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KAJIAN LAJU TRANSFOR SEDIMEN DI ESTUARIA JENEBERANG, STUDI KASUS PEMUNCULAN TOMBOLO AKTIF DI SELATAN ESTUARIA

Study of Sediment Transport Rate in Jeneberang Estuary, Case Study of Active Tombolo Emergence in the South of Estuary

SENSISTEK:Riset Sains dan Teknologi Kelautan · Vol. ume (2025) · pp. 6–10

DOI
10.62012/sensistek.v8i1.41690
ISSN
2988-2559, 2623-1506
Published
2025-03-29
Publisher
Departemen Teknik Kelautan Fakultas Teknik Universitas Hasanuddin
Language
id

Abstract

English

Sediment movement continuously at the mouth of the river causing erosion and sedimentation and shoreline changes in thearea around the estuary. Introduction behavior sedimentation in the estuary is an important initial step in determining stepefforts to address the problem of sediment deposition and movement. This study aimed to determine the pattern of propagation of waves and currents and their effects on sediment and Tombolo active or cuspate appearance. The methodology used in data collection is to perform direct measurements and the data obtained is processed by software based on finite difference especially for the analysis of wave propagation patterns and sediment movements. The results of the study conducted in the southern estuaries Jeneberang shows that the propagation pattern of waves and currents affect the movement of sediment and the intersection between the two causes that trigger the appearance of sediment deposition on Tombolo active or cuspate.

Bahasa Indonesia

Sediment movement continuously at the mouth of the river causing erosion and sedimentation and shoreline changes in the area around the estuary. Introduction behavior sedimentation in the estuary is an important initial step in determining step efforts to address the problem of sediment deposition and movement. This study aimed to determine the pattern of propagation of waves and currents and their effects on sediment and Tombolo active or cuspate appearance. The methodology used in data collection is to perform direct measurements and the data obtained is processed by software based on finite difference especially for the analysis of wave propagation patterns and sediment movements. The results of the study conducted in the southern estuaries Jeneberang shows that the propagation pattern of waves and currents affect the movement of sediment and the intersection between the two causes that trigger the appearance of sediment deposition on Tombolo active or cuspate.

Keywords

Collaboration network of the authors

25 authors · 69 co-authorship links

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Co-authorOrganisationJoint articles
Sabaruddin RahmanAffiliation unknown5
Chairul PaotonanAffiliation unknown4
Hasdinar UmarAffiliation unknown3
Tri UtariAffiliation unknown1
Didit Fahrudin Muhamad SalehAffiliation unknown1
Taufiqur RachmanAffiliation unknown1
Taufiqurrahman TaufiqurrahmanAffiliation unknown1
Ilham AlkhaerAffiliation unknown1
Ariska AriskaAffiliation unknown1
Novrian Yosua TimangAffiliation unknown1
Nur RachmiAffiliation unknown1
Muhammad AksarAffiliation unknown1
Muhammad Arsyad ThahaAffiliation unknown1
Wasir SamadAffiliation unknown1
Muhammad FikramAffiliation unknown1
Ashury DjamaluddinAffiliation unknown1
Chusnul FebriandiniAffiliation unknown1
Glenndy Lambang Prasetyadi DupuyAffiliation unknown1
Stivan LomoAffiliation unknown1
Axel Nugratama BAffiliation unknown1
Halend PutraAffiliation unknown1
Kelvin Fitrah Prawira DupuyAffiliation unknown1
Ainiyah RahmahAffiliation unknown1

Affiliations come from OpenAlex; journal OAI-PMH metadata carries none. Authors without an OpenAlex ID are matched by name, which can merge or split people.

