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This content has been downloaded from IOPscience. Please scroll down to see the full text. Download details: IP Address: 152.118.24.10 This content was downloaded on 16/02/2017 at 09:53 Please note that terms and conditions apply. Modelling land use/cover changes with markov-cellular automata in Komering Watershed, South Sumatera View the table of contents for this issue, or go to the journal homepage for more 2017 IOP Conf. Ser.: Earth Environ. Sci. 54 012103 (http://iopscience.iop.org/1755-1315/54/1/012103) Home Search Collections Journals About Contact us My IOPscience You may also be interested in: The critical land in Komering watershed as a result of land use changes from 2000-2016 period E Kusratmoko, S T Dayanti and Supriatna Surface runoff estimation from various land use in Mapili Watershed using SCS Curve Number and Geographic Information System Sri Malahayati Yusuf, David Guluda and Trisumitra Jayanegara Analysis of Land Cover Change in a Coastal Area using Remotely Sensed Data I Jaunzeme, M Kainka, M Reiniks et al. Modelling LULC for the period 2010-2030 using GIS and Remote sensing: a case study of Tikrit, Iraq Sinan Jasim Hadi, Helmi Z M Shafri and Mustafa D Mahir Spatial modelling of land use/cover change (LUCC) in South Tangerang City, Banten K Saifullah, B Barus and E Rustiadi Land use cover changes and water quality of Cipunten Agung Watershed Banten Afifa Karima and Regan Leonardus Kaswanto Temporal and spatial changes of land use and landscape in a coal mining area in Xilingol grassland Chunzhu Guan, Baolin Zhang, Jiannan Li et al. Phase transitions in two-dimensional stochastic cellular automata K Kaneko and Y Akutsu Forest fires detection in Indonesia using satellite Himawari-8 (case study: Sumatera and Kalimantan on august-october 2015) Fatkhuroyan, Trinah Wati and Andersen Panjaitan

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This content has been downloaded from IOPscience. Please scroll down to see the full text.

Download details:

IP Address: 152.118.24.10

This content was downloaded on 16/02/2017 at 09:53

Please note that terms and conditions apply.

Modelling land use/cover changes with markov-cellular automata in Komering Watershed,

South Sumatera

View the table of contents for this issue, or go to the journal homepage for more

2017 IOP Conf. Ser.: Earth Environ. Sci. 54 012103

(http://iopscience.iop.org/1755-1315/54/1/012103)

Home Search Collections Journals About Contact us My IOPscience

You may also be interested in:

The critical land in Komering watershed as a result of land use changes from 2000-2016 period

E Kusratmoko, S T Dayanti and Supriatna

Surface runoff estimation from various land use in Mapili Watershed using SCS Curve Number and

Geographic Information System

Sri Malahayati Yusuf, David Guluda and Trisumitra Jayanegara

Analysis of Land Cover Change in a Coastal Area using Remotely Sensed Data

I Jaunzeme, M Kainka, M Reiniks et al.

Modelling LULC for the period 2010-2030 using GIS and Remote sensing: a case study of Tikrit, Iraq

Sinan Jasim Hadi, Helmi Z M Shafri and Mustafa D Mahir

Spatial modelling of land use/cover change (LUCC) in South Tangerang City, Banten

K Saifullah, B Barus and E Rustiadi

Land use cover changes and water quality of Cipunten Agung Watershed Banten

Afifa Karima and Regan Leonardus Kaswanto

Temporal and spatial changes of land use and landscape in a coal mining area in Xilingol grassland

Chunzhu Guan, Baolin Zhang, Jiannan Li et al.

Phase transitions in two-dimensional stochastic cellular automata

K Kaneko and Y Akutsu

Forest fires detection in Indonesia using satellite Himawari-8 (case study: Sumatera and Kalimantan

on august-october 2015)

Fatkhuroyan, Trinah Wati and Andersen Panjaitan

Modelling land use/cover changes with markov-cellular

automata in Komering Watershed, South Sumatera

E Kusratmoko*, S D Y Albertus and Supriatna

Magister Program Department of Geography FMIPA Universitas Indonesia Gedung H

Kampus UI Depok, Indonesia

E-mail: [email protected]

Abstract. This research has a purpose to study and develop a model that can representing and

simulating spatial distribution pattern of land use change in Komering watershed. The Komering

watershed is one of nine sub Musi river basin and is located in the southern part of Sumatra

island that has an area of 8060,62 km2. Land use change simulations, achieved through Markov-

cellular automata (CA) methodologies. Slope, elevation, distance from road, distance from river,

distance from capital sub-district, distance from settlement area area were driving factors that

used in this research. Land use prediction result in 2030 also shows decrease of forest acreage

up to -3.37%, agricultural land decreased up to -2.13%, and open land decreased up to -0.13%.

