2001
DOI: 10.1016/s0378-1127(00)00360-1
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Impacts on soils from cable-logging steep slopes in northeastern Tasmania, Australia

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Cited by 31 publications
(30 citation statements)
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“…Forest operations, especially log skidding, cause major changes in soil physical properties such as increasing soil bulk density, decreasing total porosity and water content (McNeel, Ballard 1992;Bengtsson et al 1998;Laffan et al 2001;Rab et al 2004). The size, power and weight of forest machines are the main sources of soil disturbance.…”
Section: Discussionmentioning
confidence: 99%
“…Forest operations, especially log skidding, cause major changes in soil physical properties such as increasing soil bulk density, decreasing total porosity and water content (McNeel, Ballard 1992;Bengtsson et al 1998;Laffan et al 2001;Rab et al 2004). The size, power and weight of forest machines are the main sources of soil disturbance.…”
Section: Discussionmentioning
confidence: 99%
“…In comparison with our study McMahon (1995) found 71% undisturbed and shallow disturbance, 4% deep disturbance, and 37% compacted, when rubber-tired skidders were used. Laffan et al (2001) indicated that after logging by conventional ground-based skidding from steep slopes the most observations (> 70%) were slash cover (47%) and undisturbed soils (25%). Disturbed soils accounted for nearly 30% of observations with the most comprising slightly (17%) and moderately…”
Section: Soil Surface Disturbancesmentioning
confidence: 99%
“…Soil compaction and decreased total porosity are unavoidable consequences of ground skidding operations that can vary in intensity and distribution as a result of the interaction between machine and site factors at the time of harvest. The dimension of the impact varies according to many factors such as skidder passage, skid trail slope, site characteristics, harvesting machines, planning of skid roads and production season (Laffan et al 2001;Demir et al 2007;Najafi et al 2009). The number of machine passes is a key factor that significantly influences the degree of soil damage.…”
mentioning
confidence: 99%
“…As a result, the soil would experience high pressures. In the same conditions of soil tension, steep slope receives greater damage compared to gentle slope due to altering the forest hydrological function and soil morphological process (Laffan et al 2001;Moore, Wondzell 2005). Therefore, it was assumed that slope aspect carries a high weight in determining the hazard zoning status and steep slope can be called an ample window of damage (Cerdà, Doerr 2005;Cerdà, Lasanta 2005).…”
Section: Discussionmentioning
confidence: 99%