Peak flood volume and its suspended sediment at various rainfall in Kedungbulus catchment in Gombong, Central Java, Indonesia

Basuki, Tyas Mutiara; Pramono, Irfan Budi

doi:10.15243/jdmlm.2021.091.3211

Akses terbuka Jurnal SINTA 1

Peak flood volume and its suspended sediment at various rainfall in Kedungbulus catchment in Gombong, Central Java, Indonesia

Journal of Degraded and Mining Lands Management · Vol. 9 No. 1 (2021) · hlm. 3211–3217

DOI: 10.15243/jdmlm.2021.091.3211
ISSN: 2502-2458, 2339-076X
Terbit: 2021-10-01
Penerbit: Brawijaya University
Bahasa: eng
Lisensi: creativecommons.org/licenses/by-nc/4.0

Abstrak

Flood is a natural disaster that frequently happens and causes many material and immaterial losses. During flooding, the suspended sediment is carried along by the streamflow. The amount of sediment transported varies and depends on natural and anthropogenic factors. Limited studies have been conducted regarding the relationship between peak flood volume and its sediment content. Therefore, a study with the purpose to understand the relationship of rainfall characteristics, peak flood volume, and suspended sediment was undertaken in Kedungbulus Catchment in Gombong, Central Java, Indonesia. The size of Kedungbulus catchment is 37.8 km2. To collect the required data, an automatic stream water level recorder was installed in the outlet of the catchment. In addition, an automatic and two conventional rain gauges were set up inside the catchment. Hydrograph and statistical analysis were conducted on 2016-2017 data. The results showed that during the study period, the highest peak flood volume occurred on October 8, 2016. The flood duration was 490 minutes, with the time to peak was 135 minutes. At the highest peak flood volume, the stream water was 5,091,221 m3, and the suspended sediment was around 2,394 tons. Rainfall depth significantly affects the peak flood volume and its suspended sediment. The rainfall intensity and Antecedent Soil Moisture Content (ASMC) weakly correlate with peak flood volume and its suspended sediment content.

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12 penulis · 37 tautan kepenulisan bersama · 14 lintas organisasi

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Watershed
National Research and Innovation Agency
Indonesian National Institute of Aeronautics and Space

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Tampilkan sebagai tabel

Rekan penulis	Organisasi	Artikel bersama
Wahyu Wisnu Wijaya	Watershed	7
Diah Auliyani	Watershed	5
Esa Bagus Nugrahanto	Watershed	4
Rahardyan Nugroho Adi	Watershed	3
Galdita Aruba Chulafak	Indonesian National Institute of Aeronautics and Space	2
Fajar Setiawan	National Research and Innovation Agency	2
Budi Heru Santosa	National Research and Innovation Agency	2
Aldiano Rahmadya	National Research and Innovation Agency	2
Firda Maftukhakh Hilmya Nada	National Research and Innovation Agency	2
Nining Wahyuningrum	Watershed	1

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Sumber metadata: OAI-PMH (metadata jurnal) http://jdmlm.ub.ac.id/index.php/jdmlm/oai, pertama di-harvest 9 Nov 2026, terakhir terlihat 9 Nov 2026.

Metadata asli (oai_dc)

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	<dc:title xml:lang="en-US">Peak flood volume and its suspended sediment at various rainfall in Kedungbulus catchment in Gombong, Central Java, Indonesia</dc:title>
	<dc:creator>Basuki, Tyas Mutiara</dc:creator>
	<dc:creator>Pramono, Irfan Budi</dc:creator>
	<dc:subject xml:lang="en-US">flood volume</dc:subject>
	<dc:subject xml:lang="en-US">rainfall properties</dc:subject>
	<dc:subject xml:lang="en-US">suspended sediment</dc:subject>
	<dc:description xml:lang="en-US">Flood is a natural disaster that frequently happens and causes many material and immaterial losses. During flooding, the suspended sediment is carried along by the streamflow. The amount of sediment transported varies and depends on natural and anthropogenic factors. Limited studies have been conducted regarding the relationship between peak flood volume and its sediment content. Therefore, a study with the purpose to understand the relationship of rainfall characteristics, peak flood volume, and suspended sediment was undertaken in Kedungbulus Catchment in Gombong, Central Java, Indonesia. The size of Kedungbulus catchment is 37.8 km2. To collect the required data, an automatic stream water level recorder was installed in the outlet of the catchment. In addition, an automatic and two conventional rain gauges were set up inside the catchment. Hydrograph and statistical analysis were conducted on 2016-2017 data. The results showed that during the study period, the highest peak flood volume occurred on October 8, 2016. The flood duration was 490 minutes, with the time to peak was 135 minutes. At the highest peak flood volume, the stream water was 5,091,221 m3, and the suspended sediment was around 2,394 tons. Rainfall depth significantly affects the peak flood volume and its suspended sediment. The rainfall intensity and Antecedent Soil Moisture Content (ASMC) weakly correlate with peak flood volume and its suspended sediment content.</dc:description>
	<dc:publisher xml:lang="en-US">Brawijaya University</dc:publisher>
	<dc:date>2021-10-01</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
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	<dc:identifier>https://jdmlm.ub.ac.id/index.php/jdmlm/article/view/1007</dc:identifier>
	<dc:identifier>10.15243/jdmlm.2021.091.3211</dc:identifier>
	<dc:source xml:lang="en-US">Journal of Degraded and Mining Lands Management; Vol. 9 No. 1 (2021); 3211-3217</dc:source>
	<dc:source>2502-2458</dc:source>
	<dc:source>2339-076X</dc:source>
	<dc:source>10.15243/jdmlm.2021.091</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://jdmlm.ub.ac.id/index.php/jdmlm/article/view/1007/pdf</dc:relation>
	<dc:rights xml:lang="en-US">Copyright (c) 2021 Journal of Degraded and Mining Lands Management</dc:rights>
	<dc:rights xml:lang="en-US">https://creativecommons.org/licenses/by-nc/4.0</dc:rights>
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