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Adv
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2252
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[
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I
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Ap
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2252
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8
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in
m
o
s
t
ca
s
es.
Ho
wev
er
,
in
th
e
co
ld
wea
th
er
co
n
d
itio
n
s
o
f
I
f
r
an
e,
th
e
r
ed
u
ctio
n
n
e
v
er
ex
ce
e
d
ed
5
7
%
.
I
n
a
s
im
ilar
v
ein
,
C
h
eg
ar
i
et
a
l.
[1
0]
in
v
esti
g
ated
th
e
ef
f
ec
ts
o
f
t
h
e
r
m
al
in
s
u
latio
n
o
n
a
ty
p
ical
R
+1
b
u
ild
in
g
ac
r
o
s
s
th
e
s
ix
c
lim
ate
ca
teg
o
r
ies
in
Mo
r
o
cc
o
.
T
h
ey
f
o
u
n
d
th
at
th
e
r
m
al
in
s
u
latio
n
h
ad
a
s
ig
n
if
ica
n
t
im
p
ac
t
o
n
e
n
er
g
y
s
elf
-
s
u
f
f
i
cien
cy
in
all
zo
n
es,
with
a
p
ar
ticu
lar
em
p
h
asis
o
n
I
f
r
an
e
C
ity
an
d
co
m
p
ar
ab
le
c
lim
ates
.
Fu
r
th
er
m
o
r
e,
Ham
d
a
o
u
i
et
a
l.
[
1
1
]
s
h
e
d
lig
h
t
o
n
t
h
e
in
f
lu
e
n
ce
o
f
in
s
u
l
atio
n
m
ater
ials
o
n
th
e
th
er
m
al
b
eh
av
io
r
o
f
b
u
ild
i
n
g
s
an
d
th
eir
an
n
u
al
lo
a
d
.
T
h
r
o
u
g
h
d
y
n
a
m
ic
s
im
u
latio
n
s
u
s
in
g
a
tr
an
s
ien
t
s
im
u
latio
n
p
r
o
g
r
a
m
(
T
R
NSYS)
,
th
ey
test
ed
th
r
ee
s
ce
n
ar
io
s
an
d
d
is
co
v
e
r
ed
th
at
th
e
th
ir
d
s
ce
n
ar
io
,
wh
er
e
th
e
ex
ter
n
al
walls,
r
o
o
f
,
a
n
d
g
r
o
u
n
d
wer
e
p
r
o
p
er
l
y
in
s
u
lated
,
r
esu
lted
in
th
e
lo
west a
n
n
u
al
lo
ad
.
I
n
an
ex
p
e
r
im
en
tal
s
tu
d
y
,
Fan
g
et
a
l.
[
1
2
]
c
o
n
d
u
cted
a
co
m
p
ar
is
o
n
b
etwe
en
a
n
o
n
-
in
s
u
late
d
ch
am
b
er
an
d
a
ch
a
m
b
e
r
in
s
u
lated
with
ex
tr
u
d
ed
p
o
ly
s
ty
r
en
e
(
XPS).
T
h
e
f
i
n
d
in
g
s
r
ev
ea
led
th
at
th
e
im
p
lem
en
tatio
n
o
f
XPS
in
s
u
latio
n
r
esu
lted
in
a
s
ig
n
if
ican
t
r
e
d
u
ctio
n
o
f
2
3
.
5
%
i
n
co
o
lin
g
lo
a
d
d
u
r
in
g
th
e
s
u
m
m
er
s
ea
s
o
n
.
So
b
h
y
et
a
l.
[
1
3
]
c
o
n
d
u
cted
a
co
m
p
r
eh
en
s
iv
e
s
tu
d
y
in
v
o
lv
in
g
b
o
th
n
u
m
e
r
ical
s
im
u
latio
n
s
a
n
d
ex
p
er
im
en
tal
a
n
aly
s
is
o
n
a
m
o
d
e
r
n
-
s
ty
le
h
o
u
s
e
s
itu
ated
in
Ma
r
r
ak
ec
h
.
T
h
e
p
r
im
ar
y
o
b
jectiv
e
o
f
th
e
s
tu
d
y
w
as
to
ev
alu
ate
th
e
im
p
ac
t
o
f
th
er
m
al
in
s
u
latio
n
ap
p
lied
to
th
e
b
u
ild
in
g
'
s
en
v
elo
p
e
o
n
its
th
er
m
al
lo
ad
.
T
h
e
f
in
d
in
g
s
f
r
o
m
th
e
r
es
ea
r
ch
r
e
v
ea
led
t
h
at
th
e
im
p
lem
en
tatio
n
o
f
a
4
cm
XPS
in
s
u
latio
n
o
n
th
e
r
o
o
f
r
esu
lt
ed
in
a
n
o
tewo
r
th
y
r
ed
u
ctio
n
o
f
1
0
%
in
h
ea
tin
g
lo
ad
an
d
3
0
%
in
co
o
lin
g
l
o
ad
wh
en
co
m
p
a
r
ed
to
a
n
o
n
-
in
s
u
lated
h
o
u
s
e.
Mo
r
eo
v
er
,
th
e
p
r
esen
ce
o
f
5
cm
air
g
ap
ca
v
ity
walls
co
n
tr
i
b
u
ted
s
ig
n
if
ica
n
tly
to
en
e
r
g
y
s
av
in
g
s
.
I
n
s
u
latin
g
th
e
ca
v
ity
walls
led
to
a
1
3
%
d
ec
r
ea
s
e
in
h
ea
tin
g
lo
ad
an
d
a
5
%
d
ec
r
ea
s
e
in
c
o
o
lin
g
lo
ad
,
in
co
m
p
ar
is
o
n
to
a
non
-
in
s
u
lated
h
o
u
s
e.
No
tab
l
y
,
th
e
co
m
b
in
e
d
ef
f
ec
t
o
f
b
o
th
in
s
u
latio
n
s
d
em
o
n
s
tr
ated
s
u
b
s
tan
tial
en
er
g
y
s
av
in
g
s
,
with
h
ea
tin
g
an
d
co
o
lin
g
n
ee
d
s
b
ein
g
r
ed
u
ce
d
b
y
2
6
an
d
4
0
%
r
esp
ec
tiv
ely
.
I
n
th
eir
in
v
esti
g
atio
n
,
B
en
h
am
o
u
a
n
d
B
en
n
o
u
n
a
[
1
4
]
d
elv
e
d
in
to
t
h
e
in
f
l
u
en
ce
o
f
en
v
el
o
p
e
in
s
u
latio
n
o
n
th
e
ex
ter
n
al
walls
an
d
r
o
o
f
,
as
well
as
th
e
ef
f
ec
ts
o
f
s
o
lar
p
r
o
tectio
n
o
n
in
d
o
o
r
co
m
f
o
r
t,
h
ea
tin
g
lo
ad
,
a
n
d
co
o
lin
g
lo
ad
.
T
h
e
s
tu
d
y
s
p
ec
if
ically
f
o
cu
s
ed
o
n
a
v
illa
-
ty
p
e
h
o
u
s
e
s
itu
ated
in
th
e
city
o
f
Ma
r
r
a
k
ec
h
,
lo
c
ated
in
Mo
r
o
cc
o
.
Kay
n
ak
li
[
1
5
]
s
h
o
wed
in
th
eir
ar
ticle
th
at
th
e
im
p
lem
e
n
tatio
n
o
f
well
-
in
s
u
lated
e
x
ter
n
al
walls,
with
o
p
tim
ized
th
ick
n
ess
es
o
f
in
s
u
latio
n
,
r
esu
lts
in
s
u
b
s
tan
tial
r
ed
u
ctio
n
s
in
an
n
u
al
en
er
g
y
co
n
s
u
m
p
tio
n
f
o
r
h
ea
ti
n
g
an
d
co
o
lin
g
s
y
s
tem
s
.
I
t
is
u
n
f
o
r
tu
n
ate
th
at
n
o
t
all
o
f
th
ese
m
ate
r
ials
p
r
o
v
id
e
s
atis
f
ac
to
r
y
th
er
m
al
ch
ar
ac
ter
is
tic
s
,
s
u
ch
as
co
n
d
u
ctiv
ity
o
r
h
ea
t
ca
p
ac
ity
.
So
m
e
r
e
q
u
ir
e
co
m
p
lex
m
a
n
u
f
ac
tu
r
in
g
p
r
o
ce
s
s
es,
o
th
er
s
ar
e
f
in
an
cially
co
s
tly
,
an
d
s
o
m
e
p
o
s
s
ess
to
x
ic
p
r
o
p
e
r
ties
.
C
o
n
s
eq
u
en
tly
,
th
e
s
tr
ateg
y
o
f
in
teg
r
atin
g
ec
o
lo
g
ically
-
s
o
u
r
ce
d
m
ater
ials
with
in
s
u
latio
n
m
ater
ials
to
en
h
an
ce
th
er
m
al
p
er
f
o
r
m
a
n
ce
co
u
ld
p
r
o
v
e
h
ig
h
ly
b
en
e
f
icial.
T
h
is
p
i
o
n
ee
r
in
g
ap
p
r
o
ac
h
o
f
f
er
s
th
e
p
r
o
m
is
e
o
f
co
n
s
id
er
a
b
le
en
er
g
y
s
av
i
n
g
s
an
d
a
n
o
tab
le
r
e
d
u
ctio
n
in
th
e
en
v
ir
o
n
m
e
n
tal
im
p
ac
t o
f
b
u
ild
in
g
s
.
T
h
e
p
r
o
p
o
s
ed
co
n
f
ig
u
r
atio
n
f
o
r
en
h
an
cin
g
th
e
th
er
m
al
b
eh
av
io
r
o
f
a
b
u
ild
i
n
g
i
n
v
o
lv
es
th
e
u
s
e
o
f
p
o
n
ce
b
l
o
c,
an
ec
o
lo
g
ical
m
at
er
ial
co
n
s
tr
u
cted
f
r
o
m
m
etic
u
lo
u
s
ly
p
u
r
if
ied
p
u
m
ice.
