1) Lilium regale Wilson
岷江百合
1.
Phenotypic Variation of Natural Populations in Lilium regale Wilson;
岷江百合天然群体的表型多样性
2.
Study on Morphology Diversity in Lilium regale Wilson;
岷江百合的形态多样性研究
3.
An experiment was conducted to analyze the phenotypic diversities in terms of 6 phenotypic traits(height of plant ,length of petal,number of leaf,number of flowers ,length of leaf and width of leaf)using 7 natural populations of Lilium regale Wilson.
以岷江百合的7个天然群体为研究对象,对其反映主要形态特征的株高、花瓣长、叶片数、花朵数、叶片长和叶片宽等6个表型性状进行多样性分析。
2) Lilium regale
岷江百合
1.
Optimization of ISSR-PCR Reaction System for Lilium regale;
岷江百合ISSR-PCR反应体系的优化
2.
Study on the Seed Germination of Lilium regale;
岷江百合种子萌发的研究
3.
Establishment of Rapid Propagation System for Lilium regale in vitro
岷江百合离体培养快繁体系建立
3) Lilium regale
岷江百合(Lilium regale)
1.
The regeneration of salt - tolerant callus of Lilium regale was studied.
本文研究了岷江百合(Lilium regale)耐盐愈伤组织的再生过程。
4) 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
5) 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
6) 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。
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。 |
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