Impact of logging and forest fires on soil erosion in tropical humid forest in Kalimantan

Logging and/or forest fires cause a direct impact of reducing vegetation cover, and in many cases create a pre-condition for the increase of soil erosion rates during high rainfall. Such an increase in soil erosion rate may be higher than the normal threshold rate from a sustainable forest land prod...

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Autor principal: Sudarmadji, T.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: Center for International Forestry Research 2001
Materias:
Acceso en línea:https://hdl.handle.net/10568/18412
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author Sudarmadji, T.
author_browse Sudarmadji, T.
author_facet Sudarmadji, T.
author_sort Sudarmadji, T.
collection Repository of Agricultural Research Outputs (CGSpace)
description Logging and/or forest fires cause a direct impact of reducing vegetation cover, and in many cases create a pre-condition for the increase of soil erosion rates during high rainfall. Such an increase in soil erosion rate may be higher than the normal threshold rate from a sustainable forest land productivity viewpoint. Field measurement was focused on surface runoff (overland flow) and eroded soil mass on slopes of 25-35% with light and heavy intensities of logging and control plots. Both logging intensities directly increased surface runoff and eroded soil mass, especially on timber felling, skidding trails establishment and log skidding and/or hauling from the logging compartments through feeder roads to the temporary logyard. Higher rainfall amounts and intensity tended to increase the volume of surface runoff and for some cases also eroded soil mass. The volume of surface runoff was 2559 litre ha-1 year-1; 4711 litre ha-1 year-1 and 5123 litre ha-1 year-1; while the cumulative eroded soil mass was estimated to be 0.073 t ha-1 year-1; 0.046 t ha-1 year-1, and 0.060 t ha-1 year-1 for the light, heavy and control of logging intensities respectively. However, the eroded soil mass in all research plots confirmed that there was no significant relationship between soil erosion rate and logging intensity, and the eroded soil mass was lower than the tolerable/permissible/acceptable soil erosion rate. Therefore, erosion control measures in relation to land productivity after logging and fires do not need to be carried out immediately. Regarding the erosion process, the slope and its length (microtopography) was the most important factor for increasing soil erosion rate. Further, vegetation cover was important in reducing and/or minimising the occurrence of surface runoff and soil erosion.
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spelling CGSpace184122025-01-24T14:20:38Z Impact of logging and forest fires on soil erosion in tropical humid forest in Kalimantan Sudarmadji, T. logging forest fires erosion tropical forests slopes humid zones conferences Logging and/or forest fires cause a direct impact of reducing vegetation cover, and in many cases create a pre-condition for the increase of soil erosion rates during high rainfall. Such an increase in soil erosion rate may be higher than the normal threshold rate from a sustainable forest land productivity viewpoint. Field measurement was focused on surface runoff (overland flow) and eroded soil mass on slopes of 25-35% with light and heavy intensities of logging and control plots. Both logging intensities directly increased surface runoff and eroded soil mass, especially on timber felling, skidding trails establishment and log skidding and/or hauling from the logging compartments through feeder roads to the temporary logyard. Higher rainfall amounts and intensity tended to increase the volume of surface runoff and for some cases also eroded soil mass. The volume of surface runoff was 2559 litre ha-1 year-1; 4711 litre ha-1 year-1 and 5123 litre ha-1 year-1; while the cumulative eroded soil mass was estimated to be 0.073 t ha-1 year-1; 0.046 t ha-1 year-1, and 0.060 t ha-1 year-1 for the light, heavy and control of logging intensities respectively. However, the eroded soil mass in all research plots confirmed that there was no significant relationship between soil erosion rate and logging intensity, and the eroded soil mass was lower than the tolerable/permissible/acceptable soil erosion rate. Therefore, erosion control measures in relation to land productivity after logging and fires do not need to be carried out immediately. Regarding the erosion process, the slope and its length (microtopography) was the most important factor for increasing soil erosion rate. Further, vegetation cover was important in reducing and/or minimising the occurrence of surface runoff and soil erosion. 2001 2012-06-04T09:06:26Z 2012-06-04T09:06:26Z Book Chapter https://hdl.handle.net/10568/18412 en Center for International Forestry Research Sudarmadji, T. 2001. Impact of logging and forest fires on soil erosion in tropical humid forest in Kalimantan . In: Kobayashi, S., Turnbull, J.W., Toma, T., Mori, T., Majid, N.M.N.A. (eds.). Rehabilitation of degraded tropical forest ecosystems: workshop proceedings, 2-4 November 1999, Bogor, Indonesia. :35-44. Bogor, Indonesia, Bogor, Indonesia, CIFOR. CIFOR. ISBN: 979-8764-70-6..
spellingShingle logging
forest fires
erosion
tropical forests
slopes
humid zones
conferences
Sudarmadji, T.
Impact of logging and forest fires on soil erosion in tropical humid forest in Kalimantan
title Impact of logging and forest fires on soil erosion in tropical humid forest in Kalimantan
title_full Impact of logging and forest fires on soil erosion in tropical humid forest in Kalimantan
title_fullStr Impact of logging and forest fires on soil erosion in tropical humid forest in Kalimantan
title_full_unstemmed Impact of logging and forest fires on soil erosion in tropical humid forest in Kalimantan
title_short Impact of logging and forest fires on soil erosion in tropical humid forest in Kalimantan
title_sort impact of logging and forest fires on soil erosion in tropical humid forest in kalimantan
topic logging
forest fires
erosion
tropical forests
slopes
humid zones
conferences
url https://hdl.handle.net/10568/18412
work_keys_str_mv AT sudarmadjit impactofloggingandforestfiresonsoilerosionintropicalhumidforestinkalimantan