助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   glacier 的翻译结果: 查询用时:0.051秒
图标索引 在分类学科中查询
所有学科
地球物理学
气象学
自然地理学和测绘学
地质学
水利水电工程
环境科学与资源利用
林业
资源科学
工业通用技术及设备
更多类别查询

图标索引 历史查询
 

glacier
相关语句
  冰川
     The velocity for the Glacier 5Y654D48 was 272 m\5a~(-1) during 1990-2000,and for the Glacier 5Y654D497 was 213 m\5a~(-1) during 1977-1990,respectively.
     结果发现:5Y654D48冰川和5Y654D97冰川分别在1990—2000年与1977—1990年间运动速度达272 m. a-1,213.1 m.
短句来源
     It is found from the abnormal ice flow velocity that the Glacier 5Y654D48 was surging during 1990-2000 and the Glacier 5Y654D97 was surging during 1977-1990.
     分析认为,5Y654D48冰川在1990—2000年、5Y654D97在1977—1990年间曾分别发生过冰川跃动.
短句来源
     Results show that from 1970 to 2000, lake area increased from 1941.64 km2 to 1979.79 km2 with a rate of 1.27 km2/a, while glacier area decreased from 167.62 km2 to 141.88 km2 with a rate of 0.86 km2/a.
     结果表明,自1970 ̄2000年期间,纳木错湖面面积从1941.64km2增加到1979.79km2,增加的速率为1.27km2/a; 流域内冰川的面积从167.62km2减少到141.88km2,退缩速率为0.86km2/a。
短句来源
     Glacier was retreating continually. Glacier area was 218.46km~2 in 1980, 216.68 km~2 in 1990, and 215.18 km~2 in 2000. During 1980-2000, glacier retreated 3.28 km~2 in total.
     冰川在不断退缩,在1980年冰川面积是218.46km~2,到1990年冰川面积减小到216.68km~2,2000年冰川面积减小到215.18km~2,1980~2000年间共减少3.28km~2。
短句来源
     A comparative analysis performed for glacier area shows that there was area shrinkage of 67 ^89 km 2 from 1962/1966 to 2001, accounting for about 6 ^2±1 ^0% of total area.
     与中国冰川编目数据对比分析,1962/1966—2001年间研究区冰川面积退缩了67.89km2,占总面积的(6.2±1.0)%.
短句来源
更多       
  冰河
     January:The glacier phase of M&A Market
     1月并购市场:处于冰河
短句来源
     Glacier Club
     冰河高尔夫俱乐部
短句来源
     Data collected over Glacier National Park of Montana show strong angular dependence.
     从Montata冰河国家公园采集的数据显示出很强的角度依赖性。
短句来源
  “glacier”译为未确定词的双语例句
     This thiosemicarbazide was treated under the catalysis of glacier acetic acid,mercuric acetate giving 2 benzyl 5 phenylamino 1,3,4 thiodiazole and 2 benzyl 5 phenylamino 1,3,4 oxadiazole respectively.
     然后分别将其在冰醋酸、醋酸汞存在下关环 ,制得 2 苯甲基 5 苯胺基 1,3 ,4 噻二唑与 2 苯甲基 5   苯胺基 1,3 ,4 口恶二唑
短句来源
     Estimated volumes of the ancient glacier dammed lakes(named Linzhi Ancient Lakes) were 2150km~(3),835km~(3),and 81km~(3) respectively.
     估计Ⅳ~Ⅱ期堰塞湖库容量约2150km3,835km3和81km3。
短句来源
     The experimental results showed that when 0.1mol glacier acetic acid was used, the most appropriate conditions were that 0.80g solid ultrastrong acid TiO2/SO42- was used as catalyst, alcohol-acid ratio was 3:1, reaction time was three hours, and reaction temperature was between 120 and 125℃. The yield of the ester was 93.21%, which was a satisfactory result.
     实验结果表明,在冰醋酸用量为0.1mol情况下,用固体超强酸TiO2/SO42-为催化剂,催化剂用量为0.80g,醇酸摩尔比为3,反应时间为3h,反应温度为120—125℃是最适宜的反应条件,酯产率可达到93.21%,实验结果较佳.
短句来源
     N-Butyl acetate has been synthesized from the basic materials glacier acetic acid and n-butyl alcohol by catalysis of solid ultrastrong acid TiO2/SO42-.
     以固体超强酸TiO2/SO42-为催化剂,冰醋酸和正丁醇为原料合成醋酸正丁酯。
短句来源
     CO_2 Emissions From Soils of the Deglaciered Region on Hailuogou Glacier in the Past 100 Years
     近百年海螺沟冰川退缩区域土壤CO_2排放规律
短句来源
更多       
查询“glacier”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  glacier
Microorganisms Found in the Basal Horizons of the Antarctic Glacier above Lake Vostok
      
