/W
U
=
0
.
6
6
3
3
w/(
m
2
K)
(
3
)
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2088
-
8
6
9
4
I
n
t J Po
w
E
lec
&
Dr
i Sy
s
t
,
Vo
l.
1
5
,
No
.
4
,
Dec
em
b
er
20
2
4
:
2591
-
2
6
0
2
2596
T
h
e
am
b
ien
t
tem
p
er
atu
r
e
o
f
t
h
e
co
astal
e
n
v
ir
o
n
m
en
t
is
3
8
°
C
,
wh
ile
th
e
s
ea
tem
p
er
atu
r
e
i
s
2
7
.
8
7
°
C
an
d
th
e
s
k
ip
jack
tu
n
a
(
c
a
ka
la
n
g
)
tem
p
er
atu
r
e
is
2
7
°
C
.
T
h
en
,
th
e
to
tal
tr
an
s
m
is
s
io
n
lo
ad
f
r
o
m
ea
ch
s
id
e
ca
n
b
e
s
ee
n
in
(
4
)
-
(
7
)
.
-
T
o
p
s
id
e
Q
top
= U
1
.A
top
.
(
T
ambient
-
T
fish
)
Q
top
=
0
.
6
3
8
5
×
(
1
.
2
5
×
0
.
9
)
×
(
3
8
-
2
7
)
Q
top
=
0
.
6
3
8
5
×
(
1
.
1
2
5
)
×
(
1
1
)
Q
top
=
8
.
6
4
W
(
4
)
-
B
o
tto
m
s
id
e
Q
bottom
= U
2
.A
bottom
.
(
T
sea
-
T
fish
)
Q
bottom
=
0
.
6
6
3
3
×
(
1
.
2
5
×
0
.
9
)
×
(
2
7
.
8
7
-
2
7
)
Q
bottom
=
0
.
6
6
3
3
×
(
1
.
1
2
5
)
×
(
0
.
8
7
)
Q
bottom
=
0
.
6
5
W
(
5
)
-
R
ig
h
t a
n
d
lef
t sid
e
Q
right
&
left
= U
2
.A
right/left
.
(
T
ambient
-
T
fish
)
.
2
Q
right
&
left
=
0
.
6
6
3
3
×
(
0
.
6
×
0
.
9
)
×
(
3
8
-
2
7
)
x
2
Q
right
&
left
=
0
.
6
6
3
3
×
(
0
.
5
4
)
×
(
1
1
)
×
2
Q
right
&
left
=
7
.
8
8
W
(
6
)
-
Fro
n
t a
n
d
b
eh
in
d
s
id
e
Q
front
&
behind
= U
2
.A
front/behin
d
.
(
T
ambient
-
T
fish
)
.
2
Q
front
&
behind
=
0
.
6
6
3
3
×
(
1
.
2
5
×
0
.
6
)
×
(
3
8
-
2
7
)
×
2
Q
front
&
behind
=
0
.
6
6
3
3
×
(
0
.
7
5
)
×
(
1
1
)
×
2
Q
front
&
behind
=
1
1
.
0
5
W
(
7
)
B
ased
o
n
th
e
ca
lcu
latio
n
s
th
a
t
h
av
e
b
ee
n
c
o
n
d
u
cted
,
th
e
n
ad
d
u
p
all
th
e
lo
ad
s
ac
co
r
d
in
g
to
(
8
)
to
b
ec
o
m
e
th
e
t
o
tal
o
f
tr
a
n
s
m
is
s
i
o
n
lo
ad
.
Q
transmission
= Q
top
+ Q
bottom
+
Q
ri
ght
&
left
+ Q
front
&
behind
Q
transmission
=
8
.
6
4
+
0
.
6
5
+
7
.
8
8
+
1
1
.
0
5
Q
transmission
=
2
8
.
2
2
W
(
8
)
Fu
r
th
er
m
o
r
e
,
ca
lcu
latio
n
s
r
elate
d
to
th
e
in
f
iltra
tio
n
lo
ad
o
n
t
h
e
co
o
l
b
o
x
d
ev
ice
also
n
ee
d
to
b
e
co
n
d
u
cted
.
T
h
e
in
f
iltra
tio
n
lo
ad
is
th
e
lo
a
d
ca
u
s
ed
b
y
th
e
s
ee
p
ag
e
o
f
h
ea
t
in
to
th
e
co
o
lin
g
c
h
am
b
er
.
