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一冷
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  a cold
     Every year during late spring and summer, a cold water area exists on the sea surface near the east side of Subei (northern Jiangsu) shoal patch.
     每年春夏之际,在紧靠苏北浅滩东侧海面有一冷水域存在。
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     At sub-surface layer, there exists a cold core structure in the middle part of the west Indian Ocean and to the south of equator.
     在热带印度洋的中西部、赤道偏南海域的次表层终年存在一冷心结构;
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     The characteristics of Jinta Oasis on 5 July, 2004 was successfully simulated using the mesoscale model MM5 on the basis of replacing the landuse in the domain 3. The simulated results showed that in the day time, the oasis was a cold source, it maintains till 3000 m above the ground and the temperature-difference between the oasis and desert was the highest near the ground and the intensity of cold center weakened from low level to high level;
     利用中尺度数值模式MM5,替换了模式第三重嵌套模拟域中金塔绿洲及周围地区与实际不符的植被类型,对2004年7月5日金塔绿洲效应进行了较为成功的模拟。 模拟结果显示:白天绿洲是一冷源,这一现象可维持到3000m左右,临近地面沙漠绿洲温差最大,冷中心强度由低层向高层逐渐减弱;
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  primary cooling
     The paper analyzes the formation of grade 20 steel CC bloom surface longitudinal cracking in view of primary cooling and mould slag, discusses measures to eliminate cracking. Cracking ratio reduced from 39. 8% to 0. 30%.
     从一冷、保护法方面分析了20钢 (180连铸坯表面纵裂纹的形成原因,探讨了防止该裂纹的措施,使20钢 (180 铸坯表面纵裂纹出现率由原来的39.8%降为0.30%。
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  “一冷”译为未确定词的双语例句
     Besides, another cold water area is commonly observed on the surface in the region 32°N and 124°—124.5°E during late spring and summer.
     另外,春夏期间在32°N,124°—124°30′E海面,也经常观测到另一冷域的存在。
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     The effects of dissolution and precipitation of M_(23)(C,B)_6 during heating at
     含硼量不同的钢具有一个相同的临界冷却速度,在这一冷速下,M_(23)(C,B)_6,的析出量达到饱和。 M_(23)(C,B)_6的溶解、析出对淬透性和韧性有很大影响。
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     However,new style industrialization and urbanization of Chongqing are separated.
     然而重庆市新型工业化和城镇化进程中却出现了一热一冷“两张皮”现象。
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     The existence of the deep ditches on the north side of the under water delta off Subei decides the position fixation of this cold water.
     而苏北外海水下三角洲北侧海底深沟的存在决定了这一冷域的位置。
短句来源
     The main cause of the cold water area is the monthly southward migration and the climbing up against the slope of deep cold water frown the western part of the south Huanghai Sea (Yellow Sea).
     黄海西南部深层冷水的逐月南移并逆坡爬升是这一冷域的主要成因;
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  相似匹配句对
     L-1 h for buccal tablet and syrup respectively .
     L’.
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     一.
     .
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     An Application of Cold Plate Leveler
     矫直机应用
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     Heat Treatment of a Cold Working Roller
     轧辊的热处理
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     On cold fusion
     核聚变
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  a cold
The results could be valuable for using the ZnO nanostructure as a cold-cathode field-emission material.
      
These strains provide a basis for developing biodegrader preparations applicable to the bioremediation of oil-polluted sites under the conditions of a cold climate.
      
It was shown that most of the flow in the pores filled with water is directed toward a cold side and can be calculated using the disjoining pressure isotherms of unfreezing interlayers.
      
Potential drop in a laminar boundary layer on a cold electrode
      
The self-similar problem of the motion of a cold gas subjected to an instantaneous impulse is considered.
      
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  primary cooling
Primary cooling γ' precipitate size and volume fraction are considered in terms of their effects on the macroscopic stress-strain response and on distributed cyclic microplasticity within the SVE.
      
A fast and selective method has been developed for the separation of the iodine fission products in the primary cooling water of nuclear reactors.
      
The obtained values are in good agreement with literature and clearly reflect the widely different boundary conditions associated with primary cooling (contact with the mold) and secondary cooling (water jet).
      
The model, based on the commercial finite-element package ABAQUS, includes primary cooling via the mold, secondary cooling via the chill water, and ingot-base cooling.
      
Tensile tests were performed on alloy Al-4.5 pct Cu with a solidification unit dubbed the direct chill surface simulator (DCSS) that simulates the primary cooling conditions encountered during the direct chill (DC) casting process of sheet ingots.
      
