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hard component
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  硬相互作用
     Assuming that both the soft component and the hard component obey KNO scaling in the multiplicity distribution of high energy hadron-hadron collision but their respective parameters are different, the multiplicity distriblltion of the charged particle in P collision at=1800GeV is calculated. We find that(n)=47.0 which can be tested. by experiments.
     假设高能强子—强子碰撞的多重性分布中,软相互作用部分和硬相互作用部分都服从KNO无标度性,只是它们各自的参数不同.由已有的实验数据,计算出=188GeV处,碰撞的平均多重性〈n〉=47.0及其荷电粒子的多重性的分布.可供实验检验.
短句来源
  “hard component”译为未确定词的双语例句
     SOFT COMPONENT AND HARD COMPONENT IN THE STRONG INTERACTION
     强相互作用的软成分与硬成分
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     The multilayer composite including a hard component TZ-3Y20A and a plastic soft component Mo has been fabricated by particle sedimentation method.
     结果表明,当叠层材料层数和层厚比分别超过27和2时,计算得到的残余应力小于TZ-3Y20A陶瓷的抗弯强度。
短句来源
     After carefully analysing the scatter plot of pt vs. N of hadron-hadron collisions at 540GeV, we point out that the appearence of large average transverse momentum per event p t and large multiplicity N is a new experimental evidence of existing hard component at the collision.
     对sqr(s)=540Gev能量下的高能强子-强子碰撞得到的单事件平均横动量p。 对多重数N的散点图进行了仔细分析后指出;
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  相似匹配句对
     Technical Analysis of Hard Code Component
     硬件密码组件的技术分析
短句来源
     SOFT COMPONENT AND HARD COMPONENT IN THE STRONG INTERACTION
     强相互作用的软成分与硬成分
短句来源
     Livelihood was hard;
     民生艰难,思想混乱。
短句来源
     NET component.
     NET组件技术的变化,最后给出了开发.
短句来源
     hard liver;
     肝脏质地坚硬;
短句来源
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  hard component
The hard component changes reversibly with σ: the magnetic intensity of hard component increases with σ when the axis of σ is perpendicular to the magnetization, whereas it decreases with σ when the axis of σ is parallel to the magnetization.
      
Characteristics of remanent magnetization of an igneous rock under a uniaxial compression are divided into those of the soft component and those of the hard component.
      
The increase in impact strength is apparently due to the inhibition of crack propagation in the ductile component of a MLC and to an increase in the strength of the hard component associated with the small thickness of its layers.
      
With the modulation wavelength adjusted, the multilayer can be even harder than its hard component (TiC).
      
There was no evidence for an additional hard component attributable to synchrotron self-Compton emission.
      
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A result of high resolution magnetostratigraphy obtained from recent sedimentsof Gucheng Lake, Gaochun County, Jiangsu Province, was reported.The total thickness of the sediments is about 18.5m. The lithologic charactersfrom bottom to top are: brownish-yellow, yellowish-grey argillaceous fine sand,fin.e sand, silt and mud with a thickness of about 1.5m; greyish-green, bluish-greyand varicolored silt, argillaceous silt, silty clay of 3m thick; bluish-grey andlight grey sludge, silt and mud interbeds of 3m thick;...

