韩凤朋, 郑纪勇, 张兴昌. 黄土退耕坡地植物根系分布特征及其对土壤养分的影响[J]. 农业工程学报, 2009, 25(2): 50-55.
    引用本文: 韩凤朋, 郑纪勇, 张兴昌. 黄土退耕坡地植物根系分布特征及其对土壤养分的影响[J]. 农业工程学报, 2009, 25(2): 50-55.
    Han Fengpeng, Zheng Jiyong, Zhang Xingchang. Plant root system distribution and its effect on soil nutrient on slope land converted from farmland in the Loess Plateau[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2009, 25(2): 50-55.
    Citation: Han Fengpeng, Zheng Jiyong, Zhang Xingchang. Plant root system distribution and its effect on soil nutrient on slope land converted from farmland in the Loess Plateau[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2009, 25(2): 50-55.

    黄土退耕坡地植物根系分布特征及其对土壤养分的影响

    Plant root system distribution and its effect on soil nutrient on slope land converted from farmland in the Loess Plateau

    • 摘要: 为明确黄土退耕坡地植物根系分布特征及其对土壤养分的影响,在陕西神木六道沟流域选取退耕30 a的长芒草坡地和裸地坡面,利用图像处理和常规分析方法研究了长芒草根系和土壤养分在土壤剖面分布及其相互关系。结果表明:长芒草根系主要分布在0~50 cm土层,分布规律可用指数函数来模拟。有根系存在的土壤表层有机质、全氮、全磷、硝态氮和铵态氮含量均高于无根系存在的坡面。在有根系存在时土壤有机质、全氮和硝态氮的具有明显的表聚现象。0~ 50 cm有机质、全氮、硝态氮和铵态氮随深度的变化可用幂函数来表示,而全磷随深度呈线性相关。0~50 cm的土壤养分与根长密度的关系可以用线性函数来表示。其研究结果为坡面退耕地土壤管理提供科学依据。

       

      Abstract: In order to understand the root system distribution of Stipa bungeana in the soil profile and its influence on soil nutrients, two slopes were studied. One is a slope with 30 years growth of Stipa bungeana and the other is a bare slope land. They are all located in Shenmu experiment station of the Loess Plateau. The soil nutrients and root distribution in the soil profile were studied using picture management software and general analysis method. The results show that the root of Stipa bungeana mainly distributed in the soil profile of 0-50 cm and it could be simulated by an exponential function. The contents of organic matter, total nitrogen, total phosphorus, nitrate nitrogen and ammonium nitrogen on the soil surface with plant root were higher than those on the soil surface without root. The organic matter, total nitrogen and nitrate nitrogen have obvious topsoil accumulation when the soil contains roots. The changes of organic matter, total nitrogen and nitrate nitrogen in 0~50 cm along the depth of soil can be described by a power function, but the total phosphorus can be described by a linear function, and the changes of soil nutrients along the root length density can be described by linear function.

       

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