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Soil compaction on skid trails after selective logging in moist evergreen forest of Ghana

机译:加纳潮湿常绿森林选择性伐木后滑道的土壤压实

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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 surf ace soil compaction showed no significant difference over the period, illustrating the persistent effect of heav y machinery compaction on surface soil structure.
机译:土壤压实被认为是与伐木有关的主要破坏形式,它限制了根系的生长并减少了自然再生。没有关于压实度和土壤恢复程度随时间变化的信息。这项研究评估了加纳潮湿常绿森林中伐木对土壤压实的影响。在六个位置测量了滑行道上的土壤压实程度:在边缘上有两个图块,在中央有两个图块,在未采伐区域上有两个图块作为对照,并在有40年和一年历史的滑道上重复了7次。使用土壤渗透仪测量抗渗透性以确定土壤压实程度。在有40年历史的滑道中,其边缘和中心的穿透阻力比未记录的区域要高得多。在一年的滑道中,边缘的渗透率仅比未记录的高。比较这两个滑道,表层土壤压实的恢复率在此期间没有显着差异,说明了重型机械压实对表层土壤结构的持续影响。

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