Description: 关于一的微分方程数值解,一维波动方程初边值问题Crank-Nicholson格式,及追赶法-On one of the numerical solution of differential equations, one-dimensional wave equation Crank-Nicholson format, and to catch up with the Law Platform: |
Size: 3035136 |
Author:陆祥安 |
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Description: 这是将波动方程分解为上行波下行波的源程序 把两个源代码放在一起,运行即可了!-This is the wave equation will be decomposed into up-going wave downlink wave source source code of the two together, you can run the! Platform: |
Size: 2048 |
Author:陈浩 |
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Description: 地震波方程的时间空间二阶差分的数值模拟,程序用vc++6.0调试,需要matlab绘图-Seismic wave equation of time and space second-order difference of the numerical simulation, the program used vc++ 6.0 debugging, need matlab graphics Platform: |
Size: 974848 |
Author:panjun |
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Description: A numerical solution of the 2D wave equation
utt = β2 (uxx + uyy)
is required over the region R in the x, y plane
R = {(x, y)| 0 < x < a, 0 < y < b}-A numerical solution of the 2D wave equation utt = β2 (uxx+ uyy) is required over the region R in the x, y plane R = ((x, y) | 0 < x < a, 0 < y < b) Platform: |
Size: 1024 |
Author:liuzhenghao |
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Description: 纵波在弹性界面散射的左普里兹方程MATLAB代码,实现纵波散射后反射波和投射波反射系数随波入射角变化关系-Longitudinal waves in elastic interface scattering equation of the left Prydz MATLAB code, and achieve the P-wave scattering of the reflected wave after wave reflection coefficient of the waves and the projection angle of incidence changes in the relationship between Platform: |
Size: 5120 |
Author:赛亚人 |
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Description: 弹性波方程的地震波场的正演模拟,采用的是高阶精度--10阶,但是还没加边界-Elastic wave equation of seismic wave field forward modeling, using the high-order accuracy- 10 bands, but not Canadian border Platform: |
Size: 2048 |
Author:王子 |
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Description: 声波二阶方程空间十阶时间二阶在一维情况下的变网格数值模拟-Second-order wave equation of second order in time space 10 in One-Dimensional Numerical Simulation of Variable Grid Platform: |
Size: 1024 |
Author:张红静 |
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Description: This paper shows how electrical engineering undergraduates can acquire a working
knowledge of the finite element method (FEM) within a short period of time using MATLAB. For
simplicity, only first-order triangular elements are considered. The scalar wave equation for
homogeneous isotropic waveguides is used for introducing the FEM. Simple waveguide problems,
including a design problem, are discussed as examples. It is shown how the knowledge acquired can
be extended to other electromagnetic problems Platform: |
Size: 119808 |
Author:mahdi |
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Description: Cool visualization of shallow water wave equation
Employs Crank-Nicholson scheme, 2nd order accurate, CFD calculation of shallow water wave equation. If processor is slow, can decrease ni, nj, tmax. Very little viscous diffusion allowed, boundary conditions aren t great. Initial condition is a sudden column of water that drops into the ocean. provides a cool visualization of tsunami traveling up a beach, peaking, and returning to sea.
-Employs Crank-Nicholson scheme, 2nd order accurate, CFD calculation of shallow water wave equation. If processor is slow, can decrease ni, nj, tmax. Very little viscous diffusion allowed, boundary conditions aren t great. Initial condition is a sudden column of water that drops into the ocean. provides a cool visualization of tsunami traveling up a beach, peaking, and returning to sea.
Platform: |
Size: 1024 |
Author:謝一 |
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Description: 一维线性齐次波动方程,用matlab语言实现,利用边界值和边界条件进行求解-One-dimensional linear homogeneous wave equation, with the matlab language, use of boundary value and boundary conditions to solve Platform: |
Size: 141312 |
Author:李琨 |
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Description: 3D Wave equation Model forwarding by the method of pesudo-spectrum-3D Wave equation Model forwarding by the method of pesudo-spectrum Platform: |
Size: 3072 |
Author:Max |
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Description: 地震波动方程二维模拟(C语言),差分求解,波源雷克子波,文件夹中,".m"是用于作图的代码,在matlab中打开。-Earthquake fluctuations the wave equation (C language), Finite difference method, the source: Ricker wave, in the folder. .m is the code used for mapping, opened in matlab. Platform: |
Size: 279552 |
Author:jiuwu |
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