Inter
national
J
our
nal
of
Inf
ormatics
and
Communication
T
echnology
(IJ-ICT)
V
ol.
14,
No.
3,
December
2025,
pp.
1163
∼
1171
ISSN:
2252-8776,
DOI:
10.11591/ijict.v14i3.pp1163-1171
❒
1163
Soil
moistur
e
pr
ototype
soil
moistur
e
sensor
YL-69
f
or
Gaharu
(
Aquilaria
malaccensis
)
tr
ee
planting
media
Rikie
Kartadie
1
,
Muhammad
Agung
Nugr
oho
2
,
Adiyuda
Prayitna
1
,
Adi
K
usjani
3
,
Ardeana
Galih
Mardika
4
1
Department
of
Computer
Engineering,
Uni
v
ersitas
T
eknologi
Digital
Indonesia,
Y
ogyakarta,
Indonesia
2
Department
of
Informatics,
Uni
v
ersitas
T
eknologi
Digital
Indonesia,
Y
ogyakarta,
Indonesia
3
Computer
Engineering
V
ocational
Program,
Uni
v
ersitas
T
echnologi
Digital
Indonesia,
Y
ogyakarta,
Indonesia
4
Department
of
Information
T
echnology
Education,
Uni
v
ersitas
Bhineka
PGRI
T
ulung
agung,
T
ulung
agung,
Indonesia
Article
Inf
o
Article
history:
Recei
v
ed
Oct
24,
2024
Re
vised
Mar
16,
2025
Accepted
Jun
9,
2025
K
eyw
ords:
Humidity
Plant
gro
wth
Prototype
tool
Root
absorption
Soil
moisture
ABSTRA
CT
Soil
moisture,
dened
as
the
amount
of
w
ater
present
in
the
spaces
between
soil
particles,
plays
a
critical
role
in
plant
gro
wth.
Excessi
v
e
soil
moisture
can
lead
to
issues
such
as
root
rot,
de
viating
from
the
ideal
conditi
ons
required
for
root
absorption.
T
o
address
this,
we
de
v
eloped
a
prototype
tool
using
the
YL-69
soil
moisture
sensor
to
monitor
and
control
the
soil
moisture
le
v
els
in
Ag
ar
-
w
ood/Gaharu
tree
planting
media.
The
prototype
w
as
designed
to
acti
v
ate
a
w
ater
pump
when
soil
moisture
e
xceeded
80%,
ensuring
optimal
humidity
for
plant
gro
wth.
Once
the
moisture
le
v
el
dropped
belo
w
80%,
the
pump
w
as
de-
acti
v
ated
to
pre
v
ent
o
v
erw
atering.
The
YL-69
sensor
demonstrated
an
accurac
y
of
88.76%
under
controlled
conditions.
This
study
highlights
the
potential
of
using
lo
w-cost
sensors
for
automated
soil
moisture
management
in
small-scale
Gaharu
culti
v
ation.
This
is
an
open
access
article
under
the
CC
BY
-SA
license
.
Corresponding
A
uthor:
Rikie
Kartadie
Department
of
Computer
Engineering,
Uni
v
ersitas
T
eknologi
Digital
Indonesia
Jl.
Raya
Janti
Karang
Jambe
No.
143
Y
ogyakarta
55198,
Indonesia
Email:
rikie@utdi.ac.id
1.
INTR
ODUCTION
Ag
arw
ood
(Gaharu)
from
Aquilaria
malaccensis
is
a
v
aluable
non-timber
forest
product
(NTFP)
due
to
its
high
mark
et
price,
dri
v
en
by
quality
and
essential
oil
grades
[1],
and
demand,
especially
in
the
Middle
East
[2].
In
2001,
in
Pujang
an,
East
Kalimantan,
Gaharu
reached
Rp.
600,000/kg,
with
e
xport
v
alues
rising
from
US
$2
million
(1990-1998)
to
US
$39.9
million
in
2020
[3]–[5].
