1) Weihe river
渭河
1.
Analysis on the characteristics of the nitrogen pollution in Weihe River;
渭河河水氮污染特征分析
2.
Study on Secondary Pollution Problem of Weihe River's Silt;
渭河泥沙二次污染问题研究
3.
The Characteristics of Water Environment in Shaanxi Sub-Basin of Weihe River;
渭河流域陕西片的水环境特性
2) Wei River
渭河
1.
Water Environment Changes of Wei River in Guanzhong Plain in Recent Years;
关中平原近十年来渭河水环境演变研究
2.
Water Environment Evolution in the Middle and Lower Reaches of Wei River in Recent 50 Years;
50年来渭河中下游水环境演变
3.
Speciality researching on water quality of the Jing River and the Wei River;
泾河和渭河的水质特征研究
3) the Weihe River
渭河
1.
Assessment of Water Quality and Methods of Controlling Water Pollution in the Weihe River of the Central Shaanxi Plain;
陕西关中段渭河水质评价及污染控制对策
2.
Analysis on "03·8" Flood of the Weihe River;
浅析渭河“3·8”洪灾成因
3.
Influence of water and sediment adjustment by Dongzhuang reservoir on the scour and sedimentation in the lower reach of the Weihe River and water level at Tongguan station;
东庄水库调水调沙对渭河下游和潼关高程冲淤作用的研究
4) Weihe
渭河
1.
Sensitivity analysis of the third bridge of Weihe in Xianyang;
咸阳渭河三号大桥敏感性分析
2.
Response of runoff to precipitation changes——Taking a case of Weihe;
河川径流对降水变化的响应研究——以渭河为例
3.
Study on the Effect of Atmospheric Correction in the Weihe River Quality Quantitative Retrieving of Remote Sensing
渭河定量遥感水质反演中的大气校正作用研究
5) Weihe River bed
渭河河道
1.
The landform evolution of Xianyang since the end of Qin Dynasty contains two aspects,the northward moving of the Weihe River bed and the changing of the edge slope of Xianyang tableland.
秦末以来,秦都咸阳地貌演变包括渭河河道北移和咸阳原边坡地貌变化两个方面。
6) lower Weihe River
渭河下游
1.
Auto-regulating function of channel of Lower Weihe River since 1960;
1960年以来渭河下游河道的自动调整作用
2.
Stable lowering of Tongguan bed elevation and comprehensive regulation of the lower Weihe River;
潼关高程的稳定降低与渭河下游河道综合治理
补充资料:渭河
| 渭河 黄河最大支流。位于中国陕西省中部。源出甘肃省渭源县鸟鼠山,东流横贯陕西省渭河平原,于潼关注入黄河。全长818千米,流域面积13.47万平方千米。由于地质构造上的原因,北岸支流源远流长,如葫芦河、千河、泾河、洛河等,这些河流流经黄土高原,洪枯流量相差悬殊,泥沙含量大,是渭河的主要来沙支流。南岸支流较短,主要有石头河、黑河、涝峪河、灞河。流经土石山区,比降较大,水流湍急,泥沙以推移质为主 。河源至宝鸡峡出口为上游 ,河道狭窄,川峡相间,水流湍急;宝鸡峡至咸阳铁桥为中游,河床宽浅,沙洲较多,水流分散,为游荡性河床;咸阳至潼关河口为下游,河道蜿蜒曲折,单股无汊。中、下游渠道纵横,有泾惠渠、渭惠渠、洛惠渠等灌溉工程。处干旱、半干旱地区,年均降水量450~700毫米。多年平均径流量105亿立方米。6~10月为汛期,多暴雨。其中7、8、9三个月的径流约占全年的60%~70%。流域水土流失严重,水土流失面积约占流域面积60%~70%。多年平均含沙量为53千克/立方米。多年平均输沙量5.58亿吨,占黄河年输沙量的34.9%。泥沙主要来自葫芦河、泾河和洛河。 |
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