黄河中游,the middle Yellow River
1)the middle Yellow River黄河中游
1.Study on the relation of frequency between flood and sediment in the Middle Yellow River;黄河中游水沙频率关系研究
2.Interactions of environmental factors on sediment yield in the region of the middle Yellow River basin;黄河中游环境要素对流域产沙影响的交互作用
3.The paper analyzes the main characteristics of geological environment,including the characteristics of physical geography,soil and rock that easy to be eroded and landforms of soil and rock erosion of the middle Yellow River through investigation and study on geological environment of soil and rock erosion and erosion genre.通过岩土侵蚀地质环境条件及侵蚀类型调查研究,分析了黄河中游岩土侵蚀的主要地质环境特征,包括自然地理特征、易侵蚀岩土特征、地貌特征等。
英文短句/例句

1.Comparative Study on Prehistorical Cities between in Middle Yangtze River Region and Middle Yellow River Region;长江中游与黄河中游史前城址的比较
2.Formation and Evolution of the Middle Reaches of the Yellow River Since Late Cenozoic黄河中游晚新生代地貌演化与黄河发育
3.Status of Three Provinces in the Middle Reach of the Yellow River in the Great Western Development Campaign;黄河中游三省区在西部开发中的地位
4.Summary of Experiment at Pilot Point of Key Projects for Gully Control in Middle Yellow River黄河中游治沟骨干工程试点工作总结
5.Research on Runoff and Sediment Model in the Middle Yellow River Region Based on GIS;基于GIS的黄河中游水沙模型研究
6.Analysis on Characteristic of Precipitation and Variation Tendency of the Middle Yellow Rive黄河中游降水量特征及变化趋势分析
7.Characteristics of Climate Change in "Sanhuajian" Area in the Middle Reaches of Yellow River黄河中游“三花间”区气候变化特征
8.Climatic Variations in the Middle Reaches of the Yellow River during the Historical Period历史时期黄河中游流域气候变迁研究
9.Composition and Physical Nature of Loess in the Middle Reach of the Yellow River黄河中游地区黄土成份及物理力学性质研究
10.Estimate Model for Sediment Transport Process of Dali River Region on the Middle Reaches of the Huanghe River黄河中游大理河地区输沙过程的估算模式
11.Regional Evapotranspiration Estimation in Hekou-Longmen Section of the Middle Reaches of the Yellow River黄河中游河口—龙门区间陆面年蒸散量估算
12.Analysis of Variation of Water and Sediment Yield in Different Source Areas and Its Effect on Fluvial Response in Lower Yellow River黄河中游不同区来水来沙变化与下游河道演变的响应分析
13.The Origin of Neogene's Red Clay in the Middle Reaches of Yellow River;中国黄河中游地区新近纪红粘土的成因
14.Study on Treatment Direction of Coarse Sand Area in Middle Reaches of Yellow River;黄河中游粗泥沙集中来源区治理方向研究
15.Report of study on constructing terraced field by machinery in middle reaches of the Yellow River黄河中游地区机械修梯田协作研究报告
16.Application of Flow Path Equation of Winding Bend to the River Training Works on the Lower Yellow River河湾流路方程在黄河下游河道整治中的应用
17.Millet is cultivated in the middle or lower reaches of the Yellow River.在黄河中下游地区,人们种植谷子。
18.The Qiang originally lived along the middle and upper reaches of the Yellow River.羌人,最初活动于黄河中上游地区。
相关短句/例句

