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首页> 外文期刊>Bosque (Valdivia) >Estudio comparativo de los componentes del balance hídrico en un bosque nativo y una pradera en el sur de Chile
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Estudio comparativo de los componentes del balance hídrico en un bosque nativo y una pradera en el sur de Chile

机译:智利南部原生森林和草地水平衡成分的比较研究

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摘要

A comparative study of water balance was conducted in a roble-olivillo forest and a natural meadow in southern Chile. We analysed the different components of precipitation redistribution, evapotranspiration, percolation and changes in soil water content until 3 m of depth. As related to a total precipitation of 3,024 mm, evapotranspiration and percolation were 13% and 87% for the meadow, and 33% and 66% for the forest respectively. Soil water reserves varied down to 300 cm of depth in the soil of the forest while in the meadow this situation was recorded only to a depth of 1 m. It can be concluded that higher water consumption in the forest and higher percolation water in the meadow were ascribed mainly to the difference in development of both root systems and the canopy characteristic of each of these vegetation covers
机译:在智利南部的一片橄榄绿森林和天然草地中进行了水平衡的比较研究。我们分析了降水再分配,蒸散,渗流和土壤含水量变化直至3 m深度的不同组成部分。与3,024 mm的总降水量相关,草甸的蒸散量和渗滤量分别为13%和87%,森林的分别为33%和66%。森林土壤中的土壤水储量变化到300厘米深,而在草地上,这种情况仅记录到1 m深度。可以得出结论,森林中较高的耗水量和草甸中较高的渗滤水主要归因于根系发育的差异以及每种植被覆盖的冠层特性

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