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洪水限制了中国西北黑河流域下游河岸林的树木用水。

Flooding constrains tree water use of a riparian forest in the lower Heihe River Basin, Northwest China.

机构信息

Alax Desert Eco-hydrology Experimental Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; Key Laboratory of Eco-hydrology of Inland River Basin, Chinese Academy of Sciences, Lanzhou 730000, China.

Alax Desert Eco-hydrology Experimental Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; Key Laboratory of Eco-hydrology of Inland River Basin, Chinese Academy of Sciences, Lanzhou 730000, China.

出版信息

Sci Total Environ. 2021 Mar 15;760:144069. doi: 10.1016/j.scitotenv.2020.144069. Epub 2020 Dec 15.

Abstract

Riparian forests in floodplains are occasionally or regularly submerged by flooding. However, controversy exists regarding the effects of flooding on water use in riparian forests, and this controversy severely restricts our ability to better utilize limited water resources to restore damaged riparian forests in arid regions.The evapotranspiration (E) and transpiration (T) of riparian P. euphratica forests in the arid regions of northwestern China were determined using eddy covariance and sap flow technology across a 3-year period. Fortunately, the flooding introduced by ecological water diversion was occurred in 2014 and 2016 but not in 2015. Our results showed that the magnitude and seasonal pattern of E across 3 years was comparable (approximately 900 mm), but the T was higher in 2015 (431 mm) than in the other two years (288 mm in 2014 and 290 mm in 2016). The interannual patterns in the transpiration were consistent with the net ecosystem productivity at the site. Given the similar meteorological conditions (e.g. net radiation, temperature, relative humidity, and vapor pressure deficit) among the 3 years, two aspects may contributed to the suppressed tree water use and productivity under flooding: 1) the increased soil salinity reduce the roots water uptake from soil by increasing root water potential via osmotic adjustment; and 2) the depressed tree growth (e.g. the leaf area) via suspended water upward transport along soil-plant-atmosphere continuum. Although flooding is widely known beneficial for the regeneration, we suggest that it is not appropriate for the rejuvenation of phreatophyte (e.g., Populus spp.) in arid regions. Our results were drawn from only three years of measurement and therefore longer time series are needed to confirm or refine those conclusions.

摘要

中国西北干旱区河岸胡杨的蒸散量(E)和蒸腾量(T)采用涡度相关和 sap 流技术在 3 年时间跨度内进行了测定。幸运的是,生态调水引入的洪水仅在 2014 年和 2016 年发生,而在 2015 年并未发生。我们的结果表明,3 年的 E 大小和季节模式相当(约 900mm),但 2015 年的 T 较高(431mm),高于其他两年(2014 年为 288mm,2016 年为 290mm)。蒸腾的年际模式与该地点的净生态系统生产力一致。鉴于 3 年的气象条件相似(例如净辐射、温度、相对湿度和水汽压亏缺),有两个方面可能导致洪水下树木水分利用和生产力受到抑制:1)增加的土壤盐分通过渗透调节增加根水势从而减少了根系从土壤中吸收水分;2)沿土壤-植物-大气连续体向上输送的抑制树木生长(例如,叶面积)。尽管洪水被广泛认为对再生有益,但我们认为洪水并不适合干旱地区的潜水植物(例如杨树)的复壮。我们的结果仅来自 3 年的测量,因此需要更长的时间序列来确认或改进这些结论。

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