1) Shiquan River
![点击朗读](/dictall/images/read.gif)
狮泉河
1.
The climate changing trend and prediction in Northwest Tibet represented by the Shiquan River meteorological station;
西藏西北高原气候变化趋势及预测——以狮泉河站为例
2.
The Shiquan River ophiolitic mélange zone in Xizang: The delineation and significance of a new archipelagic are-basin system;
西藏狮泉河蛇绿混杂岩带——一个新的多岛弧盆系统的厘定及意义
3.
Aquatic Biotic Resources and Biology of S.stoliczkai Stoliczkai Steindachner in Shiquan River;
狮泉河水生生物资源和高原裸裂尻鱼的生物学研究
2) Shiquanhe basin
![点击朗读](/dictall/images/read.gif)
狮泉河盆地
1.
Cause of wind-blown sand disaster in Shiquanhe Basin and its control;
![点击朗读](/dictall/images/read.gif)
狮泉河盆地风沙灾害成因及其防治
2.
The paper, according to its natural, economic conditions and features of wind-sand, works out a set of comprehensive plan for controlling wind-sand in Shiquanhe basin composed of mechanical, biological and assistant measures.
根据狮泉河盆地自然、社会经济条件和风沙灾害特点,制定了由机械措施、生物措施和辅助措施组成的综合整治方案。
3) The Shiquanhe Valley
![点击朗读](/dictall/images/read.gif)
狮泉河谷地
4) Shiquanhe wide valley
![点击朗读](/dictall/images/read.gif)
狮泉河宽谷
1.
The desertification of the Shiquanhe wide valley occurs on the background of environmental degradation of the Qinghai─Xizang plateau and is strengthened with manmade irrational use of natural resources.
狮泉河宽谷区的荒漠化过程以整个青藏高原的环境演变为背景,受人为的资源利用不合理而强化。
5) Shiquanhe Hydropower Station
![点击朗读](/dictall/images/read.gif)
狮泉河水电站
1.
Experiment on relationship between maximum dry density and grain size composition for mixing material of earth-rock fill dam with clay core of Shiquanhe Hydropower Station;
狮泉河水电站粘土心墙土石坝掺合料最大干密度及颗分关系试验
2.
Quality Control of Installation and Welding of the Spiral Case (Stay Ring) of Shiquanhe Hydropower Station;
狮泉河水电站蜗壳(座环)安装焊接质量控制
3.
Optimization Adjustment on the Unit Number and Capacity of Shiquanhe Hydropower Station;
![点击朗读](/dictall/images/read.gif)
狮泉河水电站机组台数及单机容量优化调整
6) Yecheng-Shiquanhe area
![点击朗读](/dictall/images/read.gif)
叶城-狮泉河地区
补充资料:狮泉河
狮泉河 在中国西藏自治区西部。 藏语称“森格藏布”,意为“狮口河”。源出冈底斯山主峰冈仁波齐峰北部的森格喀巴林附近,源头海拔5164米,西流在扎西岗附近与噶尔藏布汇合后,向西北流出国境后,改称印度河。在中国境内河长430千米,流域面积2.75万平方千米。地处西藏干燥地区,流域年平均径流深仅25毫米,水系不发育,主要支流有生拉藏布、公前河、赤左藏布、婆肉共河、朗久河、噶尔藏布等。河流除接受雨水和冰雪融水补给外,地下水补给量占比例很大,约占年径流量的67%。径流的年内分配和年际变化比较稳定。河水温度低,年平均水温3℃,河流结冰期长,一般于10月底出现岸冰,至翌年4月的中、下旬才完全消融,其中12月至翌年2月河流还出现封冻现象。
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