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北京九龙山不同植被土壤水分特征的研究*

Study on Soil Moisture Characteristics of Different Forest Vegetations in Jiulongshan, BeiJing

  • 摘要: 通过实测的土壤水分特征曲线,分析了不同植被的土壤持水性。结果表明:土壤吸力与土壤含水量之间存在着显著的幂函数关系,它们的数学模型为:θ=aSb;土壤的持水性由好到差依次为:阴坡灌木、阴坡裸地、阴坡油松、阳坡灌木、阳坡裸地、阳坡侧柏;坡向和植被类型对土壤的持水性影响极大。同一坡向中,灌木林地的土壤持水性优于乔木林地,所有林地的表层土壤(0~20cm)的持水性均优于下层土壤(20~60cm);回归分析结果表明,在相同的立地条件下,影响土壤中、低吸力段持水性的主要因子为土壤容重、毛管孔隙度和有机质含量。

     

    Abstract: Soil moisture retention characters of different forest vegetations in Juilongshan were analysed by measurement of soil water characteristics in the field.The result showed there was a high power function correlation between the soil moisture content and the potential of soil water. The mathematical model is:θ=aSb.Soil moisture retention of different forest vegetations were ranged in order from better ones to poor ones as follows:schattenseite shrubland,schattenseite bare soil,schattenseite Pinus tabulaeformis forest soil, endroit shrubland, endroit bare soil,endroit Platycladus orientalis forest soil. Slope orientation and vegetation type are the main factors affecting the soil moisture retention. On the same slope orientation,soil moisture retention of shrub forest land was better than that of the high-forest land.In all the forest land, the soil moisture retention of superficial soil (0~20 cm) was better than that of subsurface soil (20~60 cm). On the same site,the soil factors influencing the soil moisture retention characters in medium and low suction range are soil structure, organic matter content and soil texture.

     

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