fractal properties中文是什么意思
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用"fractal properties"造句"fractal properties"怎么读"fractal properties" in a sentence
中文翻译手机版
- 分形特质
- "property"中文翻译 n. 1.财产;资产;所有物;所有地,地产;所有,所有权 ...
- "fractal" 中文翻译 : 分数维几何; 分形,分数据,碎片,拼图; 分形;碎形; 分形几何; 分形体具有分形的物体; 分形指传统欧几里德几何所不能描述的一类具有某种自相; 提出了分形
- "fat fractal" 中文翻译 : 胖分形
- "fractal analysis" 中文翻译 : 分形分析
- "fractal behavior" 中文翻译 : 分形行为
- "fractal cities" 中文翻译 : 理论和分形城市
- "fractal compression" 中文翻译 : 部分压缩,局部压缩,分形压缩,拼图压缩; 碎形压缩
- "fractal dimension" 中文翻译 : 分数维; 分维 フラクタル次元; 分形维数
- "fractal encoding" 中文翻译 : 分形编码
- "fractal geometry" 中文翻译 : 分形几何
- "fractal influence" 中文翻译 : 不规则影响程度
- "fractal modeling" 中文翻译 : 碎片造型
- "fractal noise" 中文翻译 : 分形噪波
- "fractal surface" 中文翻译 : 不规则断裂面,分形面; 分形面
- "fractal theory" 中文翻译 : 分形理论
- "multi-fractal" 中文翻译 : 多重分形
- "by properties" 中文翻译 : 按特性; 依内容
- "properties" 中文翻译 : (特性)命令修改特性; (目标属性):电影制作过程中可以在此类工具栏中修改对象属性; 具有零个或多个属性; 列表属性; 内容; 属性面板; 特性,本质; 图形特性; 显示属性; 性能; 性质; 选择属性
- "properties (" 中文翻译 : 开启项目属性设定窗口
- "fractal and geostatistical analysis" 中文翻译 : 分形和地质统计分析
- "fractal dimension geometry techniques" 中文翻译 : 二维几何技术
- "fractal dimension theory" 中文翻译 : 分数维理论
- "fractal flow max" 中文翻译 : 画面扭曲特效
- "fractal image compression" 中文翻译 : 不规则图象压缩
- "fractal net work" 中文翻译 : 分形网络
例句与用法
- The fractal properties for the non - degenerat diffusion processes
非退化扩散过程样本的分形性质 - 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
首先从分形的定义以及六角格子的形成过程两个方面说明了其分形特性。 - 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,杨新建教授在文献[ 2 ]中研究了紧集上非退化扩散过程样本的水平集和逆像集的一些分形性质,本文在这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
这样就精确地验证了在z ~ o衰变能量下的e ~ + e ~ -对撞末态强子系统是多重自相似分形,并首次用实验测出了相应的分形维数与l vy指数。 - 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
几个分形函数, weierstrass函数, besicovitch函数, rademacher函数, takagi函数等,由于它们所特有的分形性质,在分形研究中占有重要地位,因此,它们的分形维数、图象模拟的研究,也成为当前的重要课题。 - 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
提出以地貌分形特点和渡越长度为依据的地貌层次界定方案,研究指出了5km左右应为宏观临界点:不同构造地貌区、不同取向的剖线的多重分形谱值域范围宽窄表现出中低山区高山区盆地区,垂直构造地貌斜坡方向斜交方向平行方向的特点,表明了内外营力作用的不均匀性和方向性。 - 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
不同类型地貌区二维地貌表面也表现出多度域分形特征,而且随着观测尺度的增加,每个区间的分维值均表现为依次减小,表明外营力作用的影响逐渐被内营力作用所取代:不同类型地貌区在相应区间的分维值表现为高山区中低山区盆地区,体现了不同类型地貌表面粗糙性或复杂性的差异,因此分维值大小可作为地貌表面外营力侵蚀作用强度的重要指标:利用标度区的间断点和各种地貌类型表面分维值或宏观效应趋于一致,提出5 - 6km左右可作为地貌的宏观临界点,并且与利用地貌剖线研究所得到的5km这一数值是基本吻合的。
相关词汇
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