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Octo
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20
25
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p
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4
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4555
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Ali K
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d
z
1.
I
NT
RO
D
UCT
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O
N
R
is
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b
al
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latio
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s
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g
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ates
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2
0
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[
2
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,
[
3
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.
C
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allen
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tag
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ak
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en
h
o
u
s
e
m
eth
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d
s
in
s
u
f
f
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[
4
]
.
Gr
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n
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s
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f
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co
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en
v
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o
n
m
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ts
[
5
]
,
[
6
]
.
Ho
wev
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v
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s
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ely
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ea
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m
an
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al
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[
7
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.
Sm
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h
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tech
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im
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itio
n
s
[
8
]
.
T
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wid
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m
an
a
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en
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[
9
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,
[
1
0
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.
Ov
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[
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1
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p
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[
1
2
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.
D
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is
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am
o
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ts
at
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r
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[
1
3
]
.
Fer
tig
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ap
p
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f
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tili
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r
s
th
r
o
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b
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r
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s
lab
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an
d
ca
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lo
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tili
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s
e
b
y
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5
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–
2
5
%
w
ith
o
u
t
af
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esp
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wh
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d
to
cr
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r
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wth
s
tag
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r
o
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d
r
ip
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s
[
1
4
]
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2
0
8
8
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8
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0
8
I
n
t J E
lec
&
C
o
m
p
E
n
g
,
Vo
l.
15
,
No
.
5
,
Octo
b
e
r
20
25
:
4
5
5
5
-
4
5
6
8
4556
Div
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s
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s
tu
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an
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r
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[
1
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in
v
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ap
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1
6
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v
e
r
eso
u
r
ce
s
,
an
d
m
in
im
ize
e
n
v
ir
o
n
m
en
tal
im
p
ac
ts
.
Dah
lila
et
a
l.
[
1
7
]
p
r
o
p
o
s
e
an
I
o
T
-
b
ased
s
m
ar
t
f
e
r
tig
atio
n
m
an
a
g
em
en
t
s
y
s
tem
d
esig
n
ed
f
o
r
a
g
r
icu
ltu
r
al
ar
ea
s
p
r
o
n
e
to
p
o
wer
o
u
ta
g
es.
T
h
e
s
y
s
tem
in
teg
r
ates
s
en
s
o
r
s
f
o
r
r
ea
l
-
tim
e
m
o
n
ito
r
in
g
o
f
ir
r
ig
atio
n
an
d
p
o
wer
o
u
ta
g
es,
with
f
ea
tu
r
es
s
u
ch
as
au
to
m
ated
ir
r
ig
atio
n
s
ch
ed
u
lin
g
,
p
esti
cid
e
m
an
ag
em
en
t,
an
d
p
o
ly
b
a
g
clea
n
in
g
.
Dwir
atn
a
et
a
l.
[
1
8
]
in
tr
o
d
u
ce
a
m
o
d
if
ied
h
y
d
r
o
p
o
n
ic
k
it
f
e
atu
r
in
g
a
s
elf
-
f
er
tig
atio
n
s
y
s
tem
,
s
p
ec
if
ically
d
esig
n
ed
f
o
r
r
em
o
te
ar
ea
s
with
u
n
r
eliab
le
elec
tr
icity
s
u
p
p
ly
.
B
ao
et
a
l.
[
1
9
]
in
v
esti
g
ate
th
e
im
p
ac
t
o
f
in
tellig
en
t
d
r
ip
f
er
tig
atio
n
(
I
F)
o
n
wate
r
m
elo
n
p
r
o
d
u
cti
o
n
in
a
g
r
ee
n
h
o
u
s
e
en
v
ir
o
n
m
en
t
o
v
er
t
h
r
ee
g
r
o
win
g
s
ea
s
o
n
s
(
2
0
1
9
–
2
0
2
1
)
.
I
F
in
te
g
r
ates
r
ea
l
-
tim
e
s
o
il
m
o
is
tu
r
e
s
en
s
o
r
s
with
I
o
T
-
b
ased
au
to
m
ate
d
ir
r
ig
atio
n
an
d
f
er
tili
za
tio
n
to
o
p
tim
ize
wate
r
an
d
n
u
tr
ien
t
ap
p
licatio
n
.
I
m
b
er
n
ó
n
-
m
u
ler
o
et
a
l.
[
2
0
]
ev
alu
at
e
an
ad
v
a
n
ce
d
a
u
to
n
o
m
o
u
s
f
er
tig
atio
n
s
y
s
tem
d
esig
n
ed
to
o
p
tim
ize
th
e
u
s
e
o
f
v
ar
iab
le
-
q
u
ality
ir
r
ig
atio
n
w
ater
.
B
o
n
elli
et
a
l.
[
2
1
]
ev
alu
at
ed
th
e
p
er
f
o
r
m
an
ce
o
f
tim
er
-
b
ased
(
T
B
)
v
er
s
u
s
s
m
ar
t
s
en
s
o
r
-
b
ased
(
SB
)
ir
r
ig
at
io
n
s
tr
ateg
ies.
W
an
g
et
a
l.
[
2
2
]
co
n
d
u
cted
a
f
ield
ex
p
er
im
en
t
i
n
Sh
o
u
g
u
an
g
,
Sh
an
d
o
n
g
Pro
v
i
n
ce
,
to
ass
ess
th
e
ef
f
ec
ts
o
f
v
ar
io
u
s
ir
r
ig
atio
n
s
ch
ed
u
lin
g
tr
ea
tm
en
ts
—
f
ar
m
er
d
r
ip
i
r
r
ig
a
tio
n
(
FI)
,
in
tellig
en
t
ir
r
ig
atio
n
(
I
I
1
)
,
an
d
i
n
tellig
en
t
ir
r
ig
atio
n
(
I
I
2
)
—
o
n
to
m
ato
g
r
o
wth
,
ir
r
ig
atio
n
wate
r
u
s
ag
e
,
an
d
n
u
tr
ien
t
ef
f
icien
cy
ac
r
o
s
s
two
g
r
o
win
g
s
ea
s
o
n
s
.
