荒漠草原土壤盐分空间变异特征研究

Spatial Variation Characteristics of Soil Salinity in Desert Steppe

  • 摘要:
    目的 探究干旱半干旱区土壤盐分的空间变异特征,为干旱半干旱区荒漠草原植被类型的盐渍化土壤改良提供理论基础和参考价值。
    方法 以荒漠草原土壤盐分空间分布为研究内容,于2019年5月份在盐池县哈巴湖自然保护区周边的144 km2地区,采用GPS定位技术和网格取样法,对研究区域内的144个样点进行土壤取样,运用经典统计学和地统计学相结合的方法,探究不同深度土层盐分含量的空间变异特征。
    结果 ①研究区土壤pH值介于8.85 ~ 9.03,土壤盐分含量普遍较高,介于8.692 ~ 16.728 g kg−1之间,其中0 ~ 20 cm土层的土壤盐分含量最大,显著高于其他各层(P < 0.05),各层土壤盐分的变异系数范围为0.642 ~ 0.794,属于中等变异。②0 ~ 20 cm、20 ~ 40 cm、40 ~ 60 cm土层土壤盐分半方差函数最佳理论模型为指数模型,60 ~ 80 cm和80 ~ 100 cm土层为球状模型。③变程范围为2.84 ~ 14.63 km,随着土壤深度的增加,变程逐渐变大,块基比(C0/Sill)逐渐减小,空间自相关性增强。
    结论 各层土壤盐分空间分布规律基本一致,分布格局主要以斑块状分布格局为主,除20 ~ 40 cm土层的土壤盐分分布格局为条带状分布格局外,土壤盐渍化程度由东北向西南方向逐渐减轻。

     

    Abstract:
    Objective The aim was to explore the spatial variation characteristics of soil salinity in arid and semi-arid areas, which could provide a theoretical basis and reference value for the improvement of salinized soil of desert steppe vegetation types.
    Method This paper took the spatial distribution of soil salinity in desert steppe as the research content in the 144 km2 area around Haba Lake Nature Reserve in Yanchi County in May of 2019. Soil samplings were carried out by using GPS positioning technology and grid sampling method, and the spatial variation characteristics of soil salt contents at different depths were explored by using the combination of classical statistics and geostatistics.
    Result ① The soil pH value in the study area was between 8.85 ~ 9.03, and the soil salt contents were generally high, ranging from 8.692 ~ 16.728 g kg−1, and the soil salt content in the 0 ~ 20 cm soil layer was the largest, which was significantly higher than that of the other layers (P < 0.05). The variation coefficients of soil salinity in each layer ranged from 0.642 ~ 0.794, which belonged to the moderate variation. ② The best theoretical model of the semi-variance function of soil salinity in 0 ~ 20 cm, 20 ~ 40 cm and 40 ~ 60 cm soil layers was the exponential model, and the best for 60 ~ 80 cm and 80 ~ 100 cm soil layers was spherical models. ③ The ranges were 2.84 ~ 14.63 km, and with the increase of soil depth, the range gradually increased. The block-to-base ratio (C0/Sill) decreased gradually, and the spatial autocorrelation was enhanced.
    Conclusion The spatial distribution of soil salinity in each layer was basically the same, and the distribution pattern was mainly patch-like distribution pattern, except for the strip-like distribution pattern of soil salinity in the 20 ~ 40 cm soil layer, and the degree of soil salinization gradually decreased from northeast to southwest.

     

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