1) Jinsha River
金沙江
1.
Impacts of Benzilan-Ahai Reach Exploitation Scheme on Ecology and Environment in Jinsha River;
金沙江奔子栏-阿海河段开发方案对生态环境的影响
2.
Study on Eco-construction in Dry-warm Valley in Deqin Section of Lancang River & Jinsha River;
澜沧江、金沙江云南德钦段干暖河谷区生态建设探讨
3.
Water Quality of Lower Reaches of Jinsha River;
金沙江下游水质现状调查及研究
2) Jinshajiang river
金沙江
1.
Genetic analysis and stability assessment of a landslide in a reservoir area of Jinshajiang River;
金沙江某库区东爷庙滑坡成因分析及稳定性评价
2.
Study on Long-term Optimal Operation of Cascade Hydropower Plants on The Jinshajiang River;
金沙江梯级水电站发电长期优化调度研究
3.
Landslide interpretation of remote sensing images in the dry-hot valley of Jinshajiang River;
金沙江干热河谷区滑坡遥感解译研究
3) Jinshajiang
金沙江
1.
Speeding up the development of the Jinshajiang river is a strategic choice to balance energy;
加快金沙江开发是一次能源平衡的战略选择
2.
First Exploration on Transmitting Water Power of Jinshajiang River to Eastern China;
金沙江水电东送华东电网初探
3.
SHRIMP Dating of Carbpniferous Jinshajiang Ophiolite in Western Yunnan and Sichuan: Geochronological Constraints on the Evolution of the Paleo-Tethys Oceanic Crust;
滇川西部金沙江石炭纪蛇绿岩SHRIMP测年:古特提斯洋壳演化的同位素年代学制约
4) the Jinsha River
金沙江
1.
There is a bank slope of non-matrix structure at the site of a projected hydroelectric dam in the middle reaches of the Jinsha River.
金沙江中游某拟定水电站坝址区下游存在一非基质结构岸坡,覆盖层厚度巨大,以白云质角砾堆积层为主。
2.
The Jinsha River is a main sediment source of the upper Yangtze River.
金沙江是长江上游河流泥沙的主要来源。
5) the Jinshajiang River
金沙江
1.
Features of deformation and failure of bank slopes in hydroelectric development zone of the Jinshajiang River;
金沙江下游水电工程区岸坡变形破坏基本特征
2.
Evaluation and forecast of bank slopes stability from Yibin to Baihetan of the reaches of the Jinshajiang River;
金沙江下游宜宾—白鹤滩段岸坡稳定性评价与预测
3.
The chemical compositions,fiber morphology and physical pulping characteristics of Broussonetia papyrifera bark produced in dry-hot valley of the Jinshajiang River were analyzed.
对金沙江干热河谷区构树韧皮纤维的化学组成、纤维形态和成浆物理性能进行了分析,结果表明:构树韧皮的木素含量低,纤维素含量较高,达43。
6) old Jingsha River
古金沙江
补充资料:金沙江
金沙江 长江上游从中国青海省玉树县巴塘河口到四川省宜宾市岷江口的一段。金沙江古名神川、丽水、绳水,因江中产沙金,故名。是长江干流段中最长的一段,长2920千米。流域面积35.5万平方千米。支流众多,主要支流有无量河、雅砻江、普渡河、牛拦江、横江等。干流穿流在川、藏边境沙鲁里山和宁静山间,到云南省丽江纳西族自治县的石鼓以后 ,急转东北流,至无量河口,江流深切高原,形成谷深达3000米以上的虎跳峡,两岸悬崖飞瀑,水流湍急。从无量河口折向东南,到梓里以后,顺流东下。金沙江流域内97%属于山区,区内山川纵横,峰峻谷深,江中险滩栉比,礁石林立 。水量丰沛,多年平均径流量1455亿立方米(屏山站),年际变化小。落差3000余米,水力资源极为丰富,理论蕴藏量达1.1亿多千瓦,可能开发量为 8897万千瓦,约占整个长江流域水电资源的42%,约占全国的1/6。 |
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