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。
2) 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.
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。
补充资料：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。
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