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新疆
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  xinjiang
    A Study on Environmental Problems in Xinjiang's Industrialization Process
    新疆工业化进程中的环境问题研究
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    The Development and Water resources of Cities Ecosystem in Xinjiang
    新疆城市生态系统的发展与水资源
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    The Investigation of the Influence of Environment Radiation on the Residents Health Around Xinjiang Nuclear Testing Site
    新疆核试验场周围环境辐射对居民健康影响的调查研究
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    A STUDY ON 14C-PHOXIM ABSORPTIION BY XiNJIANG GRAY DESERT SOiL.
    新疆灰漠土对~14C-辛硫磷的吸附研究
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    The Level of 90Sr and 137Cs Around The Nuclear Testing Site in Xinjiang and The Residents' Dose Caused from Them
    新疆核试验场周围地区主要食品中~(90)Sr(锶)、~(137)Cs(铯)水平及其所致居民剂量
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  sinkiang
    The eco-environmental problems and protecting countermeasures in YiLi State Sinkiang Municipality
    新疆伊犁州生态环境问题与保护对策
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    The Approach of Constructing the Ecological Environment in the Arid Area Oasis——Take the Akesu Area in Sinkiang for Example
    干旱区绿洲生态环境建设之途径——以新疆阿克苏绿洲为例
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    YiLi state is located in the west of Sinkiang and had a strategic status in the development of west China.
    伊犁哈萨克自治州位于新疆西部,地处亚欧大陆腹地,西与哈萨克斯坦交界。 土地面积、资源储备和战略地位都在西部开发中居于重要地位。
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  “新疆”译为未确定词的双语例句
    A Discussion About The Conditions And The Development of Rural Economy And Environment Along River System Manasi——A Preliminary Suggestions to The Program of Developing Economy and Environment of State Farm 147
    试论新疆玛纳斯河流域农村经济与环境的现状及发展——对147团场经济与环境发展规划的初步建议
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    Approch To Coordinative Macro-development of Rural Enterprises and Environment
    新疆乡镇企业经济与生态环境保护协调发展战略的探讨(二)
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    A STUDY ON GROWTH MODEL AND ITS ECOLOGICAL PARAMETER OF PERCA FLUVIATILIS LINNAEUS IN WUBENGU LAKE
    新疆乌伦古湖河鲈(Perca fluviatilis Linnaeus)种群的生长模型及生态参数的研究
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    MODEL AND APPLICATION--STRUCTURAL OPTIMIZATION OF OASIS SHELTER FORESTS IN XINHANG
    新疆绿洲防护林体系结构优化模型与应用研究
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    The Evaluation of Oasis Forest Environment Qualities
    新疆绿洲森林环境质量评价与排序──以喀什、和田地区各县为例
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  xinjiang
Halophilic archaeon AJ6 was isolated and purified from the Altun Mountain National Nature Reserve of the Xinjiang Uygur Autonomous Region.
      
Chlorophytes of biological soil crusts in Gurbantunggut Desert, Xinjiang Autonomous Region, China
      
In this paper, chlorophytes collected from 253 biological soil crust samples in Gurbantunggut Desert in Xinjiang Autonomous Region, China were studied by field investigation and microscopical observation in lab.
      
Association study on GNB3 gene polymorphism with essential hypertension in Xinjiang Uygur group
      
The correlated study of hyperuricemia and metabolic syndromes among males of Han ethnicity in the Xinjiang Uygur Autonomous Regi
      
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  sinkiang
Most salt lakes are in northwestern China (Tibet, Qinghai, Sinkiang, Inner Mongolia).
      
Many salt lakes in Qinghai-Tibet lie at altitudes >amp;gt; 4 000 m.a.s.l.; Aiding Hu (Sinkiang) lies at -154 m.a.s.l.
      
An earthquake in the Northern Sinkiang Province, China, on November 13th, 1965, produced exceptionally strong higher-mode surface waves recorded at the Swedish seismograph stations, especially by the Galitzin seismographs at Kiruna.
      
The fundamental character of deserts in the northern Sinkiang region.
      
The distribution of halophytic plant communities of Sinkiang Region in relation to soils and groundwater.
      


In this paper some characteristics of the aerosal in a dust storm occurring April 18-20, 1980,over Bering area were described. Analysis of meteorological data showed that the dust storm was formed in Hami area of Xingjiang Province and western part of Inner Mongolia. The strong wind area moved first toward east and then southeast when it reached central part of the Inner Mongolia and Hebei Province. By means of the 326-meter observation tower and radiosounding technique the Structure of atmospheric boundary...

In this paper some characteristics of the aerosal in a dust storm occurring April 18-20, 1980,over Bering area were described. Analysis of meteorological data showed that the dust storm was formed in Hami area of Xingjiang Province and western part of Inner Mongolia. The strong wind area moved first toward east and then southeast when it reached central part of the Inner Mongolia and Hebei Province. By means of the 326-meter observation tower and radiosounding technique the Structure of atmospheric boundary layer was discussed for the dust storm.