T
h
is
s
ee
p
ag
e
o
cc
u
r
s
d
u
e
to
air
ex
ch
a
n
g
e
w
h
en
t
h
e
co
o
l
b
o
x
is
o
p
e
n
ed
[
5
1
]
.
T
h
e
air
tem
p
er
atu
r
e
in
th
e
co
o
l
b
o
x
is
T
R
=
0
°
C
with
a
r
elativ
e
h
u
m
id
ity
o
f
9
5
%
an
d
h
as
an
e
n
th
alp
y
o
f
h
U
,
R
8
.
9
9
Kj/k
g
.
O
u
ts
id
e
air
tem
p
er
atu
r
e
T
U
=
3
8
°
C
with
a
r
elativ
e
h
u
m
id
ity
o
f
4
5
%
an
d
en
th
al
p
y
h
U
8
6
.
7
k
J
/k
g
.
Nex
t,
th
e
v
o
lu
m
e
o
f
t
h
e
co
o
l
b
o
x
(
V
cb
)
is
0
.
6
7
5
m
3
b
ec
au
s
e
it
h
as
1
2
5
cm
l
o
n
g
,
9
0
cm
wid
e,
an
d
6
0
cm
h
ig
h
with
an
air
d
en
s
it
y
o
f
1
.
3
4
k
g
/m
3
.
T
h
e
n
u
m
b
er
o
f
air
ex
c
h
an
g
es p
e
r
d
ay
(
n
)
ca
n
b
e
ca
lcu
lated
b
y
(
9
)
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
t J Po
w
E
lec
&
Dr
i Sy
s
t
I
SS
N:
2088
-
8
6
9
4
Desig
n
s
ystem
a
n
d
p
erfo
r
ma
n
ce
a
n
a
lysi
s
o
f fis
h
s
to
r
a
g
e
b
o
x
b
y
u
tili
z
in
g
…
(
R
iz
a
l J
u
s
tia
n
S
etia
w
a
n
)
2597
n
=
3
×
V
cb
n
=
3
×
0
.
6
7
5
n
=
2
.
0
2
5
≈
2
tim
es
(
9
)
T
h
e
am
o
u
n
t o
f
in
f
iltra
tio
n
lo
a
d
ca
n
b
e
ca
lcu
lated
b
y
th
e
f
o
r
m
u
la
in
(
10
)
.
Q
infiltration
=
,
.
.
(
ℎ
−
ℎ
,
)
24
3600
Q
infiltration
=
1
.
34
×
0
.
675
×
(
86
.
7
−
8
.
99
)
×
2
×
1000
66
,
400
Q
infiltration
=
140
,
577
66
,
400
Q
infiltration
=
2
.
1
1
7
1
W
(
1
0
)
T
h
e
f
in
al
ca
lc
u
latio
n
r
e
q
u
ir
e
d
is
th
e
to
tal
s
y
s
tem
lo
s
s
o
n
co
o
l
b
o
x
d
ev
ice.
T
o
tal
s
y
s
tem
lo
s
s
is
g
en
er
ated
b
y
ca
lcu
latin
g
to
tal
p
r
o
d
u
ct
lo
ad
,
tr
an
s
m
is
s
io
n
lo
a
d
,
an
d
in
f
iltra
tio
n
l
o
ad
.
T
h
e
eq
u
atio
n
r
elate
d
t
o
th
is
ca
lcu
latio
n
ca
n
b
e
in
(
11
)
.
Q
system
loss
= Q
product
+ Q
t
r
a
n
sm
i
ss
i
o
n
+ Q
infiltration
(
1
1
)
Q
s
ys
tem
los
s
=
1
6
4
.
8
9
4
4
+
2
8
.
2
2
+
2
.
1
1
7
1
=
1
9
5
.
2
3
1
5
W
B
ased
o
n
th
e
ca
lcu
latio
n
,
th
e
t
o
tal
s
y
s
tem
lo
s
s
i
s
1
9
5
.
2
3
1
5
W
.
Fu
r
th
er
m
o
r
e,
th
r
ee
th
er
m
o
elec
tr
ic
co
o
ler
s
with
s
p
ec
if
icatio
n
s
o
f
1
2
V
an
d
6
A
with
a
t
o
tal
p
o
wer
o
f
2
2
8
W
(
7
6
W
/u
n
it)
ar
e
u
s
ed
.
