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10989210.Pdf EnvironmentAsia 11(2) (2018) 149-163 DOI 10.14456/ea.2018.30 EnvironmentAsia ISSN 1906-1714; ONLINE ISSN: 2586-8861 The international journal by the Thai Society of Higher Education Institutes on Environment Mapping and Zonation Level of Landslides Hazard and Risk Assessment: A Case Study of Enrekang Regency, South Sulawesi, Indonesia. Uca Sideng*, Rosmini Maru, Sukri Nyompa, Amal Arfan, Abdul Malik, Muh Rais Abidin Department of Geography, Faculty of Mathematics and Natural Sciences Universitas Negeri Makassar *Corresponding author: [email protected] Received: November 29, 2017; Accepted: :March 27, 2018 Abstract Enrekang Regency is one of the districts in South Sulawesi that often happens landslide. Therefore it is necessary to mapping and zonation areas prone to landslides. This study aims to map and determine the risk level of landslides hazard in Enrekang Regency. Zonation level of landslides hazard risk is carried out by overlay technique of: landform map, gradien slope map, geology map, soil texture map, land use map and landslides hazard map, respectively. The landscape, gradien of slope, type of rock, soil texture and land use make in five class respectively, with the value 1 until 5. The landslides risk level is performed by overlay using ArcGis 10.3.The result of analysis shows there are 3 classes of landslides risk level in Enrekang Regency that is low, medium and high, respectively. There are sequences of areas most vulnerable to landslides, there are Bungin, Buntu Batu, Anggeraja, Enrekang, Masalle, Baraka, Baroko, Alla, and Maiwa. Keywords: Mapping; Zonation; Landslide hazard; Risk assessment 1. Introduction occurred in all parts of Indonesia between 2014 until 2016 years. Events of landslides or Landslide, as one of the natural hazard movements of soil masses, rocks or in the world (Dai et al., 2002; Jian and combinations, occur on the slopes (Avanzi Xiang-guo, 2009). As well as in Indonesia, et al., 2004). The phenomenon of landslide landslide is one of the most common types occurs because the process of seeking new of natural hazards, have caused large number balance due to the interference. Landslides casualties and huge economic losses. National often occur during heavy rainstorms, especially Hazard Mitigation Agency (BNPB) noted there in the mountains regions (Lee and Yi Ho, 2009). are about 721 incidents of landslides hazard In South Sulawesi, some areas prone to 149 U. Sideng et al. / EnvironmentAsia 11(2) (2018) 149-163 landslides during the rainy season are and group exposure and capacity are also critical Enrekang, Tana Toraja, Palopo, North Luwu, in risk assessment (Wisner et al., 2004). The East Luwu, Soppeng, Wajo, Sinjai, Jeneponto, objective of assessing risk is substantially Bantaeng, and Gowa. Enrekang regency is different between landslide hazard and ranked 2nd among 24 districts/municipalities assessment of other hazards. The assessment of that enter areas prone to landslides (Environmental landslides risk aims to determine the estimated Impact Management Agency). Landslide are not loss of life, injuries, property destruction and only caused by physical factors such as slopes loss of economic activities caused by landslides and shapes but also influenced by human events. intervention (Marcato et al., 2012). The development The urge of the population to the land in of a region will increase the need for land as a Enrekang Regency is increasing as the population residence and economic activity, availability of grows. Land use in areas with steep slopes is land is not increased. Thus some residents increasing. Land cultivation that ignores occupy an uninhabitable location such as in hilly conservation methods will trigger landslides. terrain and mountain slopes that are prone to Even lately the phenomenon of forest landslides. Steep slopes of human activity will encroachment began to appear that will result trigger higher levels of vulnerability, when land in the loss of large long-rooted trees that can is being over-exploited without regard to land strengthen the soil mass bonds (Ayalew et al., carrying capacity. The type of landslides based 2005; Maru et al., 2016). The encroachment on the speed of movement can be divided into triggered the occurrence of landslides, espe- 5 (five) types: flow; avalanches; collapse; cially in the sloping areas Ayalew et al., 2005; compound; subsidence (land subsidence). Maru et al. 2016). The availability of a complete Meanwhile, the main factors causing landslides landslides hazard risk map is essential to prevent are natural factors and management factors. the occurrence of casualties and the economic Natural factors are derived from natural impact on the community (Jiana, Xiang-guo, conditions, such as: rainfall, geological 2009). Therefore Enrekang Regency is needed conditions, the existence of fracture/fault/ landslides zonation map. In addition, it can also escape, and the depth of the soil (regolith). serve as input for the preparation of the spatial