On the other hand settlement area increased up to 0.07% , and plantation land increased up to

5.56%. Based on the predictive result, land use unconformity percentage to RTRW in Komering

watershed is 18.62 % and land use conformity is 58.27%. Based on the results of the scenario,

where forest in protected areas and agriculture land are maintained, shows increase the land use

conformity amounted to 60.41 % and reduce unconformity that occur in Komering watershed to

17.23 %.

1. Introduction

Komering watershed is one sub-basin of nine sub basin in the Musi basin catchment, and in line with

the developments in Komering watershed, the various orders of life is changing rapidly following the

various needs of the community. One impact of these changes is that the pattern of use of natural

resources which are located around the community. In addition to the growth in population and

settlement area will urge the land use/cover pattern in Komering watershed change that is usually

converted from the use of agricultural land to non-agricultural so that erosion and sedimentation is high

enough. The condition of the river and the land area is seen that the upstream Komering watershed has

been impaired or decline of ecosystems and Environment [1]. The setback is particularly indicated

environmental quality include the existence of illegal logging for the area of aquaculture, plantations

and settlement areas do not pay attention to the principles of environmental sustainability and the

turbidity of the water in a river estuary Komering watershed. To prevent such degradation, monitoring

of land use/cover change in Komering watershed is very important. Therefore this study was intended

to employ Geographycal Information System and remote sensing techniques to detect land use/cover

change in Komering watershed between 1990 and 2016, and Markov-cellular automata (CA)

methodologies to simulating land use/cover change in year 2030 using Land Change Modeler tools on

Idrisi Selva software.

1

LISAT IOP PublishingIOP Conf. Series: Earth and Environmental Science 54 (2017) 012103 doi:10.1088/1755-1315/54/1/012103

International Conference on Recent Trends in Physics 2016 (ICRTP2016) IOP PublishingJournal of Physics: Conference Series 755 (2016) 011001 doi:10.1088/1742-6596/755/1/011001

Content from this work may be used under the terms of the Creative Commons Attribution 3.0 licence. Any further distributionof this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.

Published under licence by IOP Publishing Ltd

2. Method

2.1. Study Area

The research location is situated in Komering watershed, which is administratively includes three

regency, which Ogan Ulu Timur, Ogan Ulu and Ogan Ilir regencies (figure 1).

Figure 1. Map of the Komering watershed

2.2. Materials

Satellite data : Landsat images of path/row 124/63, Landsat 5 TM for 1990 and 2000, Landsat

7 ETM for 2010 and Landsat 8 OLI for 2016. The satellite acquisition date for the images was

May to August. DEM data with 30 meter resolution to create watershed boundary.

Software : Idrisi selva 17, ENVI 5.1, and Arc GIS 10.1.

2.3. Data analysis

Image classification : Classification of land use/cover was conducted using supervised

classification in ENVI 5.1 software. The classification process produced land use/cover maps

for the years 1990, 2000, 2010 and 2016. The six land use classes were generated which

included; forest, water body, settlement area, plantation, bare-land and agricultural land.

Land use change detection : land use/cover change detection was conducted by post-

classification comparison change detection using ARC GIS 10.1. This was achieved by

comparative analysis of the years 1990-2000, 2000-2010, and 2010-2016 (figure 2 and 3).

2

LISAT IOP PublishingIOP Conf. Series: Earth and Environmental Science 54 (2017) 012103 doi:10.1088/1755-1315/54/1/012103

Figure 2. Image analysis and detection process

CA –Markov Model: Markov chain and CA both are the discrete dynamic model in time and

state [2]. One inherent problem with Markov is that it provides no sense of geography. The

transition probabilities may be accurate on per category basis, but there is no knowledge of the

spatial distribution of occurrences within each landuse category [3]. CA was used to add spatial

character into the model. The Idrisi Selva 17 integrates CA with Markov very well [4]. In this

research, we take the Idrisi GIS software to simulate the land use/cover in Komering watershed.

The driving factors that used in this research are slope, elevation, distance from road, distance

from river, distance from capital sub-district, distance from settlement area.