T
h
is
p
o
w
er
is
ab
le
t
o
h
an
d
le
co
o
l b
o
x
lo
ad
p
o
wer
.
4
.
3
.
P
o
wer
g
ener
a
t
ed
I
n
T
ab
le
1
,
it
is
f
o
u
n
d
t
h
at
th
e
e
lectr
ical
p
o
wer
p
r
o
d
u
ce
d
b
y
s
o
lar
p
h
o
to
v
o
ltaic
at
f
o
u
r
d
if
f
er
e
n
t
r
esear
ch
lo
ca
tio
n
s
d
o
es
n
o
t
s
h
o
w
s
ig
n
i
f
ican
t
d
if
f
er
e
n
ce
s
.
T
h
e
t
r
ial
was
co
n
d
u
cted
o
n
f
o
u
r
d
if
f
er
en
t
b
ea
ch
es,
s
u
ch
as
Glag
ah
B
ea
ch
,
J
atim
alan
g
B
e
ac
h
,
B
ar
u
B
ea
ch
,
an
d
L
o
g
e
n
d
in
g
B
ea
ch
wh
ich
ar
e
i
n
f
o
u
r
d
if
f
er
en
t
cities.
T
h
e
s
o
lar
p
h
o
to
v
o
ltaic
p
o
wer
d
ata
wer
e
tak
en
d
u
r
in
g
th
e
tr
ial
b
y
co
n
d
u
ctin
g
o
b
s
er
v
atio
n
s
an
d
p
o
wer
ca
lcu
latio
n
s
f
o
r
n
in
e
h
o
u
r
s
f
r
o
m
m
o
r
n
in
g
to
ev
en
in
g
with
th
e
d
etail
7
AM
to
4
PM
(
GM
T
+7
)
in
s
u
n
n
y
wea
th
er
co
n
d
itio
n
s
to
g
et
th
e
h
ig
h
est
p
o
wer
r
esu
l
ts
th
at
ca
n
b
e
p
r
o
d
u
ce
d
b
y
s
o
lar
p
h
o
t
o
v
o
ltaic.
Data
was
co
llected
u
s
in
g
a
s
o
la
r
co
o
l b
o
x
d
e
v
ice
with
a
3
0
0
W
p
s
o
lar
p
h
o
to
v
o
ltaic,
y
ield
in
g
an
av
er
ag
e
o
u
tp
u
t o
f
2
5
2
7
.
2
w
atts
p
er
d
ay
.
T
ab
le
1
.
C
alcu
latio
n
o
f
s
o
lar
p
h
o
to
v
o
ltaic
p
o
wer
g
e
n
er
ated
o
n
co
o
l
b
ox
Ti
me
(
h
o
u
r
)
P
o
w
e
r
(
w
a
t
t
)
G
l
a
g
a
h
B
e
a
c
h
Jat
i
mal
a
n
g
B
e
a
c
h
B
a
r
u
B
e
a
c
h
Lo
g
e
n
d
i
n
g
B
e
a
c
h
0
7
.
0
0
A
M
1
1
7
.
9
1
1
6
.
1
1
1
7
.
5
1
1
8
0
8
.
0
0
A
M
1
2
7
.
7
1
2
7
.
4
1
2
8
.
1
1
2
8
0
9
.
0
0
A
M
2
6
1
.
8
2
6
1
.
3
2
6
0
2
6
2
.
7
1
0
.
0
0
A
M
2
7
8
2
7
8
.
4
2
7
8
.
5
2
7
9
1
1
.
0
0
A
M
2
8
9
2
9
0
2
9
0
2
8
9
0
0
.
0
0
P
M
2
9
7
2
9
6
.
6
2
9
7
2
9
6
0
1
.
0
0
P
M
2
9
7
2
9
5
2
9
7
2
9
6
.
4
0
2
.
0
0
P
M
2
9
3
2
9
3
.
9
2
9
4
2
9
1
.
3
0
3
.
0
0
P
M
2
8
8
2
9
0
2
8
9
.
2
2
8
8
0
4
.
0
0
P
M
2
7
7
.
2
2
7
8
.
3
2
7
7
.
4
2
7
8
To
t
a
l
p
o
w
e
r
(
w
a
t
t
)
2
,
5
2
6
.
