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     The results show that the thin strip under 0.1mm can be obtained through forcible large deformation hot extrusion cogging of Ag-Cu-In-Sn alloy whose In+Sn content is 20%, and the rate of finished product can get to 60% above.
     结果表明:对In+Sn含量为20%的Ag-Cu-In-Sn合金钎料,采用强制大变形热挤压开坯,可得到0.1mm以下的薄带钎料,成材率达到60%以上;
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     Remove rate of Cr(VI) may get to 66.9%,more 22.1% and 37.8% than its of PAC and PFC.
     对重金属六价铬的去除率可以达到66.9%,比较PAC和PFC六价铬的去除率22.1%和37.8%,提高了很多。
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     chitosan density 0.050%,0.045%,0.030% get to optimal effect each after lh,5h,12h.
     浓度为0.050%、0.045%和0.030%分别在1h、5h和12h后达到最佳效果。
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     The yield of delignification decrease to 3.4%,the rate of removed delignification get to 85.0%,the purification of extracted hemicellulose get to 84.8% after chlorite treatement of bagasse;
     蔗渣经亚氯酸钠脱木素后,木素含量降到了3.4%,木素脱除率达到85.0%,抽提出的半纤维素纯度达到84.8%;
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     The maximum of COD can get to 48.2 mg/L , PO43- can get to 0.04 mg/L and NH3- can get to 5.83 mg/L . The program of harnessing the moat we research are follow .
     COD_(Cr)最大达到48.2mg/L,NH_3—N最大达到5.83mg/L,PO_4~3—P最大达到0.04mg/L。
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  “get to”译为未确定词的双语例句
     The favorable callus induing medium was MS+6-BA 0.5 mg/L+2,4-D 0.5 mg/L or 2,4-D 1.0 mg/L. The callus induction frequency could get to 100%.
     最适愈伤组织诱导培养基为MS+6-BA 0.5 mg/L+2,4-D 0.5 mg/L或2,4-D 1.0 mg/L,愈伤组织诱导率均可达100%。
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     The optimal experimental parameters were 35 MPa extraction pressure,50 ℃ extraction temperature,3 h extraction time,40 meshes material granularity,95 % alcohol entrainer,1:2 materiel-liquid ratio,45 kg/h CO2 velocity,the yield of apple polyphenol may get to 0.1 %.
     最佳萃取实验工艺条件为:萃取压力35MPa,萃取温度50℃,萃取时间3h,物料粒度40目,夹带剂95%乙醇,料液比(g:mL)1∶2,CO2流速45kg/h,得率为0.1%。
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     Results:WS values get to the peak at about ω=2.5Lp/mm.
     结果:(1)在主扫描方向上总WS值的高频区(ω=2.5Lp/mm左右)出现峰值;
     Results:WS values get to the peak at about ω=2.5Lp/mm.
     结果 :( 1)在主扫描方向上总WS值的高频区 (ω =2 .5Lp/mm左右 )出现峰值 ;
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     It detectsthe object's position, and its accuracy and linearity get to 19.3μm/nW 94.6%,respectively
     它采用差分式结构实现物位探测,其测量灵敏度可达19.3μm/nW,线性度可达94.6%。
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     Get in the Game
     进入 游戏世界
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     Get On The Ball
     爬到球上去
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     They can't get into S? .
     (2)能进入S_1:“NP_1比NP_2更+_。”
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     Get to know Cambodia
     柬埔寨五日文化探秘
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But in addition to setting wage levels, determinations also delineate which jobs get to have rates set for them, and perhaps most critically, whether those delineated are identified as union or notunion.
      
This paper is concerned with the behaviour of lottery players when they get to choose their own numbers.
      
Some people might think that rather funny, but I must take good care they don't get to hear of it." And then he praised the material which he couldn't see and assured them of his delight in its charming shades and its beautiful design.
      
By means of a construction of particular multipoint iterations, we get to improve the best situation obtained for one-point methods.
      
We study topology control problems in ad hoc networks where network nodes get to choose their power levels in order to ensure desired connectivity properties.
      
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The post-irradiation effects of 30% TBP-Kerosene-HNO3 systems have been investigated by means of the hafnium number test. It has been found that a delayed variation process of long duration of the hafnium numbers after irradiation occurs when the dose is greater than 5×106 rads. This variation process can be stopped by lowering the temperature to that of liquid nitrogen and it does not appear when the dose is lower than 4.59×105 rads. The general rule is that the values of the hafnium numbers drop rapidly after...

The post-irradiation effects of 30% TBP-Kerosene-HNO3 systems have been investigated by means of the hafnium number test. It has been found that a delayed variation process of long duration of the hafnium numbers after irradiation occurs when the dose is greater than 5×106 rads. This variation process can be stopped by lowering the temperature to that of liquid nitrogen and it does not appear when the dose is lower than 4.59×105 rads. The general rule is that the values of the hafnium numbers drop rapidly after irradiation, then rise slowly, and finally get to an equilibrium value, The variation process can not be changed by sodium hydroxide solution and nitric acid solution scrub. These results suggest that the permanent and detrimental degradation products formed in irradiated 30% TBP-kerosene systems are secondary products. The effect of nitric acid concentration on the hafnium numbers has been studied. It has been found that there is a maximum at 0.5 N HNO 3 in aqueous phase for the starting values of the hafnium numbers as reported in most of the literatures.But under equilibrium conditions there is a minimum of the hafnium numbers at 0.5N HNO 3 and a maximum at 1N HNO 3. It is now universally accepted that the formation of the permanent and detrimental degradation products is the most favorable for 30% TBP-kerosene systems at 0.5N HNO3 in aqueous phase. Our experimental results show that this opinion is one-sided. In addition, we have examined effects of the methylation by diazomethane on the hafnium numbers. It has been found that the values of the hafnium numbers drop greatly after the methylation. It is indicated by the results of the methylation experiments that the detrimental degradation product is a substance containing active hydrogen.

