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Water Yield Variation due to Forestry Change in the Head-Water Area of Heihe River Basin, Northwest China

机译:中国西北黑河流域水源地林业变化引起的水量变化

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摘要

Understanding the effects of forestation on the hydrological process is crucial to protecting water resources. In this study, the upstream Heihe River Basin is selected as the study area, which is the water source area of the whole basin. The grassland and forest are the main land use types, the proportion of which in the total land area is 21% and 50%, respectively. Firstly, a scenario of forestation was designed with the actual land cover data in 1980. Then a scenario with simulated land cover data in 1980 was established, in which the forest area increases by 12%. Thereafter a hydrological simulation was carried out with the actual and simulated land cover maps and the climate observation data during 1980-2010. The results suggested that the total water yield increased by 12.57 mm under the scenario with land use change during 1980-2010 compared with the simulation with the actual land cover in 1980. However, the results also indicated that the surface runoff reduced by 22.17 mm during the same period, indicating the forest land has "sponge" effects on the water resource in the mountainous watershed. These results may provide important information that supports operational practices, such as forest regeneration programs and watershed restoration.
机译:了解造林对水文过程的影响对于保护水资源至关重要。本研究以黑河流域上游为研究区域,即整个流域的水源地。草地和森林是主要的土地利用类型,占土地总面积的比例分别为21%和50%。首先以1980年的实际土地覆盖数据设计了一个造林情景,然后以1980年的模拟土地覆盖数据建立了一个情景,其中森林面积增加了12%。此后,利用实际和模拟的土地覆盖图以及1980-2010年期间的气候观测数据进行了水文模拟。结果表明,与1980年的实际土地覆被相比,在1980-2010年土地利用变化的情况下,总产水量增加了12.57mm。然而,结果还表明,在1980-2010年期间,地表径流减少了22.17mm。同一时期,表明林地对山区流域的水资源有“海绵”效应。这些结果可能提供支持操作实践的重要信息,例如森林更新计划和流域恢复。

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