T
h
i
s
v
o
lcan
ic
s
to
n
e
i
s
r
en
o
wn
ed
f
o
r
its
m
ag
m
atic
s
t
r
u
ctu
r
e,
wh
ich
ef
f
ec
tiv
ely
e
n
h
an
ce
s
h
ea
t
tr
an
s
f
er
.
T
h
e
s
p
ec
if
ic
co
m
p
o
s
itio
n
o
f
th
e
p
o
n
ce
b
lo
c
b
lo
ck
g
u
ar
an
te
es
s
u
p
er
io
r
h
ea
t
in
s
u
latio
n
p
r
o
p
er
ties
an
d
r
em
ar
k
a
b
le
d
u
r
ab
i
lity
,
wh
ich
m
a
k
e
it
an
id
ea
l c
h
o
ice
f
o
r
s
u
s
tain
ab
le
co
n
s
tr
u
ctio
n
p
r
ac
tices.
A
n
u
m
b
e
r
o
f
s
tu
d
ies
h
av
e
h
ig
h
lig
h
ted
t
h
e
p
r
o
m
is
in
g
th
e
r
m
al
ch
ar
ac
ter
is
tics
o
f
n
ew
ec
o
lo
g
ical
m
ater
ials
in
b
u
ild
in
g
s
.
Fo
r
in
s
tan
ce
,
Ky
m
äläin
en
an
d
Sjö
b
er
g
[
1
6
]
ev
alu
ate
d
th
e
p
o
te
n
tial
o
f
b
ast
f
ib
er
s
d
er
iv
ed
f
r
o
m
f
lax
an
d
h
em
p
f
o
r
in
s
u
latio
n
ap
p
licatio
n
s
,
f
in
d
i
n
g
th
ese
m
ater
ials
to
p
o
s
s
ess
f
a
v
o
r
ab
le
p
r
o
p
er
ties
f
o
r
in
s
u
latio
n
p
u
r
p
o
s
es
.
Fo
u
r
y
ea
r
s
later
,
K
o
r
jen
ic
et
a
l.
[
1
7
]
p
r
o
p
o
s
ed
th
e
d
e
v
elo
p
m
en
t
o
f
n
ew
in
s
u
latio
n
m
ater
ials
u
s
in
g
h
em
p
an
d
f
lax
,
d
em
o
n
s
tr
atin
g
th
r
o
u
g
h
v
ar
i
o
u
s
ex
p
er
im
e
n
ts
th
eir
th
er
m
al
p
er
f
o
r
m
an
ce
c
o
m
p
ar
a
b
le
to
co
n
v
en
tio
n
al
m
ater
ials
.
Su
b
s
eq
u
en
tly
,
h
em
p
wo
o
l
as
an
in
s
u
latio
n
m
ater
ial
g
ain
ed
s
ig
n
i
f
ican
t
atten
tio
n
d
u
e
to
th
ese
f
in
d
in
g
s
[
1
8
]
.
L
e
et
a
l
.
[
1
9
]
s
tu
d
ied
th
e
im
p
ac
t
o
f
in
teg
r
atin
g
h
em
p
co
n
cr
ete
in
th
e
b
u
ild
in
g
.
T
h
e
y
f
o
u
n
d
th
at
th
is
s
o
lu
tio
n
c
o
u
ld
d
ec
r
ea
s
e
th
e
d
aily
h
u
m
id
ity
in
s
id
e,
a
n
d
r
ea
ch
ab
o
u
t
a
4
5
% r
ed
u
ctio
n
in
e
n
er
g
y
co
n
s
u
m
p
tio
n
.
I
n
ad
d
itio
n
to
p
o
n
ce
b
lo
c,
h
em
p
wo
o
l
will
also
b
e
in
teg
r
ated
in
to
th
e
b
u
ild
i
n
g
to
en
h
an
ce
i
ts
th
er
m
al
b
eh
av
io
r
.
T
h
is
in
s
u
latio
n
m
at
er
ial
h
as
s
h
o
wn
in
ter
esti
n
g
th
er
m
al
ch
a
r
ac
ter
is
tics
d
esp
ite
its
lim
ited
u
s
e
in
b
u
ild
in
g
in
s
u
latio
n
.
Sev
er
al
s
tu
d
ies
h
av
e
s
u
p
p
o
r
ted
th
is
id
e
a,
in
clu
d
in
g
t
h
e
wo
r
k
o
f
Dli
m
i
et
a
l.
[
2
0
]
wh
ich
in
v
esti
g
ated
th
e
im
p
ac
t
o
f
in
te
g
r
atin
g
h
em
p
wo
o
l
as
a
n
in
s
u
l
atio
n
m
ater
ial
in
t
h
e
wall
s
tr
u
ctu
r
e
o
f
M
o
r
o
cc
an
b
u
ild
in
g
s
,
s
p
ec
if
ically
in
t
h
e
city
o
f
Me
k
n
es
with
a
Me
d
iter
r
an
ea
n
clim
ate.
T
h
e
s
tu
d
y
s
h
o
wed
th
at
t
h
e
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2
2
5
2
-
8
8
1
4
I
n
t J Ad
v
Ap
p
l Sci
,
Vo
l.
1
3
,
No
.
4
,
Dec
em
b
er
2
0
2
4
:
974
-
98
4
976
in
teg
r
atio
n
o
f
h
em
p
wo
o
l
co
u
l
d
r
esu
lt
in
en
er
g
y
s
av
in
g
s
an
d
co
n
s
eq
u
en
tly
lead
to
a
d
ec
r
ea
s
e
in
o
v
er
all
co
s
ts
.
I
n
an
o
t
h
er
r
esear
ch
p
u
b
lis
h
ed
in
2
0
2
0
,
Dlim
i
et
a
l
.
[
2
1
]
co
m
p
ar
ed
an
i
n
s
u
lated
b
u
ild
in
g
in
th
e
s
am
e
city
with
a
s
ce
n
ar
io
wh
er
e
n
o
in
s
u
latio
n
was
p
r
esen
t.
T
h
ey
f
o
u
n
d
th
at
in
s
u
latio
n
with
h
em
p
wo
o
l
y
ield
ed
s
ig
n
if
ican
t
r
esu
lts
,
p
r
o
v
id
in
g
a
6
5
%
r
ed
u
ctio
n
wh
en
th
e
ex
ter
n
al
walls
an
d
r
o
o
f
wer
e
in
s
u
lated
.
Oth
e
r
s
tu
d
ies
h
av
e
also
ex
p
lo
r
ed
th
e
i
n
teg
r
atio
n
o
f
h
em
p
wo
o
l
in
p
ar
all
el
with
o
t
h
er
m
ater
ials
.
I
n
th
eir
wo
r
k
,
C
h
ar
ai
et
a
l.
[
2
2
]
d
em
o
n
s
tr
ated
th
at
in
te
g
r
atin
g
h
em
p
w
o
o
l
with
p
last
er
b
o
ar
d
s
ig
n
if
ican
tly
im
p
r
o
v
es
th
e
th
e
r
m
al
ef
f
icien
c
y
o
f
b
u
ild
in
g
s
.
Po
n
ce
b
lo
c
also
ex
h
ib
ite
d
in
te
r
esti
n
g
th
er
m
al
b
eh
a
v
io
r
an
d
co
u
ld
b
e
u
s
ed
as
a
co
n
s
tr
u
cti
o
n
m
ater
ial
f
o
r
its
m
ec
h
an
ical
p
r
o
p
e
r
ti
es.
On
e
o
f
th
e
s
tu
d
ies d
em
o
n
s
tr
atin
g
its
g
o
o
d
th
er
m
al
ch
ar
ac
ter
i
s
tics
is
th
e
r
esear
ch
by
B
ab
ah
ar
r
a
et
a
l.
[
2
3
]
wh
ic
h
in
v
esti
g
ated
th
e
e
f
f
ec
t
o
f
r
e
p
lacin
g
h
o
llo
w
b
r
ick
s
with
Po
n
ce
b
lo
c
i
n
th
e
wall
s
tr
u
ctu
r
e
in
th
e
cities
o
f
C
as
ab
lan
ca
an
d
Kh
o
u
r
ib
g
a.
T
h
e
r
esu
lts
s
h
o
wed
a
h
ea
tin
g
lo
a
d
r
ed
u
ctio
n
r
a
n
g
in
g
f
r
o
m
2
6
-
2
8
%
in
C
asab
lan
ca
,
a
n
d
a
r
ed
u
ctio
n
f
r
o
m
2
6
-
2
9
%
i
n
Kh
o
u
r
ib
g
a.
Ho
wev
er
,
a
d
ec
r
ea
s
e
f
r
o
m
1
6
-
1
8
%
was
o
b
s
er
v
ed
in
c
o
o
lin
g
lo
a
d
in
C
asab
lan
ca
,
an
d
f
r
o
m
1
5
-
1
7
%
i
n
Kh
o
u
r
ib
g
a,
d
ep
en
d
in
g
o
n
th
e
s
tu
d
ied
s
ce
n
ar
io
s
.
I
n
an
o
th
er
wo
r
k
,
Ou
h
aib
i
et
a
l.
[
2
4
]
co
n
d
u
cte
d
a
s
tu
d
y
o
n
th
e
in
teg
r
atio
n
o
f
p
o
n
ce
b
l
o
c
an
d
ae
r
o
g
els
in
s
em
i
-
ar
id
an
d
co
l
d
clim
ates.
T
h
e
r
esu
lts
s
h
o
wed
th
at
th
e
p
r
o
p
o
s
ed
co
n
f
ig
u
r
a
tio
n
s
im
u
ltan
eo
u
s
ly
p
r
o
v
id
e
d
co
m
f
o
r
t
f
o
r
o
cc
u
p
a
n
t
s
in
s
id
e
th
e
b
u
ild
in
g
an
d
r
esu
lted
in
a
d
ec
r
ea
s
e
o
f
ab
o
u
t
4
4
%
in
an
n
u
al
lo
ad
in
Ma
r
r
ak
ec
h
an
d
4
2
%
in
I
f
r
an
e.
