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    宁夏六盘山沙棘液流变化及耗水特性

    Characteristics of sap flow and water use of Hippophae rhamnoides community in Liupan Mountains, Ningxia

    • 摘要: 基于热平衡法实测宁夏六盘山北坡天然沙棘茎干液流通量的变化,分析沙棘液流生长季内的日内和日际变化特征,并估算沙棘群落的蒸腾量。结果表明:1)沙棘液流日变化曲线在晴天表现出明显的单峰型,在夜间仍有液流运动,夜间液流量占总全天总液流量的12.87% ~ 19.62%;液流通量主要受太阳总辐射、空气饱和水汽压差、气温和相对湿度等影响。2)6—9 月,沙棘蒸腾速率呈明显的降低趋势; 6—9 月沙棘群落蒸散量为469.4 mm,略高于同期降水量,蒸腾量约占同期蒸散量的35.11%。3)以环境因子为自变量, 以液流量为因变量, 经过逐步回归, 建立了多元线性模型, 回归方程显著。

       

      Abstract: Based on the observation of the sap flow flux of Hippophae rhamnoides by the stem heat balance method on northern slope of Liupan Mountains, this paper analyzed the daily sap flow characteristics of H. rhamnoides during the growing season, and estimated the transpiration of H. rhamnoides plantations. The curve of daily sap low showed a typical single-peak pattern, and indicated that sap flow continued till night. The ratio of nocturnal sap flow flux to total daily sap flow flux is about 12.87% to 19.62%. The daily sap flow flux could be affected by total daily solar radiation, mean vapor pressure deficit, mean air temperature and mean relative air humidity. The transpiration velocity of H. rhamnoides showed an obvious declining trend from March to September, with a total transpiration of 469.4 mm, which was a little higher than the simultaneous precipitation, and the ratio of this transpiration to simultaneous total evapotranspiration is 35.11%. The regression equation to relate environmental parameters to total transpiration was established.

       

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