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新平衡
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  new balance
     The Application Research of New Balance Scorecard
     新平衡记分卡的应用研究
短句来源
     Another of the new balance theories of ASC hydraulic pumping units——complete balance method
     ASC液压抽油机的新平衡理论之二——完全平衡函数法
短句来源
     Different from dexamethasone, the new balance due to anti-IL-9 antibody would not lead to a series of effects on account of cell immunity fun-(ction) suppression in the immune response.
     与Dex相比,应用抗IL-9抗体建立的新平衡不会造成因细胞免疫功能受抑引起的一系列不良反应。
短句来源
     One of the new balance theories of ASC hydraulic pumping units-max (min) criterion
     ASC液压抽油机的新平衡理论之一——最大(小)值判据法
短句来源
     Whether it is modern knowledge view or post-modern ones, they all hope to discover a view of curricular knowledge rooted in "curricular knowledge" itself rather than in common knowledge so as to attain a new balance between "curriculum" and "knowledge".
     无论是现代主义课程知识观,还是后现代主义课程知识观(二者共同构成现代课程知识观)都期待探索一种立足于“课程知识”本性的,而非基于一般知识论的课程知识观,以求得在“课程”与“知识”之间建立起一种新平衡
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  “新平衡”译为未确定词的双语例句
     The critical values of bamboo leaves N and K content in Fengxing county are 2.713% and 1.275% respectively.
     奉新平衡施肥毛竹林N、K 养分浓度临界值分别为2.713%和1.275%,最适值为2.825%和1.340%。
短句来源
     A balance theory and its calculation method, and a regulation method on system parameters of ASC hydraulic pumping units are proposed.
     给出ASC液压抽油机的一种新平衡理论及其计算方法和系统参数的调整方法。
短句来源
     Equilibrium points different from Lyapunov type ones are defined and classified.
     通过给出的空间结构与饱和输入下非线性控制系统的关系定义了不同于一般意义下的非线性系统的平衡点 ,并且对新平衡点进行了分类 .
短句来源
     Between two equilibrium conditions, the situation is called partial equilibrium.
     新平衡形成之前为部分平衡状态。
短句来源
     Under the action of periodic boundary pressure, the system may either be unstable or develop into a periodic movement around a new steady state.
     在周期性压力边界条件下,系统可能在新平衡位置附近产生周期运动,也可能失稳。
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  相似匹配句对
     The New Technique of Scafe Balance
     磨盘平衡技术
短句来源
     The Application Research of New Balance Scorecard
     平衡记分卡的应用研究
短句来源
     NEW ARCHITECTUR
     “建筑”
短句来源
     NEW BOOK'SHOUSE
     书馆
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     The Balance for Rotating Ball
     球体平衡
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  new balance
Fat balance was zero on day 6 but became positive after changing to the high-fat diet (1.06±0.15, 0.75±0.15, and 0.55±0.14 MJ/day for days 7, 8, and 9 respectively, p.>amp;lt;0.05), reaching a new balance on day 13, 7 days afterwards.
      
Finally, some new balance laws of energy and energy rate for generalized continuum mechanics were established.
      
Finally, some new balance laws of energy and energy rate for generalized continuum mechanics were established.
      
The new balance equations of momentum and energy rate which are essentially different from the existing results are presented.
      
The drag force acting on a blunt leading edge flat plate at hypersonic Mach number has been measured using the new balance system.
      
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After the construction of reservior in an alluvial stream, the equilibrium condition of the downstream channel will be upsetted due to the reduction of sediment supply. This will result in a change in the form and gradient of the channel. The direction of the displacement will lead to a reduction of the sediment carrying capacity of the channel, through which the river regains its equilibrium. The whole process is accomplished by the flattening of the bed slope, as suggested by the theories generally accepted...