T
h
ey
co
n
cl
u
d
ed
th
at
u
s
in
g
t
h
ese
two
m
ater
ials
co
u
ld
b
e
an
ec
o
lo
g
ical
s
o
lu
tio
n
n
o
t
o
n
ly
b
ec
a
u
s
e
o
f
th
eir
ef
f
ec
t
o
n
co
m
f
o
r
t
an
d
en
e
r
g
y
c
o
n
s
u
m
p
tio
n
b
u
t
also
d
u
e
to
th
eir
r
ed
u
ctio
n
in
g
r
ee
n
h
o
u
s
e
g
as e
m
is
s
io
n
s
.
Mo
s
t
r
esear
ch
in
th
e
liter
atu
r
e
d
o
es
n
o
t
in
v
esti
g
ate
th
e
im
p
ac
t
o
f
co
m
b
i
n
in
g
two
d
if
f
er
e
n
t
ty
p
es
o
f
in
s
u
lato
r
s
,
esp
ec
ially
n
atu
r
al
with
ec
o
lo
g
ical
m
ater
ials
.
I
n
t
h
is
co
n
tex
t,
th
is
p
ap
e
r
in
v
esti
g
ates
th
e
im
p
ac
t
o
f
th
e
in
teg
r
atio
n
o
f
p
o
n
ce
b
lo
c
an
d
h
em
p
wo
o
l
p
ar
all
el
as
in
s
u
latio
n
m
ater
ials
in
b
u
ild
in
g
co
n
s
tr
u
ctio
n
ac
r
o
s
s
d
if
f
er
en
t
clim
ate
t
y
p
es
in
Mo
r
o
cc
o
.
T
h
e
s
tu
d
y
is
d
o
n
e
u
s
in
g
T
R
NSYS
s
im
u
latio
n
s
o
f
twar
e,
an
d
th
e
im
p
ac
t
f
ac
to
r
u
s
ed
f
o
r
th
e
co
m
p
a
r
is
o
n
b
etwe
en
clim
ate
ty
p
es
will
b
e
th
e
in
s
id
e
tem
p
e
r
atu
r
e
o
f
t
h
e
b
u
ild
in
g
an
d
its
an
n
u
al
lo
ad
.
T
h
is
wo
r
k
is
co
m
p
o
s
ed
o
f
t
h
r
ee
s
ec
tio
n
s
.
T
h
e
f
ir
s
t
s
ec
tio
n
in
clu
d
es
th
e
s
tu
d
ied
ca
s
e
p
ar
am
eter
s
,
co
n
s
id
er
atio
n
s
,
a
n
d
t
h
e
p
lan
o
f
o
u
r
r
esear
ch
.
T
h
e
s
ec
o
n
d
p
a
r
t
s
h
o
ws
th
e
wo
r
k
’
s
r
esu
lts
a
n
d
th
e
n
co
n
d
u
cts
a
d
is
cu
s
s
io
n
ab
o
u
t
th
ese
r
esu
lt
s
.
T
h
e
th
ir
d
p
a
r
t
co
n
tain
s
a
co
n
clu
s
io
n
wh
e
r
e
s
o
m
e
f
u
tu
r
e
d
im
en
s
io
n
s
f
o
r
r
esear
ch
ar
e
m
en
tio
n
e
d
.
T
h
e
p
ap
er
aim
s
to
e
v
alu
ate
th
e
en
er
g
y
p
er
f
o
r
m
a
n
ce
o
f
th
e
p
r
o
p
o
s
ed
in
s
u
latio
n
m
ater
ials
in
b
u
ild
in
g
co
n
s
tr
u
ctio
n
an
d
d
eter
m
in
e
th
eir
p
o
ten
tial
f
o
r
en
er
g
y
s
av
i
n
g
s
.
Fi
n
ally
,
th
e
r
esear
ch
r
esu
lts
co
u
ld
en
co
u
r
ag
e
f
u
tu
r
e
s
tu
d
ies to
ex
p
lo
r
e
t
h
e
co
m
b
in
atio
n
o
f
e
x
is
tin
g
in
s
u
latio
n
m
a
ter
ials
.
2.
M
E
T
H
O
D
2
.
1
.
B
uil
din
g
des
cr
i
ptio
n
Ou
r
in
v
esti
g
ativ
e
s
am
p
le
is
a
ce
ll
lo
ca
ted
in
s
id
e
th
e
Facu
lty
o
f
Scien
ce
s
o
f
C
asab
lan
ca
(
A
in
C
h
o
ck
)
,
t
h
e
s
tr
u
ctu
r
e
h
as
a
f
o
o
t
p
r
in
t
o
f
9
m
2
an
d
a
t
o
tal
v
o
lu
m
e
o
f
ap
p
r
o
x
im
ately
2
7
m
3
.
T
h
e
en
t
r
an
ce
to
th
e
s
p
ac
e
f
ac
es
n
o
r
th
,
wh
ile
a
s
in
g
le
-
g
laze
d
win
d
o
w
with
a
n
alu
m
i
n
u
m
f
r
am
e
m
ea
s
u
r
es
1
m
i
n
h
eig
h
t
an
d
wid
th
Fig
u
r
e
1
.
T
h
e
walls o
f
th
e
s
tr
u
ctu
r
e
ar
e
2
9
cm
th
ick
.
T
h
e
ce
ll is
lo
ca
ted
at
an
altitu
d
e
o
f
5
7
m
an
d
in
lo
n
g
itu
d
e
an
d
latitu
d
e
r
esp
ec
tiv
ely
o
f
0
7
°3
6
W
an
d
3
3
°3
6
′
N.
T
h
e
b
u
ild
in
g
is
m
ad
e
u
p
o
f
f
o
u
r
ex
ter
io
r
walls,
a
r
o
o
f
,
an
d
a
f
lo
o
r
.
E
ac
h
ex
te
r
io
r
wall
co
n
s
is
ts
o
f
two
p
ar
t
s
o
f
ce
m
e
n
t
m
o
r
tar
with
r
ed
b
r
ick
s
s
ep
a
r
ated
b
y
an
air
g
ap
.
T
h
e
f
lo
o
r
c
o
m
p
r
is
es
s
u
cc
ess
i
v
e
lay
er
s
o
f
lim
esto
n
e
,
h
ea
v
y
co
n
cr
ete,
p
o
ly
s
ty
r
en
e,
an
d
cl
ay
,
co
v
er
ed
with
a
lay
er
o
f
ce
m
e
n
t
m
o
r
tar
,
h
o
we
v
er
,
th
e
r
o
o
f
s
tr
u
ctu
r
e
is
co
m
p
o
s
ed
o
f
th
r
ee
lay
e
r
s
o
f
ce
m
e
n
t
m
o
r
ta
r
an
d
o
n
e
lay
er
o
f
h
ea
v
y
co
n
c
r
ete,
m
o
r
e
o
v
er
a
b
itu
m
e
n
lay
er
T
ab
le
1
.
T
h
e
to
tal
r
esis
tan
ce
o
f
th
e
e
x
ter
io
r
wall
is
1
.
8
8
3
m
2
.
K/W
,
f
o
r
th
e
r
o
o
f
is
ab
o
u
t
0
.
3
6
7
m
2
.
K/W
,
f
in
ally
,
it’s a
b
o
u
t 0
.
6
7
3
m
2
.
K/W
f
o
r
th
e
f
l
o
o
r
T
ab
le
2
.
Fig
u
r
e
1
.
Pictu
r
e
o
f
th
e
st
u
d
ied
ce
ll (
b
u
ild
in
g
)
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
t J Ad
v
Ap
p
l Sci
I
SS
N:
2252
-
8
8
1
4
E
n
h
a
n
ci
n
g
en
erg
y
efficien
cy
w
ith
p
o
n
ce
b
lo
c
a
n
d
h
emp
w
o
o
l:
a
M
o
r
o
cc
a
n
c
a
s
e
…
(
Ya
s
s
er
B
o
u
kio
u
d
)
977
2
.
2
.
T
he
clim
a
t
e
o
f
M
o
ro
cc
o
T
h
e
clim
ate
in
Mo
r
o
cc
o
is
ca
teg
o
r
ized
i
n
to
s
ix
d
is
tin
ct
c
lim
atic
zo
n
es
as
d
e
f
in
ed
b
y
Mo
r
o
cc
an
th
er
m
al
r
eg
u
latio
n
s
[
2
5
]
.
T
h
e
s
e
zo
n
es
en
co
m
p
ass
n
u
m
er
o
u
s
cities
ac
r
o
s
s
Mo
r
o
cc
o
,
as
d
ep
icted
in
Fig
u
r
e
2
.
E
ac
h
zo
n
e
r
ef
lects
v
ar
y
in
g
en
v
ir
o
n
m
en
tal
co
n
d
itio
n
s
th
at
in
f
lu
en
ce
b
u
ild
i
n
g
d
esig
n
an
d
en
er
g
y
ef
f
icien
cy
s
tr
ateg
ies
.
Fig
u
r
e
2
.
Mo
r
o
cc
an
clim
atic
zo
n
es m
ap
[
2
6
]
T
ab
le
1
.
W
all
ch
ar
ac
ter
is
tics
f
o
r
th
e
r
e
f
er
en
ce
c
o
n
f
ig
u
r
atio
n
[
2
5
]
C
e
l
l
p
a
r
t
La
y
e
r
s
Th
i
c
k
n
e
ss
(
c
m)
D
e
n
si
t
y
(
k
g
/
m
3
)
Th
e
r
m
a
l
c
o
n
d
u
c
t
i
v
i
t
y
(
W
/
m.
K
)
Th
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ig
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Ex
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l
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3
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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
-
8
8
1
4
I
n
t J Ad
v
Ap
p
l Sci
,
Vo
l.
1
3
,
No
.
4
,
Dec
em
b
er
2
0
2
4
:
974
-
98
4
978
2
.
3
.
Resea
rc
h pla
ne
T
h
e
b
u
ild
in
g
u
n
d
e
r
s
tu
d
y
is
lo
ca
ted
in
C
asab
lan
ca
,
an
d
its
c
h
ar
ac
ter
is
tics
ar
e
d
etailed
in
th
e
m
eth
o
d
s
s
ec
tio
n
.
