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科尔沁沙地不同地形部位人工小叶锦鸡儿灌丛林土壤水分动态

[Soil moisture dynamics of artificial Caragana microphylla shrubs at different topographical sites in Horqin sandy land].

作者信息

Huang Gang, Zhao Xue-yong, Huang Ying-xin, Su Yan-gui

机构信息

Naiman Desert Experimental Research Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2009 Mar;20(3):555-61.

Abstract

Based on the investigation data of vegetation and soil moisture regime of Caragana microphylla shrubs widely distributed in Horqin sandy land, the spatiotemporal variations of soil moisture regime and soil water storage of artificial sand-fixing C. microphylla shrubs at different topographical sites in the sandy land were studied, and the evapotranspiration was measured by water balance method. The results showed that the soil moisture content of the shrubs was the highest in the lowland of dunes, followed by in the middle, and in the crest of the dunes, and increased with increasing depth. No water stress occurred during the growth season of the shrubs. Soil moisture content of the shrubs was highly related to precipitation event, and the relationship of soil moisture content with precipitation was higher in deep soil layer (50-180 cm) than in shallow soil layer (0-50 cm). The variation coefficient of soil moisture content was also higher in deep layer than in shallow layer. Soil water storage was increasing in the whole growth season of the shrubs, which meant that the accumulation of soil water occurred in this area. The evapotranspiriation of the shrubs occupied above 64% of the precipitation.

摘要

基于对科尔沁沙地广泛分布的小叶锦鸡儿灌丛林植被及土壤水分状况的调查数据,研究了沙地不同地形部位人工固沙小叶锦鸡儿灌丛林土壤水分状况和土壤贮水量的时空变化,并采用水量平衡法测定了蒸散量。结果表明,灌丛林土壤含水量在沙丘低地最高,其次是中部,沙丘顶部最低,且随深度增加而增大。灌丛林生长季未出现水分胁迫。灌丛林土壤含水量与降水事件高度相关,深层土壤(50 - 180厘米)土壤含水量与降水的关系比浅层土壤(0 - 50厘米)更密切。土壤含水量的变异系数也是深层高于浅层。灌丛林整个生长季土壤贮水量呈增加趋势,表明该地区土壤水分存在积累。灌丛林蒸散量占降水量的64%以上。

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