2010
DOI: 10.1016/j.foreco.2010.08.002
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Assessing the effects of initial soil characteristics, machine mass and traffic intensity on forest soil compaction

Abstract: An extensive field trial was set up in eight forest stands to examine the influence of soil texture (two stands on sand, four on loam to silt loam, two on clay), machine mass (light, heavy) and traffic intensity (1 and 5 skidding cycles) (i.e. pass back and forth on the skid trail) on soil compaction after mechanized harvesting. Dry bulk density (BD), penetration resistance (PR), micro-topography and soil carbon dioxide (CO 2 ) concentration were applied as response variables for soil compaction. Significant e… Show more

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Cited by 125 publications
(96 citation statements)
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“…However, Gayoso and Iroume (1991) stated that this may be a consequence of the problems that the skidder might face when logging in steep terrains. In this study there was not only compaction at all three depths but with increasing soil depth the compaction level also increased, which is in agreement with the results of other researchers (Cullen, 1991;Horn et al, 2004;Eliasson, 2005;Bolding et al, 2009;Ampoorter et al, 2010). This is related to the rather homogeneous weight distribution of the skidder on the flat skid trails.…”
Section: Discussionsupporting
confidence: 93%
“…However, Gayoso and Iroume (1991) stated that this may be a consequence of the problems that the skidder might face when logging in steep terrains. In this study there was not only compaction at all three depths but with increasing soil depth the compaction level also increased, which is in agreement with the results of other researchers (Cullen, 1991;Horn et al, 2004;Eliasson, 2005;Bolding et al, 2009;Ampoorter et al, 2010). This is related to the rather homogeneous weight distribution of the skidder on the flat skid trails.…”
Section: Discussionsupporting
confidence: 93%
“…Overall, the soil total porosity reduced in the layer 0.00-0.30 m in the different areas evaluated after mechanized harvest of pine, with greater intensity in the low-and highdisturbance areas, which changed to a depth of 0.60 m. Some studies that evaluated the effects of forest harvesting on soil physical properties also reported a pore volume decrease after the machines' traffic (Lopes et al, 2006;Silva et al, 2006;Ampoorter et al, 2010). These changes modified other physical attributes, since the biopores and macropores volume and aeration capacity were lower in the different areas at post-harvest to a depth of 0.30 m and in the high-disturbance areas, up to 0.60 m. Dirksen (1991) describes biopores as the soil cavities caused by the presence of earthworms and termites and development of roots within the soil.…”
Section: Resultsmentioning
confidence: 94%
“…According to Ampoorter et al (2010), clayey and clay-loamy soils are more vulnerable to damage than coarse-grained soils. The high susceptibility level for clayey type is not therefore surprising, as these soils are prone to compaction and leaching, which are the representative characteristics in high and very CART -classification and regression tree, RF -random forest high soil susceptibility sub-classes.…”
Section: Discussionmentioning
confidence: 99%