I
nte
rna
t
io
na
l J
o
urna
l o
f
Adv
a
nces in Applie
d Science
s
(
I
J
AAS)
Vo
l.
14
,
No
.
3
,
Sep
tem
b
er
20
25
,
p
p
.
9
0
7
~
9
15
I
SS
N:
2252
-
8
8
1
4
,
DOI
:
1
0
.
1
1
5
9
1
/ijaas
.
v14.
i
3
.
pp
907
-
9
15
907
J
o
ur
na
l ho
m
ep
a
g
e
:
h
ttp
:
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m
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u
rfa
c
e
d
e
n
sit
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f
so
lar
ra
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x
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2
:
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c
e
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n
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o
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3
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0
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a
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3
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0
(Ap
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);
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e
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f
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s
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lar
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d
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x
:
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0
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),
4
5
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(
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c
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r
),
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(
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),
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)
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a
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ch
)
,
1
,
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3
0
(
Ap
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)
.
K
ey
w
o
r
d
s
:
B
en
ef
its
C
h
em
ical
f
er
tili
ze
r
s
E
n
er
g
y
s
av
in
g
E
n
v
ir
o
n
m
en
tal
p
o
llu
tio
n
Hea
tin
g
R
en
ewa
b
le
en
er
g
y
So
lar
r
ad
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n
T
h
is i
s
a
n
o
p
e
n
a
c
c
e
ss
a
rticle
u
n
d
e
r th
e
CC B
Y
-
SA
li
c
e
n
se
.
C
o
r
r
e
s
p
o
nd
ing
A
uth
o
r
:
T
u
r
k
an
Hasan
o
v
a
Allah
v
e
r
d
i
Dep
ar
tm
en
t o
f
So
il Scien
ce
an
d
R
ea
l E
s
tate
C
ad
astre
,
Facu
lt
y
o
f
E
c
o
lo
g
y
an
d
So
il Scien
ce
B
ak
u
State
Un
iv
er
s
ity
Aca
d
.
Z
ah
id
Kh
alilo
v
St.
3
3
,
AZ
1
1
4
8
,
Aze
r
b
aijan
E
m
ail:
tu
r
k
an
h
esen
o
v
a@
m
ail.
r
u
1.
I
NT
RO
D
UCT
I
O
N
Hu
m
an
ity
b
eg
a
n
to
u
s
e
th
e
e
n
er
g
y
o
f
th
e
s
u
n
a
v
e
r
y
lo
n
g
tim
e
ag
o
.
B
y
p
lacin
g
m
ir
r
o
r
s
at
ce
r
tain
an
g
les,
th
ey
h
ea
ted
th
e
wate
r
in
th
e
th
er
m
al
b
ath
s
an
d
also
illu
m
in
ated
r
o
o
m
s
with
o
u
t
win
d
o
ws.
T
h
e
r
elev
an
ce
o
f
d
ev
elo
p
in
g
alte
r
n
ativ
e
en
er
g
y
s
o
u
r
ce
s
is
b
ec
o
m
in
g
a
k
e
y
asp
ec
t
o
f
e
n
s
u
r
in
g
s
u
s
tain
ab
le
de
v
elo
p
m
e
n
t.
Statis
tic
s
o
n
g
lo
b
al
en
er
g
y
c
o
n
s
u
m
p
tio
n
wo
r
r
y
in
g
l
y
in
d
icate
th
e
n
ee
d
to
f
in
d
n
ew
s
o
u
r
ce
s
.
Dete
r
io
r
atio
n
o
f
th
e
en
v
ir
o
n
m
en
t,
p
o
llu
ti
o
n
,
a
n
d
d
ep
letio
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o
f
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atu
r
al
r
eso
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ce
s
h
av
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o
r
ce
d
h
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m
an
ity
t
o
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in
k
ab
o
u
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o
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to
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tain
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tr
icity
an
d
h
ea
t
f
r
o
m
r
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le
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s
[
1
]
,
[
2
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.
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ated
p
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f
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en
v
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m
en
tal
r
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s
o
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t
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m
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[
3
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,
[
4
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.
I
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m
al
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Evaluation Warning : The document was created with Spire.PDF for Python.