I
d
r
is
e
t
a
l.
[
2
3
]
d
ev
elo
p
ed
an
in
ter
n
et
o
f
th
i
n
g
s
(
I
o
T
)
-
b
ased
f
er
tig
atio
n
s
y
s
tem
to
a
u
to
m
atica
lly
d
eliv
e
r
a
f
er
tili
ze
r
m
ix
tu
r
e
with
a
co
n
s
is
ten
t
elec
tr
ical
co
n
d
u
ctiv
ity
(
E
C
)
v
alu
e
to
p
lan
ts
.
Vo
jn
o
v
ic
et
a
l.
[
2
4
]
aim
ed
to
ex
p
lo
r
e
n
ew
m
eth
o
d
s
f
o
r
f
er
tig
atio
n
an
d
g
r
a
f
tin
g
to
o
p
ti
m
ize
cu
cu
m
b
e
r
y
ield
a
n
d
q
u
al
ity
in
th
e
g
r
ee
n
h
o
u
s
e.
T
r
ad
itio
n
al
g
r
ee
n
h
o
u
s
e
co
n
tr
o
l
s
y
s
tem
s
s
tr
u
g
g
le
with
co
m
p
lex
ity
an
d
u
n
ce
r
tain
ty
,
o
f
te
n
l
ea
d
in
g
to
in
ef
f
icien
t r
eso
u
r
ce
u
s
e
an
d
p
o
o
r
p
lan
t g
r
o
wth
.
Fu
zz
y
lo
g
ic
p
r
o
v
id
es a
m
o
r
e
ad
ap
tiv
e
an
d
in
tellig
en
t a
p
p
r
o
ac
h
b
y
m
i
m
ick
in
g
h
u
m
an
r
ea
s
o
n
i
n
g
a
n
d
h
an
d
lin
g
n
o
n
lin
ea
r
,
u
n
ce
r
tain
c
o
n
d
itio
n
s
th
r
o
u
g
h
e
x
p
er
t
-
d
e
f
in
ed
r
u
les.
T
h
is
r
esu
lts
in
m
o
r
e
ef
f
icien
t,
s
ca
lab
le,
an
d
s
u
s
tain
ab
le
g
r
e
en
h
o
u
s
e
m
a
n
ag
em
en
t,
u
ltima
tely
im
p
r
o
v
in
g
cr
o
p
y
ield
s
.
T
h
is
s
tu
d
y
p
r
esen
ts
a
f
u
zz
y
lo
g
ic
-
b
ased
alg
o
r
ith
m
f
o
r
o
p
tim
izin
g
b
i
o
-
f
er
tig
atio
n
in
a
to
m
ato
g
r
ee
n
h
o
u
s
e
in
s
o
u
th
er
n
Alg
e
r
ia.
Un
lik
e
tr
ad
itio
n
al
s
y
s
te
m
s
th
at
m
an
ag
e
o
n
ly
o
n
e
o
r
two
en
v
ir
o
n
m
en
tal
p
ar
am
eter
s
,
o
u
r
a
p
p
r
o
ac
h
in
te
g
r
ates
f
o
u
r
k
e
y
v
ar
iab
les
(
te
m
p
er
atu
r
e,
h
u
m
id
ity
,
s
o
il
p
H,
an
d
s
o
il
m
o
is
tu
r
e)
an
d
co
n
t
r
o
ls
f
iv
e
ac
tu
ato
r
s
s
i
m
u
ltan
eo
u
s
ly
(
f
an
,
h
ea
te
r
,
ir
r
i
g
atio
n
p
u
m
p
,
f
e
r
tili
za
tio
n
p
u
m
p
,
an
d
f
er
tig
atio
n
p
u
m
p
)
.
T
h
e
n
o
v
elty
lies
in
th
e
co
m
b
in
atio
n
o
f
r
ea
l
-
tim
e
s
e
n
s
o
r
d
ata,
ex
p
er
t
-
d
e
r
iv
ed
f
u
zz
y
r
u
les,
an
d
th
e
u
s
e
o
f
b
io
f
er
tili
ze
r
s
in
s
tead
o
f
ch
e
m
ical
f
er
tili
ze
r
s
—
an
en
v
ir
o
n
m
en
tally
s
u
s
tain
ab
le
p
r
ac
tice.
T
h
is
m
u
lti
-
v
ar
iab
l
e
co
n
tr
o
l
s
y
s
tem
p
r
o
v
id
es
an
ad
ap
tiv
e,
in
tellig
en
t,
a
n
d
e
n
er
g
y
-
ef
f
icien
t
s
o
lu
tio
n
f
o
r
o
p
tim
izin
g
t
o
m
ato
p
r
o
d
u
ctio
n
in
ar
id
r
eg
io
n
s
li
k
e
s
o
u
th
er
n
Alg
er
ia.
T
h
e
ar
t
icle
d
etails
th
e
alg
o
r
ith
m
d
esig
n
,
m
em
b
er
s
h
ip
f
u
n
ctio
n
s
,
f
u
zz
y
r
u
le
b
ase,
ex
p
er
im
en
tal
v
alid
atio
n
,
an
d
r
esu
lts
,
co
n
clu
d
in
g
with
f
u
tu
r
e
r
ese
ar
ch
d
ir
ec
tio
n
s
.
2.
M
E
T
H
O
D
I
n
th
is
s
ec
tio
n
,
we
p
r
esen
t
th
e
p
r
o
p
o
s
ed
alg
o
r
ith
m
s
d
ev
elo
p
ed
to
o
p
tim
ize
th
e
g
r
ee
n
h
o
u
s
e
m
icr
o
clim
ate
u
s
in
g
f
u
zz
y
lo
g
ic.
