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central-south
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  中南
     METHODS: The experiment was conducted at the Test Center, Public Health School, Central-south University from March to July 2004. Forty Kunming mices were selected and divided randomly into 4 groups: control group, hyperlipidemia model group, 0.2 and 0.5 mg/g algin groups with 10 mice in each group.
     方法:实验于2004-03/07在中南大学公共卫生学院测试中心完成,选择昆明种小鼠40只,随机分为4组,即对照组、高脂模型组及褐藻酸0.2,0.5mg/g组,每组10只。
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     Five representative samples obtained from central-south Chinahave been analyzed by this method with an error of less than 2% for carbon and 0.05% forhydrogen.
     由中南地区的五个代表性煤样所得C含量误差<2%,H含量误差<0.05%。
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
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     The history of postgraduate's education in the Central-South Industry university is the epitome of reform and development of postgraduate's education in china.
     中南工业大学的研究生教育历史是中国研究生教育改革和发展的缩影。
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     The Research on Modern Conversion of the Modality Characteristic of the Traditional Folk Residence in Hunan Central-South Region
     湘中南地区传统民居形态特征的现代转换研究
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     The Islamic Revival Movement in Central-South Asia and Its Influence on China
     论中南亚的伊斯兰复兴运动及对中国的影响
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     JIA-2 MENBER GAS RESERVOIR FORMING CONDITIONS AND THE MAIN CONTROLLING FACTORS IN THE CENTRAL-SOUTH SICHUAN TRANSITIONAL ZONE
     川中川南过渡带嘉二段成藏条件及主控因素
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     The location data of 10 earthquakes sequences of central-south America for the period 1960-1990 are collected.
     共搜集到1960~1990年中、南美洲地区10个地震序列。 其中1个是板内地震序列。
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     All these species belong to the Oriental Realm, of which 4 species belong to the South China Region accounting for 36.4%, 7 species belong to the Central-South Region accounting for 63.6%, 2 species areendemic to Hainan Island accounting for 18.2%.
     海南岛淡水龟物种密度为 3 2种 1 0 4km2 ,均为东洋界成分 ,其中华南区种 4种 ,占 3 6 4% ;
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     This article presents a systematic pathology study of inclusion body hepatitis of avian among 32 million chickens of 87 chicken farms during the period of 1994—1995 in the central-south section of Hebei province.
     介绍了河北省中南部地区 1 994— 1 995年间 ,87个鸡场 ,32 0 0万只鸡发生鸡包涵体肝炎的系统病理学研究。
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  相似匹配句对
     Central South Carolina Alliance
     州中联盟—南卡州招商引资的中流砥柱
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     Xiangya Hospital of Central South University
     中南大学湘雅医院新医疗区
短句来源
     CENTRAL-SOUTH ARCHITECTURAL DESIGN INSTITUTE
     中南建筑设计院
短句来源
     FEATURE OF THE EARTHQUAKE SEQUENCES OF CENTRAL-SOUTH AMERICA
     中南美洲地区地震序列的特征
短句来源
     CRETACEOUS NON-MARINE LAMELLIBRANCHIA FROM CENTRAL-SOUTH CHINA
     中南地区白垩纪淡水瓣鳃类
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  central-south
On a seasonal basis a decreasing trend is significant only for spring in Central-South, and for autumn in the North.
      
On a yearly basis a decreasing trend is present over all Italy, but it is statistically significant only in the Central-South.
      
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
      
Effects of Weak Acids on Canopy Leaching and Uptake Processes in a Coniferous-Deciduous Mixed Evergreen Forest in Central-South
      
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The natural vegetation of Shantung Province, in the north temperate zone, is of the aestisilvae type. As the natural conditions vary in different parts of this province, the vegetation may be divided into the following four regions: 1. Alluvial plain of the Yellow River: This region is located at the northern part of this province. The saline soil is unfavorable for the growth of most plants. The following plants are characteristic: Tamarax chinensis, Apocynum venetum, Suaeda salsa, S. glauca, Artemisin capillaris,...

