STUDY AND IDENTIFICATION OF THE HYDRAULIC CHARACTERISTICS OF UNDERGROUND RIVER

The existence of karst area in Indonesia nowadays is considered to have a strategic value. The karst topography itself is a natural structure that not only unique but also have a great potential, especially in the field of water resources. The hydrological topography is very unique and different bec...

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Main Author: Parinata, Bangun
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/46343
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:46343
spelling id-itb.:463432020-03-02T13:47:26ZSTUDY AND IDENTIFICATION OF THE HYDRAULIC CHARACTERISTICS OF UNDERGROUND RIVER Parinata, Bangun Indonesia Theses Underground river, hydraulic characteristic, green canyon, cijulang river. INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/46343 The existence of karst area in Indonesia nowadays is considered to have a strategic value. The karst topography itself is a natural structure that not only unique but also have a great potential, especially in the field of water resources. The hydrological topography is very unique and different because it constructed from limestones that inflict the surface water to become limited. Otherwise, there are so many water channel underground forming a conduit and a gap. The main purpose of this study is to find the difference of surface river and underground river based on the hydraulic characteristics by identifying the connection between amount of the discharge and rainfall of the river. This study started by collecting the secondary data from literature, then surveying the location of the study. To identify the difference between surface river and underground river, comparison between these two is needed. The comparison involved are the cross section of those two rivers and the curve that contained two factor that are the annual water discharge and rainfall intensity. The location of the study is in Cijulang River, Pangandaran Regency, West Java. The Cijulang Watershed has more than 30.000 hectare that flows in three sub-district in Pangandaran Regency. Then, the data obtained were the annual water discharge of Cijulang River and the annual rainfall of the Cijulang watershed. This data produce the curve that can be compared between those two factor and can be seen that there was a time lag between the highest rainfall to the highest water discharge in the underground river. After the analysis, can be concluded that there were differences between the surface river and underground river that can be seen on the cross sention formation and the presence of big time lag on the underground river that can’t be found on surface river. Later, the water quality of the Cijulang River that tested is not qualify as “clean water” based on Permenkes 492 year 2010, because of these water testing did not meet the regulation at some point. 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
description The existence of karst area in Indonesia nowadays is considered to have a strategic value. The karst topography itself is a natural structure that not only unique but also have a great potential, especially in the field of water resources. The hydrological topography is very unique and different because it constructed from limestones that inflict the surface water to become limited. Otherwise, there are so many water channel underground forming a conduit and a gap. The main purpose of this study is to find the difference of surface river and underground river based on the hydraulic characteristics by identifying the connection between amount of the discharge and rainfall of the river. This study started by collecting the secondary data from literature, then surveying the location of the study. To identify the difference between surface river and underground river, comparison between these two is needed. The comparison involved are the cross section of those two rivers and the curve that contained two factor that are the annual water discharge and rainfall intensity. The location of the study is in Cijulang River, Pangandaran Regency, West Java. The Cijulang Watershed has more than 30.000 hectare that flows in three sub-district in Pangandaran Regency. Then, the data obtained were the annual water discharge of Cijulang River and the annual rainfall of the Cijulang watershed. This data produce the curve that can be compared between those two factor and can be seen that there was a time lag between the highest rainfall to the highest water discharge in the underground river. After the analysis, can be concluded that there were differences between the surface river and underground river that can be seen on the cross sention formation and the presence of big time lag on the underground river that can’t be found on surface river. Later, the water quality of the Cijulang River that tested is not qualify as “clean water” based on Permenkes 492 year 2010, because of these water testing did not meet the regulation at some point.
format Theses
author Parinata, Bangun
spellingShingle Parinata, Bangun
STUDY AND IDENTIFICATION OF THE HYDRAULIC CHARACTERISTICS OF UNDERGROUND RIVER
author_facet Parinata, Bangun
author_sort Parinata, Bangun
title STUDY AND IDENTIFICATION OF THE HYDRAULIC CHARACTERISTICS OF UNDERGROUND RIVER
title_short STUDY AND IDENTIFICATION OF THE HYDRAULIC CHARACTERISTICS OF UNDERGROUND RIVER
title_full STUDY AND IDENTIFICATION OF THE HYDRAULIC CHARACTERISTICS OF UNDERGROUND RIVER
title_fullStr STUDY AND IDENTIFICATION OF THE HYDRAULIC CHARACTERISTICS OF UNDERGROUND RIVER
title_full_unstemmed STUDY AND IDENTIFICATION OF THE HYDRAULIC CHARACTERISTICS OF UNDERGROUND RIVER
title_sort study and identification of the hydraulic characteristics of underground river
url https://digilib.itb.ac.id/gdl/view/46343
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