3. Results and Discussions

3.1. Change in Komering Watershed from 1990 to 2016 Six land use/cover classes were produced. These included; forest, water body, settlement area,

agriculture land, bare-land and plantation. The results of testing the accuracy of interpretation of Landsat

imagery in 2016 visually gives kappa coefficient value by 87% and overall accuracy of 92%. The value

is compliant validation of interpretation so that proper land use/cover maps used in the study. A map of

the land use/cover interpretation of the results can be good if it has an accuracy of more than 70% [5].

Land use/cover change from 1990 to 2016 is shown in figure 4 and figure 5. The result showed that in

Komering watershed revealed a significant change in the proportions of the various land use/cover

change types of the study area from the year 1990 to 2016, forest decreased up to -1.66%, agricultural

land decreased up to -1.52%, and open land decreased up to -0.12%. On the other hand settlement area

increased up to 0.09% , and plantation land increased up to 3.21% (table 1 and 2).

LAND USE

CHANGE Map

1990-2000

LAND USE

CHANGE Map

2000-2010

LAND USE

CHANGE Map

2010-2016

Land Use Map

2000

Land Use Map

2010

Land Use Map

2016

GIS

Overlay

Land Use

Classification

Landsat 7 ETM year

2000

Landsat 7 ETM year

2010 Landsat 8 OLI

year 2016

Radiometric and Atmosferic Correction

Image cropping

validation

Composite image Landsat 5 (RGB 321)

and Landsat 7 and 8 (RGB 764)

Supervised

classification

Landsat 5 TM year 1990

Land Use Map

1990

DEM SRTM

30 meter

Watershed

delineation

3

LISAT IOP PublishingIOP Conf. Series: Earth and Environmental Science 54 (2017) 012103 doi:10.1088/1755-1315/54/1/012103

Figure 3. Landuse modelling Process

Figure 4. Komering watershed land use/cover in years 1990, 2000, 2010 and 2016

0

50000

100000

150000

200000

250000

300000

350000

Water body Forest Agriculture

land

Plantation Settlement

area

Open land

1990 2000 2010 2016

Driving factor

-slope

-elevation

-distance from road

-distance from river

- distance from

capital district

–distance from

settlement area

Verification

with field

survey

Landsat Sattelite Image (1990,

2000, 2010, 2016)

Interpretation and

classification

Land use

1990

Land use

2000

Land use

2010

Land use

2016

Land use

change map

1990-2000

Land use

change map

2000-2010

Land use

change map

2010-2016

Cellular automata/

Markov chain

Model validation

Landuse map Komering

watershed year 2030

LAND USE

CHANGE

with RTRW

scenario

4

LISAT IOP PublishingIOP Conf. Series: Earth and Environmental Science 54 (2017) 012103 doi:10.1088/1755-1315/54/1/012103

Figure 5. Land use/cover Komering watershed map year 1990 (5a), 2000(5b), 2010(5c), 2016(5d)

Table 1. Areas from different land use/cover classes in 1990, 2000, 2010, 2016.

Landuse

Area

1990 2000 2010 2016

Hectare % Hectare % Hectare % Hectare %

Water body

21.817 2,71

21.817 2,71

21.817 2,71

21.814 2,71

Forest

215.188 26,70

201.663 25,02

201.662 25,02

201.812 25,04

Agriculture

land

248.858 30,87

249.851 31,00

230.860 28,64

236.574 29,35

Plantation

287.936 35,72

300.256 37,25

319.247 39,61

313.781 38,93

Settlement

area

29.232 3,63

29.422 3,65

29.422 3,65

29.993 3,72

Open land

3.031 0,38

3.054 0,38

3.054 0,38

2.089 0,26

5

LISAT IOP PublishingIOP Conf. Series: Earth and Environmental Science 54 (2017) 012103 doi:10.1088/1755-1315/54/1/012103

Table 2. Areas changes from different land use/cover classes in 1990, 2000, 2010, 2016.

Landuse

Change

1990-2000 2000-2010 2010-2016 1990-2016

Hectare % Hectare % Hectare % Hectare %

Water body 0 0,00 0 0,00 -3 0,00 -3 0,00

Forest -13.525 -1,68 -1 0,00 151 0,02 -13.375 -1,66

Agriculture

land 992 0,12 -18.990 -2,36

5.713 0,71 -12.284 -1,52

Plantation

12.320 1,53

18.991 2,36 -5466 -0,68

25.844 3,21

Settlement

area 189 0,02 - 0,00 571 0,07 760 0,09

Open land 23 0,00 - 0,00 -966 -0,12 -942 -0,12

3.2. Land use/cover simulation Model validation is done by comparing the prediction of land use/cover in 2016 with the actual land

use/cover maps in 2016 (table 3). Validation test results obtained by the 81% which indicates that the

model simulations were done very well. The land use/cover predictive result (figure 6 and 7) in 2030

also shows decrease of forest area up to -3.37%, agricultural land decreased up to -2.13%, and open

land decreased up to -0.13% (table 4). On the other hand settlement area increased up to 0.07% , and

plantation land increased up to 5.56%. Based on the predictive result, land use/cover unconformity

percentage to RTRW in Komering watershed is 18.62 % and land use/cover conformity is 58.27%.

