非均匀性的的英文

• heteropical

• "非均匀"英文翻译    heterogeneous; inhomogeneous
• "性"英文翻译    nature; character; dispositi ...
• "的"英文翻译    4次方是 The fourth power of 2 i ...
• "不非均匀性" 英文翻译 :    inhomogeneity
• "非均匀性" 英文翻译 :    anisotropy; heterogeneity; nonhomogeneity; nonuniformity
• "弹性非均匀性" 英文翻译 :    elastic heterogeneity
• "非均匀性缺损" 英文翻译 :    nonhomogeneous defect
• "非均匀性试验" 英文翻译 :    heterogeneity test
• "非均匀性衰减" 英文翻译 :    nonuniform attenuation
• "非均匀性紊流" 英文翻译 :    inhomogeneous turbulence
• "光学非均匀性" 英文翻译 :    optical heterogeneity
• "理想非均匀性" 英文翻译 :    ideal non uniformity
• "亮度非均匀性" 英文翻译 :    luminance non uniformity; luminance nonuniformityy
• "视野非均匀性" 英文翻译 :    field nonuniformity
• "随机非均匀性" 英文翻译 :    random inhomogeneity
• "体积非均匀性" 英文翻译 :    bulk heterogeneity
• "均匀性的测验" 英文翻译 :    uniformity trial
• "不均匀性，非均一性" 英文翻译 :    non-uniformity
• "非均匀性多相性" 英文翻译 :    heterogeneity
• "非均匀性接触率" 英文翻译 :    nonhomogeneous contact rate
• "均匀性" 英文翻译 :    homogeneity; uniformity; homogenization
• "非均匀" 英文翻译 :    heterogeneous; inhomogeneous
• "非均质；非均匀" 英文翻译 :    heterogenous
• "同一货源水泥强度均匀性的评定方法" 英文翻译 :    standard test method for evaluation of cement strength uniformity from a single source
• "白均匀性" 英文翻译 :    white uniformity

