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Response of Ecological Base Flow to Water and Sediment Dispatching in Irrigation Areas Along Water-Deficient and Sediment-Laden River

机译:缺水多沙河流域灌区生态基流对水沙调度的响应

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Ecological base flow is a basic requirement of water flow for a healthy river ecosystem. But in WeiheRiver the ecological flow is not guaranteed because of the water shortage, high sediment concentrationand considerable agricultural water use along the river. In this study, Baojixia under-tableland irrigationarea was selected as a representative area to which a mathematical model of one-dimensional steadywater non-uniform sediment regulation was applied, to analyse the impact of channel desilting onguaranteeing the ecological base flow of Weihe River. The results indicated that scouring and silting ofthe channel was significantly correlated with the channel water capacity and sediment content inwater flows. In addition, channel desilting contributed to 55.9×104m3 and 79.2×104m3 water saving inthe irrigation area in January and December which belonged to the dry season. Their contribution ratesto basic flow were 3.5% and 4.9%, respectively.
机译:生态基流是健康河流生态系统水流的基本要求。但是在渭河,由于缺水,高沉积物浓度和沿河大量农业用水,无法保证生态流量。本研究以宝鸡峡平原灌区为代表区域,应用一维稳态水非均匀性泥沙调节数学模型,分析河道淤积对保证渭河生态基流的影响。结果表明,河道冲刷和淤积与河道水容量和水流中的泥沙含量显着相关。此外,1月和12月属于干旱季节的灌区,河道淤积导致节水55.9×104m3和79.2×104m3。他们对基本流量的贡献率分别为3.5%和4.9%。

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