I
n
th
is
p
a
p
er
,
we
p
r
o
p
o
s
e
a
n
ew
wall
co
n
f
i
g
u
r
atio
n
f
o
r
b
u
ild
i
n
g
s
.
T
h
is
co
n
f
ig
u
r
atio
n
will
b
e
test
ed
in
v
ar
io
u
s
s
ce
n
ar
io
s
wh
er
e
t
h
e
b
u
ild
in
g
is
l
o
ca
ted
in
A
g
ad
ir
,
Ma
r
r
ak
ec
h
,
I
f
r
an
e,
Fes
,
E
r
r
ac
h
id
ia,
an
d
T
an
g
ier
.
C
lim
atic
d
ata
f
o
r
ea
ch
zo
n
e,
p
r
o
v
id
ed
b
y
t
h
e
ME
T
E
ONORM
s
o
f
twar
e,
al
o
n
g
with
b
u
ild
i
n
g
p
ar
am
eter
s
,
will
b
e
u
s
ed
as
in
p
u
ts
f
o
r
t
h
e
d
y
n
a
m
ic
s
im
u
latio
n
s
y
s
tem
o
f
T
R
NSYS.
T
h
e
im
p
ac
t
o
f
th
e
p
r
o
p
o
s
ed
co
n
f
ig
u
r
ati
o
n
will
b
e
ass
ess
ed
b
y
ex
am
in
in
g
th
e
in
d
o
o
r
tem
p
e
r
atu
r
e
o
f
th
e
b
u
ild
i
n
g
an
d
its
c
o
o
lin
g
an
d
h
ea
tin
g
r
eq
u
ir
em
e
n
ts
.
T
h
ese
r
esu
lts
will
th
en
b
e
c
o
m
p
ar
e
d
to
a
r
ef
er
en
ce
ca
s
e
(
n
o
n
-
in
s
u
lated
b
u
ild
in
g
)
to
id
en
tify
wh
er
e
m
ax
im
u
m
e
n
er
g
y
s
av
i
n
g
s
ar
e
ac
h
iev
ed
,
th
er
e
b
y
d
e
ter
m
in
in
g
t
h
e
m
o
s
t
e
f
f
ec
tiv
e
ap
p
licatio
n
o
f
th
e
p
r
o
p
o
s
ed
co
n
f
ig
u
r
atio
n
.
Mo
r
e
d
etails
ab
o
u
t
th
e
p
r
o
p
o
s
ed
c
o
n
f
ig
u
r
atio
n
an
d
s
im
u
latio
n
p
ar
am
eter
s
will
b
e
p
r
o
v
id
e
d
in
s
u
b
s
eq
u
en
t sectio
n
s
.
2
.
4
.
T
he
s
im
ula
t
io
n a
nd
bu
il
din
g
ener
g
y
m
o
delin
g
Th
e
s
tu
d
ied
ca
s
e
was
s
im
u
lated
u
n
d
er
T
R
NSYS1
6
,
an
d
b
y
u
s
in
g
ty
p
e
5
6
u
n
d
er
th
e
m
o
d
e
T
R
NB
UI
L
D
a
s
s
h
o
wn
in
Fig
u
r
e
3
,
with
a
s
tep
o
f
1
h
o
u
r
.
T
h
e
m
o
d
el
u
s
ed
f
o
r
t
h
e
ca
lcu
latio
n
o
f
th
e
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ea
t
b
alan
ce
is
d
escr
ib
ed
in
(
1
)
.
.
=
̇
−
̇
(
1
)
W
h
er
e
C
p
is
th
e
s
p
ec
if
ic
h
ea
t,
T
int
is
th
e
in
s
id
e
tem
p
er
atu
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e
o
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th
e
ce
ll,
̇
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th
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p
o
wer
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tp
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t
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.
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eter
m
in
e
d
b
y
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u
m
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li
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r
r
elatio
n
s
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ip
b
etwe
en
t
h
e
tem
p
er
atu
r
e
ch
an
g
e
in
th
e
z
o
n
e
air
an
d
th
e
a
m
o
u
n
t
o
f
p
o
wer
s
u
p
p
lied
a
n
d
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th
e
g
lo
b
al
en
er
g
y
f
l
o
w
f
o
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o
d
e
n
.
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t
is
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d
u
s
in
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e
(
2
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.
̇
=
̇
+
̇
+
̇
+
̇
+
̇
+
̇
(
2
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W
h
er
e
̇
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ef
in
ed
as
th
e
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ate
o
f
h
ea
t
g
ai
n
r
esu
ltin
g
f
r
o
m
in
f
iltra
tio
n
an
d
v
en
tilati
o
n
ac
r
o
s
s
th
e
b
u
ild
in
g
en
v
elo
p
e,
̇
is
th
e
g
ain
d
u
e
t
o
air
f
lo
w
f
r
o
m
b
o
u
n
d
a
r
y
co
n
d
itio
n
s
.
̇
is
th
e
h
ea
t
tr
an
s
f
er
th
r
o
u
g
h
co
n
v
ec
tio
n
f
r
o
m
all
in
te
r
io
r
s
u
r
f
ac
e
s
,
̇
is
th
e
win
d
o
ws
ab
s
o
r
b
ed
s
o
lar
g
ai
n
r
ate,
̇
r
ef
er
s
to
t
h
e
r
at
e
at
wh
ich
h
ea
t
is
tr
an
s
f
er
r
e
d
ac
r
o
s
s
th
e
b
u
ild
in
g
e
n
v
elo
p
e
,
̇
r
ef
e
r
s
to
th
e
in
ter
n
al
g
ain
p
r
o
d
u
c
ed
b
y
p
e
o
p
le,
eq
u
ip
m
en
t,
illu
m
in
atio
n
,
an
d
r
ad
iato
r
s
T
h
e
E
x
p
an
d
ed
clar
if
icatio
n
co
u
ld
b
e
p
r
o
v
id
ed
b
y
th
e
T
R
NSY
S
u
s
er
m
an
u
a
l
[
2
7
]
.
Fig
u
r
e
3
.
T
R
NSYS sy
s
tem
d
iag
r
am
2
.
5
.
Sim
ula
t
i
o
n pa
ra
m
e
t
er
s
a
nd
co
ns
idera
t
io
ns
I
n
th
is
in
s
tan
ce
,
th
e
ca
lcu
latio
n
s
ar
e
p
er
f
o
r
m
ed
o
v
er
a
o
n
e
-
y
ea
r
p
er
io
d
,
co
m
m
e
n
cin
g
o
n
J
a
n
u
ar
y
1
st
an
d
e
n
d
in
g
at
m
id
n
i
g
h
t
o
n
De
ce
m
b
er
3
1
st
.
T
h
e
s
im
u
latio
n
was
co
n
d
u
cte
d
with
th
e
f
o
llo
wi
n
g
p
a
r
am
eter
s
:
th
e
tem
p
er
atu
r
e
in
s
id
e
th
e
ce
ll
wa
s
s
et
to
f
lu
ct
u
ate
b
etwe
en
2
0
a
n
d
2
6
°C
d
u
e
to
t
h
e
o
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er
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n
o
f
th
e
co
o
lin
g
an
d
h
ea
tin
g
eq
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ip
m
en
t,
with
in
f
i
ltra
tio
n
f
ix
ed
at
ap
p
r
o
x
im
ate
ly
0
.
5
l/h
.
T
h
e
in
itial
co
n
d
i
tio
n
s
ar
e
s
et
to
a
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
t J Ad
v
Ap
p
l Sci
I
SS
N:
2252
-
8
8
1
4
E
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n
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w
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h
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ter
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f
r
o
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th
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in
h
ab
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n
s
id
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to
b
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n
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lig
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le.
T
h
e
walls
an
d
r
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f
s
ar
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esti
m
ated
to
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e
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o
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ter
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ef
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icien
t o
f
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9
.
T
h
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c
ell
i
s
eq
u
ip
p
ed
with
a
lam
p
th
at
g
en
er
ates 5
W
/m
²
o
f
in
ter
n
al
h
ea
t,
an
d
th
e
d
o
o
r
s
an
d
win
d
o
ws
r
em
ain
clo
s
ed
at
all
tim
e
s
.
T
R
NSYS
1
6
will
h
an
d
le
th
es
e
co
n
s
id
er
atio
n
s
an
d
g
en
e
r
ate
in
p
u
t p
ar
am
ete
r
s
b
ased
o
n
th
em
.
2
.
6
.
T
he
inv
estig
a
t
ed
co
nfig
ura
t
io
n
Fig
u
r
e
4
s
h
o
w
s
t
h
e
s
u
g
g
ested
co
n
f
ig
u
r
atio
n
f
o
r
th
e
r
o
o
f
an
d
ex
ter
n
al
wall
,
Fig
u
r
e
4
(
a
)
p
r
o
p
o
s
ed
co
n
f
ig
u
r
atio
n
in
v
o
lv
es
in
teg
r
a
tin
g
a
lay
er
o
f
2
4
cm
o
f
p
o
n
c
eb
lo
c
with
two
1
.
5
cm
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ick
l
ay
er
s
o
f
h
em
p
wo
o
l
in
th
e
ex
ter
io
r
wall.
A
d
d
itio
n
a
lly
,
in
Fig
u
r
e
4
(
b
)
a
lay
er
o
f
3
cm
o
f
h
e
m
p
wo
o
l
will
b
e
in
te
g
r
ated
in
to
t
h
e
r
o
o
f
s
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ctu
r
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b
etwe
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e
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n
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n
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h
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co
n
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ig
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will
b
e
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tak
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g
in
to
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n
s
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e
g
lazin
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e
f
f
e
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s
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m
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tio
n
.
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o
u
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g
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ch
o
s
en
f
o
r
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is
co
n
f
ig
u
r
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n
d
u
e
to
its
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w
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-
v
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e
an
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c
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f
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m
p
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th
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es
o
f
g
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.
T
a
b
l
e
3
p
r
o
v
i
d
es
m
o
r
e
in
f
o
r
m
atio
n
ab
o
u
t th
e
s
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g
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ested
s
tr
u
ctu
r
e
,
a
n
d
T
a
b
le
4
d
escr
ib
es th
e
s
ix
clim
ate
zo
n
es.