F
ound
across
Asia
[6],
this
threatened
species
thri
v
es
in
well-drained,
sandy
loam
soils
(pH
6.15,
80%
humidity
,
22-28
°C),
not
ooded
areas
[7],
[8].
Ov
ere
xploitation
has
made
it
rare,
necessitating
culti
v
ation
with
suitable
media
[9],
[10].
Soil
moist
ure,
critical
for
nutrient
transport
and
gro
wth,
is
addressed
by
this
prototype,
which
measures
moisture
in
Gaharu
planting
media
using
the
YL-69
sensor
and
Arduino
to
aid
f
armers.
2.
TECHNIQ
UES
FOR
MEASURING
SOIL
MOISTURE
In
addition,
k
eeping
soil
moisture
at
an
ideal
le
v
el
for
plants
i
s
essential.
Soil
moisture
content
can
be
measured
using
se
v
eral
dif
ferent
methods
[11]–[13].
It
is
important
to
ensure
that
the
soil
remains
moist,
as
this
supports
optimal
plant
gro
wth
and
de
v
elopment
[14].
Also,
re
gular
monitoring
of
soil
moisture
ca
n
help
pre
v
ent
problems
such
as
a
drought
or
w
aterlogging
that
can
af
fect
plant
health.
The
most
signicant
aspects
J
ournal
homepage:
http://ijict.iaescor
e
.com
Evaluation Warning : The document was created with Spire.PDF for Python.
1164
❒
ISSN:
2252-8776
of
soil
moisture
af
fect
the
balance
of
k
e
y
nat
ural
ecosystems
such
as
seed
germination,
w
ater
inltration,
plant
transpiration,
redistrib
ution,
e
v
aporation,
and
percolation
are
all
aspects
of
plant
nutrition
and
de
v
elopment.
A
plethora
of
e
xperimental
approaches
for
measuring
soil
moisture
ha
v
e
been
de
v
eloped
in
recent
decades
[15].
2.1.
Electrical
methods
The
standard
for
electrical
estimation
of
soil
moisture
w
as
rst
introduced
in
1897
[16].
The
frame-
w
ork
measures
the
adjustment
of
the
w
ater
mass
from
a
metal
barrel
in
the
shape
of
a
mousing
circle
e
xample,
using
an
accurac
y
bala
n
c
e,
while
the
soil
moisture
measurement
approach
emplo
ys
the
electrical
resisti
vity
technique.
Resisti
vity
is
needed
in
the
estimated
clock
for
this
plastic
co
v
er
.
Using
uctuations
in
moisture
content,
the
electrical
resistance
test
calculates
the
soil’
s
resisti
vity
.
The
resisti
vity
dec
reased
from
338
Ω
M
to
8
Ω
M
while
the
v
olumetric
moisture
content
increased
from
5.8%
to
38.5%.
F
or
dry
soils,
v
alues
greater
than
50
Ω
m
cause
the
resisti
vity
to
react
[17].
T
ime
domain
reectometry
(TDR)
method
is
a
method
that
util
izes
the
dielectric
properties
of
dirt
to
estimate
soil
humidity
le
v
els.
Dielectric
stability
estimate
by
estimating
the
electromagnetic
w
a
v
e’
s
full
circle
v
elocity
time
at
a
consistent
repeat
(high
repeatability
from
30
MHz
to
3
GHz)
to
and
from
the
ground-co
v
ered
metal
terminal.
The
link
analyzer
pro
vides
high
repeating
electromagnetic
pulses
and
lters
out
reected
w
a
v
es,
ground
embedded
poles,
and
links
connecting
analyzer
and
rods
[18].
TDR
estimates
a
small
v
olume
of
soil,
so
no
data
of
horizontal
spatialization
notice
[19].
TDR
sensors
assess
soil
moisture
by
deli
v
ering
electromagnetic
pulses
into
the
soil
and
e
v
aluating
ho
w
long
the
pulses
tak
e
to
tra
v
el
through
the
soil.
