1) flood of the uncontrolled intervening area
区间洪水
1.
Meanwhile, the effect of flood of the uncontrolled intervening area is illuminated in this paper.
针对北江中下游流域的特点的复杂性,建立了以水力学方法为主的河网一维及对无资料区间采用水文学方法为辅的洪水计算耦合模型,同时说明了区间洪水的作用。
2.
According to the complex flooding characteristics of the Feilaixia reservoir basin, a flood routine model is established throngh coupling the Xin anjiang model(3 components ) and unsteady flow numerical computation model with this coupling model,the effect of flood of the uncontrolled intervening area is illuminated.
在分析北江流域暴雨洪水特性的基础上,针对飞来峡水库流域洪水的特点和复杂性,采用水文学和水力学相结合的方法,构建了飞来峡水库入库洪水计算的耦合模型,整个模型由区间洪水计算的流域水文模型和河网水力学数学模型组成,模型的计算结果表明,洪水模拟与实测过程拟合较好,精度较高。
3) regional flood
区域洪水
1.
Application of L-moments in the regional flood frequency analysis;
L-矩在区域洪水频率分析中的应用
4) Hongshuihe irrigation district
洪水河灌区
1.
Taking indigowoad root as an example,irrigation forecast suitable for indigowoad root was conducted according to the historical data in Hongshuihe irrigation district.
从节水灌溉的基本原理着手,运用农田水量平衡原理,以板蓝根灌区为例、洪水河灌区益民灌溉试验站多年试验资料为依据,作出适合当地板蓝根的灌溉预报。
6) flood pumping gathering ground
抽洪集水区
补充资料：河道洪水演进(见河道洪水演算法)
河道洪水演进(见河道洪水演算法)
neaao non郎hUi河道洪水演进yanJ县n 见河道洪水演算法。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条