Hostname: page-component-cd9895bd7-hc48f Total loading time: 0 Render date: 2024-12-23T09:38:14.910Z Has data issue: false hasContentIssue false

Physical Soil-properties Associated with Recreational Use of a Forested Reserve Area in Malaysia

Published online by Cambridge University Press:  24 August 2009

Kamaruzaman Jusoff
Affiliation:
Lecturer, Faculty of Forestry, University Pertanian Malaysia (UPM)43400 UPM Serdang, Selangor, Malaysia.

Extract

Forested areas of Kanching Recreation Forest exposed to concentrated recreational use tend to show signs of deterioration as indicated by soil parameters related to soil compaction. The results of the present study clearly indicate that such a deterioration of soil conditions has already occurred, though not on an alarming scale. Indeed the status of these soils remains favourable, as the figures for saturated hydraulic conductivity and plant-available water are still ‘satisfactory’, or at least were so during the period of study (1989). Surface runoff and sheet-erosion in intensively-used recreational sites must not, however, be looked upon in isolation when advising on recreational forest land-management.

A recent study in Kanching Forest Reserve, Malaysia, showed that recreational use of forested areas could adversely affect soil conditions. Soil bulk density and micropore space were significantly increased, but total porespace and macropore space were significantly decreased. Available water-holding capacity, saturated hydraulic conductivity, and particle-size distribution, were not significantly affected by recreational use on such sites, indicating that the status of Kanching Recreation Forest soil is still favourable for plant growth, or at least it was during the period of this study.

Type
Main Papers
Copyright
Copyright © Foundation for Environmental Conservation 1989

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Jusoff, Kamaruzaman, (1988). Soil compaction from off-road transportation machine on hill forest land. Pertanika 11(1), pp. 31–7.Google Scholar
Jusoff, Kamaruzaman & Majid, Nik Muhamad (1986). The impacts of skid trails on the physical properties of tropical hill-forest soils. Pertanika, 9(3). pp. 311–21.Google Scholar
Klute, A. (1965). Constant-head method of hydraulic conductivity determination. Pp. 213–15 in Methods of Soil Analysis, Part 1: Physical and Mineralogical Properties Including Statistics of Measurement and Sampling (Ed. Black, C.A.). Amer. Soc. Agron. Inc., Madison, Wisconsin, USA: [not available for checking].Google Scholar
Lal, R. & Akinremi, O.O. (1983). Physical properties of earthworm casts and surface soil as influenced by management. Soil Sci., 135(2), pp. 114–22.CrossRefGoogle Scholar
Mbagwu, J., Lal, R. & Scott, T.W. (1983). Physical properties of three soils in Southern Nigeria. Soil Sci., 136(1), pp. 4855.CrossRefGoogle Scholar
Zaharuddin, Abu Nasir (1981). Preliminary Study of Some Recreational Land Criteria with Special Reference to Kanching Forest Reserve and Tempters Park. Unpubl. B.S. thesis, Faculty of Forestry, Universiti Pertanian Malaysia, Serdang, Malaysia: 164 pp.Google Scholar