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Contrasting effects of wildfire and clearfelling on the hydrology of a small catchment

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dc.contributor.author Scott, DF
dc.date.accessioned 2007-06-29T09:26:04Z
dc.date.available 2007-06-29T09:26:04Z
dc.date.issued 1997-05
dc.identifier.citation Scott, DF. 1997. Contrasting effects of wildfire and clearfelling on the hydrology of a small catchment. Hydrological Processes, vol. 11(6), pp 543-555 en
dc.identifier.issn 0885-6087
dc.identifier.uri http://hdl.handle.net/10204/802
dc.description Copyright: 1997 John Wiley & Sons Ltd en
dc.description.abstract A wildfire in an afforested research catchment presented the rare opportunity to compare the hydrological effects of wildfire with the effects of clearfelling in the same catchment in the Jonkershoek Valley, in the south-western Western Cape Province of South Africa. The timber plantation, which occupies 57% of the 2 km(2) catchment, had been clearfelled and re-planted to Pinus radiata roughly five years before the fire. The effects of the two treatments on total flow, stormflow and quick-flow volumes, peak discharge and storm response ratio were determined by means of multiple regression analysis, employing the dummy variable method to test for the significance of treatments. Both clearfelling and wildfire caused significant increases in all the stream-flow variables analysed. But the clearfelling effect was dominated by large increases in total flow (96% over three years), of which storm-flow and quick-flow volumes formed only minor parts. After the wildfire, by contrast, increases in total flow were small (12%) but the storm flow increases were three- to fourfold in the first year and roughly double in the second year. The wildfire caused fire-induced water repellency in the soils which led to overland flow on mid-slope sites, where soil infiltrability normally far exceeds local rainfall intensities. It is argued that these results support the hypothesis that stream-flow generation processes were changed by the wildfire in that overland flow made a direct contribution to storm flows, but that clearfelling had no such effect. en
dc.language.iso en en
dc.publisher John Wiley & Sons Ltd en
dc.subject Clearfelling en
dc.subject Storm flow analysis en
dc.subject Stream flow generation en
dc.subject Water repellent soils en
dc.subject Wildfire en
dc.subject Water resources en
dc.title Contrasting effects of wildfire and clearfelling on the hydrology of a small catchment en
dc.type Article en
dc.identifier.apacitation Scott, D. (1997). Contrasting effects of wildfire and clearfelling on the hydrology of a small catchment. http://hdl.handle.net/10204/802 en_ZA
dc.identifier.chicagocitation Scott, DF "Contrasting effects of wildfire and clearfelling on the hydrology of a small catchment." (1997) http://hdl.handle.net/10204/802 en_ZA
dc.identifier.vancouvercitation Scott D. Contrasting effects of wildfire and clearfelling on the hydrology of a small catchment. 1997; http://hdl.handle.net/10204/802. en_ZA
dc.identifier.ris TY - Article AU - Scott, DF AB - A wildfire in an afforested research catchment presented the rare opportunity to compare the hydrological effects of wildfire with the effects of clearfelling in the same catchment in the Jonkershoek Valley, in the south-western Western Cape Province of South Africa. The timber plantation, which occupies 57% of the 2 km(2) catchment, had been clearfelled and re-planted to Pinus radiata roughly five years before the fire. The effects of the two treatments on total flow, stormflow and quick-flow volumes, peak discharge and storm response ratio were determined by means of multiple regression analysis, employing the dummy variable method to test for the significance of treatments. Both clearfelling and wildfire caused significant increases in all the stream-flow variables analysed. But the clearfelling effect was dominated by large increases in total flow (96% over three years), of which storm-flow and quick-flow volumes formed only minor parts. After the wildfire, by contrast, increases in total flow were small (12%) but the storm flow increases were three- to fourfold in the first year and roughly double in the second year. The wildfire caused fire-induced water repellency in the soils which led to overland flow on mid-slope sites, where soil infiltrability normally far exceeds local rainfall intensities. It is argued that these results support the hypothesis that stream-flow generation processes were changed by the wildfire in that overland flow made a direct contribution to storm flows, but that clearfelling had no such effect. DA - 1997-05 DB - ResearchSpace DP - CSIR KW - Clearfelling KW - Storm flow analysis KW - Stream flow generation KW - Water repellent soils KW - Wildfire KW - Water resources LK - https://researchspace.csir.co.za PY - 1997 SM - 0885-6087 T1 - Contrasting effects of wildfire and clearfelling on the hydrology of a small catchment TI - Contrasting effects of wildfire and clearfelling on the hydrology of a small catchment UR - http://hdl.handle.net/10204/802 ER - en_ZA


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