加纳潮湿常绿森林中选择性采伐后滑道上的土壤压实

A. Alexander
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引用次数: 15

摘要

土壤压实被认为是与采伐有关的主要损害形式,它限制了根系生长,减少了自然再生。没有关于随时间变化的压实和土壤恢复程度的信息。本研究评价了采伐对加纳潮湿常绿森林土壤压实的影响。在六个地点测量了滑轨上土壤压实的程度:两个在边缘,两个在中心,两个在未砍伐区域作为对照,并在40年和1年的滑轨上重复了7次。通过测量渗透阻力,利用土壤渗透仪测定土壤的压实程度。在40年的滑道中,边缘和中心的穿透阻力明显高于未伐木区域。在一年的滑痕中,穿透度仅在边缘明显高于未砍伐的痕迹。对比两种滑轨,表层土壤压实恢复速率在此期间无显著差异,说明重型机械压实对表层土壤结构的持续影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil compaction on skid trails after selective logging in moist evergreen forest of Ghana
Soil compaction has been considered as a principal form of damage associated with logging, restricting root growth and reducing natural regeneration. There is no information on the changes in compaction and extent of soil recovery over time. This study evaluates the effects of logging on soil compaction in moist evergreen forest of Ghana. The extent of soil compaction on skid trails was measured at six locations: two plots on the edges, two on the center and two on the unlogged area as a control and replicated seven times on a forty year and one year old skid trails. Penetration resistance was measured to determine the extent of soil compaction using the soil penetrometer. In the forty year old skid trail, penetration resistance was significantly higher at the edge and center as compared to the unlogged area. In the one year old skid trail, penetration was only significantly higher at the edge than the unlogged. Comparing the two skid trails, recovery rate of surface soil compaction showed no significant difference over the period, illustrating the persistent effect of heavy machinery compaction on surface soil structure.
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