Metadata source: OAI-PMH (metadata jurnal) https://journal.unhas.ac.id/index.php/SENSISTEK/oai, first harvested 2 Nov 2026, last seen 2 Nov 2026.
Original metadata (oai_dc) 
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	<dc:title xml:lang="en">KAJIAN LAJU TRANSFOR SEDIMEN DI ESTUARIA JENEBERANG, STUDI KASUS PEMUNCULAN TOMBOLO AKTIF DI SELATAN ESTUARIA</dc:title>
	<dc:title xml:lang="id">Study of Sediment Transport Rate in Jeneberang Estuary, Case Study of Active Tombolo Emergence in the South of Estuary</dc:title>
	<dc:creator xml:lang="en">Mustika, Andi Mega</dc:creator>
	<dc:creator xml:lang="en">Baeda, Achmad Yasir</dc:creator>
	<dc:creator xml:lang="id">Mustika, Andi Mega</dc:creator>
	<dc:creator xml:lang="id">Baeda, Achmad Yasir</dc:creator>
	<dc:subject xml:lang="id">tombolo active</dc:subject>
	<dc:subject xml:lang="id">sediment</dc:subject>
	<dc:subject xml:lang="id">waves</dc:subject>
	<dc:subject xml:lang="id">currents</dc:subject>
	<dc:subject xml:lang="en">tombolo active</dc:subject>
	<dc:subject xml:lang="en">sediment</dc:subject>
	<dc:subject xml:lang="en">wave</dc:subject>
	<dc:subject xml:lang="en">current</dc:subject>
	<dc:description xml:lang="en">Sediment movement continuously at the mouth of the river causing erosion and sedimentation and shoreline changes in thearea around the estuary. Introduction behavior sedimentation in the estuary is an important initial step in determining stepefforts to address the problem of sediment deposition and movement. This study aimed to determine the pattern of propagation of waves and currents and their effects on sediment and Tombolo active or cuspate appearance. The methodology used in data collection is to perform direct measurements and the data obtained is processed by software based on finite difference especially for the analysis of wave propagation patterns and sediment movements. The results of the study conducted in the southern estuaries Jeneberang shows that the propagation pattern of waves and currents affect the movement of sediment and the intersection between the two causes that trigger the appearance of sediment deposition on Tombolo active or cuspate.</dc:description>
	<dc:description xml:lang="id">Sediment movement continuously at the mouth of the river causing erosion and sedimentation and shoreline changes in the area around the estuary. Introduction behavior sedimentation in the estuary is an important initial step in determining step efforts to address the problem of sediment deposition and movement. This study aimed to determine the pattern of propagation of waves and currents and their effects on sediment and Tombolo active or cuspate appearance. The methodology used in data collection is to perform direct measurements and the data obtained is processed by software based on finite difference especially for the analysis of wave propagation patterns and sediment movements. The results of the study conducted in the southern estuaries Jeneberang shows that the propagation pattern of waves and currents affect the movement of sediment and the intersection between the two causes that trigger the appearance of sediment deposition on Tombolo active or cuspate.</dc:description>
	<dc:publisher xml:lang="en">Departemen Teknik Kelautan Fakultas Teknik Universitas Hasanuddin</dc:publisher>
	<dc:date>2025-03-29</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
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	<dc:identifier>https://journal.unhas.ac.id/index.php/SENSISTEK/article/view/41690</dc:identifier>
	<dc:identifier>10.62012/sensistek.v8i1.41690</dc:identifier>
	<dc:source xml:lang="en">SENSISTEK:Riset Sains dan Teknologi Kelautan; Volume 8, Number 1, Tahun 2025; 6-10</dc:source>
	<dc:source xml:lang="id">Riset Sains dan Teknologi Kelautan; Volume 8, Nomor 1, Tahun 2025; 6-10</dc:source>
	<dc:source>2988-2559</dc:source>
	<dc:source>2623-1506</dc:source>
	<dc:language>id</dc:language>
	<dc:relation>https://journal.unhas.ac.id/index.php/SENSISTEK/article/view/41690/12658</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2026 SENSISTEK:Riset Sains dan Teknologi Kelautan</dc:rights>
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