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Assessing karst landscape degradation based on the void development of karst aquifers in Gunungsewu, Indonesia

Journal of Degraded and Mining Lands Management · Vol. 11 No. 3 (2024) · hlm. 5707–5715

DOI
10.15243/jdmlm.2024.113.5707
ISSN
2502-2458, 2339-076X
Terbit
2024-04-01
Penerbit
Brawijaya University
Bahasa
eng
Lisensi
creativecommons.org/licenses/by-nc/4.0

Abstrak

Compared to other landforms, karst areas are among those emerging from the dissolution process that have a higher risk of land degradation. The likelihood of karst landforms being harmed is increased by urbanization and other human activities like extensive agriculture. Subsurface streams' water quality gets worse when surface pollutants infiltrate through developed karst features like sinkholes and karst ponors. There is a greater risk of land degradation as more karst features, in this case void size, develop. The purpose of this research is to assess how void development, or the degree of karstification, relates to the potential for karst spring pollution in the event that land degradation occurs on the surface of the Karst Drainage System (KDS). This research was conducted at the KDS of Beton and Gremeng Spring in the Gunungsewu karst area, Indonesia. In addition, this study also provides recommendations related to environmental management on the basis of the level of development of voids at both sites. The degree of karstification represents the phase at which a hydrogeological system has been developing, and this information was later considered in formulating strategies for protecting karst groundwater from contamination. The results show that Beton and Gremeng had a complex discharge regime with degrees of karstification at 8 and 5.5, respectively. Based on flood hydrograph components, it was further confirmed that both areas were in the mature phase. The higher the degree of karstification, the higher the vulnerability to pollution.

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  • Universitas Gadjah Mada
  • Universitas Syiah Kuala
  • Politeknik Pertanian Negeri Kupang
  • National Research and Innovation Agency
  • Tanjungpura University
  • National Central University
  • Afiliasi tidak diketahui
  • Organisasi berbeda
  • Organisasi sama
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Rekan penulisOrganisasiArtikel bersama
Indra Agus RiyantoUniversitas Gadjah Mada12
Fajri RamadhanUniversitas Gadjah Mada6
M WidyastutiUniversitas Gadjah Mada5
Margaretha WidyastutiUniversitas Gadjah Mada4
Husna DiahUniversitas Syiah Kuala4
Raden Ludhang Pradipta RizkiUniversitas Gadjah Mada3
Noor Alia SusiantiUniversitas Gadjah Mada3
Dzakwan Taufiq Nur MuhammadUniversitas Gadjah Mada3
Naufal Fattah TastianUniversitas Gadjah Mada3
Bambang Hendro SunarmintoUniversitas Gadjah Mada2
Sunarno SunarnoUniversitas Gadjah Mada2
Thomas Oka PratamaUniversitas Gadjah Mada2
Agus Budhie WijatnaUniversitas Gadjah Mada2
Setyawan PurnamaUniversitas Gadjah Mada2
Langgeng Wahyu SantosaUniversitas Gadjah Mada2
Ratri Abdatush SholihahNational Central University2
Victor Kusuma RamadanUniversitas Gadjah Mada2
Awanda Sistia RiskyUniversitas Gadjah Mada2
Alfred Umbu Kuala NgajiPoliteknik Pertanian Negeri Kupang1
Muhammad BaiquniUniversitas Gadjah Mada1
Hatma SuryatmojoUniversitas Gadjah Mada1
Setiadi SetiadiUniversitas Gadjah Mada1
Eka SulistiyowatiUniversitas Gadjah Mada1
Arif AnshoriNational Research and Innovation Agency1
Muh Aris MarfaiUniversitas Gadjah Mada1
Dini Feti AnggrainiUniversitas Gadjah Mada1
Maryadi Budi WiyonoUniversitas Gadjah Mada1
M MisqiUniversitas Gadjah Mada1
J. Susetyo Edy YAfiliasi tidak diketahui1
Imam FauziAfiliasi tidak diketahui1
Susetyo DidikAfiliasi tidak diketahui1
Wahyu Broto RAfiliasi tidak diketahui1
Rossie Wiedya NusantaraTanjungpura University1
Sudarmadji SudarmadjiUniversitas Gadjah Mada1
Tjut S. DjohanUniversitas Gadjah Mada1
Miranti ArianiUniversitas Gadjah Mada1

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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) 
<oai_dc:dc xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/  http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
	<dc:title xml:lang="en-US">Assessing karst landscape degradation based on the void development of karst aquifers in Gunungsewu, Indonesia</dc:title>
	<dc:creator>Naufal, Muhammad</dc:creator>
	<dc:creator>Adji, Tjahyo Nugroho</dc:creator>
	<dc:creator>Haryono, Eko</dc:creator>
	<dc:creator>Cahyadi, Ahmad</dc:creator>
	<dc:subject xml:lang="en-US">karst aquifer</dc:subject>
	<dc:subject xml:lang="en-US">karst drainage system</dc:subject>
	<dc:subject xml:lang="en-US">karstification degree</dc:subject>
	<dc:subject xml:lang="en-US">land degradation</dc:subject>
	<dc:subject xml:lang="en-US">void development</dc:subject>
	<dc:description xml:lang="en-US">Compared to other landforms, karst areas are among those emerging from the dissolution process that have a higher risk of land degradation. The likelihood of karst landforms being harmed is increased by urbanization and other human activities like extensive agriculture. Subsurface streams' water quality gets worse when surface pollutants infiltrate through developed karst features like sinkholes and karst ponors. There is a greater risk of land degradation as more karst features, in this case void size, develop. The purpose of this research is to assess how void development, or the degree of karstification, relates to the potential for karst spring pollution in the event that land degradation occurs on the surface of the Karst Drainage System (KDS). This research was conducted at the KDS of Beton and Gremeng Spring in the Gunungsewu karst area, Indonesia. In addition, this study also provides recommendations related to environmental management on the basis of the level of development of voids at both sites. The degree of karstification represents the phase at which a hydrogeological system has been developing, and this information was later considered in formulating strategies for protecting karst groundwater from contamination. The results show that Beton and Gremeng had a complex discharge regime with degrees of karstification at 8 and 5.5, respectively. Based on flood hydrograph components, it was further confirmed that both areas were in the mature phase. The higher the degree of karstification, the higher the vulnerability to pollution.</dc:description>
	<dc:publisher xml:lang="en-US">Brawijaya University</dc:publisher>
	<dc:date>2024-04-01</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://jdmlm.ub.ac.id/index.php/jdmlm/article/view/16456</dc:identifier>
	<dc:identifier>10.15243/jdmlm.2024.113.5707</dc:identifier>
	<dc:source xml:lang="en-US">Journal of Degraded and Mining Lands Management; Vol. 11 No. 3 (2024); 5707-5715</dc:source>
	<dc:source>2502-2458</dc:source>
	<dc:source>2339-076X</dc:source>
	<dc:source>10.15243/jdmlm.2024.113</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://jdmlm.ub.ac.id/index.php/jdmlm/article/view/16456/993</dc:relation>
	<dc:rights xml:lang="en-US">Copyright (c) 2024 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>
</oai_dc:dc>