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负相的英文

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"负相"怎么读用"负相"造句

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  • minus phase

例句与用法

  • The clique and category of xu fu ' s physiognomy texts in dunhuang ms
    敦煌写本许负相书的系属与类别
  • A strong law of the large numbers for sequence of negatively associated random variables
    负相协随机变量列的强大数律
  • Strong convergence rate of recursive probability density estimator for na sequences
    负相协下递归密度估计的强收敛速度
  • Application of main tansformer differential protection in primany negative - phase sequence system
    主变差动保护在一次负相序系统中的应用
  • Humai 16 at 20 umol / l al level , indicating that there is a negative correlation between al - induced sces and al - resistant ability in barley
    Humai16高,铝毒诱导的sce率与大麦耐铝性呈负相
  • Several influence factors to result plasma drift in hainan were analyzed . in this paper the characteristics of ionospheric parameters variation were analyzed systematically and some new results in storm - time such as seasonal behaviors were obtained ; it is the first time to investigate the ionospheric drift behavior in hainan and some new results was obtained , the relationships between each two plasma drift velocity components in storm time in hainan were found and the electric filed variation in hainan ionosphere also was obtained ; the results also show that there are big differences of the ionosphere parameters bo and bl obtained from the data with that obtained from the iri - 2001 applied for hainan ; a new phenomena was found during a strong magnetic storm , that a layer with very strong electron density and density grad was found during the recovery phase of the storm , its horizontal scale is beyond 100km and temporal scale is about 2 hours , this phenomena repeated 3 times continuously . a type of negative disturbance in high and low latitude but positive disturbance in east - asia also has been found
    本文较为系统地给出了海南地区电离层的参数变化特征,特别是得到了一些暴时与以往不同的季节特性;第一次给出了海南地区的电离层等离子体漂移特征,发现等离子体漂移暴时扰动在三个方向上有内在的联系,得到了电场变化曲线;研究结果还表明海南电离层的半厚指数和形状参数等与国际参考电离层iri - 2001存在很大差别;通过对强磁扰动事件期间的参数变化特性分析发现,在磁暴恢复相期间海南地区电离层底部存在一个电子密度非常大的高密度区,高密度区底部电子密度梯度随高度急剧增加,该区域的水平尺度可达100公里以上时间尺度约为2小时,连续出现过三次,这是一个在海南从来未发现的新现象;研究还发现了暴时东亚地区电离层扰动会出现高低纬负相而中纬正相的现象。
  • But in more situations the random variables generating counting processes may not independent identically distributed , and in all kinds of dependent relations , negative association ( na ) and positive association ( pa ) are commonly seen . the research and apply in this aspect are rather valuable . in chap 2 we prove wald inequalities and fundamental renewal theorems of renewal counting processes generated by na sequences and pa sequences ; in chap 3 we are enlightened by cheng and wang [ 8 ] , extend some results in gut and steinebach [ 7 ] , obtain the precise asymptotics for renewal counting processes and depict the convergence rate and limit value of renewal counting processes precisely ; at last , in the study of na sequences , su , zhao and wang ( 1996 ) [ 9 ] , lin ( 1997 ) [ 10 ] have proved the weak convergence for partial sums of stong stationary na sequences . however product sums are the generalization of partial sums and also the special condition of more general u - statistic
    但在更多的场合中,构成计数过程的随机变量未必相互独立,而在各种相依关系中,负相协( na )和正相协( pa )是颇为常见的关系,这方面的研究和应用也是颇有价值的,本文的第二章证明了na列和pa列构成的更新计数过程的wald不等式和基本更新定理的一些初步结果;本文的第三章则是受到cheng和wang [ 8 ]的启发,推广了gut和steinebach [ 7 ] )中的一些结论,从而得到了更新计数过程在一般吸引场下的精致渐近性,对更新计数过程的收敛速度及极限状态进行精致的刻画;最后,在有关na列的研究中,苏淳,赵林成和王岳宝( 1996 ) 》 [ 9 ] ,林正炎( 1997 ) [ 10 ]已经证明了强平稳na列的部分和过程的弱收敛性,而乘积和是部分和的一般化,也是更一般的u统计量的特况,它与部分和有许多密切的联系又有一些实质性的区别,因此,本文的第四章就将讨论强平稳na列的乘积和过程的弱收敛性,因为计数过程也是一种部分和,也可以构成乘积和,这个结果为研究计数过程的弱收敛性作了一些准备。
用"负相"造句  
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