1) Jinghe River
泾河
1.
The degradation characteristic of organic pollutants in the Jinghe River;
泾河下游可降解污染物的自净特征
2.
Discussion on Leakage in Calcareous Rock Dam Site of Dongzhuang Reservoir of Jinghe River;
论泾河东庄水库灰岩坝址渗漏问题
3.
Frequency combination method and its application in drought frequency analysis——A Case of Jinghe River;
频率组合法及其在干旱频率分析中的应用——以泾河流域干旱频率分析为例
2) Jing River
泾河
1.
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
2.
According to hydrographic data, the average runoff volume of Jing River (from 1932 to 1997)is only half of that of Wei River (from 1950 to 1997), but the suspended sediment of Jing River is 2.
泾河年均径流量仅为渭河的 1/2 倍(资料截止1997),输沙量却为渭河的 2。
3) Jinghe watershed
泾河流域
1.
Study on land-cover pattern of Jinghe watershed in Loess Plateau;
黄土高原泾河流域土地覆被格局研究
2.
Structure adjustment of regional water resources based on ecological water requirement of vegetation——A case study in Jinghe Watershed;
基于植被生态需水的区域水资源结构调整——以泾河流域为例
3.
Water Demand of Crop Plantation in Northwest China——A Case Study of the Jinghe Watershed.;
西北地区种植业需水分析——以泾河流域为例
4) Luojing Reach
罗泾河段
5) the lower reaches of the Jinghe river
泾河下游
1.
This paper puts forward some solutions to the serious disasters of landslides visiting the southern-bank of the lower reaches of the Jinghe river,which is based on an introduction to the characteristics of landslides,the classification of tableland slopes through calculating the stability coefficient,and a through analysis on the paroxysmal and short-term variable causes for landslides.
泾河下游南岸台塬边坡的滑坡灾害严重,本文中分析了滑坡的特征,通过计算边坡稳定性系数对台塬边坡进行了分类,对具有突发性和短期可变性的滑坡触发因素进行了分析,提出了滑坡治理的方法。
6) Jin river basin
泾河流域
1.
In the next place,on the basis of dynamic water balance simulation of Jin river basin based on the GRID,the natural water renewability .
其次,在基于GRID的泾河流域水量动态平衡模拟基础上,通过逐网格计算泾河流域1996年各月水资源自然更新率,来对泾河流域1996年水资源自然再生能力进行评价。
补充资料:泾河
泾河 黄河的三级支流。在中国陕西省中部。源出宁夏回族自治区南部六盘山东麓,有南北两源:南源出泾源县老龙潭,北源出固原大湾镇,两源流至甘肃省平凉市八里桥汇合,东南流经泾川,于杨家坪进入陕西长武县,东南流到高陵县陈家滩汇入渭河。全长455.1千米,流域面积4.54万平方千米。支流众多,主要有马莲河、蒲河、黑河、马拦河、泔河等。流域年平均降水量550毫米,主要集中在夏季。径流年内分配不均匀,洪、枯水流量相差悬殊,1933年8月5日张家山站最大洪水流量9200立方米/秒,1977年4月15日最小流量只有1.94立方米/秒。多年平均年径流量24.4亿立方米。流域内水土流失严重,年平均含沙量141千克/立方米,最大含沙量1430千克/立方米。古人说“泾浊渭清”,只从相对意义上说泾河含沙量比渭河含沙量高。中华人民共和国建立后,对泾河流域进行了治理、开发,上、中游修筑水库和开展大规模水土保持工作,下游开挖和扩建渠道工程。泾惠渠改建了渠首大坝,增加了引水量,扩大了下游灌溉面积。 |
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