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1)  second-order terrace of Qinhe river
沁河二级阶地
1.
The mineral water is located on the second-order terrace of Qinhe river in the westernpart of Qinshui basin.
沁水孔必轩矿泉水位于沁水盆地西部沁河二级阶地上。
2)  secondary bench of Yellow River
黄河二级阶地
3)  second terrace
二级阶地
1.
Origin of the second terraces in the Huangshui drainage area,Qinghai,China,studied based on sporopollen records.;
依据孢粉记录初探青海湟水流域二级阶地的成因
2.
<Abstrcat>Through the field research of landform and cultural sites in Guanting basin of the upper reaches of the Yellow River in Qinghai Province, the authors analyzed the structure of the second terrace of Guanting basin and concluded that the second terrace came into being in middle Holocene.
通过对黄河上游官亭盆地地貌及古文化遗址的野外考察,分析了盆地中黄河二级阶地的结构,认为该阶地形成于全新世中期。
4)  The third terrace of Huanghe river
黄河三级阶地
5)  The fifth terrace of Yellow River
黄河第五级阶地
6)  Qinhe River
沁河
1.
Ecological Investigation of Freshwater Crab and River Pollution in Basin of Qinhe River;
山西沁河流域溪蟹生态调查及河流污染现状
2.
Evaluation on the Present Situation of Water Quality and Pollution Analysis of Qinhe River s Shanxi Section;
沁河山西段水质现状评价与污染分析
3.
Evaluation on the Water Quality of Qinhe River’s Jincheng Section with the Gray Relative Analysis Method;
沁河晋城段水质灰色关联分析
补充资料:沁河
沁河

    中国黄河下游支流。源出晋东南沁源县北太岳山东麓。南流切太行山地,经安泽县,穿阳城盆地,继续南行,进入河南省纳丹河  ,在武陟县詹店附近注入黄河。全长456千米。河流上游穿行在山地和台地间,曲折蜿蜒,造成深切的河曲。进入太行山地后,流水湍急,形成峡谷,蕴藏着丰富的水力资源。出山口后在五龙口处形成冲积扇,早在2000多年前就被开辟为农田灌区,现在这里建立了完整的水利工程,是太行山南麓的主要农业生产基地。
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