The natural vegetation of Shantung Province, in the north temperate zone, is of the aestisilvae type. As the natural conditions vary in different parts of this province, the vegetation may be divided into the following four regions: 1. Alluvial plain of the Yellow River: This region is located at the northern part of this province. The saline soil is unfavorable for the growth of most plants. The following plants are characteristic: Tamarax chinensis, Apocynum venetum, Suaeda salsa, S. glauca, Artemisin capillaris, Aeluropus littoralis, Miscanthus sinensis, Phragmites karka, Carex sp. etc.. 2.Western Shantung plain: This region is located at the western part of the province. Most of the land is under cultivation and the soil is rich in calcium. There is no forest. The common trees are Populus tomentosa, P. alba P. davidiana, Ulmus spp. etc., and the herbaceous plants are Cynodon dactilon, Digitaria sanguinalis, Echinochloa colonum, Imperata cylindrica, Chenopodium album, Convolvulus chinensis,Xanthium japonicum, Crypi saculeata, Scirpus maritimus etc.. Plants which grow in the lake district largely belong to Phragmites communis, Scirpus maritimus, Zizania latifolia, Euryale ferox, Trapa bispinosa etc.. 3.Central South hilly region: This region has mostly been transformed into farms for a long time. On the hilly region there are still some remnant forests. The important trees are Pinus tabulaeformis, Biota orientalis. Quercus acutissima, Q. variabilis, Betula chinensis, Tilia mongolica etc.. On account of calcareous soil in this region, Biota orientalis is found most extensively. Gramineae leads all other herbaceous plants in abundance. The following species such as Arundinella amomala, Bothriochloa ischaemum, Setaria viridis, Pennisitum flaccidum etc. have a wide distribution. 4. Shantung Peninsula: The common native plants in this region are Pinus densiflora, Quercus dentata, Q. acutissima, Robinia pseudoacacia, Acer mono etc.. Pious densiflora is a native plant which grows all over the hilly region. Herbaceous plants are mostly Thymus serpyllum, Setaria viridis, S. lutescens etc.. Due to the oceanic climate with higher precipitation and humidity, plants enjoy a more vigorous growth than those in other regions. There develops a richer flora, some even with warm temperate elements.

山东省之位置属于温带,植物分布为落葉闊葉林區,但在鲁中南及膠東區爲丘陵地带,落葉闊葉樹乃與針葉樹成混交林澑鶕∧谥匀粭l件,可将植物分布情况列為四區: 1.黃河冲積平原區:位於北部,為黄河三角州地帶,土壤含鹽分甚重,不宜於植物之生長。樹木只有檉柳、茶棵子等;草本以黄鬚菜、鹼蓬、茵陳蒿,獐毛、芒、蘆葦、黑三稜草等最為砇姟?2.魯西平原區:為西部之黄河冲積平原,多為農田,土壤含鈣甚多。區內無森林,常見之樹木有毛白楊、白楊、山楊、榆等?荼居泄费栏ⅠR唐、芒稷、白茅、藜、旋花、蒼耳、隱花草、荆三稜等。湖泊區域多蘆葦、荆三稜、蒲姜草、芡、菱等。3.魯中南區:為丘陵地區,平緩部分已闢為農田。山區有殘留森林,主要樹種為油松、侧柏、麻櫟、栓皮櫟、堅樺、椴等;土壤石灰質,側柏之繁盛為共特點。草本以禾本科為最多,常見的如野古草、白羊草、狗尾草、白草等,此外如細葉莎草、雞眼草、蚊子草等亦為砇姟?4.膠東區:在山東半島部份,主要樹種為赤松、洋槐、麻櫟、五角楓等,赤松自山麓至山上均有分佈,且為其鄉土,此乃本區之特徵;草本以蚊子草、狗尾草、金狗尾草為最多。在海灘地上少有高大樹木,常見樹種如洋槐、旱柳等均為栽培者,野生木本植物有酸棗...

