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饱和层的英文

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"饱和层"怎么读用"饱和层"造句

英文翻译手机手机版

  • phreatic zone
  • saturated layer
  • saturated zone
  • saturation zone
  • zone of saturation

例句与用法

  • By the transfer matrixes , the solutions of 3 - d dynamic response of layered transversely isotropic saturated soils are presented
    研究了直角坐标系下横观各向同性饱和层状地基的稳态动力响应问题。
  • It was proved that the tracking error converges to the prescribed boundary layer and all the signals in the closed - loop system were bounded
    算法保证闭环系统所有信号的有界性且使得跟踪误差收敛于任意设定的饱和层内。
  • In addition , at ncku - re study site , collections of soil water contents and data of rainfall estimate infiltration and runoff in homogeneous unsaturated soil profiles , after net fuzzy - neuro training , to analyze soil infiltration behavior and determine the infiltration and runoff of the region of the subsurface
    中文摘要本研究主要目的将现地资料含水量,运用模糊类神经网路去做训练,在考虑降雨与土壤含水量,进行未饱和层剖面之地表入渗、迳流分析与推估。
  • By combining the parameter smooth projection algorithm and the integral - type lyapunov design technology with the sliding mode design technology with boundary layer , the performances for the system to avoid the parameter drift phenomena , the chattering phenomena , and the controller singularity problem were improved
    通过将参数光滑投影算法,带饱和层的滑模面设计技术以及积分型李雅普诺夫设计技术集成起来,使得算法提高了系统在抑制参数漂移、抖振现象、控制器奇异等方面的能力。
  • This model is validated by a subsurface flow separation algorithm for an ex - ample river basin , which shows that the new model can simulate the subsurface flow reasonably . keywords : subsurface runoff parameterization , boussinesq - storage equation , water storage and re - charge . hydrological processes including surface runoff , subsurface runoff , and soil water movement play a great role in land surface processes
    文中基于boussinesq - storage方程建立了同时考虑潜水面水分储存和非饱和层水分入渗两方面影响的地下径流机制,并利用流域水文资料以及地下径流分离算法验证了所建立模型的可靠性,结果表明该模型能够比较合理地模拟地下径流的变化情况
  • Thirdly , the method to calculate the 3 - d dynamic responding of layered transversely isotropic saturated soils to an arbitrary buried source in cylindrical coordinate as well as to an arbitrary harmonious source in rectangular coordinate is presented respectively . based on biot ' s wave theory , the 3 - d wave equations in cylindrical coordinate for transversely isotropic saturated poroelastic media are transformed into a group of governing different equations with 1 - order by the fourier expanding with respect to azimuth and hankel integral transform method or by the double fourier transform method with respect to horizontal coordinates in rectangular coordinate . then , transfer matrixes within layered media are derived under the continuous conditions , drainage conditions and the boundary conditions
    基于饱和土的biot波动理论,通过fouricr变换,将横观各向同性饱和土三维非轴对称波动方程转化为一组一阶常微分方程组,再经har止el变换,建立问题的状态方程,求解状态方程得到传递矩阵;利用传递矩阵,结合饱和层状地基的边界条件、排水条件及层间接触和连续条件,首次给出层状横观各向同性饱和地基在任意地展力作用下的三维非轴对称动力响应的解析解。
用"饱和层"造句  

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