TDR
of
fers
precise
depth
measurements
and
is
frequently
utilized
in
en
vironmental
research
and
monitoring
[20],
[21].
The
capacitance
technique,
this
method
estimates
w
ater
content
by
estimating
the
dielectric
c
o
ns
is-
tenc
y
,
which
can
estimate
by
capacitance.
The
dielectric
steady
of
w
ater
is
around
81
for
wet
soil,
around
3
to
5
for
dry
soil,
and
1
for
air
.
The
capacitance
technique
utilizes
to
g
auge
soil
dampness
content
because
of
the
consistent
dielectric
increments
with
e
xpanding
air
content.
Capacitance,
C
is
straightforw
ardly
relati
v
e
to
the
dielectric
steady
.
Gc
addresses
the
structure
f
actor
,
which
relies
upon
the
size
and
state
of
the
sensor
capac-
itance,
and
the
distance
between
the
electrode’
s
ar
content
estimates
by
estimating
the
dielectric
consistenc
y
,
which
estimates
by
capacitance.
The
dielectric
steady
of
w
ater
is
around
81
for
wet
soil,
around
3
to
5
for
dry
soil,
and
1
for
air
.
C
=
G
c
K
d
(1)
The
capacitance
strate
gy
utilizes
to
g
auge
soil
dampness
content
K
d
,
because
of
the
consistent
dielectric
incre-
ments
with
e
xpanding
air
content.
Capacitance,
C
is
straightforw
ardly
relati
v
e
to
the
dielectric
steady
Where
G
c
addresses
the
structure
f
actor
which
relies
upon
the
size
and
state
of
the
sensor
capacitance
and
the
distance
between
the
anodes,
the
equation
can
see
on
(1)
[22].
Figure
1
sho
ws
a
capacitance
technique
for
measuring
soil
moisture.
T
w
o
electrode
rods
that
enter
into
the
ground
mak
e
up
the
capacitance
sensor
.
The
ground
serv
es
as
a
dielectric
and
the
tw
o
electrodes
to-
gether
mak
e
up
a
capacitor
.
On
reading
equipment,
changes
in
electrical
capacity
are
read
and
sho
w
changes
in
soil
moisture
[22].
By
k
eeping
the
v
olume
of
each
sample
constant
and
concurrently
measuring
the
mass
of
each
sample,
we
reliably
estimate
soil
moisture.
This
is
achie
v
ed
by
using
one
of
the
containers
with
graduated
markings
and
ensuring
that
the
soil
le
v
el
remains
constant
while
introducing
w
ater
to
the
soil
[23].
Figure
1.
Schematic
for
the
capacitance
method
of
measuring
soil
moisture
[22]
Int
J
Inf
&
Commun
T
echnol,
V
ol.
14,
No.
3,
December
2025:
1163–1171
Evaluation Warning : The document was created with Spire.PDF for Python.
Int
J
Inf
&
Commun
T
echnol
ISSN:
2252-8776
❒
1165
2.2.
Non
electrical
methods
W
etness,
the
most
frequent
approach
for
measuring
soil
moisture
is
to
collect
a
ph
ysical
sam
ple
from
the
measurement
location.
The
samples
were
weighed,
then
dried
in
an
o
v
en
at
100
°C
to
110
°C
for
24
to
48
hours
before
being
re
weighed.
In
(2)
calculates
the
gra
vimetric
moisture
content,
often
kno
wn
as
wettability
(w).
w
=
S
oil
M
ass
w
et
−
S
oil
M
ass
dr
y
S
oil
M
ass
dr
y
(2)
The
adv
antage
of
this
system
is
that
the
sample
is
easy
to
obtain,
and
the
moisture
content
is
easy
to
determine.
The
destructi
v
e
nature
of
the
method
of
fsets
the
possibility
of
repeating
sampling
at
the
e
xact
location
in
the
eld.
Second,
w(Mg
Mg-1),
although
a
good
indication
of
moisture
status,
is
not
as
v
aluable
for
plant
scientists
as
v
olumetric
and
potenc
y
humidity
[24].