(
a)
(
b
)
Fig
u
r
e
4
.
Su
g
g
ested
co
n
f
ig
u
r
a
tio
n
in
r
o
o
f
a
n
d
ex
ter
n
al
wall
(
a)
r
o
o
f
co
n
f
ig
u
r
atio
n
an
d
(
b
)
e
x
ter
n
al
wall
co
n
f
ig
u
r
atio
n
T
ab
le
3
.
W
all
ch
ar
ac
ter
is
tics
f
o
r
th
e
s
u
g
g
ested
co
n
f
i
g
u
r
atio
n
C
e
l
l
p
a
r
t
La
y
e
r
s
Th
i
c
k
n
e
ss
(
c
m)
D
e
n
si
t
y
(
k
g
/
m
3
)
Th
e
r
m
a
l
c
o
n
d
u
c
t
i
v
i
t
y
(
W
/
m.
K
)
Th
e
r
m
a
l
c
a
p
a
c
i
t
y
(
k
J/
k
g
.
K
)
S
t
r
u
c
t
u
r
e
Ex
t
e
r
i
o
r
w
a
l
l
C
e
me
n
t
mo
r
t
a
r
1
1
,
7
0
0
1
.
1
5
1
H
e
mp
w
o
o
l
1
.
5
35
0
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0
4
1
.
2
P
o
n
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e
b
l
o
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24
3
6
5
0
.
1
2
6
1
H
e
mp
w
o
o
l
1
.
5
35
0
.
0
4
1
.
2
C
e
me
n
t
mo
r
t
a
r
1
1
,
7
0
0
1
.
1
5
1
R
o
o
f
C
e
me
n
t
mo
r
t
a
r
2
1
,
7
0
0
1
.
1
5
1
H
e
a
v
y
c
o
n
c
r
e
t
e
12
2
,
3
0
0
1
.
7
5
0
.
9
2
H
e
mp
w
o
o
l
3
35
0
.
0
4
1
.
2
C
e
me
n
t
mo
r
t
a
r
2
1
,
7
0
0
1
.
1
5
1
B
i
t
u
m
e
n
3
1
,
7
0
0
0
.
5
1
C
e
me
n
t
mo
r
t
a
r
2
1
,
7
0
0
1
.
1
5
1
T
ab
le
4
.
Stu
d
ied
clim
ate
d
escr
ip
tio
n
[
2
8
]
C
i
t
y
A
g
a
d
i
r
M
a
r
r
a
k
e
c
h
I
f
r
a
n
e
F
e
s
Er
r
a
c
h
i
d
i
a
Ta
n
g
i
e
r
A
l
t
i
t
u
d
e
(
m)
56
4
6
0
1
6
6
5
4
1
5
1
0
8
4
80
Lo
n
g
i
t
u
d
e
-
9
.
5
9
°
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7
.
9
9
°
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5
.
2
°
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0
0
°
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La
t
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t
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.
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3
4
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°
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3
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5
.
7
7
°
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C
l
i
ma
t
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A
t
l
a
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r
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t
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sert
M
e
d
i
t
e
r
r
a
n
e
a
n
T
m
a
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(
°
C
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4
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0
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4
0
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8
4
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6
2
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2
6
T
min
(
°
C
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3
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2
9
3
.
7
-
5
0
.
1
1
0
.
6
3
3
.
0
7
2
.
7
.
Resea
rc
h o
bje
ct
i
v
es a
nd
s
co
pe
T
h
e
ar
ticle
aim
s
t
o
in
v
esti
g
ate
th
e
e
f
f
ec
t
o
f
th
e
s
u
g
g
ested
ca
s
e.
I
n
t
h
e
f
ir
s
t
s
ec
tio
n
,
it
will
d
is
cu
s
s
th
e
in
f
lu
en
ce
o
f
t
h
is
s
u
g
g
esti
o
n
o
n
th
e
tem
p
er
atu
r
e
i
n
s
id
e
th
e
ce
ll.
T
h
e
ce
ll
tem
p
er
atu
r
e
f
o
r
b
o
th
co
n
f
ig
u
r
atio
n
s
Evaluation Warning : The document was created with Spire.PDF for Python.
I
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-
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4
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v
Ap
p
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,
Vo
l.
1
3
,
No
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4
,
Dec
em
b
er
2
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r
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ig
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g
s
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at
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b
e
ac
h
iev
ed
b
y
u
s
in
g
th
is
co
n
f
ig
u
r
atio
n
in
th
e
b
u
ild
in
g
.
T
h
e
s
tu
d
y
will
b
e
c
o
n
d
u
cted
in
t
h
e
s
ix
Mo
r
o
cc
an
zo
n
es
to
d
eter
m
in
e
wh
e
r
e
th
e
m
a
x
im
u
m
an
d
m
in
im
u
m
s
av
in
g
s
ca
n
b
e
ac
h
iev
ed
.
2
.
8
.
Sim
ula
t
i
o
n v
a
lid
a
t
io
n
I
n
o
r
d
er
to
en
s
u
r
e
th
e
ac
cu
r
a
cy
o
f
o
u
r
s
im
u
latio
n
p
r
o
g
r
am
,
we
c
o
n
d
u
cted
a
v
alid
atio
n
s
im
u
latio
n
b
ased
o
n
th
e
s
tu
d
y
b
y
Mo
u
r
i
d
et
a
l.
[
2
9
]
,
wh
o
p
er
f
o
r
m
ed
an
ex
p
er
im
en
tal
s
tu
d
y
o
n
a
b
u
il
d
i
n
g
in
C
asab
lan
ca
.
T
h
e
v
alid
atio
n
s
im
u
latio
n
was
ca
r
r
ied
o
u
t
o
v
er
th
r
ee
d
a
y
s
,
f
r
o
m
Ap
r
il
2
0
to
Ap
r
il
2
3
,
2
0
1
4
.
T
ab
le
5
p
r
o
v
id
es
in
f
o
r
m
atio
n
o
n
th
e
tem
p
er
at
u
r
e
d
if
f
er
e
n
ce
s
b
etwe
en
th
e
e
x
p
er
im
en
tal
d
ata
r
ep
o
r
ted
[
2
9
]
a
n
d
th
e
tem
p
er
at
u
r
es
o
b
tain
ed
f
r
o
m
o
u
r
s
im
u
latio
n
.
T
ab
le
5
also
in
clu
d
es th
e
r
elativ
e
er
r
o
r
ass
o
ciate
d
with
ea
ch
t
im
e
v
alu
e.
T
ab
le
5
.
C
o
m
p
a
r
is
o
n
o
f
in
d
o
o
r
air
tem
p
er
atu
r
es
s
im
u
lated
v
s
m
ea
s
u
r
ed
d
ata
Ti
me
(
h
)
ΔT
(
°
C
)
e
r
(
%)
4
0
.
4
2
.
1
7
8
0
.
4
5
2
.
5
16
-
0
.
5
2
.
2
7
24
0
.
7
8
3
.
6
6
32
0
.
7
7
4
.
0
5
54
0
.
1
5
4
.
0
5
64
-
0
.
3
5
1
.
7
7
Fro
m
T
ab
le
5
,
we
ca
n
o
b
s
er
v
e
th
at
th
e
d
if
f
er
en
ce
b
etwe
en
th
e
ex
p
er
im
en
tal
an
d
s
im
u
latio
n
r
esu
lts
i
s
n
o
t
s
ig
n
if
ican
t,
as
in
d
icate
d
b
y
th
e
r
elativ
e
er
r
o
r
v
alu
es,
w
h
ich
ar
e
all
less
th
an
5
%.
T
h
i
s
s
u
g
g
ests
th
at
o
u
r
s
im
u
latio
n
m
o
d
el
p
r
o
v
id
es
ac
cu
r
ate
r
esu
lts
with
s
u
f
f
icien
t
p
r
ec
is
i
o
n
.
T
h
er
e
f
o
r
e,
we
ca
n
co
n
clu
d
e
t
h
at
th
e
r
esu
lts
p
r
o
d
u
ce
d
b
y
t
h
is
m
o
d
el
alig
n
well
with
th
e
ex
p
er
i
m
en
tal
d
ata.
C
o
n
s
eq
u
en
tly
,
we
ca
n
r
ely
o
n
th
is
m
o
d
el
f
o
r
o
u
r
in
v
esti
g
atio
n
an
d
to
d
eter
m
i
n
e
th
e
im
p
ac
t o
f
u
s
in
g
th
e
p
r
o
p
o
s
ed
c
o
n
f
ig
u
r
atio
n
in
th
e
b
u
ild
in
g
.
3.
R
E
SU
L
T
S AN
D
D
I
SCU
SS
I
O
N
3
.
1
.
T
em
pera
t
ure
ins
ide t
he
ce
ll
Pre
v
io
u
s
s
tu
d
ies
h
av
e
ex
p
lo
r
e
d
th
e
im
p
ac
t
o
f
d
if
f
er
e
n
t
in
s
u
latio
n
m
ater
ials
o
n
in
d
o
o
r
te
m
p
er
atu
r
e
v
ar
iatio
n
s
an
d
a
n
n
u
al
b
u
ild
in
g
lo
ad
s
.
Ho
wev
er
,
m
o
s
t
r
esea
r
ch
d
o
es
n
o
t
in
v
esti
g
ate
th
e
i
m
p
ac
t
o
f
c
o
m
b
in
in
g
d
if
f
er
en
t
in
s
u
latio
n
m
ater
ials
,
u
n
lik
e
o
u
r
s
tu
d
y
.
T
h
e
in
d
o
o
r
tem
p
er
atu
r
e
was
ca
lcu
lated
u
s
in
g
th
e
s
im
u
latio
n
p
r
o
g
r
a
m
.
