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Effects of vegetation control on ecosystem water use efficiency within and among four grassland ecosystems in China

机译:植被控制对中国四个草地生态系统内和之中生态系统水分利用效率的影响

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摘要

Through 2–3-year (2003–2005) continuous eddy covariance measurements of carbon dioxide and water vapor fluxes, we examined the seasonal, inter-annual, and inter-ecosystem variations in the ecosystem-level water use efficiency (WUE, defined as the ratio of gross primary production, GPP, to evapotranspiration, ET) at four Chinese grassland ecosystems in the Qinghai-Tibet Plateau and North China. Representing the most prevalent grassland types in China, the four ecosystems are an alpine swamp meadow ecosystem, an alpine shrub-meadow ecosystem, an alpine meadow-steppe ecosystem, and a temperate steppe ecosystem, which illustrate a water availability gradient and thus provide us an opportunity to quantify environmental and biological controls on ecosystem WUE at different spatiotemporal scales. Seasonally, WUE tracked closely with GPP at the four ecosystems, being low at the beginning and the end of the growing seasons and high during the active periods of plant growth. Such consistent correspondence between WUE and GPP suggested that photosynthetic processes were the dominant regulator of the seasonal variations in WUE. Further investigation indicated that the regulations were mainly due to the effect of leaf area index (LAI) on carbon assimilation and on the ratio of transpiration to ET (T/ET). Besides, except for the swamp meadow, LAI also controlled the year-to-year and site-to-site variations in WUE in the same way, resulting in the years or sites with high productivity being accompanied by high WUE. The general good correlation between LAI and ecosystem WUE indicates that it may be possible to predict grassland ecosystem WUE simply with LAI. Our results also imply that climate change-induced shifts in vegetation structure, and consequently LAI may have a significant impact on the relationship between ecosystem carbon and water cycles in grasslands.
机译:通过对二氧化碳和水蒸气通量的2年至3年(2003年至2005年)的连续涡度协方差测量,我们研究了生态系统级用水效率(WUE,其定义为:季节,年际和生态系统之间的变化)。青藏高原和华北四个中国草地生态系统的初级生产总值(GPP)与蒸散量(ET)的比率。代表中国最普遍的草地类型,这四个生态系统是高山沼泽草甸生态系统,高山灌木草甸生态系统,高山草甸草原生态系统和温带草原生态系统,它们说明了水的可用量梯度,因此为我们提供了量化不同时空尺度上生态系统WUE的环境和生物控制的机会。 WUE通常在四个生态系统中与GPP密切跟踪,在生长季节的开始和结束时处于低水平,而在植物生长的活跃时期处于较高水平。 WUE和GPP之间的这种一致对应关系表明,光合作用过程是WUE季节变化的主要调节因子。进一步的研究表明,该法规主要是由于叶面积指数(LAI)对碳同化作用以及蒸腾与ET的比率(T / ET)的影响。此外,除了沼泽草甸外,LAI还以相同的方式控制WUE的逐年变化和站点之间的变化,从而导致高生产率的年份或站点伴随着较高的WUE。 LAI与生态系统WUE之间的总体良好相关性表明,仅使用LAI即可预测草地生态系统WUE。我们的结果还暗示,气候变化引起的植被结构变化,因此LAI可能会对草原生态系统碳与水循环之间的关系产生重大影响。

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