山东省之位置属于温带,植物分布为落葉闊葉林區,但在鲁中南及膠東區爲丘陵地带,落葉闊葉樹乃與針葉樹成混交林澑鶕∧谥匀粭l件,可将植物分布情况列為四區: 1.黃河冲積平原區:位於北部,為黄河三角州地帶,土壤含鹽分甚重,不宜於植物之生長。樹木只有檉柳、茶棵子等;草本以黄鬚菜、鹼蓬、茵陳蒿,獐毛、芒、蘆葦、黑三稜草等最為砇姟?2.魯西平原區:為西部之黄河冲積平原,多為農田,土壤含鈣甚多。區內無森林,常見之樹木有毛白楊、白楊、山楊、榆等?荼居泄费栏ⅠR唐、芒稷、白茅、藜、旋花、蒼耳、隱花草、荆三稜等。湖泊區域多蘆葦、荆三稜、蒲姜草、芡、菱等。3.魯中南區:為丘陵地區,平緩部分已闢為農田。山區有殘留森林,主要樹種為油松、侧柏、麻櫟、栓皮櫟、堅樺、椴等;土壤石灰質,側柏之繁盛為共特點。草本以禾本科為最多,常見的如野古草、白羊草、狗尾草、白草等,此外如細葉莎草、雞眼草、蚊子草等亦為砇姟?4.膠東區:在山東半島部份,主要樹種為赤松、洋槐、麻櫟、五角楓等,赤松自山麓至山上均有分佈,且為其鄉土,此乃本區之特徵;草本以蚊子草、狗尾草、金狗尾草為最多。在海灘地上少有高大樹木,常見樹種如洋槐、旱柳等均為栽培者,野生木本植物有酸棗、舖地胡枝子等;草本植物多蘆葦、狗尾草等。此區氣候由於受篞笳{節,雨量與溼度亦較高,故植物生長較其他三區繁盛,種類亦較多,亞熱带植物之分布亦多於他處,尤以海邊低地為甚。在自然地理上,秦嶺、淮河一線是中國南北氣候和土壤的重要分界線,也是植物的重要分界線。但是從山東的植物分布上,可以知道這條線並不能絕然的将植物分為南北二部分,因為山東仍是一个過渡的地帶,許多南方植物在魯南及膠東沿海都有分佈,如黄檀、山胡椒、烏桖、厚朴、王蘭、木犀、黄楊、谜葉樹等多种。在另一方面,北方植物分佈至山東為其最南界限者如糠椴、遼珍珠梅、遼磯松、榛等;而赤松、蒙古機、蒙椴等則南达苏北之雲台山。由此可加,山東之植物分佈上,仍在秦嶺、淮河一線之範圍内,如以淮河來作為植物之南北分界線,则并不能完全符合實際情况,尤以膠東沿海低地,南方植物種類繁多,可與淮河流域相此。因此,此一分界线之東端似有北移之必要。山東植物之分佈乃由環境条件综合影響之結果,但在不同地区,各種因素之作用並不一致,由於地形、土壤、温度和水分等之区别而使植物分布不同。本文所举植物種类和分布地點都是從各項资料所得到,作者将其分為四區,並初步提出了這種分区的理由和形成不同分布的原因。但限於材料的不够完全和水平的淺薄,因此本文的內容很不充實, 只能作为令後进一步研究山东植物地理的基础,希望大家提出补充和指出不正确的地方,而使这一项工作能够顺利的完成。

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。

China abounds in hydropower resources. Due to precipitation and topographical features, these resources concentrate principally in the Southwest, Central South and Northwest Regions. In Eastern China (including East, North and Northeast Regions), hydropower potential is comparatively less and is mainly used for taking up the peakload of thermal-based electric system, while in western China, hydropower resources are so abundant that hydroelectricity forms the bulk of electric energy supply, and the long distance...

China abounds in hydropower resources. Due to precipitation and topographical features, these resources concentrate principally in the Southwest, Central South and Northwest Regions. In Eastern China (including East, North and Northeast Regions), hydropower potential is comparatively less and is mainly used for taking up the peakload of thermal-based electric system, while in western China, hydropower resources are so abundant that hydroelectricity forms the bulk of electric energy supply, and the long distance transmission of electric power from the West to the East will play an important role in the near future.During the past 32 years, many hydropower projects have been accomplished in China. By the end of 1981, the total installed generating capacity of water power in China had been about 22 GW(the annual output of 1981 being 65 Twh), which is only 3% of the exploitable potential. So, the prospect of hydroelectric power development in China is very brilliant.

中国的水能资源非常丰富。由于降水和地形条件的影响,水能资源主要集中在西南、中南和西北地区。东部地区(包括华东、华北和东北地区)水能资源比较少,电力系统中以火电为主,水电主要担负峰荷。西部地区水能资源很丰富,电力工业以水电为主,并要考虑远距离输电,进行西电东送。三十二年来中国的水电建设成就很大。现有水电总装机容量约2200万千瓦,水电年发电量650亿度,但仅相当于可能开发水能资源的3%。在中国开发水电的前途很广阔。

 
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