I
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2
2
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I
n
t J Ad
v
Ap
p
l Sci
,
Vo
l.
14
,
No
.
3
,
Sep
tem
b
er
20
25
:
907
-
9
15
908
tr
ad
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al
f
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with
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g
r
id
s
,
as
well
as
is
s
u
es
o
f
s
u
s
tain
ab
le
d
ev
elo
p
m
e
n
t
an
d
r
e
d
u
cin
g
th
e
n
eg
ativ
e
im
p
ac
t
o
f
e
n
er
g
y
o
n
th
e
en
v
i
r
o
n
m
e
n
t
,
d
ictate
s
th
e
n
ee
d
to
d
ev
elo
p
r
en
ewa
b
le
en
er
g
y
.
Pas
s
in
g
t
h
r
o
u
g
h
th
e
atm
o
s
p
h
er
e,
s
o
lar
r
ad
iatio
n
is
wea
k
en
e
d
,
p
ar
ti
ally
p
en
etr
at
es
th
e
atm
o
s
p
h
er
e
with
d
ir
ec
t r
ay
s
,
an
d
r
ea
ch
es th
e
ea
r
th
'
s
s
u
r
f
ac
e
i
n
th
e
f
o
r
m
o
f
d
ir
ec
t a
n
d
d
if
f
u
s
e
r
ad
iatio
n
[
5
]
,
[
6
]
.
T
h
e
ef
f
icien
cy
o
f
p
r
ac
tical
u
s
e
o
f
s
o
lar
e
n
er
g
y
lar
g
ely
d
ep
en
d
s
o
n
h
o
w
ac
cu
r
ately
th
e
p
atter
n
s
an
d
s
p
ec
if
ic
d
ata
o
n
th
e
ar
r
iv
al
o
f
s
o
lar
r
a
d
iatio
n
at
th
e
lo
ca
tio
n
o
f
th
e
p
r
o
p
o
s
ed
o
p
er
atio
n
o
f
th
e
in
s
tallatio
n
s
wer
e
tak
en
in
to
ac
co
u
n
t
d
u
r
in
g
d
esig
n
d
e
v
elo
p
m
en
t.
T
h
e
d
if
f
icu
lties
in
d
ev
elo
p
in
g
s
o
lar
en
er
g
y
a
r
e
r
elate
d
to
th
e
f
ac
t
th
at
th
e
ar
ea
s
m
o
s
t
s
u
itab
le
f
o
r
its
d
ev
elo
p
m
en
t
a
r
e
lo
ca
ted
f
a
r
f
r
o
m
wate
r
s
o
u
r
ce
s
,
an
d
th
e
ar
ea
s
ad
jace
n
t
to
wate
r
s
o
u
r
ce
s
,
wh
er
e
th
e
m
a
jo
r
ity
o
f
th
e
p
o
p
u
latio
n
is
co
n
ce
n
tr
ated
,
in
tu
r
n
,
d
o
n
o
t
h
av
e
s
u
ch
f
av
o
r
ab
le
co
n
d
itio
n
s
f
o
r
th
e
p
r
o
d
u
ctio
n
o
f
s
o
lar
en
er
g
y
[
7
]
,
[
8
]
.
T
h
e
p
r
o
b
lem
o
f
p
r
ac
tical
ap
p
licatio
n
o
f
s
o
lar
en
er
g
y
co
n
tain
s
two
m
ai
n
asp
ec
ts
: its
co
n
v
er
s
io
n
i
n
to
elec
tr
ical
en
er
g
y
an
d
h
ea
t
[
9
]
.
T
h
e
p
o
s
s
ib
ilit
y
o
f
ac
cu
m
u
latin
g
lo
w
-
p
o
ten
tial
h
ea
t
in
a
s
p
ec
ially
eq
u
ip
p
e
d
e
x
ten
s
io
n
(
g
r
ee
n
h
o
u
s
e)
f
o
r
co
n
v
er
s
io
n
b
y
an
air
-
to
-
w
ater
h
ea
t
p
u
m
p
is
an
aly
ze
d
,
i
n
o
r
d
e
r
to
s
u
b
s
eq
u
e
n
tly
u
s
e
it
f
o
r
h
ea
tin
g
n
ee
d
s
.
