河西走廊荒漠区土壤物理性质沿降水梯度的变化
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国家重点基础研究发展计划课题"绿洲化的水土气生过程及其相互作用机制研究"(2009CB421302)


Change of Soil Physical Properties with Precipitation Gradient in Desert Region of Hexi Corridor
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    摘要:

    土壤质量、土壤蓄水保肥能力和土壤养分吸收利用与土壤物理性质有密切联系。在甘肃省河西走廊民乐县至高台县自东向西的天然降水梯度上,选择荒漠区的7个研究点对土壤表层(0—20cm)和亚表层(20—40cm)分别采集42个土壤样品,在野外采用张力入渗仪测定饱和导水率,室内采用常规方法对土壤容重、孔隙度、颗粒组成等项目进行了测定。结果表明,在360~100mm的降水梯度上,荒漠土壤粉粒和黏粒含量降低,砂粒含量增加;伴随着土壤的粗粒化,引起土体的风散和结构的破坏,使土壤容重增加、孔隙度降低、持水性能下降等一系列物理性质的恶化。土壤表层、亚表层饱和导水率Ksat和变异系数Cv分别为70.0%和86.3%,均是土壤表层和亚表层各物理性质中变异系数最高的。

    Abstract:

    Soil quality,soil moisture and fertilizer preservation ability,and soil nutrient uptake ability are closely related to soil physical properties.In this study,42 soil samples were collected respectively in the 0—20 and 20—40 cm soil layers from seven desert sampling plots along descending precipitation gradient in Hexi Corridor region(from Minle County to Gaotai County).Saturated soil hydraulic conductivity was measured with the tension infiltrometer in field,and bulk density,porosity,and soil particle composition were determined by general methods in lab.Results show that physical properties of the desert soils are gradually degraded.With precipitation decreasing from 360 to 100 mm,silt and clay contents are reduced and sand content is increased.Increase in soil particle size may definitely result in soil dispersion and structure destruction,further increase soil bulk density,and reduce soil porosity and water holding capacity.The variance coefficients of saturated soil hydraulic conductivity in the surface and subsurface layers are 70.0% and 86.3%,respectively,both of which are the highest among the Cv values of all the physical properties.

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王蕙,赵文智,武利玉.河西走廊荒漠区土壤物理性质沿降水梯度的变化[J].水土保持通报,2010,(6):46-51

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  • 收稿日期:2010-05-14
  • 最后修改日期:2010-06-17
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  • 在线发布日期: 2014-11-26
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