1) Minjiang River
岷江
1.
Edge effects of forest landscape in upper reaches of Minjiang River;
岷江上游森林景观边界效应
2.
Acquiring Scientific Outlook for Properly Developing Water Resources of Minjiang River;
树立科学发展观 合理开发岷江水资源
3.
Analysis on flood encounter of Jinsha river and Minjiang river;
金沙江、岷江洪水遭遇分析
2) Mingjiang River
岷江
1.
Long-term dynamics of dry valleys in the upper reaches of Mingjiang River,China;
岷江上游干旱河谷区域空间变化的定量判定
2.
Based on the actual inquiry data,the author study the distribution regularity of landslide in the Mingjiang River between Maowen and Wenchuan County,especially analysis the controlling factors such as the nature of rock and soil bodies,geological structure,and topographic features.
根据野外调查资料,研究了茂汶-汶川段岷江两岸滑坡的发育及分布规律,重点突出了控制滑坡发育的地层岩性、地质构造和地貌三大因素。
3.
The paper has calculated the real and design waste disposal amounts according to the survey of some hydro-power station in the upper reaches of Mingjiang River in July,2006,and got a loss to disposal ratio(LDR),that is,the ratio of loss to disposal in every waste disposal area.
根据2006年7月对岷江上游部分水电站弃渣场的调查,统计分析各渣场现有堆渣量与设计堆渣量的差值,从而得出各渣场流失量与堆渣量的比值,即为流弃比;分析流弃比产生的原因和组成,提出岷江上游地区以石料为主的临河型渣场流弃比取值范围,为以后该地区和其他类似地区的同类型渣场的水土流失预测提供参考。
3) Minjiang
岷江
1.
Simulation of Distributed Hydrological Cycle Model in Minjiang Upriver and Qingyijiang River Basin;
岷江中上游及青衣江流域分布式水循环模拟研究
2.
Land use pattern of Mao county in upper reaches of Minjiang;
岷江上游茂县土地利用格局
3.
This essay based on many examples and academic analyses of exploitation of Minjiang s upper reaches,wants to call on us to explore the hydroenergy with a scientific,reasonable and ordered method, and shows that the current exploitation situation of Minjiang s upper reaches should give us a warning and recollecting.
文章列举了岷江上游流域水能开发中的大量事例,呼吁应科学、合理、有序地开发利用河流水能资源,岷江上游流域水能资源的开发现状,应给人们以警醒和反思。
4) Min River
岷江
1.
Landscape pattern change in the upper valley of Min River;
岷江上游景观格局变化研究(英文)
2.
Analysis of Edge Influence's Affecting Factors in Min River upper Reaches' Landscape
岷江上游景观边界效应影响因子分析
3.
In this paper,there has been suggested a method of optimization for calculating longitudinal dispersity of natural river,and studied longitudinal dispersion of Jueqi section in Min River.
提出了计算天然河流纵向离散系数的最优化方法 ,并用此法对岷江蕨溪段的试验数据进行处理 ,计算出了该段河流的纵向离散系
5) Minjiang River Basin
岷江流域
1.
Surface Water Quality Assessment in Minjiang River Basin by Fuzzy Synthetic Evaluation Method;
岷江流域地表水水质的模糊综合评价
2.
Study on method for extraction of river network in Dujiangyan area within Minjiang River Basin based on GIS and DEM
基于GIS和DEM岷江流域都江堰区域河网水系的提取方法研究
3.
This article discusses the reasons for the Minjiang river basin s flood in the Qing Dynasty.
清代岷江流域洪灾发生的原因主要有自然因素和人为因素。
6) upper reaches of Minjiang River
岷江上游
1.
Analysis for Driving Force of Ecological Vulnerability at Upper Reaches of Minjiang River;
岷江上游生态脆弱性驱动力分析
2.
Effects of sub-watershed landscape patterns at the upper reaches of Minjiang River on soil erosion;
岷江上游小流域景观格局对土壤侵蚀过程的影响
3.
Dynamics and influence width of dry valley landscape boundary in upper reaches of Minjiang River;
岷江上游干旱河谷景观边界动态及其影响域
补充资料：岷江
| 岷江 长江上游支流。位于中国四川省中部。源出松潘县岷山南麓。岷江东源出弓杠岭，西源出郎架岭。两源于红桥关汇流后，自北向南流，经汶川县、乐山市、犍为县，于宜宾注入长江。干流长735千米，流域面积13.5万平方千米。支流多位于西岸，主要有黑水河、杂谷脑河、渔子溪、白沙河、大渡河、青衣江、马边河和越溪河等。岷江在都江堰市以上，河道穿行于崇山峻岭之间。由都江堰市进入都江堰灌区，河流分内、外两大水系，主流外江又称正南江。各河系到彭山江口复合，下至乐山市。乐山至宜宾为下游，两岸为低山起伏的丘陵区，水流平缓，河口附近有冲积阶地。流域降水丰富，多年平均径流深676毫米，年均径流量916亿立方米。5～10月为丰水期，6～9月为汛期，暴雨频繁，往往出现大洪水。11月～翌年4月为枯水期。河水含沙量较少，平均为0.2～1.0千克／立方米。多年平均输沙量4950万吨。都江堰市有著名的都江堰水利工程，灌溉成都平原。都江堰市以下可通航。 |
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