I
t
ca
n
b
e
o
b
s
er
v
e
d
f
r
o
m
Fig
u
r
e
5
wh
ich
illu
s
tr
ates
th
e
tem
p
er
atu
r
e
v
a
r
iatio
n
s
th
r
o
u
g
h
o
u
t
th
e
y
ea
r
,
th
at
th
e
tem
p
er
at
u
r
e
o
f
th
e
p
r
o
p
o
s
e
d
c
o
n
f
ig
u
r
atio
n
(
T
_
s
c)
i
s
lo
wer
th
an
in
th
e
r
e
f
er
en
ce
ca
s
e
(
T
_
r
ef
)
d
u
r
in
g
h
o
t
s
ea
s
o
n
s
,
b
u
t
h
ig
h
er
d
u
r
i
n
g
th
e
co
ld
s
ea
s
o
n
.
Ad
d
itio
n
ally
,
th
e
d
if
f
er
en
ce
b
etwe
en
th
e
r
ef
er
e
n
ce
ca
s
e
tem
p
er
atu
r
e
a
n
d
th
e
p
r
o
p
o
s
ed
ca
s
e
tem
p
er
atu
r
e
v
a
r
ies f
r
o
m
c
ity
to
city
an
d
f
r
o
m
s
ea
s
o
n
to
s
ea
s
o
n
.
Fo
r
th
e
co
ld
s
ea
s
o
n
,
th
e
s
m
allest
d
if
f
er
en
ce
b
etwe
en
th
e
two
s
ce
n
ar
io
s
i
s
o
b
s
er
v
ed
in
Ag
ad
ir
(
Fig
u
r
e
5
(
a)
)
.
I
n
co
n
tr
ast,
f
o
r
t
h
e
h
o
t
s
ea
s
o
n
,
th
e
lar
g
est
d
if
f
e
r
en
ce
is
n
o
ted
in
Ma
r
r
ak
ec
h
(
Fig
u
r
e
5
(
b
)
)
.
I
n
th
e
co
ld
clim
ate,
th
e
m
ax
im
u
m
d
i
f
f
er
en
ce
is
o
b
s
er
v
ed
in
I
f
r
an
e
(
Fig
u
r
e
5
(
c)
)
,
wh
ile
Fes
(
Fig
u
r
e
5
(
d
)
)
s
h
o
ws
th
e
s
ec
o
n
d
s
m
allest
d
if
f
er
en
ce
,
f
o
llo
win
g
Ag
ad
i
r
.
Fo
r
th
e
h
o
t
clim
ate,
E
r
r
ac
h
id
ia
(
Fig
u
r
e
5
(
e)
)
p
r
esen
ts
th
e
s
ec
o
n
d
s
m
allest
d
if
f
er
en
ce
,
af
ter
Ma
r
r
ak
ec
h
.
T
h
e
r
ef
o
r
e
,
th
e
s
u
g
g
ested
co
n
f
ig
u
r
atio
n
is
a
g
o
o
d
s
o
lu
tio
n
b
ec
au
s
e
it
p
r
o
v
i
d
es
g
o
o
d
co
m
f
o
r
t,
esp
ec
ially
in
co
ld
an
d
h
o
t
clim
ates,
wh
er
e
ac
h
iev
in
g
c
o
m
f
o
r
t
is
d
if
f
icu
lt.
An
o
th
er
o
b
s
er
v
ati
o
n
is
th
at
i
n
th
e
s
u
g
g
ested
ca
s
e,
th
e
te
m
p
er
atu
r
e
f
lu
ct
u
atio
n
co
m
p
a
r
ed
to
th
e
am
b
ien
t
tem
p
er
atu
r
e
is
less
th
an
in
th
e
r
ef
er
en
ce
ca
s
e.
Sp
ec
if
ically
,
it
is
ar
o
u
n
d
1
7
.
5
1
°C
in
Ag
ad
ir
(
Fig
u
r
e
5
(
a
)
)
,
2
3
.
5
9
°C
in
Ma
r
r
ak
ec
h
(
Fig
u
r
e
5
(
b
)
)
,
2
6
.
3
7
°C
in
I
f
r
an
e
(
Fig
u
r
e
5
(
c)
)
,
2
5
.
0
1
°C
in
Fes
(
Fig
u
r
e
5
(
d
)
)
,
2
7
.
5
9
°C
in
E
r
r
ac
h
id
ia
(
Fig
u
r
e
5
(
e
)
)
,
an
d
2
0
.
2
9
°C
in
T
a
n
g
ier
(
Fig
u
r
e
5
(
f
)
)
.
I
n
co
n
tr
a
s
t,
in
th
e
r
ef
er
e
n
ce
co
n
f
ig
u
r
atio
n
,
we
o
b
s
er
v
ed
2
1
.
1
6
°C
in
Ag
a
d
ir
,
2
7
.
1
5
°C
in
Ma
r
r
a
k
ec
h
,
3
0
.
4
2
°C
in
I
f
r
a
n
e,
2
9
.
3
9
°C
in
Fes
,
3
1
.
2
8
°C
in
E
r
r
ac
h
id
ia,
a
n
d
f
in
ally
2
4
°C
in
T
an
g
ier
.
T
h
ese
r
esu
lts
d
em
o
n
s
tr
a
te
th
at
th
is
co
n
f
ig
u
r
atio
n
m
ain
tain
s
co
m
f
o
r
tab
le
in
d
o
o
r
co
n
d
itio
n
s
.
T
h
e
p
r
o
p
o
s
ed
s
e
tu
p
en
s
u
r
es
a
h
ig
h
lev
el
o
f
co
m
f
o
r
t
r
eg
ar
d
in
g
in
d
o
o
r
tem
p
er
atu
r
es,
wh
ich
r
e
m
ain
s
s
tab
le
an
d
p
leasan
t d
esp
ite
wea
th
er
f
lu
ctu
atio
n
s
.
3
.
2
.
H
ea
t
ing
a
nd
co
o
lin
g
needs
On
e
way
to
ev
alu
ate
th
e
ef
f
ec
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a
wall
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ig
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ild
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g
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ex
am
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co
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p
o
wer
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n
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m
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tio
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d
d
eter
m
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e
th
e
p
o
ten
tial
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er
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y
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av
in
g
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o
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th
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et
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I
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8
8
1
4
E
n
h
a
n
ci
n
g
en
erg
y
efficien
cy
w
ith
p
o
n
ce
b
lo
c
a
n
d
h
emp
w
o
o
l:
a
M
o
r
o
cc
a
n
c
a
s
e
…
(
Ya
s
s
er
B
o
u
kio
u
d
)
981
f
r
o
m
2
0
-
2
6
°C
.
Hea
tin
g
was
ac
tiv
ated
wh
en
th
e
tem
p
e
r
atu
r
e
f
ell
b
elo
w
2
0
°C
,
wh
ile
co
o
lin
g
was
tr
ig
g
er
ed
wh
en
th
e
tem
p
er
at
u
r
e
r
o
s
e
a
b
o
v
e
2
6
°C
.
T
h
e
s
im
u
latio
n
was
co
n
d
u
cted
o
v
er
a
o
n
e
-
y
ea
r
p
er
i
o
d
,
with
o
u
t
tak
in
g
in
to
ac
co
u
n
t
th
e
p
r
esen
ce
o
f
o
cc
u
p
a
n
ts
.
T
h
e
r
esu
lts
o
b
tain
ed
f
r
o
m
th
e
s
u
g
g
ested
co
n
f
ig
u
r
atio
n
s
will
b
e
co
m
p
ar
ed
to
t
h
e
r
e
f
er
en
ce
ca
s
e
wh
er
e
s
im
p
le
g
lazin
g
is
u
s
ed
.
Ag
ad
ir
is
a
city
in
Mo
r
o
cc
o
with
a
u
n
i
q
u
e
Atlan
tic
clim
ate,
ch
ar
ac
ter
ize
d
b
y
co
ld
tem
p
er
atu
r
es
d
u
r
i
n
g
th
e
win
ter
s
ea
s
o
n
an
d
a
g
r
ea
ter
d
em
an
d
f
o
r
h
ea
tin
g
th
an
c
o
o
lin
g
.
I
n
t
h
is
s
tu
d
y
,
we
in
v
esti
g
ate
th
e
ef
f
ec
ti
v
en
ess
o
f
a
s
u
g
g
ested
c
o
n
f
ig
u
r
atio
n
f
o
r
r
ed
u
cin
g
en
er
g
y
c
o
n
s
u
m
p
ti
o
n
in
v
ar
io
u
s
Mo
r
o
cc
an
cities.
Fro
m
th
e
r
esu
lts
p
r
esen
ted
in
Fig
u
r
e
6
,
it
is
ev
i
d
en
t
t
h
at
th
e
p
r
o
p
o
s
ed
co
n
f
ig
u
r
atio
n
ca
n
s
i
g
n
if
ican
tly
r
ed
u
ce
e
n
er
g
y
co
n
s
u
m
p
tio
n
f
o
r
b
o
th
h
ea
tin
g
an
d
co
o
lin
g
p
u
r
p
o
s
es.
Sp
ec
if
ically
,
th
e
co
n
f
ig
u
r
atio
n
r
e
d
u
ce
s
h
ea
tin
g
r
e
q
u
ir
em
en
ts
b
y
5
4
.
6
%
an
d
co
o
lin
g
r
e
q
u
ir
em
e
n
ts
b
y
5
2
.
6
%
in
Ag
a
d
ir
(
Fig
u
r
e
6
(
a)
)
,
r
esu
ltin
g
in
a
to
tal
en
er
g
y
s
av
in
g
s
o
f
5
4
.
1
%.
Similar
ly
,
in
Ma
r
r
ak
ec
h
(
Fig
u
r
e
6
(
b
)
)
,
t
h
e
co
n
f
ig
u
r
atio
n
ac
h
iev
es
to
tal
s
av
in
g
s
o
f
5
3
.
3
%,
with
a
r
e
d
u
ctio
n
o
f
5
4
% in
h
ea
tin
g
an
d
5
2
.
6
% in
co
o
lin
g
.
Fo
r
cities
w
ith
co
ld
er
clim
ates
s
u
ch
as
I
f
r
an
e
(
Fig
u
r
e
6
(
c)
)
,
th
e
in
teg
r
atio
n
o
f
p
o
n
ce
b
lo
c
with
h
em
p
wo
o
l
r
esu
lts
in
a
to
tal
lo
ad
s
a
v
in
g
s
o
f
5
2
.
5
%,
with
5
2
.