After the construction of reservior in an alluvial stream, the equilibrium condition of the downstream channel will be upsetted due to the reduction of sediment supply. This will result in a change in the form and gradient of the channel. The direction of the displacement will lead to a reduction of the sediment carrying capacity of the channel, through which the river regains its equilibrium. The whole process is accomplished by the flattening of the bed slope, as suggested by the theories generally accepted at the present. From a study of the fluvial processes of Colorado River and some other streams, it appears that a decrease in channel gradient is one of the three possibilities only, and should not be regraded as an universal rule. In fact, the change in bed slope below an impounding reservoir depends essentially on the geologic and geographic conditions of that area. It is first considered that the channel width does not change materially in the downstream direction. In many of the sandy rivers, there exists, a layer of gravel or pebble below the finer surface material. The inclination of this layer is generally steeper than the present bed slope. After the releasing of clear water from the reservoir, the surface material is carried away and thereby exposing the coarse layer, first near the dam and gradually extended to the downstream. This will result in an uneven erosion along the direction of the flow, and the steepening of the channel gradient is the consequence of such a process. The Colorado Eiver below the Hoover Dam belongs to this case. If the distribution of the bed material in the downstream, direction is more or less uniform, and if there exists no coarse layer within a finite depth below the bed surface, the bed will be degraded as a whole and the channel gradient remains essentially at its initial value. Results of flume study seem to indicate that such is the case. The Colorado Eiver below both the Parker and the Imperial Dam also belongs to this group. Only when there is a base level within a short distance from the dam which controls the depth of scour at that neighborhood, or if ther is a tributary which brings coarser material into the lower part of the reach, will the channel slope below the dam become flatter. On the other hand, if the river is impounded in a gorge and enters a plain not far away from the dam site, the width of the channel on the alluvial fan becomes progressively wider downstream. It is then possible that the depth of degradation decreases in the downstream direction and the slope becomes flatter. This case is well illustrated by one of the rivers in U. S. S. R. It must be realized that no matter how the channel gradient below an impounding reservoir changes, it is mainly through the coarsening of the bed material which makes the channel regains its equilibrium. Two different types of the coarsening of the bed material can be distinguished from the field data available. One of which is the exposing of a gravel or pebble layer below the present alluvium. As soon as this layer is exposed, there will be a sudden jump in the bed material size, and the stream channel becomes stable again. The othertype of coarsening of bed material takes place continuously and at a much slower rate. One often fails to notice the occurence of such a phenomenon, as the size of the bed material only increases in a relatively small amount. Yet, such a small increase in bed material size results in a much significantly rise of the roughness coefficient, by remolding the sand bars on the bed surface. Both the velocity of the flow and the sediment carrying capacity of the channel will be reduced, and the river gradually re-establishes its equilibrium. It is now possible to calculate such a proeess according to the theories on sediment transport and river roughness. Following the coarsening of the bed material, the down-cutting rate of the stream channel decreases with time. Both the flume studies and field measurements indicate that the relationship between the down-cutting rate and the cumulative time of erosion is an exponential one. This study demonstrates that the fluvial processes of an alluvial channel depend very much on the hydrographic conditions of the basin, of which the stream forms a part. One can't visualize the whole aspect of the problem (?)y studying the fluvial proteases through hydraulics, view-point only.

冲积河流上修建水库以后,下游河道将失去平衡。河流为了重新建立平衡,必将发生一系列的变化。本文对这—变化的过程,提出了一些新的概念。根据枢纽下游所在地区的地质地理条件,河流的坡降可以有各种不同的变化。坡降的渐趋和缓只是三种可能性中的一种,不能当做普遍规律来看待。河槽的重新建立平衡,主要是通过河床质的粗化作用。河床质的粗化现象具有两种不同的类型。一种是河床表层复盖物因清水冲刷而外移,露出了底下属于另一地质时代的较粗的卵石层,这时河床质的粒径会发生突变。另一种是由于水流的分迭作用,河床质的变化是连续的,徐缓的。在第二种情况下,河床质的粒径虽然变化不多,但是,通过河底沙垅的加多,却可以使曼宁糙率系数有很快的增加,这就使水流的流速降低,挟沙能力减小,河流逐渐建立起新的平衡。随着河床质的渐次粗化,河床的冲刷下切率与时俱減。野外实测结果及水槽试验成果都指出冲刷率与冲刷历时之间成一指数关系。河床质中不能为水流所挟运的颗粒所占百分比愈大,冲刷率下降得愈快,河道重新恢复平衡所需要的时间也愈短。从黄河下游的具体情况来判断,将来修建枢纽以后,下游河道在承受清水冲刷时可能作整体下降,坡降的变化不会很大。黄河下游的河床质虽然很细,同样也...