6
2
,
5
2
7
2
,
5
2
8
.
7
2
,
5
2
6
.
4
A
v
e
r
a
g
e
(
w
a
t
t
)
2
,
5
2
7
.
2
T
h
e
av
er
a
g
e
e
n
er
g
y
g
e
n
er
ate
d
u
n
d
er
s
u
n
n
y
co
n
d
itio
n
s
am
o
u
n
ts
to
2
,
5
2
7
.
2
watts.
T
h
is
en
er
g
y
is
u
tili
ze
d
to
p
o
wer
th
r
ee
th
e
r
m
o
elec
tr
ic
co
o
le
r
s
,
co
llectiv
e
ly
co
n
s
u
m
i
n
g
2
2
8
watts,
as
well
as
s
u
p
p
o
r
tin
g
co
m
p
o
n
en
ts
f
o
r
a
1
0
-
h
o
u
r
d
u
r
atio
n
.
T
h
e
e
n
er
g
y
o
u
tp
u
t
d
u
r
in
g
d
ay
li
g
h
t
h
o
u
r
s
p
r
o
v
es
am
p
le
f
o
r
f
is
h
er
m
e
n
p
r
ep
ar
in
g
to
v
e
n
tu
r
e
o
u
t
to
s
ea
d
u
r
in
g
th
e
n
ig
h
t.
No
n
et
h
eless
,
in
th
e
e
v
en
t
o
f
r
ain
th
r
o
u
g
h
o
u
t
th
e
d
ay
r
esu
ltin
g
in
an
em
p
t
y
b
atter
y
,
f
is
h
er
m
en
as th
e
u
s
er
m
u
s
t c
h
ar
g
e
elec
tr
icity
f
r
o
m
th
e
g
r
id
t
o
r
ec
h
a
r
g
e
it.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2088
-
8
6
9
4
I
n
t J Po
w
E
lec
&
Dr
i Sy
s
t
,
Vo
l.
1
5
,
No
.
4
,
Dec
em
b
er
20
2
4
:
2591
-
2
6
0
2
2598
4
.
4
.
E
nerg
y
co
ns
um
ptio
n
Fig
u
r
e
5
d
em
o
n
s
tr
ates
th
at
th
e
co
o
l
b
o
x
d
ev
ice
with
o
u
t
a
t
em
p
er
atu
r
e
c
o
n
tr
o
l
s
y
s
tem
ca
n
o
n
ly
b
e
ac
tiv
e
f
o
r
5
3
0
m
in
u
tes
b
ased
o
n
th
e
test
r
esu
lts
u
s
in
g
an
d
with
o
u
t
u
s
in
g
th
e
tem
p
er
atu
r
e
c
o
n
tr
o
l
s
y
s
tem
.
T
h
is
lim
itatio
n
ar
is
es
b
ec
au
s
e
em
p
l
o
y
in
g
th
e
th
e
r
m
o
elec
tr
ic
c
o
o
le
r
(
T
E
C
)
with
o
u
t
co
n
tr
o
l
lea
d
s
th
e
s
y
s
tem
to
eith
er
co
o
l
b
elo
w
f
r
ee
zi
n
g
(
a
p
p
r
o
x
im
ately
-
4
°C
)
o
r
o
p
e
r
ate
at
m
ax
i
m
u
m
p
o
wer
.
C
o
n
v
er
s
ely
,
wh
e
n
th
e
co
n
tr
o
l
s
y
s
tem
is
im
p
lem
en
ted
,
th
e
d
ev
ice
c
an
en
d
u
r
e
f
o
r
7
0
0
m
in
u
tes,
a
s
th
e
T
E
C
is
s
o
lely
en
g
ag
ed
in
m
ain
tain
in
g
th
e
r
ef
er
en
ce
tem
p
er
at
u
r
e.
I
f
th
e
tem
p
er
atu
r
e
f
alls
with
in
th
e
s
p
ec
if
ied
r
an
g
e,
th
e
th
er
m
o
elec
tr
ic
co
m
p
o
n
en
t
au
to
m
atica
lly
d
ea
ctiv
ates.
T
h
is
co
o
lin
g
d
u
r
atio
n
p
r
o
v
es
to
b
e
s
u
f
f
icien
t
f
o
r
b
ea
ch
s
id
e
f
is
h
er
m
en
to
p
r
eser
v
e
th
eir
ca
tch
d
u
r
in
g
s
tan
d
a
r
d
f
is
h
in
g
ex
p
ed
itio
n
s
.
