conversions were merely qualitative, and highlighted on the magnitude and intensity of forest transformations on soil, water quantity and quality
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2 conversions were merely qualitative, and highlighted on the magnitude and intensity of forest transformations on soil, water quantity and quality (Daniel & Kulasingam 1974, Toebes & Goh 1973, Low & Peh 1985). Relatively little information is available to date on which quantification of the effects of such conversions are to be based with reasonable accuracy except for this study at Sungai Tekam Experimental Basin (STEB) in Pahang, Peninsular Malaysia (DID 1982, 1986), as well as on-going studies conducted by the Forest Research Institute Malaysia (Abdul Rahim & Zulkifli 1987). Studies from temperate countries show a variation of responses resulting from forest clearance
3 Table
4 Catchment
5 Legend Forest Area Catchment Boundary River System
6 three phases
7 Operation Table 3. Forest Conversion Schedules in Catchments A and B
8 Results and discussion Rainfall The study area received a relatively low annual rainfall during the study period, ranging from 1428
9 Mean 1.8 1
10 Figure
11 18-16
12 3.2 Clrai foiling
13 (1965) believes, it may be difficult to reach an objective conclusion except provide some general trends. Extreme variability of flow is quite common in all catchments as explained by
14 Figure
15 first-half of the year. Clear felling of the entire catchment and burning of fallen logs was carried out in the second-half of the year. Accordingly, the full effect of clear felling and burning is clearly depicted in the second year of treatment and the years following. Water yield increase during the transition and evaluation periods was statistically significant (p < 0.01; F value 22 and d.f of 5 & 75). Water Yield Changes
16 However, the different rates of water yield changes during transition and evaluation periods between catchments
17 Legent:
18 References ABDUL RAHIM, N., BAHARUDDIN, K. & AZMAN, H Hydrologic regime of dipterocarp forest catchments
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