A result of high resolution magnetostratigraphy obtained from recent sedimentsof Gucheng Lake, Gaochun County, Jiangsu Province, was reported.The total thickness of the sediments is about 18.5m. The lithologic charactersfrom bottom to top are: brownish-yellow, yellowish-grey argillaceous fine sand,fin.e sand, silt and mud with a thickness of about 1.5m; greyish-green, bluish-greyand varicolored silt, argillaceous silt, silty clay of 3m thick; bluish-grey andlight grey sludge, silt and mud interbeds of 3m thick; then a 7m thick section ofgrey sludge with partly sludge and silt thin interbeds; on the top of this section,there is about 4m thick dark grey, black and greyish-brown sludge with occasionallygreyish-brown silt banding. It appears that there is a tendency of varying from coarserto finer from bottom to top.566 samples with a sampling interval of 2-3cm were collected from the drilling core for magnetostratigraphic measurement, in addition, 96 auxiliary sampleswere also collected at some key horizons with different lithologic characters forrock magnetism experimental investigation.First of all, the low frequency (0.46kHz) susceptibility KLF, high frequency(4.6kHz)susceptibility KHF and frequency dependent susceptibility KFD of thesesamples were measured using a Bartington MS2 dual frequency susceptibility meter.The variation of the three kinds of susceptibility with depth and its environmentalimplications will be discussed in another paper later on.Then, to identify the magnetic minerals carrying the remanent magnetizationsof these samples, the Isothermal Remanent Magnetization(IRM) measurements withdifferent heating temperature, the Magnetic Hysteresis Loop measurement and theX-Ray Diffraction analysis were carried out for the auxiliary samples of differentlithologic characters. All of these experimental investigations suggested that thedominant magnetic mineral which carries the remanent magnetization of these samples is Magnetite accompanied with a small amount of Maghemite but also involvedsome Hematite and Goethite as hard components in these samples, and the size ofthese magnetic minerals grains are dominantly of single domain and/or pseudo-singledomain, perhaps some of them are already close to single domain/superparamagneticgrain boundary.The remanent magnetization measurement of these samples were carried out atthe paleomagnetic laboratory of institute of Geophysics, Chinese Academy of Sciences using a 2G755-R superconducting magnetometer. All of the samples were suffered thermal or alternating magnetic field treatment respectively for cleaning the secondary remanent magnetization. Figure 1 shows the results of demagnetizing treatment for some samples, and two antipodal directions of remanent magnetization arerevealed clearly, it means that there really are two polarities present in these samples.Based on the results of remanent magnetization measurement and rock magnetism experimental investigation, a magnetic polarity sequence was established inFigure2, in this sequence, it can be seen clearly that two reversed polarity events(or excursions) are revealed in the lake sediments. The one located at about 12.5mdepth in the core with an age of 10 307-9 727aB.P. is regarded as the record ofGothenburg event (about 12 000aB.P.), the difference in age is thought of beingcaused by the dating uncertainty. The another is located at about 5.5m depth in thiscore, its age was dated as 7 085-7 005aB.P., for which, there is not correlative event or excursion in the results published in the world, only that one revealed byZhu Rixiang from the peat sequence at Fangshan, Beijing, with an age of 4980─4 770aB.P. may be comparable with this, but at the moment , we can not yet makesure whether these two records of polarity reversal correspond to the same polarityevent or excursion, or even that the event or excursion itself really exsist or not,further works will be needed to confirm that.

本文报道了作者1991─1992年在江苏省高淳县固城湖沉积物岩芯中所取得的高分辨率磁性地层学研究结果。结果揭示出两个反极性事件,其中位于12.5m左右深度、年龄为10307—9727aB.P.的一次反极性事件,可能是哥德堡事件(12000aB.P.前后)在该沉积物中的记录,其年龄上的差异可能是因测年误差所致;另一位于5.5m左右深度、年龄为7085—7005aB.P.的一次反极性事件,在目前国际上已报道的资料中尚无相应年龄的反极性事件可以与之对比,只有朱日祥等在北京房山地区泥炭层中所揭示出的一个年龄为4980─4770aB.P.的反极性漂移与之接近,但两者是否为同一事件的反映,甚或该事件本身是否真实存在,目前都还不能肯定,有待今后进一步工作加以证实。

Assuming that both the soft component and the hard component obey KNO scaling in the multiplicity distribution of high energy hadron-hadron collision but their respective parameters are different, the multiplicity distriblltion of the charged particle in P collision at=1800GeV is calculated. We find that(n)=47.0 which can be tested. by experiments.

假设高能强子—强子碰撞的多重性分布中,软相互作用部分和硬相互作用部分都服从KNO无标度性,只是它们各自的参数不同.由已有的实验数据,计算出=188GeV处,碰撞的平均多重性〈n〉=47.0及其荷电粒子的多重性的分布.可供实验检验.

This paper advances a hypothesis: the soft component and the hardcomponent of the strong interaction product many charged particles in high energy multiple production. These particles obey their respective KNO-Scaling:but only their parameteres b and are not same b= 5 for the soft component andb= 13 for the hard component in the present expcrimental conditions Their respective 's vary lawly with Using this hypothesis, the experimental data of the chargedparticle multiple production in all curent...

This paper advances a hypothesis: the soft component and the hardcomponent of the strong interaction product many charged particles in high energy multiple production. These particles obey their respective KNO-Scaling:but only their parameteres b and are not same b= 5 for the soft component andb= 13 for the hard component in the present expcrimental conditions Their respective 's vary lawly with Using this hypothesis, the experimental data of the chargedparticle multiple production in all curent non-diffractive and inelastic pcollisions aredescribed very well. It predicts : the average multiplicity =47.0±0.5 and themultipicity distribution of the (n) = 47.0 ±0.5 and the multiplicity distribution of the pcollision at = 1 800GeV.

本文提出一个假设:在高能多重产生中,强相互作用的软成分和硬成分所产生的荷电粒子都服从KNO无标度分布仅仅是参数b不同和<n>不同。在现有实验条件下,软成分的b=5,硬成分的b=13;它们自各的<n>随质心能量有规律地变化。用这个假设可很好地描述已有非单绕、非弹性碰撞荷电粒子多重产生实验数据、并可预言=1800GeV处,碰撞的非单绕、非弹性消电粒子多重性分布,总的平均多重性<n>=470±0.5。

 
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