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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Effects of vegetation and slope aspect on water budget in the hill and gully region of the Loess Plateau of China.
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Effects of vegetation and slope aspect on water budget in the hill and gully region of the Loess Plateau of China.

机译:黄土高原丘陵沟壑区植被和坡向对水量的影响

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Precipitation, throughfall, stemflow and soil water content were measured, and interception, transpiration, evaporation, runoff, deep percolation and soil water recharge were estimated in the natural Liaotung Oak (Quercus liaotungensis) and regrown Black Locust (Robinia pseudoacacia) forestlands in the hill and gully region of the China Loess Plateau. Four stands (south- and north-facing slopes) of two forests were studied between May 27, 2006 and October 31, 2007. Hydrological fluxes were calculated using a coupled water and heat flow model called CoupModel. Throughfall, stemflow and soil water content were used to calibrate the model. The simulations indicated that, interception, vegetation transpiration and soil water evaporation were the main components of water consumption in the 4 stands, accounting for about 90% of the precipitation. The simulated interception and vegetation transpiration in the south-facing slope (154 and 327 mm in regrown forestland and 173 and 338 mm in natural forestland) were lower than those in the north-facing slope (219 and 344 mm in regrown forestland and 203 and 342 mm in natural forestland). Soil water evaporation in the south-facing slope (416 mm in regrown forestland and 373 mm in natural forestland) was larger than that in the north-facing slope (325 mm in regrown forestland and 330 mm in natural forestland) in the same vegetation stands. This was mainly due to greater vegetation density in the north-facing slope than in the south-facing slope. For the regrown forestlands, the simulated soil water recharge was larger under north-facing slope stands (90 mm) than under south-facing slope stands (76 mm), and the natural forestland in the north-facing slope had the largest soil water recharge (104 mm). The results indicated that vegetation species and slope aspects significantly influenced the water balance budget in the soil-vegetation-atmosphere system. The water budget differences among the 4 stands indicate that care is required for properly selecting regrown tree-species. Soil and water conservation measures must be applied scientifically when converting farmland to forest in the Loess Plateau of China, especially on the south-facing slopes.
机译:测量了天然辽东栎(辽栎栎)和再生长黑刺槐(刺槐)的截留,穿透,茎流和土壤水分,并估计了其截留,蒸腾,蒸发,径流,深层渗滤和土壤水分补给。黄土高原丘陵沟壑区的 Robinia pseudoacacia )林地。在2006年5月27日至2007年10月31日之间研究了两种森林的四个林分(南坡和北坡)。使用称为CoupModel的水和热流耦合模型计算水文通量。使用穿透力,茎流和土壤含水量来校准模型。模拟结果表明,截留,植被蒸腾和土壤水分蒸发是这4个林分耗水量的主要组成部分,约占降水量的90%。南坡(再生林地分别为154和327毫米,天然林分别为173和338毫米)的模拟截留量和植被蒸腾量低于北坡(再生林地分别为219和344毫米,203和203毫米)。 342毫米(天然林地)。在相同植被中,南坡(再生林地416毫米,天然林地373毫米)的土壤水分蒸发大于北坡(再生林地325毫米,自然林地330毫米)。 。这主要是由于北坡比南坡更大的植被密度。对于再生林,在北坡(90 mm)下模拟的土壤水补给比在南坡(76 mm)下的更大,并且北坡的天然林地的土壤补给量最大。 (104毫米)。结果表明,植被-坡度在土壤-植被-大气系统中显着影响水量平衡。 4个林分之间的水预算差异表明,需要谨慎选择正确生长的树种。黄土高原尤其是南坡耕地退耕还林必须科学地采取水土保持措施。

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