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Analysis of Langkolome River Flood, Wambona Village, Muna Regency (Case Study: Langkolome River, Wambona Village, Muna Regency)

Sultra Civil Engineering Journal (SCiEJ) · Vol. 4 No. 1 (2023) · pp. 31–42

DOI
10.54297/sciej.v4i1.460
ISSN
2716-1714
Published
2023-04-29
Publisher
Universitas Sulawesi Tenggara
Language
eng
License
creativecommons.org/licenses/by/4.0

Abstract

Rivers are natural channels on the surface of the earth to drain water, apart from that, of course, interactions between discharges, other factors such as human activities along rivers give different characteristics of river formation. the largest portion comes from land clearing activities around the Langkolome river body located in Wambona Village, South Wakorumba District, Muna Regency. Based on the results of the calculation of the flood discharge of the Langkolome River in Wambona Village from 10 years of rainfall data, namely Q10 = 128,773 m3/sec, Q25 = 244,067 m3/sec. The capacity of the Langkolome river which has an impact on flooding Q = 158,063 m3/s. The maximum rainfall is greater than the capacity of the river, so this causes flooding in the Langkolome River, Wambona Village, Muna Regency

Collaboration network of the authors

40 authors · 124 co-authorship links · showing the 40 most connected

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  • Universitas Sulawesi Tenggara
  • Affiliation unknown
  • Different organisations
  • Same organisation
  • Affiliation unknown
  • Thicker line = more joint articles · bigger circle = more articles
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Co-authorOrganisationJoint articles
Vickky Anggara IlhamUniversitas Sulawesi Tenggara19
Hujiyanto HujiyantoUniversitas Sulawesi Tenggara15
Sulaiman SulaimanUniversitas Sulawesi Tenggara11
Andi MakkawaruUniversitas Sulawesi Tenggara10
Sitti HawaUniversitas Sulawesi Tenggara9
Hakiman HakimanUniversitas Sulawesi Tenggara6
Hado HadoUniversitas Sulawesi Tenggara5
Haryono HaryonoUniversitas Sulawesi Tenggara5
La Ode Musa RachmatUniversitas Sulawesi Tenggara5
Muhammad MuhsarUniversitas Sulawesi Tenggara5
Andi Makkawaru Isazarny JassinUniversitas Sulawesi Tenggara4
Fikri Aris MunandarUniversitas Sulawesi Tenggara4
Haryono HaryonoUniversitas Sulawesi Tenggara4
Sunaryo SunaryoUniversitas Sulawesi Tenggara3
La Ode Muhamad MagribiUniversitas Sulawesi Tenggara3
Hayadi HayadiUniversitas Sulawesi Tenggara2
Syamsuddin SyamsuddinUniversitas Sulawesi Tenggara2
Lisman LismanUniversitas Sulawesi Tenggara2
La Ode Abdul MananUniversitas Sulawesi Tenggara2
Erni DanggiUniversitas Sulawesi Tenggara2
Komang Agus SaputraUniversitas Sulawesi Tenggara2
Andi Kukuh SetiawanUniversitas Sulawesi Tenggara2
Sulaiman SulaimanUniversitas Sulawesi Tenggara2
Syamsuddin SyamsuddinUniversitas Sulawesi Tenggara2
La Ode BariunUniversitas Sulawesi Tenggara1
Humairah MuljabarUniversitas Sulawesi Tenggara1
La Ode Muhammad Isman Hardiansyah BariunAffiliation unknown1
Joko Tri BrataUniversitas Sulawesi Tenggara1
Arsalim ArsalimUniversitas Sulawesi Tenggara1
Aswad AswadUniversitas Sulawesi Tenggara1
Syamsuddin SyamsuddinUniversitas Sulawesi Tenggara1
Hado HadoUniversitas Sulawesi Tenggara1
Catrin SudardjatUniversitas Sulawesi Tenggara1
Syamsuddin SyamsuddinUniversitas Sulawesi Tenggara1
Sri Jayani SafitriUniversitas Sulawesi Tenggara1
Nurmaida NurmaidaUniversitas Sulawesi Tenggara1

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://jurnal-unsultra.ac.id/index.php/scej/oai, first harvested 30 Okt 2026, last seen 30 Okt 2026.
Original metadata (oai_dc) 
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	<dc:title xml:lang="en-US">Analysis of Langkolome River Flood, Wambona Village, Muna Regency (Case Study: Langkolome River, Wambona Village, Muna Regency)</dc:title>
	<dc:creator>Hasrudin, La Ode</dc:creator>
	<dc:creator>Lakawa, Irwan</dc:creator>
	<dc:creator>Sudardjat, Catrin</dc:creator>
	<dc:creator>Sufrianto, Sufrianto</dc:creator>
	<dc:description xml:lang="en-US">Rivers are natural channels on the surface of the earth to drain water, apart from that, of course, interactions between discharges, other factors such as human activities along rivers give different characteristics of river formation. the largest portion comes from land clearing activities around the Langkolome river body located in Wambona Village, South Wakorumba District, Muna Regency. Based on the results of the calculation of the flood discharge of the Langkolome River in Wambona Village from 10 years of rainfall data, namely Q10 = 128,773 m3/sec, Q25 = 244,067 m3/sec. The capacity of the Langkolome river which has an impact on flooding Q = 158,063 m3/s. The maximum rainfall is greater than the capacity of the river, so this causes flooding in the Langkolome River, Wambona Village, Muna Regency</dc:description>
	<dc:publisher xml:lang="en-US">Universitas Sulawesi Tenggara</dc:publisher>
	<dc:date>2023-04-29</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://jurnal-unsultra.ac.id/index.php/scej/article/view/460</dc:identifier>
	<dc:identifier>10.54297/sciej.v4i1.460</dc:identifier>
	<dc:source xml:lang="en-US">Sultra Civil Engineering Journal (SCiEJ); Vol 4 No 1 (2023): Sultra Civil Engineering Journal (SCiEJ); 31-42</dc:source>
	<dc:source>2716-1714</dc:source>
	<dc:source>10.54297/sciej.v4i1</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://jurnal-unsultra.ac.id/index.php/scej/article/view/460/279</dc:relation>
	<dc:relation>10.54297/sciej.v4i1.460.g279</dc:relation>
	<dc:rights xml:lang="en-US">Copyright (c) 2023 La Ode Hasrudin, Irwan Lakawa, Catrin Sudardjat, Sufrianto Sufrianto</dc:rights>
	<dc:rights xml:lang="en-US">http://creativecommons.org/licenses/by/4.0</dc:rights>
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