Problems of such kind arise in glaciology when one estimates the stability of snow on mountain slopes or determines the catastrophic movement of a glacier; the results can also be applied to solifluction phenomena [2, 3].
      
It was assumed that the temperature at the bed of the glacier could reach the melting point due to nonstationary heating and that the conditions would be produced for motion of the glacier.
      
Here we examine the nonstationary response of a glacier to small deviations of the system parameters from critical values corresponding to the stationary state.
      
Numerical investigation and self-similar solutions of the glacier-ocean interaction problem
      
更多          


As a lofty mountain Nanshan stretches along the southern border of Kansu Corridor. In past two decades a few discussions had been given by some sdholars about its landforms and its quaternary glaciations. Based upon my field works and recent reports, we know that there are some close Connections existed between tectonic movements, geomorphic cycles and correlative deposits; and, Consequently, they may be mutually explained. according to the analysis of the facies and distribution of Cenozoic sediments, We Know...

As a lofty mountain Nanshan stretches along the southern border of Kansu Corridor. In past two decades a few discussions had been given by some sdholars about its landforms and its quaternary glaciations. Based upon my field works and recent reports, we know that there are some close Connections existed between tectonic movements, geomorphic cycles and correlative deposits; and, Consequently, they may be mutually explained. according to the analysis of the facies and distribution of Cenozoic sediments, We Know that there a peneplanation developed on the older rocks of Nanshan till pper pliocene, and the red deposits which extended over the Nansban and its adjacent regions Were laden down in the same time. Probably laterly, a crusalt movement, which included mul iple uplifts, initiated. The present geomorphic features of Nanshan are possibly resulted from them. as the dissected summit-levels, the remnants of old peneplains Can be found on many mountain tops today. As regards quaternary glaciations of Nanshan, a more important sign ification should be ascribed to the uplifts of this mountain. Perhaps boh because of the uplifts and the Climatic changs, in Nanshan two glacio pluvial periods had occured in quaternary. When the glaciers expanded all of the mountain peaks and valleys. Later on, the glacio fluvial waters were Carrying much debris and forming sedimentary units, which have been called inland molasse formation, into piedmont plain. a distinct interval, which indicat a true interglacial stage, have been found in that formation. The following table shows the main geological changes of Cenozoic of Nanshan.

河西走廊之南延伸着雄伟的祁连山,在过去20年中一些学者曾对该山的地貌和其第四纪冰期作过一些探讨。根据本人的野外工作及最近的文献资料,我们看到,在构造运动、地貌循环和相关沉积三者之间有着紧密的联系,因而,它们可以相互解释。分析岩相和新生代沉积的分布,我们得知直到上上新世,祁连山进行着准平原化的过程,同时并沉积下红色沉积,它遍及祁连山内外。后来,地壳运动开始,它包括多次上升。现代的祁连山的面貌即是多次上升的产物。古准平原的遗跡,目前可在许多山顶发现。祁连山的第四纪冰期的发生,山地上升占有重要地位,可能正是由于上升和气候变化的同时作用,祁连山发生两次冰期——多雨时期。当时冰川遍及山峰和谷地,稍后,冰融水携带大量碎屑物质带入山足平原形成内陆磨拉石建造的沉积。在该沉积岩系中发现有一清楚的间断,这代表一次真正的间冰期。祁连山新生代的主要地质事件见84页附表。

On the Tibetan Plateau, remnants of the quaternary glaciation are of general oc-curence. Cirques, U-shape valleys, glacial-scoured lakers, till plains, terminal moraines, and drift boulders are wide spread features down to 4200 m in altitude. The authors believe that there was once a fairly continuous ice cover on the Tibetan plateau in late pleistocene. Here after the snow-line was raised, and the glaciers retreated gradually to their present positions. The reasons are two-fold: (a) a general warming...