冲积河流上修建水库以后,下游河道将失去平衡。河流为了重新建立平衡,必将发生一系列的变化。本文对这—变化的过程,提出了一些新的概念。根据枢纽下游所在地区的地质地理条件,河流的坡降可以有各种不同的变化。坡降的渐趋和缓只是三种可能性中的一种,不能当做普遍规律来看待。河槽的重新建立平衡,主要是通过河床质的粗化作用。河床质的粗化现象具有两种不同的类型。一种是河床表层复盖物因清水冲刷而外移,露出了底下属于另一地质时代的较粗的卵石层,这时河床质的粒径会发生突变。另一种是由于水流的分迭作用,河床质的变化是连续的,徐缓的。在第二种情况下,河床质的粒径虽然变化不多,但是,通过河底沙垅的加多,却可以使曼宁糙率系数有很快的增加,这就使水流的流速降低,挟沙能力减小,河流逐渐建立起新的平衡。随着河床质的渐次粗化,河床的冲刷下切率与时俱減。野外实测结果及水槽试验成果都指出冲刷率与冲刷历时之间成一指数关系。河床质中不能为水流所挟运的颗粒所占百分比愈大,冲刷率下降得愈快,河道重新恢复平衡所需要的时间也愈短。从黄河下游的具体情况来判断,将来修建枢纽以后,下游河道在承受清水冲刷时可能作整体下降,坡降的变化不会很大。黄河下游的河床质虽然很细,同样也存在着粗化的可能。通过粗化作用,可以使河床下切的深度大大减低。

The two superpowers,the Soviet Union and the United States,have given much publicity to an“ecological crisis”.They claimed that environmental pollution has upset the“inherent balance”in the ecological system on which mankind relies for the existence,that it will inevitably lead to“catastrophe and death”. Such fallacies are mainly reflected in their basic views on“ecological balance” and their attitude toward it as well as the root cause of its destruction etc. It is metaphysical to regard“ecological balance”as...

The two superpowers,the Soviet Union and the United States,have given much publicity to an“ecological crisis”.They claimed that environmental pollution has upset the“inherent balance”in the ecological system on which mankind relies for the existence,that it will inevitably lead to“catastrophe and death”. Such fallacies are mainly reflected in their basic views on“ecological balance” and their attitude toward it as well as the root cause of its destruction etc. It is metaphysical to regard“ecological balance”as something absolute.With this erroneous standpoint,one will certainly fail to recognize the decisive role played by man in the relations between man and nature.This is decided by bourgeois world outlook and class nature.It is absolutely not the“erroneous actions of man- kind”that constitutes the root cause to upset“ecological balance”but the system of capitalist expolitation.Only when socialism replaces capitalism,people will be able to constantly know nature in depth and transform it,upset old equilibrium in a planned way and set up a new one and push forward the cause of socialism sys- tematically and step by step.

苏美两个超级大国大肆宣传“生态危机”,声称环境污染破坏了“人类赖以生存的生态系统的固有平衡”,必然引起“毁灭和死亡”。这种错误观点,主要反映在对生态平衡的基本看法,如何对待生态平衡以及破坏生态平衡的根源等问题上。把生态平衡绝对化是形而上学的观点。这种错误观点在对待人和自然界的关系中,必然看不到人的决定作用。这是由资产阶级世界观以及资产阶级的阶级本性所决定。破坏生态平衡的根源绝不是“人类的错误行动”,而是资本主义的剥削制度。只有社会主义代替了资本主义,才能不断深刻地认识自然、改造自然,有计划的打破旧平衡,建立新平衡,使社会主义事业有计划、有步骤的向前迈进。

The binding to isolated adipeoytes from rat epididymal fat pads of high specific activity (2.2μCi/μg) ~(125)I-pinellin has been studied. The binding of pinellin to its receptors on adipocytes is quite specific as the iodoprotein can be completely displaced by the native protein. The binding of pinellin to its receptors is a saturation process with respect to the protein. A single cell can bind a maximum of about 6-7×10~7 molecules of pinellin. The binding of ~(125)I-pinellin is proportional to the concentration...