3
%
s
av
in
g
s
in
h
ea
tin
g
a
n
d
5
4
.
3
%
in
co
o
lin
g
.
I
n
Fes
(
Fig
u
r
e
6
(
d
)
)
,
a
to
tal
s
av
in
g
s
o
f
5
3
.
1
%
is
ac
h
iev
e
d
,
with
5
3
%
in
h
ea
tin
g
a
n
d
5
3
.
5
%
in
co
o
lin
g
.
I
n
E
r
r
ac
h
id
ia
(
Fig
u
r
e
6
(
e)
)
,
s
av
in
g
s
o
f
5
3
.
3
%
an
d
5
0
.
8
%
a
r
e
o
b
tain
ed
f
o
r
h
ea
tin
g
an
d
co
o
li
n
g
,
r
esp
ec
tiv
ely
,
r
esu
ltin
g
in
a
to
tal
s
av
in
g
s
o
f
5
1
.
9
%.
I
n
T
an
g
ier
(
Fig
u
r
e
6
(
f
)
)
,
th
e
n
ew
co
n
f
ig
u
r
atio
n
ac
h
iev
es
a
to
t
al
s
av
in
g
s
o
f
ab
o
u
t
5
4
.
4
%,
with
5
3
.
8
%
in
h
ea
ti
n
g
an
d
5
6
.
5
%
in
co
o
lin
g
.
Ov
er
all,
th
e
r
esu
lts
in
d
icate
th
at
th
e
s
u
g
g
ested
co
n
f
ig
u
r
atio
n
is
ef
f
ec
tiv
e
in
r
ed
u
cin
g
e
n
er
g
y
co
n
s
u
m
p
tio
n
an
d
ac
h
iev
in
g
s
ig
n
if
ican
t
s
av
i
n
g
s
in
h
ea
tin
g
a
n
d
co
o
lin
g
n
ee
d
s
in
v
ar
i
o
u
s
Mo
r
o
cc
an
cities.
T
h
ese
f
in
d
i
n
g
s
co
u
ld
h
av
e
s
ig
n
if
ican
t
im
p
l
i
ca
tio
n
s
f
o
r
en
er
g
y
co
n
s
er
v
atio
n
a
n
d
c
o
s
t sav
in
g
s
in
th
e
r
eg
io
n
.
(
a)
(
b
)
(
c)
(
d
)
(
e)
(f)
Fig
u
r
e
5
.
An
n
u
al
v
a
r
iatio
n
o
f
am
b
ien
t te
m
p
er
at
u
r
e,
in
s
id
e
te
m
p
er
atu
r
e
i
n
th
e
r
e
f
er
en
ce
ca
s
e
,
an
d
in
s
id
e
tem
p
er
atu
r
e
in
s
u
g
g
ested
ca
s
e
o
f
(
a)
A
g
ad
ir
,
(
b
)
Ma
r
r
ak
ec
h
,
(
c)
I
f
r
a
n
e
,
(
d
)
Fes
,
(
e)
E
r
r
ac
h
i
d
ia
,
an
d
(f)
T
a
n
g
ier
R
esu
lts
an
aly
s
is
in
d
icate
s
th
at
th
e
p
r
o
p
o
s
ed
co
n
f
ig
u
r
atio
n
y
ield
s
s
ig
n
i
f
ican
t
en
e
r
g
y
s
av
in
g
s
in
v
ar
io
u
s
clim
atic
r
eg
io
n
s
,
alb
e
it
with
v
ar
y
in
g
ef
f
icien
c
y
lev
els.
No
tab
ly
,
Ag
ad
ir
d
is
p
lay
s
th
e
h
ig
h
est
h
ea
tin
g
s
av
in
g
s
,
wh
ile
I
f
r
an
e
s
h
o
ws
th
e
lo
west.
C
o
n
v
er
s
ely
,
T
an
g
ier
d
em
o
n
s
tr
ates
th
e
h
ig
h
est
co
o
lin
g
s
av
in
g
s
,
wh
ile
E
r
r
ac
h
id
ia
h
as
th
e
lo
west.
I
n
g
en
er
al,
th
e
co
n
f
i
g
u
r
atio
n
p
r
o
v
es
to
b
e
m
o
r
e
ef
f
ec
tiv
e
i
n
T
an
g
ier
an
d
less
ef
f
ec
tiv
e
in
E
r
r
ac
h
i
d
ia.
T
h
ese
f
in
d
in
g
s
u
n
d
er
s
co
r
e
th
e
im
p
o
r
tan
ce
o
f
tailo
r
in
g
en
er
g
y
-
ef
f
icien
t
s
o
lu
tio
n
s
to
lo
ca
l
co
n
d
itio
n
s
.
Ad
d
itio
n
ally
,
th
e
im
p
lem
e
n
tatio
n
o
f
th
e
s
u
g
g
ested
co
n
f
ig
u
r
atio
n
ca
n
lea
d
to
s
u
b
s
tan
tial
co
s
t
s
av
in
g
s
an
d
r
ed
u
ce
d
elec
tr
icity
b
ills
,
m
ak
in
g
it
a
p
r
ac
tical
an
d
s
u
s
tain
ab
le
s
o
lu
tio
n
f
o
r
ad
d
r
ess
in
g
h
ea
tin
g
an
d
co
o
lin
g
r
e
q
u
ir
em
e
n
ts
in
d
iv
er
s
e
clim
atic
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n
es.
Desp
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te
th
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atu
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u
s
er
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ie
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ly
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ch
ar
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ter
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th
e
m
ater
ials
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s
e
d
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th
e
p
r
o
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o
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n
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g
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r
atio
n
,
alo
n
g
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th
eir
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aig
h
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r
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ater
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ativ
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t
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o
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e
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ep
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3
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n
d
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2
2
5
2
-
8
8
1
4
I
n
t J Ad
v
Ap
p
l Sci
,
Vo
l.
1
3
,
No
.
4
,
Dec
em
b
er
2
0
2
4
:
974
-
98
4
982
en
v
ir
o
n
m
en
tal
im
p
ac
ts
,
p
ar
ticu
lar
ly
in
ter
m
s
o
f
co
s
t
-
ef
f
ec
t
iv
en
ess
an
d
s
u
s
tain
ab
ilit
y
.
C
o
m
p
ar
ativ
e
s
tu
d
ies
ac
r
o
s
s
v
ar
io
u
s
clim
ate
ty
p
es
a
r
e
al
s
o
ess
en
tial.
Fu
tu
r
e
r
esear
ch
s
h
o
u
ld
co
n
s
id
er
th
ese
asp
ec
ts
to
p
r
o
m
o
te
t
h
e
ad
o
p
tio
n
o
f
c
o
m
b
in
e
d
in
s
u
latio
n
s
o
lu
tio
n
s
.
(
a)
(
b
)
(
c)
(
d
)
(
e)
(f)
Fig
u
r
e
6
.
C
o
m
p
a
r
is
o
n
b
etwe
e
n
th
e
an
n
u
al
co
n
s
u
m
p
tio
n
f
o
r
h
ea
tin
g
an
d
co
o
lin
g
f
o
r
b
o
th
r
ef
er
en
ce
an
d
s
u
g
g
ested
co
n
f
i
g
u
r
atio
n
f
o
r
(
a
)
Ag
ad
ir
,
(
b
)
Ma
r
r
ak
ec
h
,
(
c)
I
f
r
an
e
,
(
d
)
Fes
(
e)
,
E
r
r
ac
h
id
ia
,
a
n
d
(
f
)
T
an
g
ie
r
4.
CO
NCLU
SI
O
N
T
h
e
p
r
esen
t
s
tu
d
y
em
p
l
o
y
ed
a
d
y
n
am
ic
s
im
u
latio
n
a
p
p
r
o
ac
h
u
s
in
g
T
R
NSYS
to
in
v
es
tig
ate
th
e
ef
f
ec
ts
o
f
co
m
b
in
in
g
d
if
f
er
e
n
t
m
ater
ials
in
b
u
ild
in
g
co
n
s
tr
u
c
tio
n
.
Sp
ec
if
ically
,
p
o
n
ce
b
lo
c
was
co
m
b
in
ed
with
h
em
p
wo
o
l,
a
n
at
u
r
al
in
s
u
latio
n
m
ater
ial,
in
b
o
th
t
h
e
b
u
il
d
i
n
g
'
s
r
o
o
f
an
d
ex
ter
io
r
wall
d
u
e
to
th
eir
f
av
o
r
a
b
le
lo
w
th
er
m
al
co
n
d
u
ctiv
ity
p
r
o
p
er
ties
.
T
h
e
o
b
jectiv
e
o
f
th
is
s
tu
d
y
was
to
e
v
alu
ate
th
e
i
m
p
ac
t
o
f
in
teg
r
atin
g
b
o
th
m
in
er
al
an
d
n
atu
r
al
in
s
u
l
atio
n
m
ater
ials
.
T
h
e
an
aly
s
is
co
m
m
en
ce
d
with
a
th
e
r
m
al
b
e
h
av
io
r
as
s
ess
m
en
t,
with
th
e
in
ter
n
al
tem
p
e
r
atu
r
e
o
f
th
e
b
u
ild
i
n
g
ce
ll
b
ein
g
th
e
p
r
im
ar
y
p
ar
am
ete
r
.
T
h
e
f
i
n
d
in
g
s
in
d
icate
th
at
th
e
in
s
id
e
tem
p
er
atu
r
e
was
h
ig
h
er
in
th
e
s
u
g
g
ested
ca
s
e
co
m
p
ar
ed
to
th
e
r
ef
er
en
ce
d
u
r
in
g
th
e
co
ld
s
ea
s
o
n
,
wh
ile
it
was
lo
wer
in
th
e
p
r
o
p
o
s
e
d
ca
s
e
th
an
th
e
r
ef
er
e
n
ce
d
u
r
in
g
t
h
e
h
o
t
s
ea
s
o
n
.
