Korelasi Antara Debit Aliran dan Sedimen Melayang (Suspended Load) di Sungai Data’ Kabupaten Pinrang

Ahmad, Zulfikar Ali; Nathan, Muh.; Lias, Syamsul Arifin

doi:10.20956/ecosolum.v8i1.6894

Jurnal

Korelasi Antara Debit Aliran dan Sedimen Melayang (Suspended Load) di Sungai Data’ Kabupaten Pinrang

Jurnal Ecosolum · Vol. 8 No. 1 (2019) · pp. 21–26

DOI: 10.20956/ecosolum.v8i1.6894
ISSN: 2654-430X, 2252-7923
Published: 2019-07-11
Publisher: Universitas Hasanuddin
Language: en

Abstract

The hydrological process that occurs in a watershed is related to erosion process, sediment transport and downstream deposition. Land use changes and watershed management practices will also affect erosion and sedimentation. The purpose of this study was to determine the magnitude of flowrate, suspended load concentration (suspended load), and floating sediment discharge and correlation of floated sediment discharge and flowrate at the Data’ River. Measuring river characteristics is done by measuring river water flow and river slope. Sediment collection floated with EWI (equal with incerentment) method. Laboratory analysis was carried out by calculating the amount of flow discharge, sediment concentration, and sediment discharge. The results showed the lowest amount of flow discharge occurred on 17/12/2016 with a value of 0.271 m3/s with a floating sediment concentration of 17.167 mg / L, and the sediment discharge floated at 0.402 tons/day. The correlation between flow discharge and floating sediment discharge using a sccatter diagram shows that the determination value R2 is 0.9754 with the equation y = 0.1x + 0.4355.

Keywords

Collaboration network of the authors

18 authors · 27 co-authorship links

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Co-author	Organisation	Joint articles
Asmita Ahmad	Affiliation unknown	2
Muh. Jayadi	Affiliation unknown	2
Nur Isra	Affiliation unknown	1
Muhammad Fitrah Khairul Anami	Affiliation unknown	1
Risma Neswati	Affiliation unknown	1
Irfandi Felix	Affiliation unknown	1
. Syahrul	Affiliation unknown	1
Naurha Rhamadani	Affiliation unknown	1
Sartika Laban	Affiliation unknown	1
Muhammad Asyraf	Affiliation unknown	1
Sri Sulva Nensi	Affiliation unknown	1
Hazairin Zubair	Affiliation unknown	1
Engki Fatiawan	Affiliation unknown	1
Dea Aurelia Pantilen	Affiliation unknown	1
Muhammad Rifki Munir	Affiliation unknown	1

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/ecosolum/oai, first harvested 2 Nov 2026, last seen 2 Nov 2026.

Original metadata (oai_dc)

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	<dc:title xml:lang="en">Korelasi Antara Debit Aliran dan Sedimen Melayang (Suspended Load) di Sungai Data’ Kabupaten Pinrang</dc:title>
	<dc:creator xml:lang="en">Ahmad, Zulfikar Ali</dc:creator>
	<dc:creator xml:lang="en">Nathan, Muh.</dc:creator>
	<dc:creator xml:lang="en">Lias, Syamsul Arifin</dc:creator>
	<dc:subject xml:lang="en">floated sediment</dc:subject>
	<dc:subject xml:lang="en">flow discharge</dc:subject>
	<dc:subject xml:lang="en">Data’ River</dc:subject>
	<dc:description xml:lang="en">The hydrological process that occurs in a watershed is related to erosion process, sediment transport and downstream deposition. Land use changes and watershed management practices will also affect erosion and sedimentation. The purpose of this study was to determine the magnitude of flowrate, suspended load concentration (suspended load), and floating sediment discharge and correlation of floated sediment discharge and flowrate at the Data’ River. Measuring river characteristics is done by measuring river water flow and river slope. Sediment collection floated with EWI (equal with incerentment) method. Laboratory analysis was carried out by calculating the amount of flow discharge, sediment concentration, and sediment discharge. The results showed the lowest amount of flow discharge occurred on 17/12/2016 with a value of 0.271 m3/s with a floating sediment concentration of 17.167 mg / L, and the sediment discharge floated at 0.402 tons/day. The correlation between flow discharge and floating sediment discharge using a sccatter diagram shows that the determination value R2 is 0.9754 with the equation y = 0.1x + 0.4355.</dc:description>
	<dc:publisher xml:lang="en">Universitas Hasanuddin</dc:publisher>
	<dc:date>2019-07-11</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:type xml:lang="en">Peer-reviewed Article</dc:type>
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	<dc:identifier>https://journal.unhas.ac.id/index.php/ecosolum/article/view/6894</dc:identifier>
	<dc:identifier>10.20956/ecosolum.v8i1.6894</dc:identifier>
	<dc:source xml:lang="en">Jurnal Ecosolum; Vol. 8 No. 1 (2019): JUNI; 21-26</dc:source>
	<dc:source>2654-430X</dc:source>
	<dc:source>2252-7923</dc:source>
	<dc:source>10.20956/ecosolum.v8i1</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://journal.unhas.ac.id/index.php/ecosolum/article/view/6894/4856</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2019 Jurnal Ecosolum</dc:rights>
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