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1)  Jingjiang Flood Diversion District
荆江分蓄洪区
1.
Historic evolution perspective and flood risk management of the Jingjiang Flood Diversion District in the Yangtze River Basin;
长江荆江分蓄洪区历史演变、前景和风险管理
2)  Jingjiang flood diversion district
荆江分洪区
1.
0 was introduced,and the slope and aspect were analyzed of the DEM of the Jingjiang flood diversion district.
0来构建DEM的方法,并对生成的荆江分洪区DEM进行了坡度分析。
3)  diversion of floodwater in Jingjiang Area
荆江分洪
4)  flood diversion and storage areas
分蓄洪区
1.
In 1950 s, we have founded 14 flood diversion and storage areas in the middle reach of the Yangtze River,in which,Jingjiang,Honghu,and Dujiatai are the three most important flood diversion and storage areas.
分蓄洪区是平原防洪的一种重要措施。
5)  flood diversion area
分蓄洪区
1.
Improvement of boundary treatment in mathematical model of flood diversion area;
分蓄洪区数学模型中边界处理的改进
2.
Analysis of effect of application of Honghu flood diversion area on lowering water level of the Yangtze River
洪湖分蓄洪区启用对降低长江水位效果分析
3.
Based on this,a plane 2-D water mathematical model for the flood diversion area is set up.
在此基础上,建立了平面二维水流数学模型,并将该模型运用到湖北龙骨湖、沉底湖分蓄洪区实际计算中,取得了令人满意的结果。
6)  flood diversion and detention area
分蓄洪区
1.
Numerical simulation of canals boundary in flood diversion and detention area
分蓄洪区内河渠边界模拟方法
2.
Numerical simulation of flood evolution in flood diversion and detention area with well-shaped canals
含井字形河渠的分蓄洪区洪水演进数值模拟
补充资料:荆江
荆江

    长江自中国湖北省枝城市到湖南省城陵矶段的别称。长约430千米,因属于古代的荆江而得名。有上荆江和下荆江之分 。上荆江(枝城—藕池口),河道比较稳定 ;下荆江(藕池口—城陵矶),河道蜿蜒曲折,素有九曲回肠之称。荆江北岸是江汉平原,南岸是洞庭湖平原,地势低洼,由于荆江河道弯曲,洪水宣泄不畅,故极易溃堤成灾,有“万里长江,险在荆江”之说。为了抗御洪水,历代在荆江北岸修筑有荆江大堤。
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