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Simulated water balance of forest and farmland in the hill and gully region of the Loess Plateau in China.

机译:黄土高原丘陵沟壑区森林和农田模拟水平衡

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Large-scale vegetation establishment has not only helped to prevent serious soil and water loss on the Loess Plateau of China but also led to reduced water availability and soil desiccation. Examining the water balance of forested and farmed land allowed us to determine water consumption of vegetation and understand the mechanisms of soil desiccation, important factors for the sustainable conversion of farmland to forest in this area. The effects of forests and crops on the water balance within the soil-vegetation-atmosphere system were studied using a coupled water and heat flow model known as "CoupModel", which was calibrated on the basis of field measurements of soil water content, surface runoff, throughfall, stemflow, leaf area index, vegetation cover, canopy height and depth of root system in the hill and gully region of the Loess Plateau. Data were collected between 27 May 2006 and 31 October 2007. Two types of planted vegetation (acacia forest and farmland) in the Yan'gou watershed in the northern part of the Shaanxi Province were chosen to examine water transfer in the absence of soil texture (silt loam) differences and to explore the importance of vegetation type in relation to water balance. The simulations indicated that vegetation type and slope aspect significantly influenced the magnitude of every water balance component in the soil-vegetation-atmosphere system. Compared to forest, farming the land reduced interception (69.1-78.3%) and transpiration (37.3-40.4%), while increasing surface runoff by a factor of 5.0-40.2 and soil evaporation by 3.1-32.0%. Thus, farming resulted in 1.1-1.2 times more soil water storage than afforestation. Therefore, canopy interception and transpiration are responsible for soil desiccation in plantation forests. Simulation differences in water balance between acacia forest and farmland highlight that when converting farmland to forest on the Loess Plateau of China, tree species should be selected with care; this is particularly important on south-facing slopes.
机译:大规模的植被建设不仅有助于防止中国黄土高原水土流失的严重,而且还导致水利用量减少和土壤干燥。通过检查林地和耕地的水平衡,我们可以确定植被的耗水量并了解土壤干燥的机制,这是该地区农田可持续转化为森林的重要因素。利用被称为“ CoupModel”的水热耦合模型,研究了森林和农作物对土壤-植被-大气系统内水平衡的影响,该模型是根据土壤含水量,地表径流的现场测量结果进行校准的,通流,茎流,叶面积指数,植被覆盖度,黄土高原丘陵和沟壑区根系的冠层高度和深度。在2006年5月27日至2007年10月31日期间收集了数据。选择了陕西北部盐沟流域的两种种植植被(洋槐林和农田),以研究在没有土壤质地的情况下的水分转移(淤泥壤土)的差异,并探讨植被类型对水平衡的重要性。模拟表明,植被类型和坡度对土壤-植被-大气系统中每个水分平衡成分的大小都有很大影响。与森林相比,耕种土地减少了截留(69.1-78.3%)和蒸腾(37.3-40.4%),同时使地表径流增加了5.0-40.2倍,土壤蒸发增加了3.1-32.0%。因此,耕作导致的土壤蓄水量比造林多1.1-1.2倍。因此,林冠截留和蒸腾作用是人工林中土壤干燥的原因。相思林和农田之间水平衡的模拟差异表明,在中国黄土高原退耕还林时,应谨慎选择树种。这在朝南的斜坡上尤为重要。

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