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central-south china
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  中南地区
     An Investigation and Study on All People Body-building in Cities in Central-South China
     中南地区城市居民参与全民健身运动的现状调查及发展研究
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     When studying the biology of the Actinidia/Psevdasphondylia interaction in Central-south China we found evidence suggesting that under certain circumstances the gall insect modifies the reproductive mode of the dioecious host plant.
     在中国中南地区研究对萼猕猴桃—瘿蚊的相互关系过程中,我们的记载表明该造瘿昆虫在一定情形下可能改变其寄主植物的雌雄异株之生殖模式。
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     Changsha city is one of the severest polluted cities by acid rain in Central-south China.
     长沙市是中南地区酸雨污染最为严重的城市之一。
短句来源
     Applying the methods of investigation,visit and statistics,the authors investigate and analyzed the present condition and proble ms of all people body-building exercises of city people in central-south China and put forward countermeasures to solce the problems.
     采用调查、访问、统计等方法 ,探索了中南地区城市居民参与全民健身运动的目的态度、职业与学历状况、次数和时间、体育项目、对社会体育指导员的要求等基本特点和规律 ,并对现状中存在的主要问题 ,提出了相应的对策
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     Forest Hydrological Characteristics and the Biogeochemical Processes of Major Nutrients in Shaoshan Subtropical Forest, Central-south China
     中亚热带韶山森林水文特征与主要营养物的生物地球化学过程研究
短句来源
     Characteristics of uranium resources in central-south China and discussion on the new round uranium prospecting potential in south China
     中南铀矿资源特征及新一轮找矿前景探讨
短句来源
     CRETACEOUS NON-MARINE LAMELLIBRANCHIA FROM CENTRAL-SOUTH CHINA
     中南地区白垩纪淡水瓣鳃类
短句来源
     THE SPATIAL CHARACTERISTICS OF MONTHLY MEAN RAINFALL ANOMALIES OVER CENTRAL-SOUTH CHINA IN RELATION TO THE DISCHARGE AT THE UPPER CHANG-JIANG
     我国中南地区降水的分布特征及其对长江流量的影响
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     Etiologic and Epidemiologic Studies on Acute Infectious Diarrhea in Central-south China
     中南四省(区)急性感染性腹泻病原学及流行病学研究
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     On the drought of South China
     我国南方干旱成因与对策
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     SPRING IN THE SOUTH OF CHINA
     中国之春之江南春
短句来源
     CENTRAL CHINA AREA
     非物质文化遗产——我们的精神家园 华中地区
短句来源
     The Modernization in Central China
     我国中部地区的现代化浅析
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     Sediment Structure and Bioturbance in Central South China Sea
     南海中部沉积结构和生物扰动
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  central-south china
Inorganic nitrogen deposition and leaching in stream water were monitored from January, 2001 to December, 2004 in a subtropical evergreen mixed forest in central-south China.
      
Input-Output Budgets for Inorganic Nitrogen Under Acid Rain in a Subtropical Evergreen Mixed Forest in Central-South China
      


First, the spatial distribution of rainfall anomalies of Central-South China (23-34°N, 100-113°E) was examined by means of the empirical orthogonal function analysis. The data used in this paper are collected from 60 stations, monthly mean rainfall observations from April to October during the last 27 years (1953-1979). The monthly mean rainfall anomalies in Central-South China have been classified into fourteen types. The first four types ane characterized by the seasonal migration of the rain-belt,and...

First, the spatial distribution of rainfall anomalies of Central-South China (23-34°N, 100-113°E) was examined by means of the empirical orthogonal function analysis. The data used in this paper are collected from 60 stations, monthly mean rainfall observations from April to October during the last 27 years (1953-1979). The monthly mean rainfall anomalies in Central-South China have been classified into fourteen types. The first four types ane characterized by the seasonal migration of the rain-belt,and each of the other types reflects a definite structure which can be easily interpreted with synoptic-climatological knowledge.Secondly, the correlation coefficients were calaulated to show the relationships between the rainfall and the discharge at the upper Changjiang for every month from April to October. The results show that regions in which correlation coefficients are higher than 0.37 (at 5% significant level) shift obviously with the season. The region or the socalled key region, in which rainfall is more important for the discharge, sometimes coincides with the variance centers of the first eigenvector and sometimes not. In most cases this key region is in accordance with the second eigenvector, or even the third eigenvector. It turns out that in spite of the close relation between the rainfall and the discharge at the upper Chang-Jiang, both of then are somewhat independent in their variations. So, we must pay more attention to the difference between them in studying the formation of discharge anomolies and in making long-range forecast of droughts and floods at the upper Chang-Jiang.

本文分析了23—34°N,100—113°E所包围地区内汎期(4—10月)月雨量的分布特征,及其对长江上游流量的影响。在上述范围内选取了60个雨量站,资料年代从1953到1979年计27年。采用特征向量分析,把这一地区汎期月雨量的分布归纳为14种型,并讨论了各型的特征。同时计算了长江上游各月平均流量与同期各站雨量的相关,根据相关分布图,探讨了各月雨量分布对长江上游流量的影响。

A map of sediment types in scale of 1:3,000,000 is compiled on the analytical data including grain size, the composition of sand fraction, the light and heavy detrital minerals, clay minerals, the fauna identification of foraminifera, calcareous nannoplankton, radiolarian, diatom and spore-pollen, chemical quantitative analysis and 14C dating et al of 130 surface sediment samples from the central South China Sea involving water depth of 480-4400 m in two cruises of October 1983 and June 1984. Based on...

A map of sediment types in scale of 1:3,000,000 is compiled on the analytical data including grain size, the composition of sand fraction, the light and heavy detrital minerals, clay minerals, the fauna identification of foraminifera, calcareous nannoplankton, radiolarian, diatom and spore-pollen, chemical quantitative analysis and 14C dating et al of 130 surface sediment samples from the central South China Sea involving water depth of 480-4400 m in two cruises of October 1983 and June 1984. Based on the map main types and distribution of the sediments as well as deep sea sedimentation are discussed.

本文以1983年10月和1984年6月两个航次期间在南海中部海域内采集的130个站位的沉积物组分全面鉴定(粒度、砂级全组分、轻重碎屑矿物、粘土矿物、有孔虫、钙质超微、放射虫、硅藻和孢粉等生物鉴定、化学定量分析、少量~(14)C测年等)为基础,以1∶300万南海中部沉积物类型图为依据,讨论了沉积物主要类型、分布和沉积作用特点。

Six assemblages and five subassemblages of benthic foraminifera are established on the basis of 53 surface sediment samples from the central South China Sea. Planktonic foraminifera in surface sediments of this area can be divided into four assemblages of different water depths. The main factors controlling the distribution of foraminifera in the area are dissolution of deep-sea carbonate, water masses, sea-floor relief and relict sediment.

本文根据南海中部海区53个表层沉积物样的有孔虫分析,初步确定了六个底栖有孔虫组合和五个亚组合,而浮游有孔虫可分为四个不同水深的组合。控制本区有孔虫分布的主要因素是深海碳酸盐溶解作用、水团、海底地形以及残留沉积。

 
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