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首页> 外文期刊>Canadian Journal of Forest Research >Soil deformation and its recovery in logging trails of drained boreal peatlands
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Soil deformation and its recovery in logging trails of drained boreal peatlands

机译:排水博科尔泥土伐木轨迹的土壤变形及其恢复

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摘要

Forestry-drained peatlands occupy approximately 15 million ha in boreal and temperate zones. In Finland, they represent almost one-fourth of the total forest area. They are subjected to the same harvesting operations as upland forests. Although the soil deformation caused by timber harvesting is well documented in upland forests, the knowledge on the soil disturbance induced by the harvesting machinery on peat soils is still lacking. To address this, we collected soil samples from six peatland sites that were thinned using a harvester-forwarder combination. Peat samples were taken from the trails formed by the machinery and outside the trails to a depth of 10 cm. To assess the recovery of soil properties after the disturbance, we sampled sites along a chronosequence with respect to time since harvesting. Soil deformation under the machinery appeared to increase the bulk density and field capacity of peat and decrease its total porosity; however, disturbed plots and control plots started to resemble each other in their soil properties within 15 years. The results imply that peat soil is sensitive to disturbance but has a high recovery potential.
机译:林业排水的泥炭地占据了大约1500万公顷的北方和温带区。在芬兰,他们代表了森林总面积的四分之一。它们作为高地森林对其相同的收获行动。虽然木材收获引起的土壤变形在高地森林中有很好的记录,但仍然缺乏对收获机械诱导的土壤紊乱的知识。为了解决这个问题,我们从使用收割机转发器组合稀释的六个泥炭兰地点收集土壤样本。泥炭样品从机器形成的小径和小径外部取出10厘米的深度。为了评估干扰后的土壤性质的回收,我们沿着收获以来的时间沿着一定时间进行了采样的景点。机械下的土壤变形似乎增加了泥炭的堆积密度和场容量,降低了其总孔隙率;然而,扰乱的地块和控制图开始在15年内的土壤性质中彼此相互作用。结果意味着泥炭土壤对干扰敏感但具有高恢复潜力。

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