C
o
n
s
eq
u
en
tly
,
th
e
s
y
s
tem
u
s
in
g
tem
p
er
atu
r
e
c
o
n
tr
o
l
ca
n
r
u
n
u
n
in
ter
r
u
p
ted
ly
f
o
r
o
v
er
1
0
h
o
u
r
s
.
T
h
is
r
esu
lt
is
also
b
etter
th
an
th
e
im
p
lem
en
tatio
n
o
f
co
n
v
en
tio
n
a
l
ice
th
er
m
o
s
th
at
u
s
e
ice
cu
b
e
s
.
Fig
u
r
e
5
p
r
o
v
id
es
a
co
m
p
a
r
is
o
n
b
etwe
en
th
e
d
e
v
i
ce
an
d
a
c
o
n
v
e
n
t
io
n
al
ice
th
er
m
o
s
.
C
o
o
l
b
o
x
d
e
v
ices
eq
u
ip
p
ed
with
tem
p
er
atu
r
e
co
n
tr
o
l
ex
ce
l
in
m
ain
tain
in
g
a
r
ef
er
en
ce
tem
p
er
at
u
r
e
r
an
g
e
o
f
4
°C
to
5
°C
.
I
n
co
n
tr
ast,
tr
ad
itio
n
al
ice
f
lask
s
ca
n
o
n
ly
ac
h
iev
e
tem
p
er
atu
r
e
s
as
lo
w
a
s
1
3
°C
.
T
h
ese
f
in
d
in
g
s
af
f
ir
m
th
at
th
e
C
o
o
l
B
o
x
,
in
teg
r
ate
d
with
tem
p
er
atu
r
e
c
o
n
tr
o
l,
em
er
g
es
as th
e
m
o
s
t e
f
f
ec
tiv
e
an
d
ef
f
ic
ien
t d
ev
ice.
Fig
u
r
e
5
.
C
o
m
p
a
r
is
o
n
o
f
en
er
g
y
co
n
s
u
m
p
tio
n
f
o
r
s
o
lar
C
o
o
l Bo
x
with
an
d
with
o
u
t te
m
p
er
atu
r
e
co
n
tr
o
l
4
.
5
.
T
em
pera
t
ure
re
g
re
s
s
io
n
Var
io
u
s
m
eth
o
d
s
ar
e
em
p
lo
y
ed
to
in
cr
ea
s
e
th
e
q
u
ality
v
alu
e
o
f
th
e
f
is
h
b
y
co
n
tr
o
lli
n
g
s
to
r
ag
e
co
n
d
itio
n
s
.
Sin
ce
tem
p
er
atu
r
e
is
th
e
p
r
im
ar
y
f
ac
to
r
th
at
af
f
ec
ts
th
e
v
alu
e
o
f
th
e
ca
tch
,
it
is
ess
en
tial
to
in
v
esti
g
ate
co
n
tr
o
lled
tem
p
er
at
u
r
e.
Fis
h
er
m
en
d
o
n
o
t
n
ee
d
ex
ce
s
s
iv
ely
l
o
w
o
r
f
r
ee
zi
n
g
tem
p
er
atu
r
es w
h
en
s
to
r
in
g
t
h
e
f
is
h
th
ey
ca
tch
at
s
ea
.
T
h
eir
m
ain
g
o
al
is
to
co
o
l
th
e
f
is
h
to
in
h
ib
it
b
ac
ter
ial
g
r
o
wth
an
d
p
r
eser
v
e
its
f
r
esh
n
ess
b
ef
o
r
e
b
r
in
g
in
g
it
to
th
e
co
astal
ar
ea
o
r
m
ar
k
et.
T
h
e
f
is
h
t
h
ey
s
ell
ar
e
f
r
esh
f
is
h
,
n
o
t
f
r
o
ze
n
f
is
h
[5
2
]
.
Fre
s
h
f
is
h
is
d
ee
m
ed
to
p
o
s
s
ess
h
ig
h
er
q
u
a
lity
in
th
e
m
ar
k
et
co
m
p
ar
e
d
to
f
r
o
ze
n
f
is
h
,
as
f
r
o
ze
n
s
to
r
ag
e
ca
n
d
im
in
is
h
th
e
p
r
o
tein
q
u
ality
o
f
f
is
h
d
u
e
to
d
en
atu
r
atio
n
[
5
3
]
.
