Landslide frequency and its relationship with urban development in landform above groundwater basin area of Bogor, Indonesia

Fata, Yulia Amirul; Hendrayanto, Hendrayanto; Febrianti, Nur

doi:10.15243/jdmlm.2022.093.3561

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Landslide frequency and its relationship with urban development in landform above groundwater basin area of Bogor, Indonesia

Journal of Degraded and Mining Lands Management · Vol. 9 No. 3 (2022) · hlm. 3561–3572

DOI: 10.15243/jdmlm.2022.093.3561
ISSN: 2502-2458, 2339-076X
Terbit: 2022-04-01
Penerbit: Brawijaya University
Bahasa: eng
Lisensi: creativecommons.org/licenses/by-nc/4.0

Abstrak

The presence of groundwater in the groundwater basin increases the potential of rainwater seeping into the soil and reaching the groundwater system. As a result, the soil takes longer to get saturation and maintain its stability. The groundwater basin stability is also influenced by the layer's lithological, soil, and morphological properties above the groundwater system and human activities on the land. The purpose of this study was to characterize the groundwater basins, non-groundwater basins, and landslides that happened in those locations in the tropical region of Bogor, Indonesia. The characteristics of landslide events, including lithological, groundwater table, soil, slope, and land use in each groundwater basin zone, were evaluated using quantitative descriptive analysis. The result showed 686 landslides from 2015 to 2019 that mainly occurred in the discharge zone, characterized by slope classes of >45%, soil types of Technosol (Inceptisols), Quaternary lithology periods, and settlement land use. The landslide type in the groundwater basin is dominated by surface landslides, while the landslides in the non-groundwater basin are mostly shallow landslide types.

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Erizal Erizal	Afiliasi tidak diketahui	4
Budi Kuncahyo	IPB University	2
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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">Landslide frequency and its relationship with urban development in landform above groundwater basin area of Bogor, Indonesia</dc:title>
	<dc:creator>Fata, Yulia Amirul</dc:creator>
	<dc:creator>Hendrayanto, Hendrayanto</dc:creator>
	<dc:creator>Febrianti, Nur</dc:creator>
	<dc:subject xml:lang="en-US">discharge</dc:subject>
	<dc:subject xml:lang="en-US">groundwater basin</dc:subject>
	<dc:subject xml:lang="en-US">landslide</dc:subject>
	<dc:subject xml:lang="en-US">non-groundwater basin</dc:subject>
	<dc:subject xml:lang="en-US">recharge</dc:subject>
	<dc:subject xml:lang="en-US">urban development</dc:subject>
	<dc:description xml:lang="en-US">The presence of groundwater in the groundwater basin increases the potential of rainwater seeping into the soil and reaching the groundwater system. As a result, the soil takes longer to get saturation and maintain its stability. The groundwater basin stability is also influenced by the layer's lithological, soil, and morphological properties above the groundwater system and human activities on the land. The purpose of this study was to characterize the groundwater basins, non-groundwater basins, and landslides that happened in those locations in the tropical region of Bogor, Indonesia. The characteristics of landslide events, including lithological, groundwater table, soil, slope, and land use in each groundwater basin zone, were evaluated using quantitative descriptive analysis. The result showed 686 landslides from 2015 to 2019 that mainly occurred in the discharge zone, characterized by slope classes of &amp;gt;45%, soil types of Technosol (Inceptisols), Quaternary lithology periods, and settlement land use. The landslide type in the groundwater basin is dominated by surface landslides, while the landslides in the non-groundwater basin are mostly shallow landslide types.</dc:description>
	<dc:publisher xml:lang="en-US">Brawijaya University</dc:publisher>
	<dc:date>2022-04-01</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
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	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://jdmlm.ub.ac.id/index.php/jdmlm/article/view/1168</dc:identifier>
	<dc:identifier>10.15243/jdmlm.2022.093.3561</dc:identifier>
	<dc:source xml:lang="en-US">Journal of Degraded and Mining Lands Management; Vol. 9 No. 3 (2022); 3561-3572</dc:source>
	<dc:source>2502-2458</dc:source>
	<dc:source>2339-076X</dc:source>
	<dc:source>10.15243/jdmlm.2022.093</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://jdmlm.ub.ac.id/index.php/jdmlm/article/view/1168/pdf</dc:relation>
	<dc:rights xml:lang="en-US">Copyright (c) 2022 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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