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Analysis of infield rainwater harvesting and land use change impacts on the hydrologic cycle in the Wami River basin

机译:INFIELD雨水收获和土地利用变化影响对皖西河流域水文循环的影响

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The management of water resources in a river basin experiencing the expansion of agricultural activities requires a proper understanding of impacts on its hydrologic cycle. This study focused on the analysis of impacts of infield rainwater harvesting (IRWH) and future agricultural expansion as land and water uses change (LWUC) on the hydrologic cycle in the Wami River basin (Tanzania) using the Soil and Water Assessment Tool (SWAT). In the SWAT model, IRWH was implemented by fragmenting rainwater harvesting hydrological response units (HRUs) from cropland HRUs and assigning them as potholes for rainwater impoundment. LWUC was implemented by customizing land cover types and their corresponding model parameters in all original HRUs, and introducing projected water uses in the model. The study thus demonstrated the successful modelling of IRWH and land use change in the SWAT model using HRU fragmentation and customization approaches, respectively. The results indicated that IRWH applications in croplands led to a large increase in evapotranspiration (ET) and the soil water content, and a decrease in percolation, especially in the dry years. However, the average annual streamflow showed negligible changes when IRWH was implemented, even in 50% of current low-coverage croplands in the river basin. Thus, IRWH applications in the river basin are recommended. The results also indicated that LWUC caused huge changes in ET, the soil water content, percolation and the streamflow from the river basin. The average annual streamflow was predicted to decrease by 26% due to LWUC. However, land use change alone without projected water uses was predicted to cause a minor decrease of about 1% in the average annual streamflow. Therefore, further studies on the eco-hydrology of the river basin under various water use scenarios are recommended prior to the expansion of agricultural areas.
机译:河流流域水资源管理,经历农业活动扩张需要对其水文周期的影响进行适当的理解。本研究专注于infieD雨水收集(IRWH)和未来农业扩张的影响分析,因为陆地和水分使用土壤和水评估工具(SWAT)在瓦米河流域(坦桑尼亚)的水文周期上使用变化(LWUC) 。在SWAT模型中,IRWH通过从农田HRU的雨水收集水文反应单元(HRU)来实现,并将其分配为雨水蓄水池的坑洼。 LWUC是通过在所有原始HRU中定制土地覆盖类型及其相应的模型参数来实现,并在模型中引入投影用水。因此,研究表明,使用HRU碎片和定制方法分别使用HRU碎片和定制方法成功建模IRWH和SWAT模型中的土地利用变化。结果表明,农田中的IRWH应用导致蒸散(ET)和土壤含水量的大幅增加,渗透性降低,特别是在干燥年份。然而,当IRWH实施时,年平均年度流出表现出可忽略的变化,即使在河流域的当前低覆盖耕地中的50%中,也是如此。因此,建议使用河流域的IRWH应用。结果还表明,LWUC导致河流河流域的ET,土壤含水量,渗透和流出巨大变化。由于LWUC,预计平均年度流流量预计将减少26%。然而,预计单独的土地利用变化没有投影用水用途,在年平均年度流流量下会导致小幅下降约1%。因此,在扩建农业领域之前建议进一步研究在各种水域中河流盆地的生态水文。

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