Pre
v
io
u
s
s
tu
d
ies
in
d
icate
th
at
f
r
ee
zin
g
f
is
h
r
esu
lts
in
s
h
o
r
t
-
ter
m
p
h
y
s
ical
ch
an
g
es,
en
c
o
m
p
ass
in
g
weig
h
t
lo
s
s
,
co
lo
r
alter
ati
o
n
,
an
d
s
tr
u
ct
u
r
al
m
o
d
if
icatio
n
s
in
d
u
ce
d
b
y
th
e
f
o
r
m
atio
n
o
f
ice
cr
y
s
tals
[
5
4
]
,
[
5
5
]
.
Pre
s
er
v
in
g
f
is
h
f
r
esh
n
ess
ca
n
b
e
ac
h
iev
ed
th
r
o
u
g
h
r
ef
r
ig
er
ated
s
to
r
a
g
e
with
in
tem
p
er
atu
r
es
r
an
g
in
g
f
r
o
m
0
°C
to
4
°C
[
5
6
]
,
[
5
7
]
.
Oth
er
r
esear
ch
s
u
g
g
ests
th
at
s
to
r
in
g
f
i
s
h
at
5
°C
is
also
s
u
f
f
icien
t
to
m
ain
tain
f
r
e
s
h
n
ess
[
58
]
,
[
59
]
.
Acc
o
r
d
in
g
to
r
ef
er
en
ce
s
o
n
f
r
esh
f
is
h
,
r
e
s
ea
r
ch
er
s
ty
p
ically
s
tip
u
late
a
r
ef
er
en
ce
tem
p
er
at
u
r
e
r
an
g
e
o
f
0
-
5
°C
.
T
h
e
o
b
jectiv
e
o
f
e
v
alu
atin
g
th
e
tem
p
er
atu
r
e
co
m
p
ar
is
o
n
th
e
co
o
l
b
o
x
with
tem
p
e
r
atu
r
e
co
n
tr
o
l,
c
o
o
l
b
o
x
with
o
u
t
tem
p
er
atu
r
e
c
o
n
tr
o
l,
an
d
co
n
v
en
tio
n
al
ice
th
er
m
o
s
is
to
ass
e
s
s
th
e
d
ev
ice
'
s
ef
f
e
ctiv
en
ess
in
co
o
lin
g
f
is
h
,
aim
in
g
to
p
r
eser
v
e
th
e
f
r
esh
n
ess
an
d
q
u
ality
o
f
th
e
f
is
h
ca
p
tu
r
ed
b
y
f
is
h
er
m
en
.
I
n
t
h
e
ex
p
er
im
en
t
,
two
v
ar
iab
les
wer
e
c
o
n
s
id
er
ed
:
te
m
p
er
atu
r
e,
m
o
n
ito
r
ed
with
a
t
em
p
er
atu
r
e
s
en
s
o
r
,
a
n
d
co
o
lin
g
s
p
ee
d
,
esti
m
ated
b
y
o
b
s
er
v
in
g
elap
s
ed
tim
e
u
s
in
g
a
tim
er
.
Fig
u
r
e
6
illu
s
tr
ates
th
e
g
r
a
p
h
d
e
p
ictin
g
th
e
ex
p
e
r
im
en
tal
r
esu
lts
.
T
h
e
m
ax
im
u
m
tem
p
er
atu
r
e
ac
h
iev
ab
le
b
y
a
C
o
o
l
B
o
x
d
ev
ice
wi
th
o
u
t
u
tili
zin
g
tem
p
er
atu
r
e
co
n
tr
o
l
is
-
4
°C
.
T
h
e
r
esear
ch
r
esu
lts
also
s
h
o
w
th
at
u
s
in
g
a
co
n
v
en
tio
n
al
ice
th
er
m
o
s
f
illed
with
ice
c
u
b
es
ca
n
o
n
l
y
r
ea
ch
a
tem
p
er
atu
r
e
as
lo
w
as
1
3
°C
.
