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首页> 外文期刊>Canadian Journal of Forest Research >Soil physical property changes at the North American Long-Term Soil Productivity study sites: 1 and 5 years after compaction
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Soil physical property changes at the North American Long-Term Soil Productivity study sites: 1 and 5 years after compaction

机译:北美长期土壤生产力研究地点的土壤物理性质变化:压实后的1年和5年

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The impact of forest management operations on soil physical properties is important to understand, since management can significantly change site productivity by altering root growth potential, water infiltration and soil erosion, and water and nutrient availability. We studied soil bulk density and strength changes as indicators of soil compaction before harvesting and 1 and 5 years after harvest and site treatment on 12 of the North American Long-Term Soil Productivity sites. Severe soil compactiontreatments approached root-limiting bulk densities for each soil texture, while moderate compaction levels were between severe and preharvest values. Immediately after harvesting, soil bulk density on the severely compacted plots ranged from 1% less than to 58% higher than preharvest levels across all sites. Soil compaction increases were noticeable to a depth of 30 cm. After 5 years, bulk density recovery on coarse-textured soils was evident in the surface (0-10 cm) soil, but recovery was less in thesubsoil (10-30 cm depth); fine-textured soils exhibited little recovery. When measured as a percentage, initial bulk density increases were greater on fine-textured soils than on coarser-textured soils and were mainly due to higher initial bulk density values in coarse-textured soils. Development of soil monitoring methods applicable to all soil types may not be appropriate, and more site-specific techniques may be needed for soil monitoring after disturbance.
机译:必须理解森林经营活动对土壤物理特性的影响,因为经营管理可以通过改变根系的生长潜力,水的渗透和土壤侵蚀以及水和养分的可利用性来显着改变站点生产力。我们在北美长期土壤生产力的12个站点上研究了土壤容重和强度变化,作为收获前和收获后1年和5年以及土壤处理的5年指标。严重的土壤压实处理接近每种土壤质地的根部极限密度,而中等的压实水平介于严重和收获前之间。收获后,在所有地点,紧压土地上的土壤容重立即比收获前的水平低1%至高58%。在30厘米深处,土壤压实度明显增加。 5年后,表层(0-10厘米)土壤中粗纹理土壤的容重恢复很明显,而深层土壤(10-30厘米深度)的容重恢复较小;质地细密的土壤几乎没有恢复。当以百分数测量时,细纹理土壤的初始容重增加比粗纹理土壤的大,主要是由于粗纹理土壤的初始容重更高。开发适用于所有土壤类型的土壤监测方法可能并不适当,并且可能需要更多针对特定地点的技术来进行扰动后的土壤监测。

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