QUANTITATIVE ASSESSMENT OF SOIL EROSION POTENTIAL IN THE CIKAPUNDUNG SUB-WATERSHED, WEST JAVA USING REMOTE SENSING AND GIS METHODS.
Cikapundung Sub-watershed is located in Bandung City, Bandung District, and West Bandung District. This area is susceptible to soil erosion because of frequent heavy rainfalls and steep terrains. Soil erosion can cause loss of soil structure, crops production decreases, and disrupt people’s daily...
Saved in:
Main Author: | |
---|---|
Format: | Final Project |
Language: | Indonesia |
Subjects: | |
Online Access: | https://digilib.itb.ac.id/gdl/view/69750 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
id |
id-itb.:69750 |
---|---|
spelling |
id-itb.:697502022-11-24T08:57:43ZQUANTITATIVE ASSESSMENT OF SOIL EROSION POTENTIAL IN THE CIKAPUNDUNG SUB-WATERSHED, WEST JAVA USING REMOTE SENSING AND GIS METHODS. Priska Handoko, Felicia Geologi, hidrologi & meteorologi Indonesia Final Project Cikapundung Sub-watershed, Geographic Information Systen, remote sensing, soil erosion capability, Soil Erosion Status, quantitative assessment,. INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/69750 Cikapundung Sub-watershed is located in Bandung City, Bandung District, and West Bandung District. This area is susceptible to soil erosion because of frequent heavy rainfalls and steep terrains. Soil erosion can cause loss of soil structure, crops production decreases, and disrupt people’s daily activities. It can also lead to landslides which can harm people and nearby buildings. Therefore, mapping of soil erosion in this Sub-watershed is needed. This study uses quantitative calculation with remote sensing and GIS (Geographic Information System) methods. The analysis was done by calculating every factor that is causing soil erosion using SES (Soil Erosion Status). The factors are lithology, geomorphology, slope, drainage, soil texture, lineament density, and land cover. SES method is a method to calculate soil erosion potential by using the mean of the erosion factors’ values. Soil erosion potential is divided into 5 categories: Category I with a soil loss rate of <15 ton/ha/year, category II with a soil loss rate 15-60 ton/ha/year, category III with a soil loss rate 61-180 ton/ha/year, category IV with a soil loss rate of 181-400 ton/ha/year, and category V which has a soil loss rate >400 ton/ha/year. The results are Cikapundung Sub-Watershed has a soil erosion capability range from category I to V. Category I covers 47% of total area. Then, categories II and III each encompass 11% of the area. Lastly, category IV and V covers 19% and 12% area respectively. Areas with high erosion potential are mostly in the north of the Sub-Watershed i.e scarp of Lembang Fault, south of Mt. Tangkuban Perahu, and around Lembang City. text |
institution |
Institut Teknologi Bandung |
building |
Institut Teknologi Bandung Library |
continent |
Asia |
country |
Indonesia Indonesia |
content_provider |
Institut Teknologi Bandung |
collection |
Digital ITB |
language |
Indonesia |
topic |
Geologi, hidrologi & meteorologi |
spellingShingle |
Geologi, hidrologi & meteorologi Priska Handoko, Felicia QUANTITATIVE ASSESSMENT OF SOIL EROSION POTENTIAL IN THE CIKAPUNDUNG SUB-WATERSHED, WEST JAVA USING REMOTE SENSING AND GIS METHODS. |
description |
Cikapundung Sub-watershed is located in Bandung City, Bandung District, and
West Bandung District. This area is susceptible to soil erosion because of frequent
heavy rainfalls and steep terrains. Soil erosion can cause loss of soil structure,
crops production decreases, and disrupt people’s daily activities. It can also lead
to landslides which can harm people and nearby buildings. Therefore, mapping of
soil erosion in this Sub-watershed is needed. This study uses quantitative
calculation with remote sensing and GIS (Geographic Information System)
methods. The analysis was done by calculating every factor that is causing soil
erosion using SES (Soil Erosion Status). The factors are lithology,
geomorphology, slope, drainage, soil texture, lineament density, and land cover.
SES method is a method to calculate soil erosion potential by using the mean of
the erosion factors’ values. Soil erosion potential is divided into 5 categories:
Category I with a soil loss rate of <15 ton/ha/year, category II with a soil loss rate
15-60 ton/ha/year, category III with a soil loss rate 61-180 ton/ha/year, category
IV with a soil loss rate of 181-400 ton/ha/year, and category V which has a soil
loss rate >400 ton/ha/year. The results are Cikapundung Sub-Watershed has a soil
erosion capability range from category I to V. Category I covers 47% of total area.
Then, categories II and III each encompass 11% of the area. Lastly, category IV
and V covers 19% and 12% area respectively. Areas with high erosion potential
are mostly in the north of the Sub-Watershed i.e scarp of Lembang Fault, south of
Mt. Tangkuban Perahu, and around Lembang City. |
format |
Final Project |
author |
Priska Handoko, Felicia |
author_facet |
Priska Handoko, Felicia |
author_sort |
Priska Handoko, Felicia |
title |
QUANTITATIVE ASSESSMENT OF SOIL EROSION POTENTIAL IN THE CIKAPUNDUNG SUB-WATERSHED, WEST JAVA USING REMOTE SENSING AND GIS METHODS. |
title_short |
QUANTITATIVE ASSESSMENT OF SOIL EROSION POTENTIAL IN THE CIKAPUNDUNG SUB-WATERSHED, WEST JAVA USING REMOTE SENSING AND GIS METHODS. |
title_full |
QUANTITATIVE ASSESSMENT OF SOIL EROSION POTENTIAL IN THE CIKAPUNDUNG SUB-WATERSHED, WEST JAVA USING REMOTE SENSING AND GIS METHODS. |
title_fullStr |
QUANTITATIVE ASSESSMENT OF SOIL EROSION POTENTIAL IN THE CIKAPUNDUNG SUB-WATERSHED, WEST JAVA USING REMOTE SENSING AND GIS METHODS. |
title_full_unstemmed |
QUANTITATIVE ASSESSMENT OF SOIL EROSION POTENTIAL IN THE CIKAPUNDUNG SUB-WATERSHED, WEST JAVA USING REMOTE SENSING AND GIS METHODS. |
title_sort |
quantitative assessment of soil erosion potential in the cikapundung sub-watershed, west java using remote sensing and gis methods. |
url |
https://digilib.itb.ac.id/gdl/view/69750 |
_version_ |
1822278573670531072 |