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Home > english-chinese > "integral transform method" in Chinese

Chinese translation for "integral transform method"

积分变换法

Related Translations:
viewing transform:  取景变换
airy integral:  亚里积分
probability integral:  概率积分几率积分
integral unit:  成套机组积分部件联合机组全套部件
integral scattering:  积分散射
integral error:  积分误差
integral hinge:  整体交连
complete integral:  完全积分完全原函数
circulation integral:  圆周积分
integral pattern:  整模式, 整图象
Example Sentences:
1.The solving process of the d ' alembert ' s differential equation using fourier ' s triple integral transform method
用重傅氏积分变换法求解达朗贝尔方程
2.Considering the elasticity of the foundation , the author uses the same integral transform method and analyses the presence of the pore water and the effect of the rigidity of the foundation on the dynamic response of the foundation
对于饱和地基上弹性基础的扭转振动情况,本文采用同样的方法分析了半空间孔隙水的存在和基础刚度对动力响应的影响。
3.( 5 ) discuss some mathematical models of the pollutant transport problems in some local river flow fields . by integral transform method , the paper establishes the usual finite difference approximation scheme to solve the numerical solutions and gives examples for the computation of the approximating solutions , moreover , discusses one - dimensional characteristic finite difference method for a convection - diffusion equation under usual conditions
( 5 )针对水域中污染物输移问题的数学模型,通过积分变换法,得到了简化模型在理想化条件下的近似精确解,同时给出数值算例,并且对非理想化条件下模型的特征差分方法进行了讨论。
4.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。
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