T
wo
d
esig
n
s
wer
e
co
n
s
id
er
e
d
as
f
in
is
h
in
g
m
ater
ials
f
o
r
t
h
e
e
x
ten
s
io
n
:
d
o
u
b
le
-
lay
er
p
o
ly
ca
r
b
o
n
ate
with
a
n
ai
r
g
ap
an
d
e
n
er
g
y
-
s
av
in
g
g
lass
.
T
h
e
u
s
e
o
f
s
o
lar
en
er
g
y
to
h
ea
t
th
e
co
o
lan
t
to
m
ee
t
th
e
n
ee
d
f
o
r
h
ea
tin
g
is
b
ec
o
m
in
g
in
cr
ea
s
in
g
l
y
p
o
p
u
la
r
.
T
h
is
is
d
u
e,
am
o
n
g
o
th
e
r
th
i
n
g
s
,
to
t
h
e
r
a
p
id
r
ed
u
ctio
n
o
f
t
h
e
p
lan
et'
s
n
atu
r
al
r
eso
u
r
ce
s
an
d
,
as
a
r
esu
lt,
th
e
r
i
s
e
in
p
r
ices
f
o
r
f
o
s
s
il
f
u
els.
T
o
d
ay
,
th
e
u
s
e
o
f
s
o
lar
en
e
r
g
y
f
o
r
th
e
c
o
n
s
tr
u
ctio
n
o
f
en
e
r
g
y
-
ef
f
icien
t
o
r
p
ass
iv
e
h
o
u
s
es
is
wid
esp
r
ea
d
.
T
h
er
e
a
r
e
m
an
y
ex
a
m
p
les
o
f
n
o
t
o
n
ly
th
e
c
o
n
s
tr
u
ctio
n
o
f
n
ew
p
ass
iv
e
h
o
u
s
es,
b
u
t
also
th
e
r
ec
o
n
s
tr
u
ctio
n
o
f
o
ld
u
n
ec
o
n
o
m
i
ca
l
b
u
ild
in
g
s
u
s
in
g
th
e
b
asic
p
r
in
cip
les
o
f
en
er
g
y
ef
f
icien
cy
ar
o
u
n
d
th
e
wo
r
ld
.
I
t
is
q
u
ite
co
m
m
o
n
t
o
u
s
e
air
s
o
lar
co
llecto
r
s
an
d
o
th
er
m
eth
o
d
s
o
f
ac
cu
m
u
latin
g
s
o
lar
h
ea
t
to
im
p
r
o
v
e
th
e
en
er
g
y
ef
f
icien
cy
o
f
in
d
o
o
r
s
p
ac
es.
Ho
wev
e
r
,
it
i
s
wo
r
th
n
o
tin
g
th
at
th
e
ef
f
icien
cy
o
f
s
o
lar
h
ea
tin
g
d
ir
ec
tly
d
ep
en
d
s
o
n
th
e
an
g
le
o
f
in
cid
e
n
ce
o
f
th
e
s
u
n
'
s
r
ay
s
.
T
ec
h
n
o
lo
g
ies
h
av
e
b
ee
n
d
ev
el
o
p
ed
th
at
allo
w
f
o
llo
win
g
th
e
an
g
le
o
f
in
cid
e
n
ce
o
f
th
e
s
u
n
'
s
r
ay
s
th
r
o
u
g
h
o
u
t
t
h
e
y
ea
r
o
r
d
ay
.
T
h
e
id
ea
o
f
u
s
in
g
ad
d
itio
n
al
ex
ten
s
io
n
s
to
ac
cu
m
u
late
s
o
lar
h
ea
t
an
d
u
s
e
it
later
d
u
r
in
g
th
e
d
ar
k
h
o
u
r
s
h
as
lo
n
g
b
ee
n
d
escr
ib
ed
in
s
cien
tific
p
ap
er
s
.