The
amount
of
w
ater
that
is
accessible
to
plants
(for
transpiration)
or
the
ener
gy
status
of
w
ater
cannot
al
w
ays
be
determined
by
measuring
the
w
ater
content
of
soil
(or
other
porous
media).
W
ater
will
o
w
from
high-ener
gy
to
lo
w-ener
gy
re
gions,
with
w
ater
potential
indicating
the
ener
gy
condition
[24].
The
v
olumetric
moisture
content,
other
non
electrical
method
is
v
olumetric
moisture
content
[24].
Groundw
ater
status
can
determine
by
v
olume
(
m
3
m
−
3
),
where
is
the
v
olume
of
the
liquid
phase
per
unit
v
olume
of
b
ulk
soil.
This
method
is
a
popular
method
for
pro
viding
soil
moisture
status
information.
Ho
we
v
er
,
measurements
at
the
site
must
be
repeated,
especially
during
irrig
ation
scheduling.
If
Θ
is
the
de
gree
of
wetnes
s,
and
the
density
of
the
soil
is
kno
wn,
it
can
calculate
by
(3).
Θ
=
w
×
ρ
b
ρ
w
(3)
Where
Θ
is
the
de
gree
of
wetness,
w
is
wetness
(
M
g
M
g
−
1
),
ρ
b
is
the
b
ulk
density
of
the
soil
(
M
g
m
−
3
),
and
ρ
w
is
the
b
ulk
density
of
w
ater
(
M
g
m
−
3
).
The
b
ulk
density
of
the
soil
can
be
calculated
with
a
formula
on
(4).
ρ
b
=
dr
y
soil
w
eig
ht
V
ol
ume
of
sampl
er
(4)
In
this
prototype,
we
combine
tw
o
methods,
t
he
electrical
capacitance
technique
and
the
wetness
non-electrical
technique.
T
o
get
data
from
electrical
de
vices
which
use
the
YL-69
sensor
,
we
collect
data
by
connecting
it
to
Arduino.
3.
RESEARCH
METHOD
W
e
conducted
this
study
on
3
Ag
arw
ood
(Gaharu)
tree
planting
media
(can
see
on
subsection
4.2)
with
identical
treatments.
Sensors
were
placed
on
each
medium,
and
the
sensor
measurements’
results
were
recorded
for
each
medium.
W
e
carried
out
this
process
by
studying
the
characteristics
of
Ag
arw
ood
trees,
creating
prototypes,
and
comparing
the
sensor
measurement
results
with
manual
calculations.
3.1.
Resear
ch
model
The
soil
moisture
control
system
for
Ag
arw
ood
trees
uses
a
YL-69
sensor
,
16x2
LCD,
Arduino
Me
g
a
2560,
motor
dri
v
er
,
and
DC
pump.
The
sensor
measures
soil
moisture,
and
the
Arduino
process
es
the
data
(Khalaf,
2021),
displaying
results
on
the
LCD
to
control
the
pump.
3.2.
Pr
ototype
design
3.2.1.
Hard
war
e
design
This
stage
includes
design
using
fritzing
softw
are,
softw
are
design
(source
code
compilation),
and
component
design.
Each
step
in
the
design
stage
will
be
interconnected
so
that
the
researcher
can
return
to
the
pre
vious
step
if
there
is
a
f
ailure.
The
design
uses
a
fritzing
application
to
support
the
primary
data
collection
of
components
and
the
placement
of
the
pin
wires
that
need
in
the
de
v
elopment
of
the
prototype.
The
design
results
are
a
reference
in
the
form
of
components
used
in
conducting
de
v
elopment.
More
details
can
be
seen
in
Figure
2.
Soil
moistur
e
pr
ototype
soil
moistur
e
sensor
YL-69
for
Gaharu
(Aquilaria
malaccensis)
...
(Rikie
Kartadie)
Evaluation Warning : The document was created with Spire.PDF for Python.
1166
❒
ISSN:
2252-8776