T
h
e
s
y
s
tem
in
te
g
r
ates
v
ar
i
o
u
s
s
en
s
o
r
s
,
ac
tu
ato
r
s
,
an
d
a
m
icr
o
co
n
tr
o
ller
t
o
m
o
n
ito
r
a
n
d
c
o
n
tr
o
l
m
u
ltip
le
k
ey
en
v
ir
o
n
m
e
n
tal
p
ar
a
m
eter
s
,
in
clu
d
in
g
i
n
ter
n
al
air
tem
p
er
atu
r
e,
in
ter
n
al
air
h
u
m
id
ity
,
s
o
il
p
H,
an
d
s
o
il
m
o
is
tu
r
e.
B
y
em
p
lo
y
in
g
f
u
zz
y
in
f
er
en
ce
tec
h
n
iq
u
es,
t
h
e
alg
o
r
ith
m
s
d
y
n
am
ically
ad
ju
s
t
co
n
tr
o
l
ac
tio
n
s
to
en
h
an
ce
th
e
ef
f
icien
c
y
o
f
b
i
o
-
f
er
tig
atio
n
an
d
p
r
o
m
o
te
o
p
ti
m
al
p
lan
t
g
r
o
wth
co
n
d
itio
n
s
.
2
.
1
.
P
r
o
po
s
ed
a
lg
o
rit
hm
I
n
th
is
s
ec
tio
n
,
we
p
r
esen
t
th
e
p
r
o
p
o
s
ed
alg
o
r
ith
m
th
at
em
p
lo
y
s
f
u
zz
y
lo
g
ic
to
m
o
n
ito
r
a
n
d
co
n
tr
o
l
f
o
u
r
c
r
itical
p
ar
am
eter
s
in
th
e
g
r
ee
n
h
o
u
s
e:
in
ter
n
al
air
tem
p
er
atu
r
e,
i
n
ter
n
al
air
h
u
m
id
it
y
,
s
o
il
p
H,
an
d
s
o
il
m
o
is
tu
r
e.
T
h
ese
p
ar
am
eter
s
ar
e
ess
en
tial
f
o
r
m
ain
tain
in
g
a
s
tab
le
m
icr
o
clim
ate
an
d
s
u
p
p
o
r
tin
g
h
ea
lth
y
p
lan
t
g
r
o
wth
.
B
y
ap
p
ly
in
g
f
u
zz
y
l
o
g
ic
tech
n
iq
u
es,
th
e
s
y
s
tem
en
s
u
r
es
ad
ap
tiv
e
d
ec
is
io
n
-
m
a
k
in
g
th
at
im
p
r
o
v
es
m
icr
o
clim
ate
r
eg
u
latio
n
an
d
e
n
h
an
ce
s
th
e
ef
f
icien
cy
o
f
b
io
-
f
er
tig
atio
n
.
T
h
e
f
u
zz
y
s
y
s
tem
u
s
es
m
em
b
er
s
h
ip
f
u
n
ctio
n
g
r
ap
h
s
to
illu
s
tr
ate
h
o
w
i
n
p
u
t
p
ar
am
eter
s
r
el
ate,
wh
er
e
ea
ch
x
-
ax
is
v
alu
e
co
r
r
esp
o
n
d
s
to
two
y
-
ax
is
v
alu
es
[
2
5
]
.
Fu
zz
y
lo
g
ic,
wid
ely
u
s
ed
in
m
an
y
f
ield
s
in
clu
d
in
g
n
etwo
r
k
in
g
,
h
el
p
s
co
n
v
er
t
m
u
ltip
le
in
p
u
ts
in
t
o
a
s
in
g
le
o
u
tp
u
t
[
2
6
]
,
[
2
7
]
.
T
h
is
s
tu
d
y
a
d
o
p
ts
th
e
Ma
m
d
an
i
m
o
d
el
[
2
8
]
—
o
n
e
o
f
th
e
m
o
s
t w
id
ely
u
s
ed
f
u
zz
y
in
f
er
e
n
ce
m
eth
o
d
s
—
f
o
llo
win
g
a
f
o
u
r
-
s
t
ep
f
u
zz
y
p
r
o
ce
s
s
[
2
7
]
in
Fig
u
r
e
1
.
Alg
o
r
ith
m
1
p
r
o
v
i
d
es th
e
p
s
eu
d
o
c
o
d
e
f
o
r
co
n
tr
o
l
lin
g
th
e
g
r
ee
n
h
o
u
s
e'
s
m
icr
o
cli
m
ate.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
n
t J E
lec
&
C
o
m
p
E
n
g
I
SS
N:
2088
-
8
7
0
8
Dev
elo
p
men
t o
f a
fu
z
z
y
lo
g
ic
-
b
a
s
ed
g
r
ee
n
h
o
u
s
e
s
ystem
fo
r
o
p
timiz
in
g
…
(
A
ch
o
u
a
k
To
u
h
a
mi
)
4557
Fig
u
r
e
1
.
Ou
r
ap
p
r
o
ac
h
’
s
f
u
zz
y
p
r
o
ce
s
s
m
o
d
el
Alg
o
r
ith
m
1
.
