Surface Run-Off and Soil Erosion in 11 Year Old Acacia and Sengon Stands: Surface Run-Off and Soil Erosion in Acacia and Sengon Stands

Difa, Geva Alfinda; Karyati; Sarminah, Sri; Karmini, Karmini

doi:10.24259/perennial.v20i2.36538

Jurnal

Surface Run-Off and Soil Erosion in 11 Year Old Acacia and Sengon Stands: Surface Run-Off and Soil Erosion in Acacia and Sengon Stands

Limpasan Permukaan dan Erosi Tanah pada Tegakan Akasia dan Sengon Umur 11 Tahun: Limpasan Permukaan dan Erosi Tanah pada Tegakan Akasia dan Sengon

PERENNIAL · Vol. 20 No. 2 (2024) · hlm. 56–66

DOI: 10.24259/perennial.v20i2.36538
ISSN: 2685-6859, 1412-7784
Terbit: 2024-10-31
Penerbit: Forestry Faculty of Hasanuddin University
Bahasa: en

Abstrak

Inggris

Indonesia is a country with geographical conditions located in tropical rain climates, causing variations in rainfall levels. High and varied rainfall can lead to surface run-off and soil erosion. This study aims to determine (1) the rate of surface run-off and soil mass erosion in acacia (Acacia mangium/A. mangium) stand, sengon (Falcataria moluccana/F. moluccana) stand, and open land; (2) the status of erosion hazard index, erosion hazard class, and erosion hazard levels occurring in A. mangium stand, sengon stand, and open land; (3) the relationship between rainfall and surface run-off and soil mass erosion. Erosion Measurement Plots (EMP) measuring 4 m × 10 m were established in the study site, consisting of three plots namely EMP A. mangium, EMP sengon, and EMP open land with steep slopes (25-45%). The total measured surface runoff (SR) during the study period at EMP A. mangium was 335.37 m³/ha/year, EMP sengon was 950.77 m³/ha/year, and EMP open land was 2,646.95 m³/ha/year. Meanwhile, Eroded Soil Mass (ESM) during the study period at EMP A. mangium was 0.85 tons/ha/year, EMP sengon was 2.39 tons/ha/year, and EMP open land was 195.45 tons/ha/year. The Erosion Hazard Index (EHI) value at EMP A. mangium and EMP sengon was classified as low, while at EMP open land was classified as very high. The Erosion Hazard Class (EHC) in EMP A. mangium and EMP sengon belongs to EHC I (very low), while in EMP open land belongs to EHC IV (high). Erosion Hazard Level (EHL) at EMP A. mangium and EMP sengon was included in the currently class, while at EMP open land was included in the very heavy class. The information about surface runoff and soil erosion on different land covers can be used as considerations in soil management, especially for post-mining lands.

Bahasa Indonesia

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13 penulis · 29 tautan kepenulisan bersama · 11 lintas organisasi

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Mulawarman University
Yogyakarta State University
Jilin University

Organisasi berbeda
Organisasi sama
Afiliasi tidak diketahui
Garis lebih tebal = lebih banyak artikel bersama · lingkaran lebih besar = lebih banyak artikel

Tampilkan sebagai tabel

Rekan penulis	Organisasi	Artikel bersama
Karyati Karyati	Mulawarman University	2
Sahrul Gunawan	Mulawarman University	1
KARYATI KARYATI	Mulawarman University	1
Karmini	Mulawarman University	1
Kusno Yuli Widiati	Mulawarman University	1
Muna Karhani	Yogyakarta State University	1
Rita Eka Izzaty	Yogyakarta State University	1
Herwin Herwin	Yogyakarta State University	1
Rendi Rendi	Jilin University	1

Afiliasi berasal dari OpenAlex; metadata OAI-PMH jurnal tidak memuatnya. Penulis tanpa ID OpenAlex dicocokkan berdasarkan nama, sehingga dua orang bisa tergabung atau satu orang bisa terpisah.

Sumber metadata: OAI-PMH (metadata jurnal) https://journal.unhas.ac.id/index.php/perennial/oai, pertama di-harvest 5 Nov 2026, terakhir terlihat 8 Nov 2026.

Metadata asli (oai_dc)