On the Tibetan Plateau, remnants of the quaternary glaciation are of general oc-curence. Cirques, U-shape valleys, glacial-scoured lakers, till plains, terminal moraines, and drift boulders are wide spread features down to 4200 m in altitude. The authors believe that there was once a fairly continuous ice cover on the Tibetan plateau in late pleistocene. Here after the snow-line was raised, and the glaciers retreated gradually to their present positions. The reasons are two-fold: (a) a general warming of the world climate, (b) dessication of Tibet due to further uplift. The latter is evidenced by the obvious shrinkage of many lakes on the plateau. By correlating the moraines of this glaciation with the terrace of Zi-Ling Tsangpo and Yamdrok, we reach at the conclusion that this great Ice Cover was of late pleistocene in age. Since that time the glacier retreated in three recessional stages:

王明业等同志这篇论文提供了不少西藏高原上古冰川沉积以及其他遗迹的资料。从这些遗迹的分布来看,肯定有一个时期冰川的范围远比现代为大,那时冰川会从一些山谷通过一些低的山口漫溢到另一些山谷中,会覆盖广大的山麓地区,甚至达到盆地的中心。也可以想见某些宽平的山顶上可能有平顶冰川或所谓冰帽覆盖。在这种情况下,冰川的厚度一定也比现代为大,冰川的类型也更复杂的多。但是对于西藏高原这样一个广大的地区来说,作者等的观察范围以及获得的资料究竟还是非常有限,在达到的地区内也未见到有巨厚的,延续很广的冰碛物存在,所以据此即说除雅鲁藏布江谷地和金沙江、澜沧江、怒江的峡谷外西藏高原断续出现的冰盖是相当普遍的(虽然作者等也声明说和格林兰、南极洲的冰盖不一样),结论似乎下得太早。所引waxler的关于晚更新世雪线下降随的资料仅适用于一般海洋性气候的冰川作用区,是否能用到象西藏这样大陆性很强的地区是值得怀疑的。但是无论如何,作者等的资料是很宝贵的,关于西藏高原古冰川覆盖类型的问题,目前也确实还难说孰是孰非,所以我们还是把本文发表出来,以供对西藏古冰川研究的参考。

Under the action of gravity, the powerful driving forces of recent tectonic movement affecting the studied plateau and adjacent areas are stemming from the crust of Qinghai-Xizang Plateau. Therefore, in Southwest China took place a flow of crustal materials toward the southeastern direction. Such flow possesses rather special nature, unlike the downhill sliding of the glacier. In the front of the flow can be found recent tectonic activities with different features due to the variations of resistance encountered....

Under the action of gravity, the powerful driving forces of recent tectonic movement affecting the studied plateau and adjacent areas are stemming from the crust of Qinghai-Xizang Plateau. Therefore, in Southwest China took place a flow of crustal materials toward the southeastern direction. Such flow possesses rather special nature, unlike the downhill sliding of the glacier. In the front of the flow can be found recent tectonic activities with different features due to the variations of resistance encountered. Moreover, the occurrence of earthquakes in Southwest China is also constrained by the material flow.The authors suggest that since the driving forces of recent tectonic activities in this area are in close relation to gravitational effect, the localized recent tectonic processes would be ascribed to the category of gravity tectonics.

在重力作用下,青藏高原巨厚的地壳成为高原及其邻区现代构造运动的强大动力源。在其驱动下,我国西南地区存在着往南东方向运动的地壳物质流,它具有独特的运动方式,与冰川下滑运动有所不同。在地壳物质流动过程中,由于阻力的差异,可以表现出不同的构造活动性。西南地区地震的发生受到地壳物质流动的控制。西南地区现代构造运动的动力源与重力关系十分密切,因而可属于重力构造范畴。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关glacier的内容
在知识搜索中查有关glacier的内容
在数字搜索中查有关glacier的内容
在概念知识元中查有关glacier的内容
在学术趋势中查有关glacier的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社