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First in this paper the mean 2-year mean winter and summer wind fields below 6kmover Tibetan Plateau and its surrounding are presented.In winter the main features on 1.5km(fig.1)and 3 km(fig.2)level are the splitting of the westlies over the plateau,the lineof convergence to the east of the plateau and the“dead-water”regions(characterized by calmwind and little disturbances,except small local vortices)respectively to the east and west of theplateau.On 6km(fig.4)the minor features disappear but the splitting...

First in this paper the mean 2-year mean winter and summer wind fields below 6kmover Tibetan Plateau and its surrounding are presented.In winter the main features on 1.5km(fig.1)and 3 km(fig.2)level are the splitting of the westlies over the plateau,the lineof convergence to the east of the plateau and the“dead-water”regions(characterized by calmwind and little disturbances,except small local vortices)respectively to the east and west of theplateau.On 6km(fig.4)the minor features disappear but the splitting is still evident.Insummer in the vicinity of the plateau low level wind blows cyclonically around it(fig.6—7).Surround this large cyclonic whirl are small systems.On 6km(fig.8)the wind blows anticy-clonically around the plateau.The center of the this anticyclone may be located at the SE cornerof the plateau.This kind of vertical structure of this wind field indicates that the temperatureover the plateau is higher than the surrounding.The region of high temperature is estimated toreach at least as high as 9 km.There is strong vertical motion in the vicinity of the plateau.In winter on its SE the motionis upward,while in the rest of the region the motion is in the main downward.In summer themean motion fundamentally upward velocity reaches about 1 cm/sec,on 6km.Mean advection and temperature gradient(fig.5 for winter and fig.9 for summer)between 3—6km are also calculated from the wind data under geostrophic assumption.Secondly the heat balance over the plateau is estimated from the calculation of short waveabsorption,codensation heating,long wave cooling,temperature advection,adiabatic cooling(or warming)due to vertical motion and turbulent heat transfer from the ground.From thiscalculation it is concluded that Tibetan Plateau is a heat source in summer,while in winter theresult is not very conclusive.Probably in winter the SE part of it plays a role of warm sourcewhile the rest of the plateau plays a role of cold source.

本文利用1954—1956年的高空及地面记录,作出了平均流场,并计算了垂直速度、冷暖平流及辐射等,得出下面几点结论:1)冬季在1.5千米及3千米的西风,在高原西边有明显的分支,东边有明显的会合,且在东西两边各有一“死水区”(风速很小),在高原北面形成了高压脊,而在其南面形成了低槽,到了6千米除了二个“死水区”消失以外,其余基本上没有变化。2)夏季1.5千米及3千米在高原附近的流线,绕高原作气旋性旋转,而到了6千米则相反而呈反气旋性旋转,其中心在高原西南部分,且随高度增加而向西偏。3)夏季在高原上基本上是上升运动,可能达到9千米;冬季在高原上估计可能是下沉运动(除西南角有部分上升运动)。4)夏季可以肯定高原是一个热源,而冬季除了西南角有—部分是热源外,其他地区可能是一冷源。

The effects of dissolution and precipitation of M_(23)(C,B)_6 during heating at

采用定量相分析,硼自射线照象等技术,对不同含硼量的中碳钢40 MnB,在高温加热及冷却过程中,M_(23)(C,B)_6的溶解、析出行为及对钢性能的影响进行了研究。发现析出的M_(23)(C,B)_6的数量及粒度随着钢中的含硼量增加及冷却速度的减小而增加;含硼量不同的钢具有一个相同的临界冷却速度,在这一冷速下,M_(23)(C,B)_6,的析出量达到饱和。M_(23)(C,B)_6的溶解、析出对淬透性和韧性有很大影响。含硼量较低的钢,在相同条件下M_(23)(C,B)_6的析出量较小,且易于溶解,故钢具有较好的综合性能,并对热履历的变化不敏感。提出了一些稳定钢性能的建议。

The cold cracking susceptibility of six marks of HSLA steels has been investigated by means of the implant test and discussed as to the effects of chemical composition of the steels, diffusible hydrogen of the welded zone and maximum hardness under bead.

本文采用插销试验方法研究了六种国产低合金高强钢的冷裂敏感性;讨論了各种材料的化学成份,接头含氢量和最大硬度对冷裂敏感性的影响。试验结果表明,采用热影响区最大硬度较Pcm,可以更好地反映热影响区微观组织对钢材冷裂敏感性的影响。在插销试验的基础上,归纳出如下的关系式: σ_(cr)=132.3-27.5lg([H]+1)-0.216HV+0.0102t_(100) 这一冷裂敏感性的判据对于扩大插销试验的应用是有意义的。

 
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