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1)  Zulihe River basin in Gansu
陇西祖厉河流域
2)  Zuli river basin
祖厉河流域
1.
Investigation of LUCC and ET in Zuli river basin of the loess plateau using remotely sensed data
基于遥感技术的祖厉河流域LUCC与蒸散发研究
2.
Analysis of the Precipitation Character and Changing Trend on Zuli River Basin
祖厉河流域降水特征及变化趋势分析
3)  Zuli River
祖厉河
1.
Fractal Dimension of the River Networks and Developing Stage of Drainage Geomorphic of Zuli River Basin;
祖厉河流域水系分维与地貌发育阶段浅析
2.
Influence of inter-basin water diversion project to runoff of Zuli River Basin;
跨流域引水工程对祖厉河流域径流的影响研究
3.
The Zuli River Basin is located in the central region of Gansu, belongs to a typical arid and semi-arid type of climate, its vegetation covered badly, holders of water weak, and main characteristics of dropping and raising sharply, rapid runoff in a short time.
祖厉河流域位于甘肃中部地区,属于典型干旱半干旱气候类型下的流域,流域内植被覆盖率差,持水能力弱,河流特性多以暴涨暴落、历时短、产流迅猛为主要特征。
4)  West Liaohe Basin
西辽河流域
1.
The land reclamation and its influence on environment in West Liaohe Basin from 1902 to 1990;
近百年来西辽河流域土地开垦及其对环境的影响
5)  West Liao river basin
西辽河流域
1.
Study on water resources rational allocation in West Liao River Basin
西辽河流域水资源合理配置研究
2.
But Qi Dan nation rose and established very strong Liao Dynasty in the west Liao river basin and controlled almost the north of China during 10 Century, thus left a lot of historical writings(historical books and travels) and ruins.
西辽河流域在辽代早期和辽代之前 ,是自然环境较好的“辽泽”,其自然景观为面积广大的平沙地 ,其上生长乔木、灌木和草本 ,为疏林草原 ,还有较大面积的下湿地和较多湖泊 ,没有出现流动沙丘。
6)  Moxi river
磨西河流域
1.
On the basis of field investigation and former researches,35 typical debris flow gullies were found out,which threat the local residents,vistors,farmlands,electric power stations,water resource facilities,roads,cableways and other tourism equiments along Moxi river,Sichuan province,Southwest China.
在实地调查和前人研究的基础上,查明了贡嘎山东坡磨西河流域内泥石流沟的分布状况、暴发规律及危害特征等;并根据近20年来流域内发生的典型泥石流灾害,分析了泥石流发生前的降雨过程,发现磨西河流域内泥石流发生的当日雨量和前6 d有效雨量之间具有明显的幂函数关系,据此以泥石流发生的当日雨量和前6 d有效雨量为指标,初步探讨了磨西河流域内泥石流暴发的雨量值。
补充资料:祖厉河
祖厉河

    黄河上游支流。位于中国甘肃省中部,兰州市东侧。源出会宁县南华家岭。北流经会宁县、清远县入黄河。因流域地层含盐碱较多,水味苦咸,故又称苦水河。河水含沙量较高。
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