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Kecamatan Muara Gembong is located in Kabupaten Bekasi, Jawa Barat has  36 km of coastline. Therefore, the coastal area of Kecamatan Muara Gembong has unique coastal morphology, because there are sedimentation and erosion that affect the survival of local communities. Therefore, survey o...

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Main Author: IHSAN IRAQI (NIM : 15108017) ; (Pembimbing :Dr. rer. nat. Wiwin Windupranata, S.T., M.Si. ; , MUSTAFA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/19027
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:19027
spelling id-itb.:190272017-10-09T10:51:11Z#TITLE_ALTERNATIVE# IHSAN IRAQI (NIM : 15108017) ; (Pembimbing :Dr. rer. nat. Wiwin Windupranata, S.T., M.Si. ; , MUSTAFA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/19027 Kecamatan Muara Gembong is located in Kabupaten Bekasi, Jawa Barat has &#61617; 36 km of coastline. Therefore, the coastal area of Kecamatan Muara Gembong has unique coastal morphology, because there are sedimentation and erosion that affect the survival of local communities. Therefore, survey of coastal morphology is needed <br /> <br /> <br /> <br /> <br /> <br /> <br /> to determine the morphological phenomena along the coastal area in order to form a system or a way of tackling, land use planning system, and evaluating impact of sedimentation system in coastal area of Kecamatan Muara Gembong. Survey of coastal morphology which is needed to obtain the morphology data of <br /> <br /> <br /> <br /> <br /> <br /> <br /> Kecamatan Muara Gembong Coastal Area is divided into two activities, namely sediment sampling and investigation of the coastline. The sample of sediment in Kecamatan Muara Gembong is taken by manual process. Sediment movement is happened when the value of actual shields parameter larger than its critical shields parameter value. In addition, the fall velocity calculation speed is compared to the flow velocity that generates the type of sediment displacement. The current direction <br /> <br /> <br /> <br /> <br /> <br /> <br /> is used to determine the direction of the sediment movement at the fastest flow velocity of high tide and low tide. Coastal classification is used to recognize the basic conditions and potential of the Muara Gembong coastal. The result of sediment movement and sediment displacement calculation shows the that it moves on high tide, meanwhile on low tide only three out of ten sample that indicates movement. All the sediment that moved suspended into water. After the observation occurred, Muara Gembong coastal Located on stable tectonic control, Located off back to the ocean, Has steep slope, Has Very fine sand, Its vegetation dominated by mangrove, Classified into Primary coast (mostly influenced by land process), Its ocean process mostly influenced by wave movement. 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 Kecamatan Muara Gembong is located in Kabupaten Bekasi, Jawa Barat has &#61617; 36 km of coastline. Therefore, the coastal area of Kecamatan Muara Gembong has unique coastal morphology, because there are sedimentation and erosion that affect the survival of local communities. Therefore, survey of coastal morphology is needed <br /> <br /> <br /> <br /> <br /> <br /> <br /> to determine the morphological phenomena along the coastal area in order to form a system or a way of tackling, land use planning system, and evaluating impact of sedimentation system in coastal area of Kecamatan Muara Gembong. Survey of coastal morphology which is needed to obtain the morphology data of <br /> <br /> <br /> <br /> <br /> <br /> <br /> Kecamatan Muara Gembong Coastal Area is divided into two activities, namely sediment sampling and investigation of the coastline. The sample of sediment in Kecamatan Muara Gembong is taken by manual process. Sediment movement is happened when the value of actual shields parameter larger than its critical shields parameter value. In addition, the fall velocity calculation speed is compared to the flow velocity that generates the type of sediment displacement. The current direction <br /> <br /> <br /> <br /> <br /> <br /> <br /> is used to determine the direction of the sediment movement at the fastest flow velocity of high tide and low tide. Coastal classification is used to recognize the basic conditions and potential of the Muara Gembong coastal. The result of sediment movement and sediment displacement calculation shows the that it moves on high tide, meanwhile on low tide only three out of ten sample that indicates movement. All the sediment that moved suspended into water. After the observation occurred, Muara Gembong coastal Located on stable tectonic control, Located off back to the ocean, Has steep slope, Has Very fine sand, Its vegetation dominated by mangrove, Classified into Primary coast (mostly influenced by land process), Its ocean process mostly influenced by wave movement.
format Final Project
author IHSAN IRAQI (NIM : 15108017) ; (Pembimbing :Dr. rer. nat. Wiwin Windupranata, S.T., M.Si. ; , MUSTAFA
spellingShingle IHSAN IRAQI (NIM : 15108017) ; (Pembimbing :Dr. rer. nat. Wiwin Windupranata, S.T., M.Si. ; , MUSTAFA
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author_facet IHSAN IRAQI (NIM : 15108017) ; (Pembimbing :Dr. rer. nat. Wiwin Windupranata, S.T., M.Si. ; , MUSTAFA
author_sort IHSAN IRAQI (NIM : 15108017) ; (Pembimbing :Dr. rer. nat. Wiwin Windupranata, S.T., M.Si. ; , MUSTAFA
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
title_sort #title_alternative#
url https://digilib.itb.ac.id/gdl/view/19027
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