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我国东部
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  eastern china
     Spatial and Temporal Variations of the Vegetation Growing Season in Warm-temperate Eastern China during 1982 to 1999
     1982~1999年我国东部暖温带植被生长季节的时空变化
短句来源
     The lacustrine basins in Eastern China mainly developed lithologic subtle reservoirs and unconformity ones.
     我国东部的陆相盆地则主要发育岩性油气藏、不整合油气藏等两种类型的隐蔽油气藏。
短句来源
     only δDH2o of inclusions in quartz of the Yushan ore district is - 89.5‰ which is within the range of δD values (-70‰ to - 90‰ ) of meteoric water during Cretaceous time in eastern China;
     仅彭水郁山矿床石英中包裹体水的D值(-89.2‰)落在我国东部侏罗纪~白垩纪时期大气水的D值范围(-70‰~90‰。)
短句来源
     Study of Summer Monsoon Features of 1998 in Eastern China
     1998年我国东部大陆夏季风特征研究
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     By exploration of self operation and joint venture, several major oil fields, such as QHD32 6, NB35 2, CFD11 1, BZ25 1 and PL19 3, are successively found, resulting in a great breakthrough in Bohai Sea`s exploration, which will play an important role in developing offshore petroleum industry and stabilizing oil production in the eastern China.
     通过自营和合作勘探 ,相继发现了 QHD32 - 6、NB35 - 2、CFD11- 1、BZ2 5 - 1、PL19- 3等一批大中型油田 ,实现了渤海海域油气勘探的重大突破和转折 ,对海洋石油事业的持续发展和保持我国东部石油稳产将起重大作用
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  in eastern china
     The lacustrine basins in Eastern China mainly developed lithologic subtle reservoirs and unconformity ones.
     我国东部的陆相盆地则主要发育岩性油气藏、不整合油气藏等两种类型的隐蔽油气藏。
短句来源
     only δDH2o of inclusions in quartz of the Yushan ore district is - 89.5‰ which is within the range of δD values (-70‰ to - 90‰ ) of meteoric water during Cretaceous time in eastern China;
     仅彭水郁山矿床石英中包裹体水的D值(-89.2‰)落在我国东部侏罗纪~白垩纪时期大气水的D值范围(-70‰~90‰。)
短句来源
     Study of Summer Monsoon Features of 1998 in Eastern China
     1998年我国东部大陆夏季风特征研究
短句来源
     Competitive Advantages of Tourism Products In Eastern China
     我国东部旅游地带旅游产品的竞争优势
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     Gemological Characteristics of the Sapphire in Eastern China
     我国东部蓝宝石的宝石学特征
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  east of china
     The 500-year 1° × 1° grid precipitation anomaly series in the east of China have been used to compartmentalize precipitation spatial patterns in these regions during the last 500 years.
     利用我国东部近500年1°×1°格点式降水量距平场的复原资料,划分出我国近500年降水分布型;
短句来源
     the north flows coming from north of Okhotsk sea,the east flows coming from north of north-west pacific,and the north–west flow coming from the east of lake Baykal are jointed nearby 60°N,115~120°E,makes the velocity of north wind inbreaking the east of China speed up,Taiyuan is controled by the coherent north–west flow,it is drought.
     而来源于鄂霍次克海北部的偏北气流、西北太平洋的偏东气流以及贝加尔湖以东的西北气流在60°N,115~120°E附近汇合,使入侵我国东部的偏北气流风速加大,太原在一致的西北气流控制之下,汛期偏旱。
短句来源
     Taking the paving works of an international airport runway in the east of China as the sample, the article analyzes in detail the selection of PCN calculation method, the choice of calculation parameters and the calculation course of PCN for the composite runway pavement, which have a certain of value for reference to calculate PCN of the similar engineering runway pavements.
     该文以我国东部某国际机场跑道加铺工程作为实例,对复合道面PCN计算方法的选择、计算参数的选取、以及PCN的计算过程进行了详细的分析,对于类似工程道面PCN的计算具有一定的参考价值。
短句来源
     A STUDY OF THE CHARACTERISTICS OF SUMMER DRYNESS AND WETNESS IN EAST OF CHINA DURING 40 YEARS
     近40年我国东部夏季旱涝气候特征
短句来源
     QJ depression is situated in one of the typical block salt-lake basins in the east of China.
     QJ凹陷处于我国东部一个典型的断陷式盐湖相沉积盆地中.
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  “我国东部”译为未确定词的双语例句
     According to the analysis of 19 cores from 5 wells and the geothermal data of 8 wells , the regional averagegeothermal gradient and uncorrected heatflow in the Huoshaoshan oilfield of the eastern Junggar basin were calculated23. 696℃/km and 40. 84mW/m~2. These two values were both lower than the average of the basins of the east partof China and global continents.
     以5口井19块岩心和8口井地温测量资料求得准噶尔盆地东部火烧山油田区域平均地温梯度为23.696℃/km,未经地形等校正的大地热流值为40.84mW/m~2,这两数值均低于我国东部其他盆地和全球大陆平均值。
短句来源
     This record shows that both the onset and termination of the YD event occurred within 11 0~10 0kaB.P.
     其记录表明,这一突变事件起止于约11.0~10.0kaB.P.,并于约10.5kaB.P.前后达最甚,与欧洲及格陵兰以及我国东部和新疆北疆地区等基本一致。
短句来源
     Results show that the spatial distribution of summer extreme precipitation in East China is significantly correlated with the same season SST in the sea area of 130~170°E,5~25°N;
     结果表明,我国东部夏季极端降水与同期太平洋SST的遥相关主要在太平洋130~170°E,5~25°N之间海域;
短句来源
     In rift basins of East China occurs mantle source gas pool with 3He/4He ratio of 2.7~6.4Ra, and such mantle gases migration and accumulation are related to the regional deep faulting.
     我国东部裂谷盆地中存在3He/4He比值为2.7~6.4Ra的幔源气藏,幔源气的运移和聚集成藏与区域深大断裂有关。
短句来源
     CO_2/3He ratio of the mantle-derived CO2 gas pools ranges from 107 to 1013 in petroliferous basins in East China. This differs greatly from the constant CO_2/3He ratio of 2×109 ~ 7×109 of the manile-derived CO2 gas whileSeparatng from the basalt magma.
     我国东部含油气盆地幔源CO2气藏的CO2/3He比率在107-1013之间,与幔源气体脱离玄武岩浆时恒定的CO2/3He比率(2×109~7×109)相比较发生了很大的变化。
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  eastern china
This trend was similar to that in western China, and distinctly higher than that in eastern China.
      