So
lar
en
e
r
g
y
is
o
n
e
o
f
th
e
s
o
u
r
ce
s
o
f
r
en
ewa
b
le
en
er
g
y
,
b
u
t
in
t
h
e
Go
b
u
s
tan
r
eg
io
n
d
u
r
in
g
th
e
c
o
ld
s
ea
s
o
n
,
th
e
u
s
e
o
f
s
o
lar
e
n
er
g
y
is
d
if
f
icu
lt
d
u
e
to
lo
w
o
u
ts
id
e
tem
p
er
atu
r
es
[
1
0
]
–
[
1
2
]
.
An
o
th
e
r
m
an
d
at
o
r
y
co
n
d
itio
n
wh
e
n
d
esig
n
in
g
a
p
ass
iv
e
h
o
u
s
e
is
th
e
u
s
e
o
f
r
ec
u
p
er
atio
n
.
Hea
t
p
u
m
p
s
allo
w
y
o
u
t
o
co
llect
an
d
s
av
e
th
e
m
ax
im
u
m
am
o
u
n
t
o
f
en
e
r
g
y
r
ec
ei
v
ed
f
r
o
m
th
e
s
u
n
.
T
h
u
s
,
a
two
-
s
to
r
y
f
r
am
e
h
o
u
s
e
with
a
n
attac
h
ed
g
r
ee
n
h
o
u
s
e
was
co
n
s
id
er
ed
in
a
s
cien
tific
p
ap
e
r
.
T
o
tr
an
s
f
er
h
ea
t
f
r
o
m
th
e
ex
ten
s
io
n
to
th
e
n
o
r
t
h
er
n
wall,
a
s
y
s
tem
o
f
p
ip
es w
ith
wate
r
as a
h
ea
t c
ar
r
ier
is
u
s
ed
[
1
3
]
,
[
1
4
]
.
2.
RE
S
E
ARCH
M
E
T
H
O
D
I
n
th
is
ar
ticle,
th
e
o
b
ject
o
f
s
tu
d
y
is
a
p
r
iv
ate
r
esid
en
tial
h
o
u
s
e
with
th
e
p
o
s
s
ib
ilit
y
o
f
p
ar
tially
s
atis
f
y
in
g
h
ea
tin
g
n
ee
d
s
with
ac
cu
m
u
lated
s
o
lar
en
er
g
y
co
ll
ec
ted
b
y
a
h
ea
t
p
u
m
p
in
an
e
x
ten
s
io
n
-
g
r
ee
n
h
o
u
s
e
(
Fig
u
r
e
1
)
.
T
h
e
f
o
llo
win
g
tas
k
s
wer
e
s
et:
i)
to
d
eter
m
in
e
t
h
e
th
er
m
al
p
er
f
o
r
m
an
ce
o
f
t
h
e
o
b
ject
u
n
d
er
s
tu
d
y
,
ii)
to
ca
lcu
late
th
e
h
ea
t
in
p
u
t
f
r
o
m
s
o
lar
r
ad
iatio
n
i
n
to
th
e
g
r
ee
n
h
o
u
s
e
f
o
r
ea
ch
m
o
n
th
o
f
th
e
h
ea
tin
g
p
er
io
d
,
an
d
iii)
to
ev
al
u
ate
th
e
ef
f
icien
cy
o
f
u
s
in
g
th
e
h
ea
t
o
f
s
o
lar
r
ad
iatio
n
.
An
a
n
aly
s
is
o
f
th
e
r
esu
lts
o
f
ca
lcu
latin
g
th
e
in
f
lu
x
o
f
s
o
lar
r
ad
iatio
n
in
to
th
e
ex
ten
s
io
n
v
o
lu
m
e
is
c
ar
r
ied
o
u
t
,
a
n
d
a
co
m
p
ar
is
o
n
with
th
e
esti
m
ated
h
ea
tin
g
lo
ad
is
m
ad
e
,
as sh
o
w
n
in
Fig
u
r
e
2
.
Ma
in
p
ar
t
:
d
escr
ip
tio
n
o
f
t
h
e
o
b
ject:
–
C
o
n
s
tr
u
ctio
n
s
ite: G
o
b
u
s
tan
(
l
o
w
-
h
u
m
id
ity
zo
n
e
)
.
