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重庆段
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  chongqing section
     Researches on Slope Treatment Schemes for Chongqing Section (K63 KM) of Chongqing-Guizhou Expressway
     渝黔高速公路重庆段K63公里边坡处治方案研究
短句来源
     The Status of Small Towns Sewage in Chongqing Section of Three Gorges Reservoir and Selection of Sewage Treatment Process
     三峡库区重庆段小城镇的污水现状与处理工艺优选
短句来源
     Study on Effect of Sediment on Diatom's Growth in Chongqing Section of the Three Gorges Reservoir Area
     三峡库区重庆段泥沙对硅藻生长影响试验研究
短句来源
     Studies on the Ecological Function Regionalization in the Three Gorges Reservoir Area:The Case of Chongqing Section
     长江三峡库区(重庆段)沿江区域生态功能区划
短句来源
     A study on the impact of the Three Gorges Reservoir on potential eutrophication in backwaters of tributaries of Chongqing section of Yangtze River
     三峡水库重庆段一级支流回水河段富营养化潜势研究
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  “重庆段”译为未确定词的双语例句
     Application of QUAL2E Model to Chongqing Urban Section of the Yangtze River
     QUAL2E模型在长江重庆段水质模拟中的应用研究
短句来源
     Health Surveillance Report in Chongqing Segment of the Three Gorges Area in 1997-2002
     三峡库区重庆段1997-2002年人群健康监测报告
短句来源
     The heavy metals level of soils in water-level-fluctuating zone of the ThreeGorges Reservoir is lower than Tertiary Soil Quality Standard. According to the research,the mean Cu concentration is 37.0mg/kg,ranging from 10.7 to 80.2mg/kg;
     三峡库区重庆段淹没区土壤重金属含量均低于国家土壤环境标准三级,其中铜含量范围为10.7~80.2mg/kg,均值为37.0 mg/kg;
短句来源
     Study on Flow Model of the Three Gorges Area in Chongqing Region
     三峡库区重庆段水流模型研究
短句来源
     Comparative study of the pollution loading of nourishing substances —— nitrogen and phosphorus in Chongqing segment of the Three Gorges Reservoir
     三峡库区重庆段富营养化物质氮磷污染负荷比较研究
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  相似匹配句对
     Study on Flow Model of the Three Gorges Area in Chongqing Region
     三峡库区重庆水流模型研究
短句来源
     STUDY ON WATER ENVIRONMENTAL CAPACITY OF YANGTZE RIVER AND JILAING RIVER IN CHONGQING
     长江、嘉陵江重庆水环境容量研究
短句来源
     Chongqing Authors and Their Recent Books
     重庆
短句来源
     Bing Xin in Chongqing
     冰心在重庆
短句来源
     3, horizontal section.
     3.水平
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This article dpscribed the status of water resources and natural en-vironmnent,gave the brief introduction of water quality of Yangtze River andJialing River as well as tributries in Chongqing.

概述了重庆市的水资源以及长江、嘉陵江重庆段的自然环境状况,同时对两江和次级河流的水质现状也作了简洁的描述。

We deduce a one-dimensional water quality model which is suitable for anysection concentration evaluating from the characteristics of feature of the pollutant reso-urce of Yangtze River and Jialing River in Chongqing.we also illustrated the initialconditions of the model.

根据长江嘉陵江重庆段污染物的来源特点,推导出适用于计算两江干流任意断面污染物浓度的一维水质数学模型,并对模型使用的初始条件作了说明。

The Huangling anticline was divide of the ancient Yangtze and Jinsha river at the beginning of Quaternary period. Because of continental elevation resulted from the collision of Indian plate with Eurasian plate, the ancient Jinsha river was captured by the ancient Yangtze river at 0.15-0.20 Ma.B.P. at a height of 155-170 m . This is supported by the existence of refluent tributaries, reversed terraces and wind gaps. Among the current rivers on the world formed at the beginning of Quaternary period, the river...

The Huangling anticline was divide of the ancient Yangtze and Jinsha river at the beginning of Quaternary period. Because of continental elevation resulted from the collision of Indian plate with Eurasian plate, the ancient Jinsha river was captured by the ancient Yangtze river at 0.15-0.20 Ma.B.P. at a height of 155-170 m . This is supported by the existence of refluent tributaries, reversed terraces and wind gaps. Among the current rivers on the world formed at the beginning of Quaternary period, the river capture of the Yangtze Gorges is a special example and shows close relation to ancient climate and neotectonism. So study on evolutional history of the river has important significance.

李四光有“黄陵背斜为华西、华东的分水岭,岭西之水流入归州盆地和四川盆地,岭东之水则向东流,袭夺……”的正确论断,但他“(袭夺)年代是第三纪末至早更新世初”的见解则过早。黄陵背斜西侧之水属古金沙江东支流,仅香溪至重庆段内竟有73.3%的支流呈倒插;巫山至故陵镇82.5km间的T6、T5、T4阶地面沿江呈西倾,而T3、T2、T1阶地面沿江呈东倾,二者刚好反向。在重庆、奉节分别发现了鹅岭风口和白帝城风口,二者与倒插支流、反向阶地共同证实了此段属掉向(被袭夺)流段。由于2.0Ma以来印度板块与亚欧板块碰撞所导致的西域上升,黄陵背斜遭冰后期和其它外营力剥蚀、降低,古金沙江南下水路被横断山封堵,西支流只好向东支流涌来,又借黄陵背斜东坡古长江向源侵蚀之机,终于0.15~0.20Ma间切开黄陵背斜分水岭,形成新型长江

 
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