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Evapotranspiration of a Populus euphratica Oliv. forest and its controlling factors in the lower Heihe River Basin,rNorthwest China

机译:胡杨的蒸发蒸腾作用。黑河下游流域的森林及其影响因素

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摘要

Evapotranspiration (ET) within an ecosystem is crucial for the water-limited environment that currently lacks adequate quantification in the arid region of Northwest China, mainly covered by phreatophytes, such as the Populus euphratica Oliv. tree and the Tamarix ramosissima Ledeb. shrub species. Accordingly, ET was measured for an entire year using ed-dy covariance (EC) in P. euphratica stands in the lower Heihe River Basin, Northwest China. During the growing season, the total ET was 850 mm, with a mean of 4.0 mm/d, which is obviously more than that observed at tree-level and stand-level scales, which was likely due to the different level of soil evaporation induced by irrigation via water conveyance. Factors associated with ET fall into either environmental or plant eco-physiological categories. Environmental factors ac-count for at least 79%variation of ET, and the linear relationship between ET and the groundwater table (GWT) revealed the potential water use of P. euphratica forests under the non-water stress condition with the GWT less than 3 m deep. Plant eco-physiological parameters, specifically the leaf area index (LAI), have direct impact on the seasonal pattern of ET, which provides a valuable reference to the wide-area estimates of ET for riparian forests by using LAI. In conclusion, P. euphratica forests have high water use after water conveyance, which may be the result of long-term adapting to local climates and limited water availability.
机译:生态系统内的蒸散量(ET)对于目前在中国西北干旱地区(主要由植物类植物,如胡杨)覆盖的水有限的有限环境至关重要。树和the柳ramosissima Ledeb。灌木种类。因此,在中国黑河下游流域的胡杨林中,使用ed-dy协方差(EC)对整年的ET进行了测量。在生长季节,总ET为850 mm,平均为4.0 mm / d,明显高于树木和林分尺度的观测值,这很可能是由于不同程度的土壤蒸发引起的通过输水灌溉。与ET相关的因素分为环境或植物生态生理两大类。环境因子至少占ET的79%,并且ET与地下水位(GWT)之间的线性关系表明,在非水分胁迫条件下,GWT小于3的胡杨林潜在用水量米深。植物生态生理参数,特别是叶面积指数(LAI),直接影响着ET的季节性模式,这为使用LAI对河岸森林的ET的大范围估计提供了宝贵的参考。总之,胡杨林在输水后需要大量用水,这可能是长期适应当地气候和有限水供应的结果。

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  • 来源
    《寒旱区科学(英文版)》 |2017年第2期|175-182|共8页
  • 作者单位

    Alax Desert Eco-hydrology Experimental Research Station, Northwest Institute of Eco-Environment and Resources, Ch-inese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Key Laboratory of Eco-hydrology of Inland River Basin, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Gansu Hydrology and Water Resources Engineering Research Center, Lanzhou, Gansu 730000, China;

    Alax Desert Eco-hydrology Experimental Research Station, Northwest Institute of Eco-Environment and Resources, Ch-inese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Key Laboratory of Eco-hydrology of Inland River Basin, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Gansu Hydrology and Water Resources Engineering Research Center, Lanzhou, Gansu 730000, China;

    Alax Desert Eco-hydrology Experimental Research Station, Northwest Institute of Eco-Environment and Resources, Ch-inese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Key Laboratory of Eco-hydrology of Inland River Basin, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Gansu Hydrology and Water Resources Engineering Research Center, Lanzhou, Gansu 730000, China;

    Alax Desert Eco-hydrology Experimental Research Station, Northwest Institute of Eco-Environment and Resources, Ch-inese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Key Laboratory of Eco-hydrology of Inland River Basin, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Alax Desert Eco-hydrology Experimental Research Station, Northwest Institute of Eco-Environment and Resources, Ch-inese Academy of Sciences, Lanzhou, Gansu 730000, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-19 03:41:28
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