Fu
r
th
e
r
m
o
r
e,
t
h
e
r
esu
lts
d
em
o
n
s
tr
ate
th
at
th
e
p
r
o
p
o
s
ed
ca
s
e
p
r
o
v
id
es
less
tem
p
er
atu
r
e
f
lu
ctu
atio
n
t
h
r
o
u
g
h
o
u
t
th
e
y
ea
r
,
th
u
s
en
s
u
r
i
n
g
g
r
ea
ter
c
o
m
f
o
r
t
in
s
id
e
t
h
e
ce
ll
.
T
h
e
s
tu
d
y
also
d
is
co
v
e
r
ed
th
at
th
e
m
i
n
im
u
m
f
lu
ctu
atio
n
v
alu
e
was
o
b
s
er
v
ed
in
Ag
ad
ir
,
wh
ile
th
e
m
ax
im
u
m
was r
ec
o
r
d
ed
in
E
r
r
ac
h
id
ia.
I
n
th
e
s
ec
o
n
d
s
ec
tio
n
,
we
e
v
alu
ated
th
e
ef
f
icien
c
y
o
f
th
e
p
r
o
p
o
s
ed
b
u
ild
in
g
co
n
f
ig
u
r
atio
n
an
d
in
v
esti
g
ated
its
im
p
ac
t
o
n
h
ea
tin
g
an
d
co
o
lin
g
n
ee
d
s
.
O
u
r
r
esu
lts
s
h
o
w
a
s
ig
n
if
ican
t
d
ec
r
ea
s
e
in
t
h
ese
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
t J Ad
v
Ap
p
l Sci
I
SS
N:
2252
-
8
8
1
4
E
n
h
a
n
ci
n
g
en
erg
y
efficien
cy
w
ith
p
o
n
ce
b
lo
c
a
n
d
h
emp
w
o
o
l:
a
M
o
r
o
cc
a
n
c
a
s
e
…
(
Ya
s
s
er
B
o
u
kio
u
d
)
983
r
eq
u
ir
em
e
n
ts
,
r
esu
ltin
g
in
en
er
g
y
s
av
in
g
s
th
at
v
ar
y
ac
r
o
s
s
d
if
f
er
en
t
clim
atic
zo
n
es.
T
h
e
m
ax
im
u
m
en
er
g
y
s
av
in
g
s
in
h
ea
ti
n
g
wer
e
o
b
s
er
v
ed
i
n
Ag
a
d
ir
,
with
a
r
e
d
u
ctio
n
o
f
ab
o
u
t
5
4
.
6
%,
wh
ile
th
e
lo
west
en
e
r
g
y
s
av
in
g
s
wer
e
r
ec
o
r
d
e
d
in
I
f
r
a
n
e,
with
a
r
ed
u
ctio
n
o
f
ab
o
u
t
5
2
.
3
%.
Similar
ly
,
th
e
h
ig
h
es
t
v
alu
e
o
f
c
o
o
lin
g
s
av
in
g
s
was
f
o
u
n
d
in
T
a
n
g
ier
,
with
a
r
ed
u
ctio
n
o
f
5
6
.
5
%,
wh
ile
th
e
lo
west
o
n
e
was
r
ec
o
r
d
ed
in
E
r
r
ac
h
i
d
ia,
with
a
r
ed
u
ctio
n
o
f
5
0
.
8
%.
B
a
s
ed
o
n
th
ese
f
in
d
in
g
s
,
we
co
n
clu
d
e
th
at
th
e
p
r
o
p
o
s
ed
b
u
ild
i
n
g
c
o
n
f
ig
u
r
atio
n
is
m
o
r
e
ef
f
ec
tiv
e
in
T
an
g
ier
,
with
a
to
tal
en
er
g
y
s
av
in
g
o
f
5
4
.
4
%,
wh
ile
it i
s
les
s
ef
f
ec
tiv
e
in
E
r
r
ac
h
id
ia.
Desp
ite
th
e
v
ar
iatio
n
in
ef
f
icien
c
y
d
e
p
en
d
in
g
o
n
th
e
clim
ate
zo
n
e,
th
e
s
u
g
g
ested
co
n
f
ig
u
r
atio
n
p
r
o
v
id
es
s
i
g
n
if
ican
t
en
er
g
y
s
av
in
g
s
in
all
clim
atic
zo
n
es in
Mo
r
o
cc
o
.
I
n
co
n
clu
s
i
o
n
,
th
e
p
r
o
p
o
s
ed
co
n
f
ig
u
r
atio
n
is
an
ef
f
ec
tiv
e
an
d
ef
f
icien
t
s
o
lu
tio
n
in
ter
m
s
o
f
b
o
t
h
in
d
o
o
r
c
o
m
f
o
r
t
an
d
en
er
g
y
s
av
in
g
s
.
T
h
is
s
tu
d
y
d
em
o
n
s
tr
ates
th
at
in
co
r
p
o
r
atin
g
m
u
ltip
le
ty
p
es
o
f
in
s
u
latio
n
m
ater
ials
with
in
a
b
u
ild
in
g
ca
n
b
e
a
d
v
an
ta
g
eo
u
s
an
d
b
e
n
ef
icial
f
o
r
in
v
esto
r
s
.
I
t
m
ay
en
co
u
r
a
g
e
r
esear
ch
er
s
to
ex
p
lo
r
e
an
d
d
ev
elo
p
f
u
r
t
h
er
in
teg
r
atio
n
s
o
f
d
iv
er
s
e
in
s
u
latio
n
m
ater
ials
.
Fu
tu
r
e
s
tu
d
ies
co
u
ld
in
v
esti
g
ate
th
e
ec
o
n
o
m
ic
an
d
en
v
ir
o
n
m
en
tal
im
p
ac
ts
o
f
s
u
ch
m
u
lti
-
in
s
u
latio
n
co
n
f
ig
u
r
atio
n
s
.
A
d
d
itio
n
ally
,
co
m
p
a
r
ativ
e
s
tu
d
ies
co
u
ld
an
aly
ze
th
is
p
r
o
p
o
s
ed
ap
p
r
o
ac
h
ag
ai
n
s
t
o
th
er
s
u
tili
zin
g
d
if
f
er
e
n
t c
o
m
b
in
atio
n
s
o
f
in
s
u
lato
r
s
.
ACK
NO
WL
E
DG
E
M
E
NT
S
T
h
e
au
t
h
o
r
ex
p
r
ess
es
s
in
ce
r
e
g
r
atitu
d
e
t
o
th
e
Su
p
er
i
o
r
S
ch
o
o
l
o
f
T
ec
h
n
o
l
o
g
y
(
E
ST)
,
Un
iv
er
s
ity
o
f
Hass
an
I
I
o
f
C
asab
lan
ca
,
f
o
r
p
r
o
v
id
i
n
g
ess
en
tial
r
eso
u
r
ce
s
an
d
s
u
p
p
o
r
t.
Sp
ec
ial
th
an
k
s
to
Pro
f
ess
o
r
s
Yo
u
s
s
ef
Me
jd
o
u
b
a
n
d
Kao
u
tar
Sen
h
aji
R
h
az
i f
o
r
th
eir
in
v
alu
ab
le
g
u
id
an
ce
an
d
m
en
to
r
s
h
ip
.
RE
F
E
R
E
NC
E
S
[
1
]
L.
A
d
i
t
y
a
e
t
a
l
.
,
“
A
r
e
v
i
e
w
o
n
i
n
s
u
l
a
t
i
o
n
mat
e
r
i
a
l
s
f
o
r
e
n
e
r
g
y
c
o
n
s
e
r
v
a
t
i
o
n
i
n
b
u
i
l
d
i
n
g
s,
”
R
e
n
e
w
.
S
u
s
t
a
i
n
.
E
n
e
rg
y
Re
v
.
,
v
o
l
.
7
3
,
p
p
.
1
3
5
2
–
1
3
6
5
,
Ju
n
.
2
0
1
7
,
d
o
i
:
1
0
.
1
0
1
6
/
j
.
r
ser.
2
0
1
7
.
0
2
.
0
3
4
.
[
2
]
L.
F
.
C
a
b
e
z
a
,
A
.
C
a
st
e
l
l
,
M
.
M
e
d
r
a
n
o
,
I
.
M
a
r
t
o
r
e
l
l
,
G
.
P
é
r
e
z
,
a
n
d
I
.
F
e
r
n
á
n
d
e
z
,
“
Ex
p
e
r
i
me
n
t
a
l
st
u
d
y
o
n
t
h
e
p
e
r
f
o
r
ma
n
c
e
o
f
i
n
s
u
l
a
t
i
o
n
m
a
t
e
r
i
a
l
s
i
n
M
e
d
i
t
e
r
r
a
n
e
a
n
c
o
n
s
t
r
u
c
t
i
o
n
,
”
E
n
e
r
g
y
B
u
i
l
d
.
,
v
o
l
.
4
2
,
n
o
.
5
,
p
p
.
6
3
0
–
6
3
6
,
M
a
y
2
0
1
0
,
d
o
i
:
1
0
.
1
0
1
6
/
j
.
e
n
b
u
i
l
d
.
2
0
0
9
.
1
0
.
0
3
3
.
[
3
]
M
.
O
z
e
l
,
“
Ef
f
e
c
t
o
f
i
n
su
l
a
t
i
o
n
l
o
c
a
t
i
o
n
o
n
d
y
n
a
mi
c
h
e
a
t
-
t
r
a
n
sf
e
r
c
h
a
r
a
c
t
e
r
i
st
i
c
s
o
f
b
u
i
l
d
i
n
g
e
x
t
e
r
n
a
l
w
a
l
l
s
a
n
d
o
p
t
i
m
i
z
a
t
i
o
n
o
f
i
n
s
u
l
a
t
i
o
n
t
h
i
c
k
n
e
ss
,
”
En
e
rg
y
B
u
i
l
d
.
,
v
o
l
.
7
2
,
p
p
.
2
8
8
–
2
9
5
,
A
p
r
.
2
0
1
4
,
d
o
i
:
1
0
.
1
0
1
6
/
j
.
e
n
b
u
i
l
d
.
2
0
1
3
.
1
1
.
0
1
5
.
[
4
]
M
.
E
L
W
a
z
n
a
e
t
a
l
.
,
“
Ex
p
e
r
i
me
n
t
a
l
a
n
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F.
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5
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1
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