Mo
n
ito
r
i
n
g
o
f
th
e
in
ter
n
al
m
icr
o
clim
ate
F
u
z
z
y
i
n
p
u
t
s
:
I
n
t
e
r
n
a
l
a
i
r
t
e
m
p
e
r
a
t
u
r
e
(
T
i
)
,
i
n
t
e
r
n
a
l
a
i
r
h
u
m
i
d
i
t
y
(
H
i
)
,
i
n
t
e
r
n
a
l
s
o
i
l
p
H
(
P
i
)
,
i
n
t
e
r
n
a
l
s
o
i
l
m
o
is
t
u
r
e
(
S
i
)
,
t
e
m
p
e
r
at
u
r
e
t
h
r
e
s
h
o
l
d
(
T
t
)
,
h
u
m
i
d
i
t
y
t
h
r
e
s
h
o
l
d
(
Ht
)
,
p
H
th
r
e
s
h
o
l
d
(
P
t
)
,
s
o
i
l
m
o
is
t
u
r
e
t
h
r
e
s
h
o
l
d
(
S
t
)
.
Fu
zz
y
o
u
tp
u
ts
: o
p
tim
al
tem
p
er
atu
r
e,
o
p
tim
al
h
u
m
id
ity
,
o
p
tim
al
s
o
il p
H,
o
p
tim
al
s
o
il m
o
is
tu
r
e.
1.
I
n
itialize
in
p
u
t p
ar
a
m
eter
s
.
2.
Def
in
e
f
u
zz
y
s
ets an
d
m
em
b
er
s
h
ip
f
u
n
ctio
n
s
f
o
r
ea
c
h
p
ar
a
m
eter
.
3.
C
ap
tu
r
e
th
e
r
ea
l
-
tim
e
v
al
u
es o
f
th
e
in
p
u
t p
ar
am
eter
s
.
4.
Fu
zz
if
y
th
e
in
p
u
t p
ar
a
m
eter
s
: Calcu
late
th
e
d
eg
r
ee
o
f
m
em
b
er
s
h
ip
f
o
r
e
ac
h
in
p
u
t v
ar
ia
b
le.
5.
Per
f
o
r
m
f
u
zz
y
in
f
er
en
ce
: A
p
p
l
y
f
u
zz
y
r
u
les b
ased
o
n
in
p
u
t p
ar
am
eter
s
to
g
en
e
r
ate
f
u
zz
y
o
u
tp
u
t.
6.
Ag
g
r
eg
ate
th
e
r
esu
lts
f
r
o
m
all
f
u
zz
y
r
u
les.
7.
Def
u
zz
if
y
th
e
o
u
tp
u
t: C
o
n
v
er
t
th
e
f
u
zz
y
o
u
tp
u
t in
to
a
p
r
ec
is
e
co
n
tr
o
l
v
alu
e.
8.
A
d
j
u
s
t
t
h
e
g
r
e
e
n
h
o
u
s
e
s
y
s
t
e
m
s
(
h
e
a
t
i
n
g
,
v
e
n
t
i
l
at
i
o
n
,
i
r
r
i
g
a
ti
o
n
,
f
e
r
t
i
g
a
t
i
o
n
)
b
a
s
e
d
o
n
t
h
e
d
e
f
u
z
z
i
f
i
e
d
o
u
t
p
u
t
.
9.
R
ep
ea
t th
e
p
r
o
ce
s
s
in
r
ea
l
-
tim
e
to
m
ain
tain
th
e
o
p
tim
al
m
icr
o
clim
ate.
Fu
zz
y
lo
g
ic
u
s
es
lin
g
u
is
tic
v
ar
iab
les
—
r
an
g
in
g
b
etwe
en
tr
u
e
an
d
f
alse
—
to
r
ep
r
esen
t
th
e
s
tr
en
g
th
o
f
r
elatio
n
s
h
ip
s
am
o
n
g
m
etr
ics
a
n
d
to
d
eter
m
in
e
t
h
e
r
esu
ltin
g
o
u
tp
u
t
[
2
6
]
,
[
2
7
]
.
T
ab
le
1
d
ef
in
es
h
o
w
th
e
f
u
zz
y
lo
g
ic
s
y
s
tem
in
ter
p
r
ets
r
ea
l
-
wo
r
ld
s
en
s
o
r
v
alu
es
(
lik
e
tem
p
e
r
atu
r
e
an
d
h
u
m
id
ity
)
an
d
d
ec
i
d
es
wh
at
to
d
o
with
o
u
tp
u
t
d
e
v
ices
(
lik
e
a
f
an
o
r
h
ea
ter
)
u
s
in
g
f
u
zz
y
s
ets.
T
h
e
m
em
b
er
s
h
ip
f
u
n
ctio
n
s
h
a
p
es
wer
e
ch
o
s
en
f
o
r
th
eir
s
im
p
licity
an
d
s
u
itab
ilit
y
to
th
e
in
p
u
t
d
ata.
T
h
eir
b
o
u
n
d
ar
ies
wer
e
d
ef
in
ed
th
r
o
u
g
h
ex
p
er
t
in
p
u
t
f
r
o
m
f
a
r
m
er
s
an
d
a
g
r
o
n
o
m
is
ts
an
d
b
y
an
al
y
zin
g
r
ea
l
e
n
v
ir
o
n
m
en
tal
d
at
a,
en
s
u
r
in
g
ac
c
u
r
ate
r
ep
r
esen
tatio
n
o
f
lin
g
u
is
tic
ter
m
s
an
d
r
ea
l
-
wo
r
ld
co
n
d
itio
n
s
.
T
ab
le
1
.