–
Pu
r
p
o
s
e
o
f
t
h
e
p
lace
:
r
esid
en
ti
al
; in
d
o
o
r
ai
r
tem
p
er
at
u
r
e,
t
air
=
2
0
°C
.
–
P
lace
h
eig
h
t
:
8
.
2
m
,
n
u
m
b
er
o
f
f
lo
o
r
s
:
2
,
to
tal
ar
ea
:
9
5
m
2
.
–
C
alcu
lated
p
ar
am
eter
s
o
f
o
u
td
o
o
r
air
,
f
o
r
h
ea
tin
g
d
esig
n
:
air
tem
p
er
atu
r
e
o
f
th
e
c
o
ld
est
f
i
v
e
-
d
ay
p
er
io
d
with
0
.
9
2
t
5
,
o
u
td
o
o
r
air
=
-
22
°C
,
d
u
r
atio
n
o
f
th
e
p
e
r
io
d
with
av
er
ag
e
d
aily
tem
p
e
r
atu
r
e
≤
8
°C
,
z
period
=1
9
9
d
ay
s
,
a
v
er
ag
e
tem
p
er
atu
r
e
f
o
r
th
is
p
er
io
d
t
period
=
-
4
.
3
°C
.
–
G
r
ee
n
h
o
u
s
e
d
im
en
s
io
n
s
3
×
6
.
4
m
,
r
o
o
f
h
as
a
s
lo
p
e
o
f
2
0
°,
h
e
ig
h
t
at
th
e
ju
n
ctio
n
with
th
e
h
o
u
s
e
h
=3
.
8
m
,
as sh
o
wn
in
Fig
u
r
e
1
.
Po
ly
s
ty
r
en
e
co
n
cr
ete
is
ad
o
p
ted
as
th
e
m
ain
m
ater
ial
f
o
r
th
e
walls
o
f
th
e
r
esid
en
tial
b
u
ild
in
g
.
T
h
er
m
al
en
g
in
ee
r
in
g
ca
lcu
latio
n
o
f
th
e
wall
is
p
er
f
o
r
m
ed
tak
in
g
in
to
ac
co
u
n
t
h
eter
o
g
e
n
e
ities
.
T
h
e
elem
en
ts
o
f
th
e
c
u
r
tain
wall
v
e
n
tilated
f
ac
ad
e
ar
e
a
d
o
p
te
d
as
th
er
m
al
en
g
in
ee
r
i
n
g
h
ete
r
o
g
e
n
eities:
s
elf
-
tap
p
in
g
s
cr
ews
7
0
m
m
lo
n
g
an
d
4
.
2
m
m
in
d
iam
eter
,
a
wo
o
d
e
n
b
ea
m
with
a
cr
o
s
s
-
s
ec
tio
n
o
f
5
0
×
5
0
m
m
.
T
h
er
e
ar
e
4
elem
en
ts
o
f
th
er
m
al
en
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I
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Ap
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N:
2252
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4
Mo
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u
r
e
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Evaluation Warning : The document was created with Spire.PDF for Python.
I
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N
:
2
2
5
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I
n
t J Ad
v
Ap
p
l Sci
,
Vo
l.
14
,
No
.
3
,
Sep
tem
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20
25
:
907
-
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15
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8
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Evaluation Warning : The document was created with Spire.PDF for Python.
I
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N
:
2
2
5
2
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8
8
1
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I
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t J Ad
v
Ap
p
l Sci
,
Vo
l.
14
,
No
.
3
,
Sep
tem
b
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20
25
:
907
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15
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is
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6
V,
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u
r
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6
s
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u
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a)
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Fig
u
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6
(
b
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(
Fig
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(
c
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Fig
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d
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CO
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Evaluation Warning : The document was created with Spire.PDF for Python.
I
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t J Ad
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Ap
p
l Sci
I
SS
N:
2252
-
8
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1
4
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Evaluation Warning : The document was created with Spire.PDF for Python.
I
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Ap
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l Sci
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N:
2252
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8
8
1
4
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h
a
m
m
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d
.
m
a
d
n
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e
@iu
b
.
e
d
u
.
Evaluation Warning : The document was created with Spire.PDF for Python.