说明:双击或选中下面任意单词,将显示该词的音标、读音、翻译等;选中中文或多个词,将显示翻译。
您的位置:首页 -> 词典 -> 滹沱河湿地
1)  Hutuohe River wetland
滹沱河湿地
2)  the Ganghuang section of Hutuohe Wetland
滹沱河岗黄段湿地
1.
By combining reality,through real example,and by employing AHP evaluation assessment,the level analysis appraise of the Ganghuang section of Hutuohe Wetland with development scale of certain sight-seeing agriculture 6 areas is carried out,and exploration is made ebout the effective way to the principle that the development sight-seeing agriculture should be followed along the wetland.
结合实际,通过实证分析,应用AHP(层次分析法)评价法,对滹沱河岗黄段湿地具有一定观光农业发展规模的6个区域进行层次分析评价,并针对湿地沿岸发展观光农业所应遵循的原则探索有效途径,为河北省周边观光农业旅游开发提供依据。
3)  Hutuo River groundwater
滹沱河地下水
4)  Hutuo River
滹沱河
1.
Evaluation and Study on Influence of Human to Wetlands in Ganghuang Section of Hutuo River;
滹沱河岗黄段湿地人类活动影响评价研究
2.
Discussion on the Pattern of Rehabili-tation of the Ecological Environment of Dry Waterways——With the Study of the Ecological Comprehensive Improvement of the Hutuo River(Shijiazhuang Section)as an Example;
干旱河道的生态环境修复模式探索——以滹沱河(石家庄段)生态环境综合治理研究为例
3.
Simulation analysis on temperature field and stress distribution during construction of Inverted Siphon Project of Hutuo River;
滹沱河倒虹吸施工期温度场及温度应力仿真分析
5)  Hutuohe river
滹沱河
1.
Studies on the Phytoremediation to Heavy Metals Pollution in the Hutuohe River Wetland;
滹沱河岗黄段湿地重金属污染的植物修复探讨
2.
The Quality Control of Regulation Project of Hutuohe River;
滹沱河治理工程质量管理
3.
Studies on the Current Situation,Conservation and Utilization of Plant Resouces in the Hutuohe River Wetland;
滹沱河岗黄段湿地植物资源现状及其保护利用前景
6)  the Hutuo River
滹沱河
1.
Formation of Dyke Building and Bank Protection in Channel Improvement of the Hutuo River and Its Evaluation;
滹沱河河道治理堤防护岸形式及其评价
2.
Study of Regulating and Storage Function of the Hutuo River s Underground Reservoir;
石家庄市滹沱河地下水库调蓄功能研究初探
3.
A Study on Watercourse Shifts of the Hutuo River on the Plain since the Ming Dynasty;
明以降滹沱河平原段河道变迁研究
补充资料:滹沱河
滹沱河

    子牙河北源。位于中国河北省西部。源出山西省五台山,穿切太行山东流入河北平原,沿途纳牧马河、清水河、冶河等河流,在献县臧家桥与滏阳河汇合为子牙河。全长605千米(至献县闸),流域面积(至北中山)2.39万平方千米,上游流经黄土高原,河水挟带大量泥沙,下游淤浅,常遇洪水溃决成灾。中华人民共和国建立后,通过在上游兴修水库调蓄洪水,中下游加固河堤,减免了洪水内涝灾害。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条