Table 3. Major land use/cover conversions from 1990 to 2016

2016 Water body

(hectares)

Forest

(hectares)

Agriculture Land

(hectares)

Plantation

(hectares)

Settlement area

(hectares)

Open land

(hectares) 1990

Water body 22,088 2 1 2 3 0

Forest 64 207,128 1,360 12,725 301 0

Agriculture land 0 0 246,838 14,148 422 23

Plantation 0 0. 0. 295,763 256 0

Settlement area 0 0 0 0 30,187 0

Open land 150 208 527 79 2,199

Table 4. Land use/cover classes and land use/cover change between 2016 and 2030.

Landuse

2016 2030 % change

hectare % hectare % hectare %

Water body 21,814 2.71 21,816 2.71 1 0.00

Forest 201,812 25.04 174,670 21.67 -27,141 -3.37

Agriculture land 236,573 29.35 219,404 27.22 -17,169 -2.13

Plantation 313,780 38.93 358,612 44.49 44,831 5.56

Settlement area 29,992 3.72 30,540 3.79 547 0.07

Open land 2,088 0.26 1,017 0.13 -1,070 -0.13

6

LISAT IOP PublishingIOP Conf. Series: Earth and Environmental Science 54 (2017) 012103 doi:10.1088/1755-1315/54/1/012103

Based on The RTRW scenario, where forest in protected areas and agriculture land are maintained,

shows increase the land use/cover conformity amounted to 60.41 % and reduce unconformity that occur

in Komering watershed to 17.23 % (table 5). Similarly, the use of land agricultural land has not achieved the expected objective because it does not change the broad decline of agricultural land changes,

however, this scenario is very possible to be applied.

Table 5. Land use/cover classes and land use/cover change between 2016 and 2030 with RTRW

scenario

Landuse

2016 2030 % change

Hectare % hectare % hectare %

Water body 21,814 2.71 21,816 2.71 1. 0.00

Forest 201,812 25.04 189,580 23.52 -12,231 -1.52

Agriculture land 236,573 29.35 219,353 27.21 -17,219 -2.14

Plantation 313,780 38.93 343,703 42.64 29,922 3.71

Settlement area 29,992 3.72 30,541 3.79 548 0.07

Open land 2,088 0.26 1,067 0.13 -10,20 -0.13

Figure 6. Land use/cover change Komering watershed map year 2030 without skenario

7

LISAT IOP PublishingIOP Conf. Series: Earth and Environmental Science 54 (2017) 012103 doi:10.1088/1755-1315/54/1/012103

Figure 7. Land use/cover change Komering watershed map year 2030 with scenario

4. Conclusion This research presents the results for analysing and predicting land use/cover change by using remote

sensing data and CA-Markov model. From this study of land use/cover changes in Komering watershed

from 1990 to 2016, some conclusions were obtain the decrease in forest areas from 26.7 % to 25.04%

is closed related with increase in plantation areas from 35.72% to 38.93%. The simulation of land

use/cover in the year 2030 indicated that the forest and agricultural land decreased rapidly and change

to plantation area.

References

[1] BPDAS 2009 Laporan Hasil Identifikasi dan Karakteristik Sub Das Komering. Sumatera Selatan

[2] Tiur Vera Damayanti Peruge, Samsu Arief H, Sakka 2012 Model Of Land Use Change Of Use

Cellular Automata - Markov Chain In The Mamminasata (Makassar: Universitas Hassanudin)

[3] Eastman JR 2003 IDRISI Kilimanjaro Guide to GIS and Image Processing Worcester (MA: Clark

University)

[4] Clark Labs 2006 IDRISI Andes software Worcester (MA: Clark University)

[5] Purwadhi, Hardiyanti S F 2001 Interpretasi Citra Digital (Jakarta : Grasindo)

8

LISAT IOP PublishingIOP Conf. Series: Earth and Environmental Science 54 (2017) 012103 doi:10.1088/1755-1315/54/1/012103