本文讨论了1980年4月北京地区一次尘暴过程的气溶胶特征。气象资料分析表明,这次尘暴大风形成于新疆哈密及内蒙西部一带,开始大风区向东移动,到内蒙、河北一带又转向东南方向移动。利用325米气象塔和探空资料讨论了尘暴过程大气边界层的结构。 尘暴气溶胶浓度比平时要高一个量级,气溶胶中元素含量是用中子活化法分析的。分析结果说明,元素Eu和Ta只存在于尘暴气溶胶中,其它元素基本一样,但其含量变化较大。富集因子的计算表明,气溶胶中元素Se、As、Br、Sb主要来源于煤的燃烧。 从形成尘暴的气象背景的讨论和尘暴气溶胶中元素资料的分析,初步认为,这次尘暴气溶胶主要是由形成尘暴大风地区及其移动路经地区的沙土微粒被风带入高空混合而形成的。

The lakes of Xinjiang have had greatly changes since liberation. All the lakes there can be divided into 5 types according to their change in area.. 1. dried up, 2. almost dried up, 3. shrinking, 4. changed mot much and, 5. expanding.The lakes in desert area tend to dry up, (for examples, the Nop Nor, the Manasi lake etc.) the lakes in the plain tend to shrink, (the Bositeng lake, the Wulungu lake etc.) and the lakes in mountain area remain their niginal out-look, (the sailimu lake, the Kanasi lake etc.)Recent...

The lakes of Xinjiang have had greatly changes since liberation. All the lakes there can be divided into 5 types according to their change in area.. 1. dried up, 2. almost dried up, 3. shrinking, 4. changed mot much and, 5. expanding.The lakes in desert area tend to dry up, (for examples, the Nop Nor, the Manasi lake etc.) the lakes in the plain tend to shrink, (the Bositeng lake, the Wulungu lake etc.) and the lakes in mountain area remain their niginal out-look, (the sailimu lake, the Kanasi lake etc.)Recent changes in the lakes mainly include salinization of water quality and shrinkage in area and deepth. In the year 1958 the mineralization of the Bositeng lake was less than 0.4g/l, while in 1975 it rose to 1.5g/l, and in 1980 to 1.8g/l.The average annual increase was 0.06g/l which is quite amazing, in the year 1959 the Wulungu lake was 482.8 M. above-sea-level, while in 1969 it went down to 480.0 M. and in 1980 to 478.8M. 4 M. It has a total drop of about the last two decades.These changes make a profound impact on the ecosystem of the lakes. The area of desertifaication increased rapidly from 12% to 52% during the year from 1958 to 1978 around the Nop Nor region where a big lake had disappeared Biological resourses were degenarated in most of the lakes. Fishery output of the Wulungu lake decreased from 4000 tons to less an one thousand ton per years.Reed resourses of the Bositeng lake decreased from 0.4 million tons to 0.25 million tons per year during the same period.The cause of the changes is basically due to the influence of human activities. Large-scale reclamation reeds a huge amount of irrigation water from the rivers and it has to drain off salt water into the lakes. On the other hand, recent cyclical decrease of runoff is another important reason of the changes.The methods to prevent the lakes from becoming arid land and the way to utilize the lakes for multiple purposes are also discussed

三十年来,新疆湖泊发生了较大的变化,按湖泊水面变化可分为干涸、基本干涸、缩小、变化不明显和扩大等五种类型,本文简要分析了湖泊变化的原因,湖泊变化和自然环境之间的关系。

This paper deals with distribution of titahium, zirconium and yttrium as index elements based on analytical data of soil samples collected from area of Tulufan, Xinjiang. They are derived from eight parent materials. Contents of Ti, Zr and Y were determined by X-ray fluorescence, with Ti and Zr the hightest in soils from andesite, while that of Y is comparatively high in soils from alluviation sediments. No obvious difference is found between Ti, Zr and Y in topsoil and bedsoil, except for Ti and Y in soils...

This paper deals with distribution of titahium, zirconium and yttrium as index elements based on analytical data of soil samples collected from area of Tulufan, Xinjiang. They are derived from eight parent materials. Contents of Ti, Zr and Y were determined by X-ray fluorescence, with Ti and Zr the hightest in soils from andesite, while that of Y is comparatively high in soils from alluviation sediments. No obvious difference is found between Ti, Zr and Y in topsoil and bedsoil, except for Ti and Y in soils from wind deposits, lake sediments and shale.

本文根据新疆吐鲁番地区八种母质发育的土壤中Ti、Zr、Y的X射线荧光法分析数据,对这三种元素在土壤中的分布以及用它们之间的比值来判断该地区土壤剖面各层次的母质来源是否相同等问题进行初步探讨。结果表明,不同母质发育的土壤中元素含量有一定差异,而在大多数母质发育的土壤的表、底土间元素含量无明显差异;该地区土壤中zr/Y比和Ti/Zr比可用来判断土壤剖面不同层次的母质来源,两个结果较为一致,对于各层次间元素对比值较接近的剖面,认为是同一母质来源。

 
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