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Comparison of runoff generation methods for land use impact assessment using the SWAT model in humid tropics

机译:利用SWAT模型在潮湿热带中使用SWAT模型的土地利用影响评估的比较

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摘要

Hydrological responses due to deforestation in a humid tropical catchment were analyzed using two runoff generation methods available in the Soil Water Assessment Tool (SWAT) model: the Curve Number (CN) and the Green-Ampt (GA) methods. The calibrated model, which performed well in simulating runoff under present land use condition in the Batanghari River Basin, Indonesia (42,960?kmsup2/sup), was then used to simulate runoff using past and future land use scenarios. Simulations showed similar changes in the annual water budget: decreasing evaporation and increasing total discharge. However, the two methods showed opposite changes in flow regimes: high flow increased (13%) under the CN while low flow increased (27%) under the GA. These results are associated with differences in runoff generation mechanisms, where surface runoff contributes to total discharge to a much larger extent under the CN (43%) than the GA (4%). Land use changes caused a reduction in infiltration rate, leading to higher high flow under the CN, while high flow did not change under the GA. Instead, lower evapotranspiration increased groundwater flow under the GA, and thus the steady low flow increased. This study suggests that the runoff generation method should be selected carefully based on the dominant flow pathway of a catchment, particularly for land use impact studies in the humid tropics.
机译:使用土壤水分评估工具(SWAT)模型中可用的两种径流发电方法分析了由于潮湿的热带集水区中的砍伐热带集水区的水文反应:曲线数(CN)和绿色AMPT(GA)方法。校准模型,在印度尼西亚邦康汉里河流域的当前土地使用条件下进行了良好的模型(42,960?Km 2 ),用于使用过去和未来的土地使用场景模拟径流。模拟显示年度水预算中的类似变化:蒸发量减少,总放电增加。然而,这两种方法显示出流量制度的相反变化:在CN下的高流量增加(13%),而GA下的低流量增加(27%)。这些结果与径流产生机制的差异有关,其中表面径流在比GA(4%)下的CN(43%)下的总排出量大得多。土地利用变化导致渗透率降低,导致CN下的高流量,而高流量在GA下没有变化。相反,较低的蒸发量增加了Ga下的地下水流,因此增加了稳定的低流量。本研究表明,应根据集水机会的主要流动途径仔细选择径流发电方法,特别是对于潮湿的热带地区的土地利用影响研究。

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