Floristic analysis and distribution pattern of alien plants in Shandong Province, eastern China
      
Bird community patterns in response to the island features of urban woodlots in eastern China
      
canadensis has become an invasive weed in eastern China, and has caused serious damages to agricultural production and ecosystems in several provinces in China.
      
Study on successions sequence of evergreen broad-leaved forest in Gutian Mountain of Zhejiang, Eastern China: species diversity
      
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  in eastern china
This trend was similar to that in western China, and distinctly higher than that in eastern China.
      
Bird community patterns in response to the island features of urban woodlots in eastern China
      
canadensis has become an invasive weed in eastern China, and has caused serious damages to agricultural production and ecosystems in several provinces in China.
      
This discovery is important because it can help us have a further understanding of the mechanism of magma degassing and accumulation of the inorganic CO2 in eastern China.
      
Bohaiwan basin, covering an area of 200 000 km2, is one of the most important oil-bearing basins in Eastern China.
      
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  east of china
The impact of modifications of the surface characteristics on local climate is simulated with a numerical mesoscale model in the Yangtze delta region, east of China.
      
In this evolution process, several scattered lakes merge into one large lake in the east of China.
      
Similar fjords are easily found along the east of China and they share a similar origin because of the Quaternary glaciation in the region.
      
In the Dawu Well Field, a karst-fractured aquifer in Zibo City, in the east of China, has been seriously polluted by petrochemicals from the operation of petrochemical plants.
      
