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regional combination     
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  地域组合
     A Study on Regional Combination Type and Exploitation Mode of Natural Resources in Gansu Province
     甘肃省自然资源地域组合类型与开发模式研究
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     Dynamic Change of Regional Combination Law of Drought and Flood Disasters in Jilin Province
     吉林省旱涝灾害地域组合规律的动态变化
短句来源
     This paper expounds on the development process of port group system from port regional combination to port transportation system, relationship among port regional combinations which is characterized by competition and cooperation, so as to establish the evaluation indices concerning integrated development of port group system.
     阐述港口群系统从港口地域组合到港口运输体系的演变发展过程,形成各个港口地域组合之间既相互竞争又相互合作的关系,从而建立港口群系统整体发展的评价指标。
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     A STUDY ON THE SUSTAINABLE DEVELOPMENT AND THE DEVELOPMENT FROM OF REGIONAL COMBINATION OF PORTS IN LIAONING
     辽宁港口地域组合形成、发展与可持续发展研究
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     The main objectives of this paper are as follows: 1.To discuss the essential characteristics and the regional combination forms of the regional systems of the oil industries in the Sirte Basin;
     本文的主要目的在于: 1 探讨锡尔特盆地石油工业地域体系的特点和地域组合型式;
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  区域联合
     Relevant theories include the theory of regional combination and regional coordination, the theory of bearing capacity input-output potential mode and balance sheet mode.
     相关理论包括区域联合与区际协调论、承载力理论、投入产出潜力理论和资产负债表理论。
短句来源
     to reinforce regional combination and cooperation;
     加强区域联合和合作 ;
短句来源
     People have paid more and more attention to tourism regional combination,and scopeeconomy and benefit that are brought by it have manifested their special merits outstandingly.
     旅游区域联合已经越来越受到人们的重视,区域联合带来的规模经济效益突显出其特殊的价值。
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  区域整合
     Study on the Regional Combination between the West of Hubei and the East of Chongqing in Setting up the Big Three Gorges Tourism and Economy Circle
     论"大三峡旅游经济圈"构建中的鄂西与渝东区域整合
短句来源
  地域组合规律
     Dynamic Change of Regional Combination Law of Drought and Flood Disasters in Jilin Province
     吉林省旱涝灾害地域组合规律的动态变化
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The present paper comprises four sections.The first section gives a brief history of the development of the Insti tute of Geography. There contain four stages: the early-established stage (1950-1955) , the development stage (1956-1966) , the stage during the Cultural Revolution (1960-1976), and then one of restoration and expansion(1977-1983) . Details and the main scientific research work for each stage is described.The second section begins with the work for the production and construction of our country,...

The present paper comprises four sections.The first section gives a brief history of the development of the Insti tute of Geography. There contain four stages: the early-established stage (1950-1955) , the development stage (1956-1966) , the stage during the Cultural Revolution (1960-1976), and then one of restoration and expansion(1977-1983) . Details and the main scientific research work for each stage is described.The second section begins with the work for the production and construction of our country, among there includes 1).the research work with comprehensive reference value; 2) . comcerning agriculture; 3). with regard to industry, communication and transportation, and water conservancy; 4). in relation to the protection of environment, and the causes and prevention an treatment of some endemic diseases in connection with water and soil.In the third section, work on basic theory is summarized in the following aspects. 1) studies on the laws of transfer and transformation of matter and energy in geographical environment and their regional differentiation, including such studies as heat and water balance, laws of distribution and motion of chemical elements in the geographical environment, interaction between ocean and atmosphere, and the monsoon climate in South East Asia. 2) studies on the theory of geographical zonation and regional differentiation, such as the theory and methodology of natural regionalization, and regional physical geography; 3) studies on the process of formation and historical evolution of the geographical environment, including such studies as geographical processes, the Holocene Paleogeography, the geographical environment and its changes during the historic times; 4) studies on the theory of regional combination of productive forces, including distribution of industry and regional programme; 5) studies on cartographic theory and methodology, including mapping integration of the general map, mapping for special topic, comprehensive mapping principle and methods.In the fourth section we expound the application of experimental technology and new techniques to geography, including such studies as the techniques of determination and experiment in the laboratory, the mapping techniques by computer and geographical information system, remote sensing techniques and remote measurement etc.

