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difference equation相关的网络例句

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与 difference equation 相关的网络例句 [注:此内容来源于网络,仅供参考]

The electrostatic potential was calculated by solving the Poisson- Boltzmanne equation using the finite difference method.

三种金属硫蛋白的静电势通过有限差分方法求解Poisson-Boltzmann方程得到。

In this paper, the oscillation of forced neutral difference equations with positive and negative coefficients is studied and two sufficient conditions of this equation to be oscillatory are obtained.

研究了一类具有强迫项正负系数中立型差分方程的振动性,获得了方程振动的两个充分条件。

On the basis of this, the finite difference forward simulation program of crosswell seismic wave equation was compiled.

在此基础上,编制了跨孔波场交错网格有限差分正演程序,并应用该程序对半空间粘弹性跨孔模型进行了正演计算,得到了震源在不同位置时的波场快照及地震记录图。

Using difference method, the first-order and the second-order differential equations of fractional derivative can become the first-order ordinary differential equation, and the high precision direct integration can be used for the solution.

所论方法首先引入差分格式,将含有分数阶导数的一阶和二阶微分方程变为一阶的常微分方程,然后再用精细积分方法逐步积分进行求解。

To obtain the unknown intermediate vector function needs to solve a Fredholm integral equation of the first kind, the solution of which can only be determined with a difference of a vector proportional to the normal of the boundary and its integration on the boundary must zero.

可是要求出该积分表达式中待定的边界上的向量密度函数要导致求解第一类Fredholm 积分方程。

Produced the gradient wind equation and showed examples of gradient wind (and its difference from the geostrophic wind) in 500mb height maps.

推导出梯度风方程并在500毫八高度地图中举出梯度风的例子(以及它与地转风的不同之处)。

The solution to the one dimensional hyperbolic runoff equations and sediment equation are obtained respectively by using the characteristics method and finite difference method.

利用水力学原理建立了坡面降雨径流和土壤侵蚀模型,分别采用特征线法和有限差分法对径流量和土壤侵蚀量进行了求解,并针对具体降雨事件进行了模拟计算,计算结果与试验小区实测值基本一致。

The solitary wave can be generated considering Goring and Raichlen's movement of a paddle. The proposed original linear solution for the solitary wave generation is expressed in the hypergeometric function. Two disadvantages of the original solution with large trailing wave and skewed wave profile are found by comparing with the theory of solitary wave derived from Boussinesq's equation. The difference between the original linear solution and the solitary wave theory results from the nonlinearity and dispersion of generated waves in the flume.

本文并以弱非线性的孤立波造波问题做为解析之对象,由於孤立波造波板速度为一超越函数,造成解析上的困难;本文以 hypergeometric 函数推求常微分方程式之全解,并与理论波形解比较后,发现由於未考虑非线性及分散性过强等问题,使得线性暂态解较理论波形拉长与歪斜,可能无法有效描述孤立波造波问题,故针对线性之分散关系做出修正。

This paper gives a 45 degree up-going wave equation with an absorbing layer and constructs its implicit difference scheme.

给出了附加吸收层的三维45°上行波方程,构造了该方程的一种隐式差分格式。

In chapter two,We present a globally nonlinear implicit difference scheme,i.e., a nonlinear iterative algorithma has to be used to solve the system of the nonlinear algebraic equation at each discrete time step.

第二章构造了一个非线性隐差分格式,在每一个时间层上需要迭代求解非线性方程组,该格式可以保证离散电荷和离散能守恒。

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