L
in
g
u
is
tic
v
ar
iab
les a
n
d
Me
m
b
er
s
h
i
p
f
u
n
ctio
n
s
V
a
r
i
a
b
l
e
t
y
p
e
V
a
r
i
a
b
l
e
Li
n
g
u
i
s
t
i
c
t
e
r
ms (
M
F
s)
Ty
p
e
o
f
M
F
R
a
n
g
e
I
n
p
u
t
I
n
t
e
r
n
a
l
a
i
r
t
e
m
p
e
r
a
t
u
r
e
(
°
C
)
Lo
w
,
A
v
e
r
a
g
e
,
H
i
g
h
Tr
i
a
n
g
u
l
a
r
[0
-
5
0
]
I
n
t
e
r
n
a
l
a
i
r
h
u
mi
d
i
t
y
(
%)
Lo
w
,
M
o
d
e
r
a
t
e
,
H
i
g
h
Tr
i
a
n
g
u
l
a
r
[0
-
1
0
0
]
S
o
i
l
p
H
A
c
i
d
i
c
,
N
e
u
t
r
a
l
,
B
a
si
c
Tr
i
a
n
g
u
l
a
r
[3
-
9]
S
o
i
l
m
o
i
s
t
u
r
e
(
%)
D
r
y
,
m
o
d
e
r
a
t
e
l
y
w
e
t
,
S
a
t
u
r
a
t
e
d
Tr
i
a
n
g
u
l
a
r
[0
-
1
0
0
]
O
u
t
p
u
t
F
a
n
(
S
p
e
e
d
%)
O
f
f
,
Lo
w
,
H
i
g
h
Tr
i
a
n
g
u
l
a
r
[0
-
1
0
0
]
H
e
a
t
e
r
(
P
o
w
e
r
%)
O
f
f
,
Lo
w
,
H
i
g
h
Tr
i
a
n
g
u
l
a
r
[0
-
1
0
0
]
W
a
t
e
r
p
u
m
p
1
f
o
r
i
r
r
i
g
a
t
i
o
n
(
%)
O
f
f
,
Lo
w
,
H
i
g
h
Tr
i
a
n
g
u
l
a
r
[0
-
1
0
0
]
W
a
t
e
r
p
u
m
p
2
f
o
r
f
e
r
t
i
l
i
z
a
t
i
o
n
(
%)
O
f
f
,
Lo
w
,
H
i
g
h
Tr
i
a
n
g
u
l
a
r
[0
-
1
0
0
]
W
a
t
e
r
p
u
m
p
3
f
o
r
f
e
r
t
i
g
a
t
i
o
n
(
%)
O
f
f
,
Lo
w
,
H
i
g
h
Tr
i
a
n
g
u
l
a
r
[0
-
1
0
0
]
T
h
e
f
u
zz
y
g
r
a
p
h
f
o
r
t
h
e
air
tem
p
er
atu
r
e
p
ar
am
eter
,
with
lo
w,
av
e
r
ag
e,
a
n
d
h
ig
h
m
em
b
er
s
h
ip
f
u
n
ctio
n
s
,
is
s
h
o
wn
in
Fig
u
r
e
2
.
50
°C
is
th
e
h
ig
h
est
r
ec
o
r
d
ed
tem
p
e
r
atu
r
e
in
th
is
in
v
esti
g
atio
n
.
T
h
e
air
h
u
m
id
ity
f
u
zz
y
g
r
ap
h
,
wh
ic
h
r
an
g
es
f
r
o
m
0
%
to
1
0
0
%,
is
s
h
o
wn
in
Fig
u
r
e
3
.
T
h
e
r
e
a
r
e
th
r
ee
ty
p
es
o
f
air
h
u
m
id
ity
: lo
w,
m
o
d
er
ate,
an
d
h
ig
h
.
T
h
e
f
u
zz
y
s
o
il
p
H
ch
ar
t,
wh
ic
h
is
d
iv
id
ed
in
to
th
r
ee
ca
teg
o
r
ies
:
ac
id
ic,
n
eu
tr
al,
an
d
b
asic
,
is
s
h
o
wn
in
Fig
u
r
e
4
.
T
h
e
f
u
zz
y
ch
a
r
t
f
o
r
s
o
il
m
o
is
tu
r
e,
wh
ic
h
is
d
iv
id
ed
in
to
t
h
r
ee
ca
teg
o
r
ies
:
d
r
y
,
m
o
d
er
ately
wet
,
an
d
s
atu
r
ated
,
is
s
h
o
wn
in
Fig
u
r
e
5
.
Fig
u
r
e
6
s
h
o
ws th
e
f
u
zz
y
m
em
b
er
s
h
ip
f
u
n
ctio
n
f
o
r
t
h
e
h
ea
ter
,
with
p
o
wer
lev
els
ca
teg
o
r
ized
as
lo
w,
o
f
f
,
o
r
h
ig
h
b
ased
o
n
tem
p
er
at
u
r
e
d
ev
iatio
n
s
f
r
o
m
th
e
th
r
esh
o
l
d
.
Fig
u
r
e
7
d
is
p
lay
s
th
e
f
u
zz
y
m
e
m
b
er
s
h
ip
f
u
n
ctio
n
f
o
r
th
e
f
a
n
,
with
p
o
we
r
lev
el
s
d
eter
m
in
ed
b
y
tem
p
e
r
atu
r
e
a
n
d
h
u
m
id
ity
lev
els
r
elativ
e
to
th
eir
o
p
tim
al
th
r
esh
o
ld
s
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2
0
8
8
-
8
7
0
8
I
n
t J E
lec
&
C
o
m
p
E
n
g
,
Vo
l.
15
,
No
.
5
,
Octo
b
e
r
20
25
:
4
5
5
5
-
4
5
6
8
4558
Fig
u
r
es
8
,
9
,
an
d
1
0
illu
s
tr
ate
th
e
f
u
zz
y
m
em
b
er
s
h
ip
f
u
n
ctio
n
s
f
o
r
ir
r
ig
atio
n
,
f
e
r
tili
za
tio
n
,
an
d
f
er
tig
atio
n
.
I
r
r
ig
atio
n
co
n
tr
o
l
d
ep
en
d
s
o
n
s
o
il
m
o
is
tu
r
e
an
d
h
u
m
id
ity
lev
els,
with
p
o
wer
l
ev
els
s
et
to
lo
w,
o
f
f
,
o
r
h
ig
h
ac
co
r
d
in
g
ly
.
