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Effect of soil and water conservation forests on soil erodibility in typical black soil region of China

机译:水土保持林对典型黑土区土壤侵蚀性的影响

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Black soil area is one of six water erosion areas in China, where ecological environment is more fragile (Luo et al., 1995). The reasons causing soil erosion were not only the natural factors, but also long -term unreasonable land use and destruction of vegetation ( Li et al., 2006 ). Soil and water conservation forest is an effective biological practice for erosion control. This has been demonstrated in regulating precipitation power distribution to reduce soil erosion, thereby reducing soil loss ( Xu et al., 2006), and in reducing soil erodibility through the formation of litter and soil organic matter to improve soil structure ( Shen et al., 2000). Most of research on soil erodibility was focused on the composition of the soil particles, infiltration characteristics, organic matter content, and soil structure (Zhang et al., 2001), and on micro -aggregate content expressed by the indicators based on dispersion coefficient, dispersion rate, aggregate state (Guo et al., 1992) in Loess Plateau (Jiang,1964; Li et al., 1990). No investigation was reported in Black soil areas (Liao et al., 2008).
机译:黑土区是中国六个水蚀区之一,那里的生态环境更加脆弱(Luo等,1995)。造成水土流失的原因不仅是自然因素,而且还包括长期不合理的土地利用和植被破坏(李等人,2006)。水土保持林是控制侵蚀的有效生物实践。在调节降水功率分布以减少土壤侵蚀,从而减少土壤流失(Xu等,2006),以及通过形成凋落物和土壤有机质以改善土壤结构来降低土壤易蚀性方面,这已得到证明(Shen等。 ,2000)。大多数关于土壤易蚀性的研究都集中在土壤颗粒的组成,入渗特性,有机质含量和土壤结构上(Zhang等,2001),以及基于分散系数的指标所表示的微骨料含量,黄土高原的分散速率,聚集状态(Guo等,1992)(Jiang,1964; Li等,1990)。在黑土地区没有调查报告(Liao等,2008)。

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