The binding to isolated adipeoytes from rat epididymal fat pads of high specific activity (2.2μCi/μg) ~(125)I-pinellin has been studied. The binding of pinellin to its receptors on adipocytes is quite specific as the iodoprotein can be completely displaced by the native protein. The binding of pinellin to its receptors is a saturation process with respect to the protein. A single cell can bind a maximum of about 6-7×10~7 molecules of pinellin. The binding of ~(125)I-pinellin is proportional to the concentration of cells in the incubation mixture provided a sufficiently high concentration of labeled protein is used relative to the cell concentration. The binding capacity decreases with increasing temperature. The binding at 37℃ is only 10% of that at 0℃. Equilibrium binding of pinellin to its receptor occurs rapidly both at 24℃ and 0℃. The complex formed dissociates slightly during an 80 min. period of incubation at 24℃ (only 8% of the bound protein dissociates) but dissociates rapidly when the temperature of the medium is changed from 0℃ to 37℃. Both the single sugar, α-methyl-D-mannopyranoside, even at a concentration of 0.1M and the polysacoharide mannan at a concentration of 2mg/ml, do not cause dissociation of the complex. ConA causes the complex to dissociate rapidly but partially. ConA at a low concentration (5×10~(-8)M)causes a slight fall in the binding of ~(125)I-pinellin to fat cells. The degree of inhibition by ConA increases with increasing concentrations of ConA, but complete inhibition of the binding has not been observed even at the concentration of 2.5×10~(-5)M. The binding of ~(125)I-pinellin to its receptor is not inhibited by insulin even at high concentrations.

本文对分离的大鼠附睾脂肪细胞与半夏蛋白结合的若干性质进行了探讨。脂肪细胞与半夏蛋白的结合是专一的,非标记半夏蛋白可完全地置换~(125)Ⅰ-半夏蛋白。脂肪细胞上半夏蛋白受体与半夏蛋白的结合对半夏蛋白而言是一饱和过程,饱和曲线呈反曲形,但Scatchard图形则是一不规则的曲线,提示脂肪细胞上可能存在不止一种半夏蛋白受体。根据饱和曲线计算,每个脂肪细胞可结合大约6~7×10~7个分子半夏蛋白。当反应液中~(125)Ⅰ-半夏蛋白浓度对细胞而言足够高时,半夏蛋白与其受体的结合随溶液中细胞浓度的增高而增加。半夏蛋白与其受体的结合随温度的升高而减少,37℃的结合量仅为0℃的10%左右。在24℃时,半夏蛋白与其受体的结合很快达到平衡,但自然解离则极慢。在0℃达到平衡的半夏蛋白-受体复合物,当移置到37℃时,则很快解离,达到新的平衡,提示复合物在0℃比在37℃稳定。反应液中α-甲基甘露糖苷浓度为0.1M或甘露聚糖浓度为2毫克/毫升时,均观察不到它们有促使复合物解离的作用。伴刀豆球蛋白A具有显著的但不完全的抑制半夏蛋白与其受体结合的能力,它也能使半夏蛋白-受体复合物部分解离。胰岛素即使浓度高达2.5×10~(-5)M亦不抑制...

本文对分离的大鼠附睾脂肪细胞与半夏蛋白结合的若干性质进行了探讨。脂肪细胞与半夏蛋白的结合是专一的,非标记半夏蛋白可完全地置换~(125)Ⅰ-半夏蛋白。脂肪细胞上半夏蛋白受体与半夏蛋白的结合对半夏蛋白而言是一饱和过程,饱和曲线呈反曲形,但Scatchard图形则是一不规则的曲线,提示脂肪细胞上可能存在不止一种半夏蛋白受体。根据饱和曲线计算,每个脂肪细胞可结合大约6~7×10~7个分子半夏蛋白。当反应液中~(125)Ⅰ-半夏蛋白浓度对细胞而言足够高时,半夏蛋白与其受体的结合随溶液中细胞浓度的增高而增加。半夏蛋白与其受体的结合随温度的升高而减少,37℃的结合量仅为0℃的10%左右。在24℃时,半夏蛋白与其受体的结合很快达到平衡,但自然解离则极慢。在0℃达到平衡的半夏蛋白-受体复合物,当移置到37℃时,则很快解离,达到新的平衡,提示复合物在0℃比在37℃稳定。反应液中α-甲基甘露糖苷浓度为0.1M或甘露聚糖浓度为2毫克/毫升时,均观察不到它们有促使复合物解离的作用。伴刀豆球蛋白A具有显著的但不完全的抑制半夏蛋白与其受体结合的能力,它也能使半夏蛋白-受体复合物部分解离。胰岛素即使浓度高达2.5×10~(-5)M亦不抑制~(125)Ⅰ-半夏蛋白与其受体的结合。

 
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