The east of China became the south-east monsoon area, whereas the south-west became the south-west monsoon area and the north-west turned into an arid inland region.
      
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Using radio-soundings and pilot ballon wind observations of January andJuly 1956,the water vapour transfer and water balance over Eastern Chinaare calculated.Together with the seasonal variations of monsoon circulation,the transferof water vapour in summer is quite different from that in winter.However,in both seasons the inflow of water vapour from the south are much moretmportant than that either from west or from north.In comparison with theiotal transfer,the eddy transfer in general is less important,but...

Using radio-soundings and pilot ballon wind observations of January andJuly 1956,the water vapour transfer and water balance over Eastern Chinaare calculated.Together with the seasonal variations of monsoon circulation,the transferof water vapour in summer is quite different from that in winter.However,in both seasons the inflow of water vapour from the south are much moretmportant than that either from west or from north.In comparison with theiotal transfer,the eddy transfer in general is less important,but it is relativelyremarkable along the frequent paths of disturbances in the said season.During month of July 1956,this continent is shown to be a water sourceEvapotransporation is larger than precipitation.

本文利用1956年1月和7月探空和测风纪录,计算了我国东部大陆的水汽输送和7月的水份平衡.随着季风环流的转变,我国水汽输送冬夏有显著的不同.但无论冬夏均以南方海洋输入的水汽为最主要.在水汽的总输送量中,涡流输送一般只佔次要地位.最大涡流输送位于我国中部,冬季它与高压移动路径一致,夏季与极锋平均位置相合.1956年7月我国大陆是个水汽源地,蒸腾量大于降水量.

Based on the 10-years surface synoptic charts (1951 to 1960), monthly frequencies of cyclones and low pressure centers passing 2.5°× 2.5°latitude-longitude grids in Eastern Asia are analized and the main tracks are studied and classified.The cyclones are most frequent in middle part of Mongolia and north-east China, and none south of 20°N. Most of the low pressures occurred south of 45°N are very weak. Spring is the season of cyclonic activity.

本文利用1951—1960年的亚洲地面天气图,分月統計东亚地区(70°E以东,55°N以南)每2.5°×2.5°經緯格內低压中心通过的頻数,繪制了頻数分布图,确定出低压移动的主要路径,此外,还繪制了冬半年和夏半年低压发生(初現)頻数分布图、頻数百分率的随緯度分布和沿120°E与110°E經线上低压中心通过頻数的各月綜合图。結果得出:1.东亚大陆中緯度西风带的低压主要出現在蒙古人民共和国中部到我国的东北地区,20°N以南不出現溫带低气压;2.45°N以南的我国大陆上低压很弱,大多数不閉合,只有在我国东部或入海后才发展;3.日本东南面海上是低压路径的集中带;4.春季低压出現最为頻繁,秋季次之,夏季我国江淮流域低压有所增多。 最后,对低压路径进行了分类,把东亚的溫带低气压划为五大类和十一亚类,并对各类低压分别作了簡要的叙述。

China is one of the countries with the most numerous species of Dendrolimus in theworld. There are 13 known species. According to the research on the classification anddistribution of Dendrolimus in the country, by the Institute of Zoology, Academia Sinica,during the past years, the results indicate distinctly that their geographic distribution andthe distribution of their host-plant are closely related. Selecting the highest grade flora of China, we draw a line which divides the wholecountry into two main portions:...