Management factors consist of: land use, road plan of Enrekang Regency. infrastructure, and settlement density Hazard risk is the possibility of a hazard 2. Material and Methods occurring causing a special loss rate. Risk needs to be assessed so that it can determine the amount of the loss that has been estimated and a. Location of the study area it can be anticipated in a region (UNDRO, 1992). Enrekang Regency is located in south Many experts have developed a formulation in Sulawesi, Indonesia. The Enrekang Regency assessing hazard risks. And in general hazard lies between at the 119040’53’’- 120006’33’’ risk is a combination of hazard and vulnerability. east- longitude and 3014’36’’- 3050’00’’ south- However, in addition to these factors, individual latitude. Enrekang Regency is 1,786.01 km2 in 150 U. Sideng et al. / EnvironmentAsia 11(2) (2018) 149-163 size. Boundary of Enrekang Regency is north tabular data, which is paired with GIS analysis of Tanah Toraja Regency, South of Sidenreng in spatial analysis and scoring based assessment. Rappang Regency, West of Tana Toraja Regency In this research there are 5 variables for the and Pinrang Regency and east of Luwu Regency. determination of landslides prone areas that Enrekang regency has a varied topography of refer to the Studies Center for Natural Hazard hills, mountains and valleys with a height of (Pusat Studi Bencana Alam: PSBA) UGM 47 to 3,293 meters above sea level and has no (2001). The variables are as follows: landform, coastal area. The hills and the mountains are slope, rock type, soil texture and land use. The 84.96%, while the flat area is only 15.04%. The variable used to determine the risk assessment rainy season occurs in November-July, while the for a landslides hazard is population density, dry season occurs in August-October (Figure 1). the number of people per unit area that will be threatened in case of landslides hazard. In this This research was conducted by using study using units of hectares (ha). quantitative descriptive approach, by compiling Figure 1. Location of the study area 151 U. Sideng et al. / EnvironmentAsia 11(2) (2018) 149-163 Literature review Field observation Collecting data Data of Landsat 8 Topography population density DEM Image map Population Landform Land-use Geology Soil texture Map of spatial and Slope map density map map map map map regional planning To determine the landslides Scoring hazard risk index Overlapping map Landslides hazard risk index (LHI) 10.3 Arcgis LHI = 0.36 BL + 0.36 L + 0.07 G + 0.14 T + 0.07 PLL Class prone to landslide Zonation of landslide prone area Overlay Overlay Landslides risk map based on Overlay map of spatial and regional plans with the map prone landslids hazard population density Recommendations for spatial and regional arrangements based on area prone landslides hazard Enrekang Regency Figure 2. Landslide disaster risk management and land use planning strategy 152 U. Sideng et al. / EnvironmentAsia 11(2) (2018) 149-163 b. Parameter in hazard assessment. and Moya, 2008). Enrekang Regency did not have data of landslides events that have Influencing factors of landslide hazard in occurred both time and spread. Therefore, a region are landform, slope, geology, soil and to map the spread of landslides hazard using land use (Hadmoko et al., 2010; Marcato et al., semi-quantitative method, that is based on 2012). In addition, landslide can be triggered factors that can cause landslides, geology by various external factors such as rainfall (based on type of rock), soil (texture), slope intensity, earthquake, changes in groundwater (gradient slope), and land use (land management) level and river bank erosion (Dai et al., 2002; (Harp et al., 2009). This research is using scoring Harp et al., 2009). Human activities such as technique on each parameter. Scoring for each the construction of roads cutting slopes and assessment variable is based on the level of clearing of land can also trigger landslide influence variables in giving impact of landslides (Jaiswal et al., 2010). The probability of hazard. The higher the value of score, the higher accurrence is one of the key components of the vulnerability. Determination of total value of the risk equation. To assess this probability in score is done by overlay of landform map, slope, landslides risk analysis, using two different geology, soil texture and land use (Sartohadi et al., approaches have been traditionally and 2010). The criteria for determining landslides probability is obtained by means of the statistical prone areas are shown in Table 1. analysis of the past landslides event (Corominas Figure 3. Slope map of Enrekang Regency 153 U. Sideng et al. / EnvironmentAsia 11(2) (2018) 149-163 Soil samples are taken on each every of Enrekang District and ground checks sources. land unit. The land unit are made by overlay Land use maps were obtained from SPOT 5 between gradient slope map, land use map satellite images, the result of cooperation and geological map.
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