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    黄河河岸带5种植物类型根系结构特征对土壤渗透性的影响

    Effects of root structure characteristics of 5 plant types on soil infiltration in the Yellow River riparian

    • 摘要: 河岸植被缓冲带在涵养水源和保持水土方面具有重要的生态服务功能。为探讨河岸带不同植物类型根系结构特征与土壤渗透性之间的关系,在黄河下游河岸带郑州段选取5种单一植物的土壤和根系(0~10、10~20和20~30 cm)进行研究。结果表明:1)0~10 cm土层土壤渗透性为狗牙根>白茅>芦苇>艾蒿>水莎草;10~20和20~30 cm土层土壤渗透性为白茅>芦苇>艾蒿>狗牙根>水莎草。2)随着土层深度增加,狗牙根和水莎草根系结构特征参数和土壤渗透性逐渐降低,艾蒿则相反,而芦苇和白茅呈先增高后降低的趋势。3)根系直径在0.5~2 mm范围内的根系特征参数与土壤入渗特征指标之间存在显著线性相关性(P < 0.05)。4)Kostiakov模型更适宜拟合黄河河岸带土壤水分入渗过程,随着根长密度和根表面积密度的增加,Kostiakov模型参数a逐渐减小,参数b逐渐增大。白茅和芦苇的综合土壤渗透性能最好;狗牙根在0~10 cm土层有较强的渗透性;直径介于0.5~2 mm的根系对土壤渗透性的改善作用最好。

       

      Abstract:
      Background Riparian vegetation buffer zone has important ecological functions in soil and water conservation. However, serious vegetation degradation and soil erosion occur in this buffer zone due to various human disturbances. Thus, we characterized the root structure of five plant species and explored their relationships with soil infiltration.
      Methods The soil and root systems of 5 species (Imperata cylindrica, Phragmites australis, Cynodon dactylon, Artemisia argyi and Juncellus serotinus) in three soil layers (0-10 cm, 10-20 cm, and 20-30 cm) in the riparian zone of lower Yellow River were sampled and analyzed. The soil infiltration was measured using the Double Ring method. The root morphology and structure analysis system (WinRHIZO) was used to analyze root length density, root surface density, and root volume density, while the root system was dried to determine the root biomass. The infiltration process was simulated by the Horton model, Philip model and Kostiakov model.
      Results 1) The soil infiltration in 0-10 cm soil layer tended to be C. dactylon > I. cylindrical > P. australis > A. argyi > J. serotinus. The soil infiltration in the 10-20 cm and 20-30 cm soil layers was in this order: I. cylindrical > P. australis > A. argyi > C. dactylon > J. serotinus. 2) As the soil depth increased, the root structure parameters and soil infiltration of C. dactylon and J. serotinus decreased, that of A. argyi increased, while those of I. cylindrica and P. australis increased first and then decreased. 3) There were linear relationships among the root length density, root surface area density, root volume density, initial soil infiltration rate, stable infiltration rate, and average infiltration rate. The root biomass correlated with both soil stable infiltration rate and average infiltration rate. There was linear correlation between the characteristics of root system with diameter of 0.5-2.0 mm and soil infiltration characteristic index (P < 0.05). 4) Among the models, the Kostiakov model was more suitable to simulate the soil water infiltration processes. The model's parameter "a" decreased while parameter "b" increased with the increased root length density and root surface area density.
      Conculsions Our results indicate that the root system characteristics of the plant species significantly affect soil infiltration. The overall soil infiltration of I. cylindrica and P. australis is the highest among five species. C. dactylon has a relatively better soil infiltration in the 0-10 cm soil layer, and the roots within 0.5-2.0 mm diameter play the key role in soil infiltration processes.

       

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