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1)  Yongding River
永定河
1.
Phosphorus Speciation in Sediments of the Yongding River and Its Significance;
永定河沉积物中磷的存在形态及其指示意义
2.
Mutagenicity of toxic organic pollutants in Yongding River (Guanting Reservoir-Sanjiadian), Beijing;
北京永定河(官厅—三家店)水体有毒有机污染物的致突变性研究
3.
Impact analysis of historical forest change on Yongding River;
历史上森林变迁对永定河的影响
2)  Yongdinghe River
永定河
1.
Persistent Organochlorinated Pesticides in Water from Guanting Reservoir and Yongdinghe River, Beijing;
北京官厅水库-永定河水系水体中持久性有机氯农药污染
2.
The study of VOCs in Guanting Reservoir and Yongdinghe River;
官厅水库及永定河水中挥发性有机物分布规律
3.
The Study of Distribution of N, P and heavy metals in Guanting Reservoir and Yongdinghe River;
官厅水库及永定河枯水期水体氮、磷和重金属含量分布规律
3)  new Yongding River
永定新河
1.
Experiment of treating the wastewater of the new Yongding River;
永定新河污染水体处理试验
4)  the Records of the Yong-ding River
《永定河志》
1.
Not until in 1698 had a special organization been set up to harness the river,and the event also promoted the subsequent compiling of two records of the river,the Records of the Yong-ding River and the Continuous Records of the Yong-ding River,which is a good example of the interaction between social changes and historiography.
清政府的治河所为 ,促进了相应的志书编纂 ,先后出现了《永定河志》和《永定河续志》二部志书。
5)  Yongdingxin River estuary
永定新河口
1.
Based on the distribution regularities of stratigraphic sandy soil in the Tianjin Yongdingxin River estuary area,the in-situ standard penetration test(SPT) method and the indoor dynamic triaxial test method were used to make the sandy soil liquefaction discrimination.
根据天津永定新河口滩涂地层沙性土分布规律,采用现场标准贯入试验和室内动三轴试验两种方法进行了沙性土的液化判别。
6)  Yongding River Basin
永定河流域
1.
A Study of Groundwater Cycle in Yongding River Basin by Using δD,δ~(18)O and Hydrochemical Data;
基于δD和δ~(18)O及水化学的永定河流域地下水循环特征解析
补充资料:永定河
永定河

    海河流域五大水系之一。位于中国河北省西北部。上源有两支:南支为桑干河,发源于山西省宁武县管涔山,东流纳黄水河、浑河、御河等进入河北省境内再纳壶流河;北支洋河,源出内蒙古兴和县,于河北省境内张家口市纳清水河。原两支于河北省怀来县朱官屯汇流,汇流后始称永定河,自官厅水库建成后,两支均汇入官厅水库,官厅以下称永定河。经官厅山峡,至北京三家店出山,过卢沟桥以下形成地上河。向东流至屈家店与北运河(见京杭运河)汇合  。全长681千米  ,流域面积5.1万平方千米(至屈家店)。上游流经黄土高原,河水含沙量仅次于黄河,故有小黄河、浑河之称。下游淤浅,河道迁徙无定,故又有无定河之称。清康熙三十七年(1698)为保护京城北京,筑永定大堤以固河槽,后定名永定河,但河水仍变化无常,经常决堤成灾。中华人民共和国建立后,在官厅以上先后兴建大、中、小型水库517座,总库容达33亿立方米。其中,以官厅水库的库容为最大,约22.7亿立方米。1970年开挖了永定新河,从屈家店到北塘,然后入渤海,以分泄汛期洪水,防止水害。
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