China is one of the countries with the most numerous species of Dendrolimus in theworld. There are 13 known species. According to the research on the classification anddistribution of Dendrolimus in the country, by the Institute of Zoology, Academia Sinica,during the past years, the results indicate distinctly that their geographic distribution andthe distribution of their host-plant are closely related. Selecting the highest grade flora of China, we draw a line which divides the wholecountry into two main portions: the eastern and western divisions. The former, wherethe climate is humid and pine forests are luxuriant, is the main distributional region ofDendrolimus, while the latter, where weather is arid and with plenty of desert stepp-es, generally there are no Dendrolimus. At the same time, it has also been discoveredthat the distribution of Dendrolimus is not only closely related to altitude, but also tolatitude. According to the distribution of their host-plant, Larix olgensis var. koreanaand Pinus massoniana (with the isotherm of an average temperature of January at--12℃ and 0℃), we assume to subdivide the eastern division to 3 regions as north-eastern, northern and southern districts of China. In each of the districts there are dif-ferent distributions of Dendrolimus. Generally in the northeastern district of China, theD. sibiricus Tschetv. is distributed. The northern and the southern districts of China mayagain be subdivided into its own inland and coastal parts. The D. tabulaeformis Tsaiet Liu is distributed in the terrestrial and the D. spectabilis Butler in the coastal partof northern district of China. A great part of southern district of China is distributedwith coastal D. punctatus Walker, and the southwestern inland region is distributed withthe D. latipennis Walker, D. xichangensis Tsai et Liu and D. kikuchii Mats. The divisionbetween inland and coastal parts within the two districts mainly depends upon the dis-tribution of the host-plant of Pinus tabulaeformis Carr. and Pinus massoniana Lamb.

我国的松毛虫种类已知的有13种,是世界上已记载的松毛虫种类最多的国家。 根据中国科学院动物研究所历年来在国内所收集的松毛虫种类和分布的资料,结合已知主要松树种类的天然分布进行综合分析的结果,显示出松毛虫不同种类的地理分布与其寄主植物的天然分布有着密切的相关。例如西伯利亚松毛虫的分布只限制在东北地区兴安落叶松、黄花松的天然分布范围里,油松毛虫在油松分布区,赤松毛虫在赤松分布区,云南极毛虫在云南极分布区以及马尾松毛虫在马尾松分布区等。 由于这些松树种类彼此间的天然分布界限十分明显而基本上少有重迭,因此试将我国东部地区松毛虫不同种类的地理分布按照其寄主植物划分为以下三个部分、五个松毛虫区: 一、东北部分 北界大兴安岭,南至安东—沈阳线(相当于全国一月份平均-12℃等温线),是西伯利亚松毛虫主要分布区,也是兴安落叶松和黄花松天然分布所在地。故名1)西伯利亚松毛虫区。 二、华北部分 北界西伯利亚松毛虫区,南至淮河流域(相当于全国一月份平均0℃等温线),是油松毛虫和赤松毛虫主要分布区,也是油松和赤松的主要分布所在。因此可分为2区: 2)油松毛虫区 主要位置在冀热山地和黄土高原东部,是油松毛虫分布区,是油松分布...

我国的松毛虫种类已知的有13种,是世界上已记载的松毛虫种类最多的国家。 根据中国科学院动物研究所历年来在国内所收集的松毛虫种类和分布的资料,结合已知主要松树种类的天然分布进行综合分析的结果,显示出松毛虫不同种类的地理分布与其寄主植物的天然分布有着密切的相关。例如西伯利亚松毛虫的分布只限制在东北地区兴安落叶松、黄花松的天然分布范围里,油松毛虫在油松分布区,赤松毛虫在赤松分布区,云南极毛虫在云南极分布区以及马尾松毛虫在马尾松分布区等。 由于这些松树种类彼此间的天然分布界限十分明显而基本上少有重迭,因此试将我国东部地区松毛虫不同种类的地理分布按照其寄主植物划分为以下三个部分、五个松毛虫区: 一、东北部分 北界大兴安岭,南至安东—沈阳线(相当于全国一月份平均-12℃等温线),是西伯利亚松毛虫主要分布区,也是兴安落叶松和黄花松天然分布所在地。故名1)西伯利亚松毛虫区。 二、华北部分 北界西伯利亚松毛虫区,南至淮河流域(相当于全国一月份平均0℃等温线),是油松毛虫和赤松毛虫主要分布区,也是油松和赤松的主要分布所在。因此可分为2区: 2)油松毛虫区 主要位置在冀热山地和黄土高原东部,是油松毛虫分布区,是油松分布所在地。 3)赤松毛虫区 主要位置在山东半岛、辽东半岛?

 
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