Fer
tili
za
tio
n
is
r
eg
u
lated
b
ased
o
n
s
o
il
p
H,
ad
ju
s
tin
g
p
o
wer
lev
els
b
ased
o
n
d
e
v
iatio
n
s
f
r
o
m
th
e
o
p
tim
al
r
an
g
e.
Fer
ti
g
atio
n
co
n
s
id
er
s
b
o
th
s
o
il
p
H
an
d
m
o
is
tu
r
e,
co
m
b
in
in
g
c
o
n
d
itio
n
s
to
d
eter
m
in
e
th
e
ap
p
r
o
p
r
iate
co
n
tr
o
l p
o
wer
lev
el.
T
h
e
f
u
zz
y
r
u
le
b
ase
u
s
ed
to
c
o
n
n
ec
t
th
e
i
n
p
u
t
-
o
u
tp
u
t
m
em
b
er
s
h
ip
f
u
n
ctio
n
s
is
s
h
o
wn
in
Fig
u
r
e
1
1
.
I
n
o
u
r
s
tu
d
y
,
we
h
av
e
8
1
r
u
le
s
.
T
h
e
f
u
zz
y
r
u
les
wer
e
p
r
im
a
r
ily
f
o
r
m
u
lated
b
ased
o
n
ex
p
e
r
t
k
n
o
wled
g
e
f
r
o
m
lo
ca
l
f
ar
m
er
s
,
ag
r
o
n
o
m
is
ts
,
an
d
g
r
ee
n
h
o
u
s
e
tech
n
ician
s
,
c
o
m
b
in
ed
with
o
b
s
er
v
atio
n
s
f
r
o
m
p
r
ev
io
u
s
s
tu
d
ie
s
an
d
r
ea
l
-
wo
r
l
d
b
eh
a
v
io
r
o
f
t
h
e
cr
o
p
u
n
d
e
r
v
ar
y
in
g
clim
at
ic
an
d
s
o
il
co
n
d
itio
n
s
[
2
8
]
–
[
3
0
]
.
T
h
e
I
F
-
T
HE
N
g
u
id
elin
es
lis
ted
in
T
a
b
le
2
g
o
v
er
n
h
o
w
th
e
f
u
zz
y
i
n
f
er
en
c
e
s
y
s
tem
f
u
n
ctio
n
s
.
T
o
co
n
n
e
ct
d
if
f
er
e
n
t
lan
g
u
ag
e
v
ar
iab
les,
th
ese
r
u
les u
s
e
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I
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I
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&
C
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7
an
d
a
liq
u
id
o
r
g
a
n
ic
f
e
r
tili
ze
r
(
m
ad
e
b
y
s
o
ak
in
g
s
h
ee
p
m
an
u
r
e
in
wate
r
)
with
a
p
H
o
f
4
.
2
5
.
B
o
th
m
ea
s
u
r
em
en
ts
wer
e
tak
en
at
2
5
°C
,
a
s
s
h
o
wn
in
Fig
u
r
e
1
4
.
Fig
u
r
e
1
4
.
Me
asu
r
ed
th
e
m
ix
t
u
r
e
with
a
p
H
m
ete
r
3
.
2
.
1
.
Ste
ps
o
f
t
he
e
x
perim
en
t
T
h
e
ex
p
e
r
im
en
tal
s
tep
s
in
clu
d
ed
:
a.
Af
ter
m
ea
s
u
r
in
g
th
e
p
H
v
alu
e
s
,
1
0
m
l
o
f
th
e
liq
u
id
f
er
tili
ze
r
was
ad
d
ed
to
th
e
tap
wate
r
u
s
in
g
a
p
i
p
ette
an
d
m
ix
e
d
th
o
r
o
u
g
h
ly
to
p
r
ep
ar
e
th
e
f
er
tig
atio
n
s
o
lu
tio
n
.
b.
T
h
e
p
H
elec
tr
o
d
e
is
p
lace
d
in
to
th
e
m
ix
tu
r
e
,
an
d
th
e
p
H
v
alu
e
is
r
ea
d
d
ir
ec
tly
f
r
o
m
th
e
co
n
n
ec
te
d
elec
tr
o
n
ic
m
eter
'
s
d
is
p
lay
.
c.
Af
ter
ea
ch
m
ea
s
u
r
em
en
t,
th
e
p
H
elec
tr
o
d
e
is
r
in
s
ed
with
d
is
till
ed
wate
r
,
lef
t
f
o
r
ten
s
ec
o
n
d
s
,
an
d
th
en
wip
ed
with
J
o
s
ep
h
p
ap
e
r
to
p
r
ep
ar
e
it f
o
r
th
e
n
e
x
t m
ea
s
u
r
em
en
t a
f
ter
ad
d
itio
n
al
f
er
tili
ze
r
is
ad
d
ed
.
d.
W
e
m
ea
s
u
r
e
th
e
p
H
o
f
t
h
e
m
ix
tu
r
e
an
d
r
ep
ea
t th
e
p
r
o
ce
s
s
u
n
t
il we
o
b
tain
th
e
f
o
llo
win
g
r
esu
lts
in
T
ab
le
3
.
T
ab
le
3
.
p
H
r
esu
lts
an
d
th
e
v
o
lu
m
e
o
f
th
e
m
ix
tu
r
e
u
s
in
g
a
p
H
m
eter
V
o
l
u
me
o
f
t
h
e
samp
l
e
b
e
f
o
r
e
a
d
d
i
n
g
t
h
e
f
e
r
t
i
l
i
z
e
r
p
H
o
f
t
h
e
sam
p
l
e
b
e
f
o
r
e
a
d
d
i
n
g
t
h
e
f
e
r
t
i
l
i
z
e
r
V
o
l
u
me
o
f
f
e
r
t
i
l
i
z
e
r
a
d
d
e
d
V
o
l
u
me
o
f
t
h
e
samp
l
e
a
f
t
e
r
a
d
d
i
n
g
t
h
e
f
e
r
t
i
l
i
z
e
r
p
H
o
f
t
h
e
sam
p
l
e
a
f
t
e
r
a
d
d
i
n
g
t
h
e
f
e
r
t
i
l
i
z
e
r
Th
e
1
st
c
a
se
5
0
0
m
l
6
.