the middle reaches of the Yellow River黄河中游
1.Sediment yield and delivery in the middle reaches of the Yellow River basin, especially at the loess hill and gully areas, is a primary cause of rapid bed accretion at the lower reaches of the Yellow River.黄河中游,尤其是以黄土丘陵沟壑区为代表的那些多沙区的侵蚀产沙是引起黄河下游河道严重淤积的主要原因。
2.There have been abundant research results on sediment variation in the middle reaches of the Yellow river.自 2 0世纪 80年代起 ,有关黄河中游地区泥沙变化的研究已取得了丰富的成果。
3)middle reaches of the Yellow River黄河中游
1.Environmental change and disasters in middle reaches of the Yellow River in history:influence on migration and development of capital;古代黄河中游的环境变化和灾害——对都城迁移发展的影响
2.Formation mechanism of interior drainage areas and closed drainage areas of the Ordos Plateau in the middle reaches of the Yellow River, China based on an analysis of the water cycle;黄河中游鄂尔多斯高原内流区与闭流区的形成机理——基于水循环的分析
3. A review over the environmental aquatic chemistry in the middle reaches of the Yellow River on the selected aspects,including apparent complexation capacity,conditional stability constants,liquidsolid distribution, the ion exchange pH range and isotherms.综述了黄河中游水质化学若干问题的研究动态,例如,表观络合容量,条件稳定常数,液-固分配作用,离子交换pH范围和等温线。
4)middle reaches of Yellow River黄河中游
1.Definition on source area of centralized coarse sediment in middle reaches of Yellow River with method of marginal analysis;用边际分析法确定黄河中游粗泥沙集中来源区
2.Effect of soil-retaining dams on flood and sediment reduction in middle reaches of Yellow River;黄河中游地区淤地坝减洪减沙及减蚀作用研究
3.The analysis of precipitation distribution & change of Shan-Shan sector in middle reaches of Yellow River in recent 50years;黄河中游山陕区间近50a降水分布特征及其变化特点分析
5)the middle reaches of Yellow River黄河中游
1.Analysis of the rainstorm and flood in Fugu at "July 30.2003"of the middle reaches of Yellow River;黄河中游府谷“2003.07.30”暴雨洪水分析
2.On the Establishing Time of the Early China in the Middle Reaches of Yellow River According to Shiji·Wudi Benji;读《史记·五帝本纪》论黄河中游早期国家形成的时间
3.The periodicity and encounter probabilities of midsummer drought in the middle reaches of Yellow River were analyzed using the methods of maximumentropy spectrumanalysis and wavelet analysis according the midsummer drought index of the middle reaches of Yellow River and its sections from 1955 to 2002.本文利用黄河中游及其分区1955~2002年盛夏干旱指数资料,采用最大熵谱分析和小波分析方法,对黄河中游盛夏干旱变化的周期性特点和各分区不同干旱等级之间的遭遇概率进行了统计分析。
6)the upper and middle Yellow River黄河中上游
延伸阅读

黄河中游水电规划黄河中游水电规划hydropower resources of Huanghe (Yellow) river system  Huong He shu一x一shu一neng zlyuon黄河水系水能资源[hydropower resourees ofHuanghe(Yellow)river system〕据1950年《中华人民共和国水力资源普查成果》统计,黄河水系水能资源理论蕴藏量为3552亿kw·h/a,其中技术可开发资源117。亿kw·h/a。黄河水系水能资涯t占中国比重仅为6%.水系内部干支流水能资源t的分布见表。黄河水系可能开发水能资派统计衰┌─────┬───┬────┬──┬──┬───┬──────┬─────────────┐│河流名称 │流城 │多年平均│河道│落差│利用 │ 理论魏藏t │可能开发资娜 ││ │面积 │流t │长度│(m) │水头 │(亿kw·h/a) ├──┬────┬─────┤│ │(kmZ) │ (m3/s)│(km)│ │(m) │ │电站│装机容t │ 年发电t ││ │ │ │ │ │ │ │厘数│ (MW) │(亿kw·h) │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│黄河全水系│ │ │ │ │ │3552 │4 15│28003 │1 170 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│其中:干流 │752443│1744.5 │5464│4830│3012 │2607.5 │43 │25136 │1037 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│流河流城 │25527 │163 │673 │2631│ │126.8 │l4 │594 │34。4 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│大通河流域│15130 │92。3 │558 │2793│884 │101.7 │1l │541 │28.1 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│渭河流域 │134766│324 │818 │2905│80。7 │75.1 │10 │93 │3。9 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│其他支流 │ │ │ │ │ │640.9 │337 │1 639 │66.6 │└─────┴───┴────┴──┴──┴───┴──────┴──┴────┴─────┘注:资料来源为1980年《中华人民共和国水力资琢普查成果》。 黄河干流全长5464 km,流经青海、四川、甘肃、宁夏、内蒙古、陕西、山西、河南、山东等省(自治区),注人渤海。