• A numerical program developed based on meso - damage mechanics , was adopted to simulate the deformation , damage and fracture , i . e . the whole failure process of brittle composite matrix reinforced by particles under uniaxial tensile load
  摘要在材料细观非均匀性的基础上研究了含粒径不同颗粒的脆性基复合材料的宏观力学性质和破坏过程的尺寸效应。
• It was shown by numerical simulations that the dib technique was effective in capturing the rock heterogeneity , and it paved a new way for quantifying the effect of local heterogeneity on macroscopic failure process and seepage characteristics
  结果表明，基于数字图像的技术是表征岩石细观非均匀性的一种有效方法，为研究非均匀性对于岩石破裂过程及渗流特性的影响提供了一个重要的手段。
• A digital image - based ( dib ) technique was proposed to characterize and quantify the heterogeneity of rock , and it was implemented into rfpa ( rock failure process analysis ) code in order to simulate the complete failure process of rock under both the external loading and fluid pressure
  本文提出了用数字图像处理技术表征岩石非均匀性的基本方法，并通过把该技术实施到岩石破裂过程分析程序rfpa中，来模拟非均匀岩石在外载荷和渗流耦合作用下发生破裂的整个过程。
• Regard - ing the surface runoff mechanism , liang and xie 1 , 2 presented a new surface runoff parameterization which dynamically represents both the horton and dunne runoff generation mechanisms within within a model grid cell together with a consideration of the subgrid - scale het - erogeneity , which can be applied to not only humid regions but also droughty regions as well 3 , 4 . regard - ing the soil water movement , xie et al . 5 developed an unsaturated flow numerical model based on the finite element method , and xie et al . 6 presented another numerical model to compute soil moisture and water flow flux together by means of a mixed finite element method
  在地表径流方面,文献1 3发展了一种同时考虑蓄满超渗产流机制及次网格非均匀性的新的径流机制模型,并用其改进了陆面模式vic variable infiltration capacity中的径流计算,该模型既适用于湿润地区也适用于干旱地区4 .在土壤水模型方面,文献5采用有限元质量集中法发展了非饱和土壤水流的数值模型,文献6则采用混合有限元法建立了非饱和土壤水分含量和通量计算的数值模型
• A new analytical expression of heterogeneous spatial precipitation is given which are the lorenz curve and the coefficient of gini . we can express the degree of heterogeneous about the spatial distribution of precipitation by use of this method , and we can declare whether it is possible have the fond or not
  文章引进了一种新的描述非均匀性的方法：洛仑兹( lorenz )曲线和基尼系数，利用它们可以更加准确的表示出降水量场空间分布的非均匀程度，并能据此判定有无洪涝灾害形成可能。
• The paper explored the pdf of the spatial distribution of the day precipitation . the result shows that the weibull distribution is good on describing the heterogeneous of the spatial distribution of the day precipitation in china . the exponential distribution is n ' t ideally suited to the day precipitation
  利用负指数分布和weibull分布拟合全国范围内的逐日降水水平空间概率分布模式，发现负指数分布模式并不能很好的拟合大范围区域逐日降水量场空间分布型，而weibull分布的拟合效果很好，表明用weibull分布描述中国区域逐日降水量空间分布非均匀性的分布律是非常适宜的。
• Third , based on the parameterization of the related land surface characteristics , using the probability density functions ( pdf ) and the grossly dynamic resistance method , a statistical - dynamical parameterization scheme is put forward . the mean evapotranspiration flux of lower reaches of the yangtze river is calculated by tins scheme and the results are compared with the formers " conclusions . finally , the calculated results by the statistical - dynamical parameterization scheme are compared with the mosaic method
  第三，在进行了有关地表特征物理量的参数化后，结合拟合的概率密度函数，根据总体动力掌阻抗法，提出了一种考虑网格区整体非均匀性的统计-动力参数化方案，并采用这种方案计算了长江三角洲地区的平均蒸发散通量，计算结果与以前研究者的研究成果进行了比较验证。
• At first , we introduce the working flow of ir image processing and the structure of the image processor , then we present the goal of the design : image pre - processing and data communication . in the part of the image pre - processing , the factors causing the nonuniformity of fpas are analyzed particularly , and several . resolutions are presented , which characters are illustrated at last . according to the design requirement , we decided to implement the two - point nonuniformity correction method in fpga
  在图像预处理部分，首先就红外成像传感器非均匀性的成因进行了详细分析，总结了红外成像传感器非均匀性校正的主要方法，分析了各种方法的优缺点；根据成像制导信息处理机实时处理的要求，利用现场可编程门阵列实现了基于浮点运算的两点法非均匀性校正模块。
• In this paper , starting with the physical mechanics of land surface hydrologic process and the introduction of the theory in probability statistic distribution , an analytical expression of heterogeneous evapotranspiration efficiency is given which takes heterogeneous soil water content ' s subgrid scale spatial variability into account , through which the parameterization scheme of subgrid scale soil surface ' s evapotranspiration efficiency ( which is generally called mosaic method ) is modified to a statistic - dynamic scheme in which a whole heterogeneity of the grid region is considered
  本文从陆面水文过程的物理机制出发，引进概率统计分布理论，推导出一种由非均匀土壤含水量次网格尺度空间变率所形成的非均匀蒸发散率解析表达式，从而将通常的次网格尺度地表蒸散率的参数化方案( mosaic方法) ，改进为考虑网格区整体非均匀性的统计-动力参数化方案。
• Second , the bar of the frequency - distribution and the curve of lorenz and the g coefficient are talked about the spatial distribution of day to day precipitation . the results show that the heterogeneous of day precipitation is strong on every day in a year . the spatial distribution model is left skew all in four seasons and it is different from the monthly precipitation
  其次利用全国700个测站逐日降水资料的空间分布频数直方图及洛伦兹曲线和基尼系数阐述了我国逐日( 24小时)降水非均匀性的事实，直方图显示全国范围内逐日降水的水平空间分布型在四季都是一种明显左偏态型，与月降水量的水平空间分布型略有不同；基尼系数值的月际变化也与月降水量的变化相反。