9
7
1
0
ml
5
1
0
m
l
6
.
8
4
Th
e
2
nd
c
a
se
5
1
0
m
l
6
.
8
4
1
0
ml
5
2
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l
6
.
1
8
Th
e
3
rd
c
a
se
5
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m
l
6
.
1
7
1
0
ml
5
3
0
m
l
5
.
9
6
3
.
2
.
2
.
Ana
ly
s
is
o
f
re
s
ults
T
h
e
ex
p
er
im
en
t
s
h
o
wed
th
at
a
d
d
in
g
2
0
m
l
o
f
o
r
g
an
ic
f
er
tili
ze
r
to
5
0
0
m
l
o
f
wate
r
with
an
in
itial
p
H
o
f
6
.
9
4
–
6
.
9
7
ad
ju
s
ts
th
e
m
i
x
tu
r
e’
s
p
H
to
f
all
with
in
th
e
o
p
tim
al
r
an
g
e
(
6
–
6
.
8
4
)
f
o
r
t
o
m
ato
p
lan
ts
.
Ad
d
in
g
m
o
r
e
th
a
n
2
0
m
l
ca
u
s
ed
th
e
p
H
to
f
all
b
el
o
w
th
e
s
u
itab
le
r
a
n
g
e.
T
h
is
r
esu
lt
was
co
n
f
ir
m
e
d
th
r
o
u
g
h
r
ep
ea
te
d
test
in
g
in
Fig
u
r
e
1
5
.
Fig
u
r
e
1
5
.
R
esu
lts
u
s
in
g
a
p
H
m
eter
3
.
2
.
3
.
P
ro
o
f
Ass
u
m
in
g
we
h
av
e
5
0
0
m
l
o
f
wate
r
th
at
we
wis
h
t
o
u
s
e
f
o
r
f
er
tili
za
tio
n
,
th
is
is
eq
u
iv
alen
t
to
1
0
0
%,
s
o
2
0
m
l
o
f
liq
u
id
f
er
tili
ze
r
is
eq
u
iv
ale
n
t
to
4
%
(
1
)
a
n
d
(
2
)
:
T
o
tal
v
o
lu
m
e
o
f
wate
r
=5
0
0
m
l
an
d
v
o
l
u
m
e
o
f
f
er
tili
ze
r
ad
d
ed
=
2
0
m
l
.
Evaluation Warning : The document was created with Spire.PDF for Python.
I
SS
N
:
2
0
8
8
-
8
7
0
8
I
n
t J E
lec
&
C
o
m
p
E
n
g
,
Vo
l.
15
,
No
.
5
,
Octo
b
e
r
20
25
:
4
5
5
5
-
4
5
6
8
4562
No
w,
to
f
in
d
th
e
p
er
c
en
tag
e
o
f
f
er
tili
ze
r
in
th
e
s
o
lu
tio
n
:
=
(
)
×
100
(
1
)
Su
b
s
titu
te
th
e
v
alu
es:
=
(
20
500
)
×
100
=
4
%
(
2
)
W
e
k
n
o
w
th
at
2
0
m
l
o
f
f
er
tili
ze
r
is
n
ee
d
ed
f
o
r
5
0
0
m
l
o
f
wate
r
,
wh
ich
is
eq
u
iv
alen
t
to
4
%.
So
,
th
e
am
o
u
n
t
o
f
f
er
tili
ze
r
r
eq
u
ir
e
d
f
o
r
an
y
v
o
lu
m
e
o
f
wate
r
ca
n
b
e
ca
lc
u
lated
b
ased
o
n
t
h
is
r
atio
(
3
)
.
=
(
×
4
500
)
(
3
)
An
d
,
th
e
v
o
lu
m
e
o
f
f
e
r
tili
ze
r
ad
d
ed
is
:
=
(
×
20
500
)
(
4
)
3
.
3
.
Resul
t
s
T
h
is
s
tu
d
y
a
p
p
lied
a
r
ea
l
b
e
n
ch
m
ar
k
o
v
er
a
s
p
r
in
g
s
ea
s
o
n
(
Ma
y
1
4
–
2
2
)
,
u
s
in
g
ca
p
tu
r
ed
d
ata
o
n
in
ter
n
al
air
tem
p
er
atu
r
e,
h
u
m
i
d
ity
,
s
o
il
p
H,
a
n
d
s
o
il m
o
is
tu
r
e.
T
h
e
o
b
jectiv
e
was
to
m
ain
ta
in
th
ese
p
ar
am
ete
r
s
with
in
th
r
esh
o
ld
s
d
ef
in
ed
in
c
o
n
s
u
ltatio
n
with
lo
ca
l f
ar
m
er
s
as sh
o
wn
in
T
ab
le
4
an
d
to
o
p
tim
ize
to
m
ato
p
lan
t
f
er
tig
atio
n
u
s
in
g
a
b
io
-
f
e
r
tig
atio
n
ap
p
r
o
ac
h
.
R
esu
lts
p
lo
tted
in
MA
T
L
AB
s
h
o
w
th
at
all
f
o
u
r
p
ar
a
m
eter
s
wer
e
ef
f
ec
tiv
ely
co
n
tr
o
lled
,
e
n
s
u
r
in
g
ef
f
icien
t f
e
r
tig
atio
n
.
T
ab
le
4
.
