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Hydraulic lift in a Neotropical savanna: Experimental manipulation and model simulations

机译:新热带稀树草原的液压举升:实验操作和模型模拟

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The objective of this study was to assess the magnitude of hydraulic lift in Brazilian savannas (Cerrado) and to test the hypothesis that hydraulic lift by herbaceous plants contributes substantially to slowing the decline of water potential and water storage in the upper soil layers during the dry season. To this effect, field observations of soil water content and water potentials, an experimental manipulation, and model simulations, were used. Savannas of central Brazil exhibit consistent changes in tree density along shallow topographic gradients, from open savannas with relatively few trees in the lower portions of the topographic gradients to woodlands with a relatively high density of trees in the upper portions of the gradient. Herbaceous plant abundance follows the opposite trend. The diel recovery of soil water storage was higher in sites with more abundant herbaceous vegetation. Experimental removal of the above ground portion of herbaceous plants in a site with low tree density, during the dry season, substantially enhanced diel recovery of water potentials in the upper soil layers, consistent with the release of hydraulically lifted water from their shallow roots. In a site with high tree density, the release of hydraulically lifted water by woody plants contributed only 2% to the partial daily recovery of soil water storage, whereas the herbaceous layer contributed the remaining 98%. Non saturated water flow in the same savanna type contributed 8% to the partial daily recovery of soil water potential at the beginning of the dry season, decreasing to near 0% after 20 days of drought. During a 70-day rainless period the soil water potential dropped to 2.0MPa near the soil surface. The simulation model predicted that without hydraulic lift, water potential in the upper soil layers in relatively dense savannas would have dropped to 3.8MPa. The maximum contribution of hydraulic lift to the upper 100cm of soil was 0.7mmdayp# near the middle of the dry season. During the peak of the dry season, hydraulic lift can replace 23% of the ecosystem evapotranspiration in a site with high tree density and consequently greatly influences the water economy and other ecosystem processes in the Cerrado.
机译:这项研究的目的是评估巴西热带稀树草原(塞拉多)的水力提升幅度,并检验以下假设:在干旱期间,草本植物的水力提升极大地减缓了上层土壤中水势和储水量的下降。季节。为此,使用了土壤含水量和水势的实地观察,实验操作和模型模拟。巴西中部的热带稀树草原在浅层地形梯度上显示出一致的树木密度变化,从地形梯度下半部分树木稀少的开阔稀树草原到梯度上层树木密度相对较高的林地。草本植物的丰度则相反。在草本植物丰富的地区,土壤储水的diel回收率较高。在旱季期间,在树木密度低的地方实验性去除草本植物的地上部分,大大提高了上部土壤层中水势的diel回收,这与从浅根中释放水力提升的水相一致。在树木密度高的地方,木本植物释放水力提升的水仅对部分每日的土壤蓄水量贡献2%,而草本层贡献了其余的98%。在干旱季节开始时,相同稀树草原类型的非饱和水流量对土壤水势的部分日恢复量贡献了8%,在干旱20天后下降至接近0%。在70天的无雨期中,土壤表面附近的土壤水势降至2.0MPa。模拟模型预测,如果没有水力提升,则相对茂密的稀树草原上层土壤中的水势将降至3.8MPa。在旱季中期,水力提升对土壤上部100cm的最大贡献为0.7mmdayp#。在干旱季节的高峰期,水力提升可以代替树木密度高的地点的生态系统蒸散量的23%,因此极大地影响了塞拉多的水经济和其他生态系统过程。

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