T
h
is
tem
p
er
atu
r
e
r
ed
u
ctio
n
d
o
es
n
o
t
r
ea
ch
th
e
r
ef
e
r
en
ce
tem
p
er
atu
r
e
s
o
it
is
n
o
t
en
o
u
g
h
to
m
ai
n
tain
th
e
f
is
h
’
s
f
r
esh
n
ess
.
B
ased
o
n
th
ese
ex
p
er
im
e
n
t
test
s
,
r
esear
ch
er
s
estab
lis
h
ed
a
b
e
n
ch
m
ar
k
tem
p
er
atu
r
e
r
a
n
g
e
o
f
4
–
5
°C
to
r
eg
u
late
th
e
o
p
er
atio
n
o
f
th
e
c
o
o
l b
o
x
d
ev
ice.
Sin
ce
th
e
d
e
v
i
ce
'
s
tem
p
er
atu
r
e
h
as th
e
p
o
ten
t
ial
to
d
i
p
b
el
o
w
th
e
f
r
ee
zin
g
p
o
in
t
(
b
el
o
w
0
°C
)
,
t
h
e
im
p
lem
e
n
ta
tio
n
o
f
a
tem
p
e
r
atu
r
e
c
o
n
tr
o
l
m
ec
h
a
n
is
m
b
ec
o
m
es
ess
en
tial.
T
o
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
t J Po
w
E
lec
&
Dr
i Sy
s
t
I
SS
N:
2088
-
8
6
9
4
Desig
n
s
ystem
a
n
d
p
erfo
r
ma
n
ce
a
n
a
lysi
s
o
f fis
h
s
to
r
a
g
e
b
o
x
b
y
u
tili
z
in
g
…
(
R
iz
a
l J
u
s
tia
n
S
etia
w
a
n
)
2599
m
ain
tain
th
e
r
e
f
er
en
ce
tem
p
er
a
tu
r
e
s
tab
le
with
in
th
e
r
a
n
g
e
o
f
0
–
5
°C
,
th
e
c
o
o
l
b
o
x
d
ev
ice
e
m
p
lo
y
s
an
a
u
to
m
atic
tem
p
er
atu
r
e
m
an
ag
em
e
n
t
s
y
s
tem
.
T
h
is
tech
n
iq
u
e
n
o
t
o
n
ly
c
o
n
s
er
v
es
en
er
g
y
b
u
t
also
en
s
u
r
es
th
e
f
r
esh
n
ess
o
f
th
e
f
is
h
b
y
p
r
ev
en
tin
g
f
r
ee
zi
n
g
an
d
m
ai
n
tain
in
g
th
e
d
esire
d
tem
p
er
atu
r
e.
T
h
e
tem
p
e
r
atu
r
e
s
en
s
o
r
co
n
tin
u
o
u
s
ly
m
o
n
ito
r
s
th
e
s
to
r
ag
e
r
o
o
m
,
an
d
o
n
ce
it
d
etec
ts
a
tem
p
e
r
atu
r
e
with
in
th
e
r
ef
er
en
ce
r
an
g
e
o
f
0
-
5
°C
,
th
e
en
e
r
g
y
s
u
p
p
ly
to
th
e
th
er
m
o
elec
tr
ic
s
y
s
tem
is
au
to
m
atica
lly
cu
t
o
f
f
.
T
h
is
s
y
s
tem
ca
n
s
av
e
en
er
g
y
b
y
n
o
t
n
ee
d
i
n
g
to
b
e
ac
tiv
e
co
n
tin
u
o
u
s
ly
,
m
ain
tain
in
g
s
to
r
ag
e
tem
p
er
atu
r
e
s
tab
le
in
th
e
r
ef
er
en
ce
tem
p
er
atu
r
e.
T
h
en
,
th
e
d
ev
ice
ca
n
u
s
e
en
er
g
y
f
r
o
m
th
e
b
atter
y
f
o
r
m
o
r
e
th
an
1
7
0
m
in
u
tes
th
an
th
e
d
ev
ice
w
ith
o
u
t
tem
p
er
atu
r
e
co
n
tr
o
l.
C
o
n
v
er
s
ely
,
if
th
e
te
m
p
er
atu
r
e
s
u
r
p
ass
es
5
°C
,
th
e
en
er
g
y
s
u
p
p
ly
to
th
e
th
e
r
m
o
elec
tr
ic
co
o
ler
is
au
to
m
atica
lly
ac
tiv
ated
.
Fig
u
r
e
6
.