T
h
r
esh
o
ld
s
o
f
th
e
f
o
u
r
clim
atic
p
ar
am
eter
s
f
o
r
th
e
t
o
m
ato
g
r
ee
n
h
o
u
s
e
M
i
n
i
m
u
m
t
h
r
e
s
h
o
l
d
M
a
x
i
m
u
m
t
h
r
e
s
h
o
l
d
Te
mp
e
r
a
t
u
r
e
1
5
°
C
2
5
°
C
H
u
mi
d
i
t
y
6
0
%
7
0
%
S
o
i
l
p
H
6
6
.
8
S
o
i
l
m
o
i
s
t
u
r
e
7
0
%
8
0
%
I
n
o
u
r
wo
r
k
,
we
u
s
ed
s
ix
ac
tu
a
to
r
s
in
th
e:
a.
First f
an
to
r
eg
u
late
th
e
tem
p
e
r
atu
r
e.
b.
Seco
n
d
f
an
to
r
e
g
u
late
th
e
h
u
m
id
ity
.
c.
Hea
ter
to
r
eg
u
late
th
e
tem
p
er
a
tu
r
e.
d.
W
ater
p
u
m
p
1
t
o
d
is
tr
ib
u
te
wa
ter
.
e.
W
ater
p
u
m
p
2
t
o
d
is
tr
ib
u
te
b
i
o
-
f
er
tili
ze
r
.
f.
W
ater
p
u
m
p
3
t
o
d
is
tr
ib
u
te
liq
u
id
b
io
-
f
er
tili
ze
r
(
wate
r
+
b
io
-
f
er
tili
ze
r
)
.
Fig
u
r
es
1
6
,
1
7
,
1
8
an
d
1
9
p
r
e
s
en
t
m
o
n
ito
r
in
g
o
f
th
e
air
tem
p
er
atu
r
e,
air
h
u
m
id
ity
,
s
o
il
p
H,
an
d
s
o
il
m
o
is
tu
r
e
o
v
er
a
s
eq
u
en
ce
o
f
h
o
u
r
s
,
r
esp
ec
tiv
ely
.
T
h
ese
f
ig
u
r
es
illu
s
tr
ate
th
e
in
d
o
o
r
air
tem
p
er
atu
r
e,
i
n
d
o
o
r
air
h
u
m
id
ity
,
in
d
o
o
r
s
o
il
p
H,
an
d
in
d
o
o
r
s
o
il
m
o
is
tu
r
e.
Af
te
r
a
p
p
ly
in
g
o
u
r
f
u
zz
y
lo
g
ic
alg
o
r
ith
m
,
we
o
b
s
er
v
ed
th
at
th
e
f
o
u
r
in
ter
n
al
m
icr
o
clim
atic
p
ar
am
eter
s
o
f
o
u
r
g
r
e
en
h
o
u
s
e
we
r
e
well
ad
j
u
s
ted
with
in
th
e
s
p
ec
if
ied
th
r
esh
o
ld
s
.
Sp
ec
if
ically
,
th
e
m
ea
s
u
r
ed
p
ar
am
ete
r
s
,
o
v
er
t
h
e
s
eq
u
en
ce
o
f
h
o
u
r
s
,
r
em
a
in
ed
b
etwe
en
th
e
m
in
im
u
m
an
d
m
ax
im
u
m
th
r
esh
o
ld
s
.
Ad
d
itio
n
ally
,
th
e
ac
tu
ato
r
s
,
in
clu
d
in
g
th
e
h
ea
ter
,
f
an
s
,
a
n
d
t
h
r
ee
wate
r
p
u
m
p
s
,
f
u
n
ctio
n
ed
ef
f
ec
tiv
ely
to
r
eg
u
late
th
e
in
ter
n
al
m
icr
o
clim
ate
an
d
f
er
tig
ate
th
e
to
m
ato
p
lan
ts
.
I
n
o
u
r
s
tu
d
y
,
we
h
av
e
8
1
ca
s
es.
Fo
r
in
s
tan
ce
:
C
a
s
e
1
.
I
f
(
(
tem
p
er
at
u
r
e
<
1
5
°
C
)
AND
(
h
u
m
i
d
ity
<
6
0
%)
AND
(
s
o
il
m
o
is
tu
r
e
<
7
0
%)
AND
(
p
H
<
6
)
)
OR
(
(
tem
p
er
atu
r
e
<
15
°C
)
AND
(
h
u
m
id
ity
<
6
0
%)
AND
(
s
o
il m
o
is
tu
r
e
<
7
0
%)
AND
(
p
H
>
6
.
8
)
)
,
th
en
t
h
e
ac
tu
ato
r
s
f
o
r
th
e
h
ea
ter
,
wate
r
p
u
m
p
1
,
an
d
wate
r
p
u
m
p
3
ar
e
ac
tiv
ated
.
Af
ter
a
f
ew
s
ec
o
n
d
s
,
th
e
ac
tu
ato
r
s
s
to
p
wo
r
k
in
g
,
an
d
t
h
e
ca
p
tu
r
ed
p
a
r
am
eter
s
s
tab
ilize
b
etwe
en
th
e
m
in
im
u
m
an
d
m
ax
im
u
m
th
r
esh
o
ld
s
.
C
a
s
e
2
.
I
f
(
(
tem
p
e
r
atu
r
e
is
o
p
tim
al)
AND
(
h
u
m
id
ity
<
6
0
%)
AND
(
s
o
il
m
o
is
tu
r
e
<
7
0
%)
AN
D
(
p
H
<
6
)
)
O
R
(
(
tem
p
er
atu
r
e
is
o
p
tim
al)
AN
D
(
h
u
m
id
ity
is
o
p
tim
al)
AND
(
s
o
il
m
o
is
tu
r
e
<
7
0
%)
AND
(
p
H
>
6
.
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Evaluation Warning : The document was created with Spire.PDF for Python.