本文对地理研究所三十年的科研工作进行了回顾。其中对科研工作的发展按四个时期作了简要分析。重点介绍了为生产和建设服务的工作,扼要总结了地理学基础理论研究方面的工作,最后阐述了实验技术的发展与新技术的应用。

There are obvious regional differentiation in the Hengduan Mountainous Region.According to the regional combination of temperature-moisture regimes and relief characteristics, 5 zones and 9 regions may be divided:Ⅰ .Peripheral tropical mountain zone with monsoon rainforest and semi-evergreen monsoon rainforest.Ⅰ 1.Southern and southwestern Yunnan basin region.Ⅱ .Southern subtropical mountain zone with monsoon evergreen broad-leaved forest.Ⅱ 1 .South western Yunnan middle mountain, mountain plateau and...

There are obvious regional differentiation in the Hengduan Mountainous Region.According to the regional combination of temperature-moisture regimes and relief characteristics, 5 zones and 9 regions may be divided:Ⅰ .Peripheral tropical mountain zone with monsoon rainforest and semi-evergreen monsoon rainforest.Ⅰ 1.Southern and southwestern Yunnan basin region.Ⅱ .Southern subtropical mountain zone with monsoon evergreen broad-leaved forest.Ⅱ 1 .South western Yunnan middle mountain, mountain plateau and valley region.Ⅲ .Middle subtropical mountain zone with evergreen broad-leaved and Pinus yunnanensis forests.Ⅲ 1 .Southwestern Sichuan middle mountain, deep gorge region. Ⅲ2. Western Yunnan high and middle mountains, deep gorge region. Ⅳ.Temperate mountain zone with montane coniferous forest on the Qinghai-Xizang Plateau.Ⅳ 1.Min and Qionglai Mountains middle and high mountains region. Ⅳ2.High mountain, deep gorge region at the middle reaches of Jinsha, Lancang and Nu Rivers.Ⅳ 3.High mountain,deep gorge region at the upper reaches of Jinsha. Lancang and Nu Rivers.Ⅴ .Subpolar zone with alpine shrubby meadow on the Qinghai-Xizang Plateau.Ⅴ 1,Zoige hill plateau region.Ⅴ 2. Sertar-Serxu plateau, broad valley region.

横断山区地域分异明显。各自然地理要素作地带性组合,自然地理环境呈水平分异,农业土地利用也大体呈纬向带状分布。根据温度和水分条件的地域组合及地势差异,将横断山区划分为5个自然地带、9个自然区,并与以往的方案进行了比较,阐述了自然地带界线的划分及各带特征。

Physical factors and human factor are two dominant factors forming erosion environment of the Loess Plateau. Temporal inheritance, obvious regional difference, continental monsoon climate and unique regional combination of erosion factors are the basic charateristics of the erosion environment in this area. The two main erosion factors, regetation and precipitation, with obvious zonal differnence, belong to zonal factors, while other physical factors and human factor belong to non-zone factors. Influenced...

Physical factors and human factor are two dominant factors forming erosion environment of the Loess Plateau. Temporal inheritance, obvious regional difference, continental monsoon climate and unique regional combination of erosion factors are the basic charateristics of the erosion environment in this area. The two main erosion factors, regetation and precipitation, with obvious zonal differnence, belong to zonal factors, while other physical factors and human factor belong to non-zone factors. Influenced by this, the temporal and spatial distributions of eroded sediment in the area also have obvious differential law. The area with high sediment and coarse sediment yield in the Loess Plateau results mainly from the disadvantageous combination of these factors.

自然因素和人为因素是构成黄土高原侵蚀环境的两大主导因素。时间上的继承性、空间上的明显区位分异、大陆性季风气候以及独特的侵蚀产沙因素的区域组合等构成了该地区侵蚀环境的基本特征,尤以植被和降雨这两个主要侵蚀因子的地带性分异明显,属于地带性因素;其它自然因素和人为因素则属非地带性因素。受这一环境的影响,该地区的侵蚀产沙的时空分布也表现出明显的分异规律,其中的多沙粗沙区就是诸因素独特组合的结果。

 
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