C
o
m
p
a
r
is
o
n
o
f
en
er
g
y
co
n
s
u
m
p
tio
n
f
o
r
s
o
lar
co
o
l
b
o
x
with
an
d
with
o
u
t te
m
p
er
at
u
r
e
co
n
t
r
o
l
4
.
6
.
M
a
inte
na
nce
a
nd
d
ura
bil
it
y
T
h
e
s
o
lar
-
p
o
wer
ed
co
o
l
b
o
x
tech
n
o
lo
g
y
an
d
its
r
elate
d
co
m
p
o
n
e
n
ts
r
eq
u
ir
e
r
o
u
tin
e
m
ai
n
ten
an
ce
to
en
s
u
r
e
o
p
tim
al
p
e
r
f
o
r
m
an
ce
an
d
lo
n
g
e
v
ity
.
Ho
wev
er
,
th
is
is
n
o
t
an
in
s
u
r
m
o
u
n
tab
le
o
b
s
tacle
in
th
e
d
ev
elo
p
m
en
t
o
f
an
in
n
o
v
ativ
e
s
o
lar
-
p
o
wer
ed
co
o
l
b
o
x
f
o
r
tr
a
d
itio
n
al
f
is
h
er
m
en
.
So
m
e
ac
tio
n
s
th
at
n
e
ed
to
b
e
tak
e
n
ar
e
d
esig
n
in
g
th
e
c
o
o
l
b
o
x
with
d
u
r
ab
le
an
d
r
o
b
u
s
t
m
ater
ials
to
with
s
tan
d
th
e
h
ar
s
h
m
ar
in
e
en
v
i
r
o
n
m
en
t,
in
clu
d
i
n
g
ex
p
o
s
u
r
e
to
s
altwate
r
an
d
r
o
u
g
h
h
a
n
d
lin
g
d
u
r
in
g
f
is
h
in
g
ac
t
iv
it
ies.
Selectin
g
th
e
r
ig
h
t
m
at
er
ials
an
d
a
r
u
g
g
e
d
d
esig
n
ca
n
i
n
cr
ea
s
e
th
e
r
eliab
ilit
y
an
d
life
s
p
an
o
f
th
e
c
o
o
l
b
o
x
.
Mo
r
e
o
v
er
,
alth
o
u
g
h
t
r
ad
itio
n
al
f
is
h
er
m
en
m
ay
f
ac
e
ch
allen
g
es
in
ac
ce
s
s
in
g
m
ain
ten
an
ce
s
er
v
ices
o
r
s
p
ar
e
p
ar
ts
in
r
em
o
te
ar
ea
s
,
th
is
c
an
b
e
o
v
er
co
m
e
b
y
p
r
o
v
id
i
n
g
ad
e
q
u
ate
tr
ain
in
g
an
d
m
ain
ten
an
ce
g
u
id
an
ce
to
th
e
f
is
h
er
m
en
.
W
ith
a
g
o
o
d
u
n
d
er
s
tan
d
in
g
o
f
h
o
w
to
m
ain
tain
an
d
r
ep
air
th
e
co
o
l
b
o
x
,
f
is
h
er
m
e
n
ca
n
i
n
d
ep
e
n
d
en
t
ly
m
ain
tain
th
e
d
ev
ice
an
d
ex
t
en
d
its
s
er
v
ice
life
.
Ad
d
itio
n
ally
,
d
ep
en
d
en
ce
o
n
wea
th
er
co
n
d
itio
n
s
is
in
d
ee
d
a
co
n
s
id
er
atio
n
i
n
th
e
u
s
e
o
f
a
s
o
lar
-
p
o
wer
ed
c
o
o
l
b
o
x
.
Ho
wev
er
,
b
y
tak
i
n
g
in
t
o
ac
co
u
n
t
th
e
p
atter
n
s
o
f
s
ea
b
r
ee
ze
s
an
d
lan
d
b
r
ee
ze
s
in
th
e
I
n
d
o
n
esian
ar
ch
i
p
elag
o
,
wh
ich
ca
n
i
n
f
lu
en
ce
r
ain
f
all
an
d
cl
o
u
d
y
c
o
n
d
itio
n
s
,
th
e
co
o
l
b
o
x
c
an
b
e
d
esig
n
ed
with
ad
eq
u
ate
en
er
g
y
s
to
r
ag
e
ca
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