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fractal properties in Chinese

Pronunciation:
How to pronounce "fractal properties""fractal properties" in a sentence

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  • 分形特質(zhì)

Examples

  • The fractal properties for the non - degenerat diffusion processes
    非退化擴散過程樣本的分形性質(zhì)
  • Fractal properties of vegetation pattern
    植被格局的分形特征
  • At first , the fractal property of hexangular lattice is illustrated from two aspects which are the definition of fractal and the form of hexangular lattice
    首先從分形的定義以及六角格子的形成過程兩個方面說明了其分形特性。
  • Furthermore , the fractal properties of the level sets and inverse image of compact sets of n - dimension non - degenerate diffusion processes is also considered by professor yang in [ 2 ] , and some new results are obtained in this paper
    另外，楊新建教授在文獻[ 2 ]中研究了緊集上非退化擴散過程樣本的水平集和逆像集的一些分形性質(zhì)，本文在這方面也做了一些工作。
  • In this way , the self - similar multi - fractal property of the hadronic system produced in z0 ( ) decay is strictly confirmed and the corresponding fractal dimensions and levy index are obtained in the first time using the high statistics data from the l3 experiment at lep
    這樣就精確地驗證了在z ~ o衰變能量下的e ~ + e ~ -對撞末態(tài)強子系統(tǒng)是多重自相似分形，并首次用實驗測出了相應(yīng)的分形維數(shù)與l vy指數(shù)。
  • Futhermore , fractal analysis has achieved some important development . several fractal functions , such as the weierstrass functions , the besicovitch functions , the rademacher functions , the takagi functions , etc , and their graph dimensions and fractal properties are investigated extensively due to the special fractal structures
    幾個分形函數(shù)， weierstrass函數(shù)， besicovitch函數(shù)， rademacher函數(shù)， takagi函數(shù)等，由于它們所特有的分形性質(zhì)，在分形研究中占有重要地位，因此，它們的分形維數(shù)、圖象模擬的研究，也成為當前的重要課題。
  • After that , the multifractal spectra dq - q are computed by fixed - mass method . the results show that in the studied scaling range different types of landscapes and profiles in different directions perform different fractal properties , that is , the d value and crossover length ^ decrease in turns with the landform type from high - moutain , mid - low mountain to basin , and the profile parallel to wear grooves often has lower d values ( < 1 . 5 ) than those perpendicular to wear grooves do ( 1 . 5 ) in the same section
    提出以地貌分形特點和渡越長度為依據(jù)的地貌層次界定方案，研究指出了5km左右應(yīng)為宏觀臨界點：不同構(gòu)造地貌區(qū)、不同取向的剖線的多重分形譜值域范圍寬窄表現(xiàn)出中低山區(qū)高山區(qū)盆地區(qū)，垂直構(gòu)造地貌斜坡方向斜交方向平行方向的特點，表明了內(nèi)外營力作用的不均勻性和方向性。
  • Furthermore , the dq value ranges of profile multifarctal spectra in different landform types and in different directions of the same sections perform different properties and anisotrpies . it can be concluded that the landscape fractal properties depends closely on the int ensity , manner and inhomogenity of exogenic and inogenic processess , and with the properties , we can study quantatively the dynamic geomorphic process . by using the same methods just above , local fractal dimensions d , crossover length tc and the multifractal spectra dq - q of two large - scale landform profiles ( across and along tianshan mountain ranges respectively ) are calculated . the results show that in the studied scaling range the two profiles perform different scaling properties , and both of them can be divided to three evident different linear scaling subsections
    不同類型地貌區(qū)二維地貌表面也表現(xiàn)出多度域分形特征，而且隨著觀測尺度的增加，每個區(qū)間的分維值均表現(xiàn)為依次減小，表明外營力作用的影響逐漸被內(nèi)營力作用所取代：不同類型地貌區(qū)在相應(yīng)區(qū)間的分維值表現(xiàn)為高山區(qū)中低山區(qū)盆地區(qū)，體現(xiàn)了不同類型地貌表面粗糙性或復(fù)雜性的差異，因此分維值大小可作為地貌表面外營力侵蝕作用強度的重要指標：利用標度區(qū)的間斷點和各種地貌類型表面分維值或宏觀效應(yīng)趨于一致，提出5 - 6km左右可作為地貌的宏觀臨界點，并且與利用地貌剖線研究所得到的5km這一數(shù)值是基本吻合的。
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