本文借助铪指数实验研究了30%TBP-煤油-硝酸体系的辐照后效应。发现在上述体系中,当辐照剂量大于5×10~6拉德时,铪指数有一个持续很久的变化过程。这一变化过程能借助液氮的低温使其停止变化。当辐照剂量低于4.59×10~5拉德时就没有这个变化过程。实验证明,除了铪指数的“起始值”外,还存在一个“平衡值”,两者有很大的差别,因此,文献上所提出的0.5N的水相硝酸浓度对生成永久性有害降解产物是最有利的浓度这一结论是不全面的。实验结果表明,有害降解产物是一个含有活泼氢的次级辐解产物。

The Yangtze River Estuary is an estuary with large amount of runoff and strong tide. The average discharge of the Yangtze River is only 29,400 m3/s, while the average discharge of flood tide may get to 227,400 m3/s. The amount of sediment is about 483 million tons/yr. The dynamic interaction of these two strong forces leads to form the Yangtze River Estuary. According to the regional geological and geomorphological characteristics and their effects on heavy minerals of sediment, the source of the sediment...

The Yangtze River Estuary is an estuary with large amount of runoff and strong tide. The average discharge of the Yangtze River is only 29,400 m3/s, while the average discharge of flood tide may get to 227,400 m3/s. The amount of sediment is about 483 million tons/yr. The dynamic interaction of these two strong forces leads to form the Yangtze River Estuary. According to the regional geological and geomorphological characteristics and their effects on heavy minerals of sediment, the source of the sediment at the Yangtze River Estuary can be considered as coming from 3 supplying regions, namely, the Yangtze River upstream(x1),the abandoned delta of the Yellow River at the north of Jiangsu Province (x2) and the Hangzhou Bay (x3). The converging region is the Yangtze River Estuary (y). Sampling stations are set up in the supplying regions and the converging region. According to the statistics of heavy minerals of nearly 20,000 grains of sediment collected during geological and geomorphological investigations, the author holds that heavy mineralogical characters of sediment of the Yangtze River Estuary are governed by the geological and geomorphological conditions of the watershed. According to the principle of equilibrium of sediment load, equations of the heavy mineralogical classification are presented.By means of Least Squares Method, a normal equation for calculating the converging percentages from all the supplying regions is given below:Where are the coefficients related toheavy minerals. The result shows that 96.1% of the sediment comes from the Yangtze River upstream, 7.0% from the abandoned delta of the Yellow River and-3.1% from the Hangzhou Bay.When the converging percentage of sediment from the Yangtze River upstream is known, and the total amount of sediment at Datong station is also known as 483 million tons per year, the amount of sediment at the Yangtze River Estuary (d>0.01mm) is computed, which is 359 million tons per year. This value agrees quite well with the value of 349.4 million tons per year calculated from the topographic maps of 1915 and 1963 of the Yangtze River Estuary.

根据长江口及其补给区的大量泥沙的重矿物鉴定表明,沙样中重矿含量百分数较为稳定,故能用矿物分析法计算出长江口泥沙(d>0.01毫米)的来源与数量.计算表明有96.1%来自长江补给区.据长江大通站多年平均的年输沙量推算,长江口的泥沙量为3.590亿吨/年.经1915年和1963年的长江口实测地形图比较量算的验证,两者相差2.7%.本研究法对于河口无泥沙测验与地形测量资料的情况下,研究泥沙来源与数量具有理论与实际的意义.

The dissipative structure is an ordered structure. When a system is far away from state of equilibrium in the condition of nonequilibrium and interchanges some energy and material with outside circumstances, this structure will be formed and maintained. Starting from analysing practical data, we attempt to use this theory, and discuss the tectono-geochemical problem of some rock and ore formation systems in faults.1. Ordered structure. In the geological condition, this is due to the open system in which there...

The dissipative structure is an ordered structure. When a system is far away from state of equilibrium in the condition of nonequilibrium and interchanges some energy and material with outside circumstances, this structure will be formed and maintained. Starting from analysing practical data, we attempt to use this theory, and discuss the tectono-geochemical problem of some rock and ore formation systems in faults.1. Ordered structure. In the geological condition, this is due to the open system in which there are energy and material in geochemical action, so that the entropy gradually tends to reduce and substance get to evolved from non-order to ordered structures. In the process of rock and ore formation in faults, various layer-bands and layer-levels will be formed in rock material.2. Functional action: The activities of physics-chemistry which include a pressure-creeping and thermal-diffusing as well as liquid over-flowing have been shown. 3. Fluctuating cycIe: In the process of metamorphism of rock and ore formation in faults, various changes of pressure, temperature and liquid show a fluctuating wave and periodic cycle. This plays an important part in the occurrence of rock and mineral and the formation of ordered structures in fault zones.4. The above-mentioned ordered structure, functional action and fluctuating cycle are mutually related to each other as following correlogramFinally, we have cited a few examples of mineral deposits in the middle and lower reaches of the Yangtse River, and the dissipative activities of rock-forming minerals and mineral-forming elements have been preliminarily established.

借鉴于耗散结构(Dissipative structure)理论,从非平衡态的观念探讨了断裂成岩成矿系统中的有关问题。其中包括:开放系统、有序结构、功能作用和涨落旋回等。

 
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