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	<dc:title xml:lang="en">Surface Run-Off and Soil Erosion in 11 Year Old Acacia and Sengon Stands: Surface Run-Off and Soil Erosion in Acacia and Sengon Stands</dc:title>
	<dc:title xml:lang="id">Limpasan Permukaan dan Erosi Tanah pada Tegakan Akasia dan Sengon Umur 11 Tahun: Limpasan Permukaan dan Erosi Tanah pada Tegakan Akasia dan Sengon</dc:title>
	<dc:creator xml:lang="en">Difa, Geva Alfinda</dc:creator>
	<dc:creator xml:lang="en">Karyati</dc:creator>
	<dc:creator xml:lang="en">Sarminah, Sri</dc:creator>
	<dc:creator xml:lang="en">Karmini, Karmini</dc:creator>
	<dc:subject xml:lang="id">Acacia mangium</dc:subject>
	<dc:subject xml:lang="id">Falcataria moluccana</dc:subject>
	<dc:subject xml:lang="id">Lahan Terbuka</dc:subject>
	<dc:subject xml:lang="id">Erosi Massa Tanah</dc:subject>
	<dc:subject xml:lang="id">Limpasan Permukaan</dc:subject>
	<dc:subject xml:lang="en">Acacia mangium</dc:subject>
	<dc:subject xml:lang="en">Open Land</dc:subject>
	<dc:subject xml:lang="en">Soil Mass Erosion</dc:subject>
	<dc:subject xml:lang="en">Surface Run-off</dc:subject>
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Indonesia is a country with geographical conditions located in tropical rain climates, causing variations in rainfall levels. High and varied rainfall can lead to surface run-off and soil erosion. This study aims to determine (1) the rate of surface run-off and soil mass erosion in acacia (Acacia mangium/A. mangium) stand, sengon (Falcataria moluccana/F. moluccana) stand, and open land; (2) the status of erosion hazard index, erosion hazard class, and erosion hazard levels occurring in A. mangium stand, sengon stand, and open land; (3) the relationship between rainfall and surface run-off and soil mass erosion. Erosion Measurement Plots (EMP) measuring 4 m × 10 m were established in the study site, consisting of three plots namely EMP A. mangium, EMP sengon, and EMP open land with steep slopes (25-45%). The total measured surface runoff (SR) during the study period at EMP A. mangium was 335.37 m³/ha/year, EMP sengon was 950.77 m³/ha/year, and EMP open land was 2,646.95 m³/ha/year. Meanwhile, Eroded Soil Mass (ESM) during the study period at EMP A. mangium was 0.85 tons/ha/year, EMP sengon was 2.39 tons/ha/year, and EMP open land was 195.45 tons/ha/year. The Erosion Hazard Index (EHI) value at EMP A. mangium and EMP sengon was classified as low, while at EMP open land was classified as very high. The Erosion Hazard Class (EHC) in EMP A. mangium and EMP sengon belongs to EHC I (very low), while in EMP open land belongs to EHC IV (high). Erosion Hazard Level (EHL) at EMP A. mangium and EMP sengon was included in the currently class, while at EMP open land was included in the very heavy class. The information about surface runoff and soil erosion on different land covers can be used as considerations in soil management, especially for post-mining lands.



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Indonesia is a country with geographical conditions located in tropical rain climates, causing variations in rainfall levels. High and varied rainfall can lead to surface run-off and soil erosion. This study aims to determine (1) the rate of surface run-off and soil mass erosion in acacia (Acacia mangium/A. mangium) stand, sengon (Falcataria moluccana/F. moluccana) stand, and open land; (2) the status of erosion hazard index, erosion hazard class, and erosion hazard levels occurring in A. mangium stand, sengon stand, and open land; (3) the relationship between rainfall and surface run-off and soil mass erosion. Erosion Measurement Plots (EMP) measuring 4 m × 10 m were established in the study site, consisting of three plots namely EMP A. mangium, EMP sengon, and EMP open land with steep slopes (25-45%). The total measured surface runoff (SR) during the study period at EMP A. mangium was 335.37 m³/ha/year, EMP sengon was 950.77 m³/ha/year, and EMP open land was 2,646.95 m³/ha/year. Meanwhile, Eroded Soil Mass (ESM) during the study period at EMP A. mangium was 0.85 tons/ha/year, EMP sengon was 2.39 tons/ha/year, and EMP open land was 195.45 tons/ha/year. The Erosion Hazard Index (EHI) value at EMP A. mangium and EMP sengon was classified as low, while at EMP open land was classified as very high. The Erosion Hazard Class (EHC) in EMP A. mangium and EMP sengon belongs to EHC I (very low), while in EMP open land belongs to EHC IV (high). Erosion Hazard Level (EHL) at EMP A. mangium and EMP sengon was included in the currently class, while at EMP open land was included in the very heavy class. The information about surface runoff and soil erosion on different land covers can be used as considerations in soil management, especially for post-mining lands.



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	<dc:publisher xml:lang="en">Forestry Faculty of Hasanuddin University</dc:publisher>
	<dc:date>2024-10-31</dc:date>
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	<dc:type xml:lang="en">Peer-reviewed Article</dc:type>
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	<dc:identifier>https://journal.unhas.ac.id/index.php/perennial/article/view/36538</dc:identifier>
	<dc:identifier>10.24259/perennial.v20i2.36538</dc:identifier>
	<dc:source xml:lang="en">PERENNIAL; Vol. 20 No. 2 (2024): Vol. 20 No. 2, October 2024; 56-66</dc:source>
	<dc:source xml:lang="id">PERENNIAL; Vol 20 No 2 (2024): Vol. 20 No. 2, Oktober 2024; 56-66</dc:source>
	<dc:source>2685-6859</dc:source>
	<dc:source>1412-7784</dc:source>
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