LANDSLIDE SUSCEPTIBILITY ZONATION OF SUNGAI PENUH WATERSHED AND SUROUNDING AREAS USING FREQUENCY RASIO (FR) AND ARTIFICIAL NEURAL NETWORK (ANN)
The Sungai Penuh watershed and surroundings are part of the Sungai Penuh City, Jambi Province. This area is included in the medium to high of landslide susceptibility. The morphological condition of the area is in the form of steep hills. This is one of the controlling factor for landslides. The...
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Format: | Theses |
Language: | Indonesia |
Subjects: | |
Online Access: | https://digilib.itb.ac.id/gdl/view/55975 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | The Sungai Penuh watershed and surroundings are part of the Sungai Penuh City,
Jambi Province. This area is included in the medium to high of landslide
susceptibility. The morphological condition of the area is in the form of steep
hills. This is one of the controlling factor for landslides. The landslide
susceptibility maps currently available are still at a provincial scale. The purpose
of this research to determine landslide susceptibility maps on a more detailed
scale, namely the sub-watershed scale. The method used to analyze the
susceptibility of landslides consists of two types, namely bivariate statistical
method and machine learning method. The bivariate statistical method is the
frequency ratio (FR) and the machine learning method is the artificial neural
network (ANN). The machine learning method is expected to take advantage of
the speed and accuracy of calculating the landslide susceptibility map.
Based on field observations and identification by remote sensing on the Google
Earth Pro image, there were 98 landslides in the study area. The landslide event
data is then divided into two groups randomly with three data set distribution,
namely scenario A training data by 60% with testing data by 40%, scenario B
training data by 70% with testing data 30%, with scenario C training data by
85% with testing data by 15%. Futhermore, twenty parameters were tested to
determine their effect on landslides, namely elevation, slope, aspect, curvature,
topography wetness index (TWI), stream power index (SPI), lithology, distance to
fault, distance to lineament, lineament density, earthquake, rainfall, distance to
drainage, drainage density, flow direction, springs density, land use, distance to
road, NDVI, and NDWI. Based on the results of the evaluation of the area under
(AUC), kappa coefficient, seed cell area indeks (SCAI), and spatial domain the
best method is the artificial neural network (ANN) method with scenario B. |
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