在正方形网格钻井布局模型的基础上，讨论了非均匀网格定位模型。
Based on the model of well-drilling layout with square grid, the model with non-uniformity grid is discussed.
同种方法在非均匀网格下的格式精度较在均匀网格下低0 ~1阶。
Besides, the precision under non-uniform grid format was lower 0 ~ 1 order than in uniform grid with the same methods.
针对点云数据量大的特点，提出了基于非均匀网格的点云数据缩减算法。
This paper proposes an algorithm of data reduction based on asymmetric gridding in connection with the vast amount of point data.
针对计算高精度需要，纳入了适合非均匀网格、采用附加源项实现的QUICK格式。
QUICK method, which was adapted to non-uniformly grid and implemented by an additional source, was adopted for high-required precision.
文章针对逆向工程中的特殊简化要求，提出了一种强制约束下的非均匀网格简化算法。
In this paper, aiming at some special requirements of mesh simplification in reverse engineering, a non-uniform mesh simplification algorithm based on forcible constraint is presented.
为了降低模型误差，引入非均匀网格，并且自适应的在参数变化快的地方用较细网格，其他地方用较粗网格。
In order to reduce model error, we use non-uniform grid, if the parameter's changing is fast, we use fine grid, else we use coarse grid.
采用坐标变换方法，将物理平面中任意几何区域上的非均匀网格剖分映射到计算平面中规则区域上的均匀网格剖分。
In this paper, an one to one maping is used to transfer an arbitrary domain and a nonuniform grid on it in physical plane to a rectangular domain with a uniform grid in computational plane.
根据电极不同的摇动方式，非均匀偏置离散网格。
According to the electrode orbiting patterns, the scattered meshes were non-uniformly offset.
基于非均匀FDTD网格的电磁场模拟是一种解决诸多实际电磁场问题的通用、有效方法。
The electromagnetic simulation based on Non-uniform FDTD mesh is a generalized and efficient method to solve many practical electromagnetic problems.
“双网格”方法和相应的算法为非均匀边界条件控制下河道演变的数值模拟提供了保证。
The dual grid method can provide a useful tool for numerically simulating the fluvial processes with non-uniform boundary conditions.
基于非均匀FDTD网格的电磁场模拟是解决电磁场问题的一种有效方法。
The electromagnetic simulation based on Non-uniform FDTD mesh is a generalized and efficient method to solve many electromagnetic problems.
计算结果证明，当采用非均匀圆柱坐标系下FDTD法计算时，圆柱坐标系下网格波阻抗可以较准确地计算由于网格尺寸不同造成的数值反射误差。
The results showed that MWI in cylindrical coordinates can be used to accurately calculate the numerical reflection error caused by different mesh increments in non uniform FDTD.
将多重网格技术与变形玻恩迭代法相结合，对轴对称二维非均匀介质分布进行了反演。
The profile of a two-dimensional axisymmetric inhomogeneous medium is reconstructed by using the distorted Born iterative method and multi-grid technique.
根据其优化思想 ，在非均匀笛卡尔坐标系网格条件下 ，推导得到了更为通用的GODRP格式优化系数公式。
In this paper, the derivation and formulation of the GODRP scheme were improved for non-uniform Cartesian grids in a more general form.
同时用并联网格电阻发热的概念处理非均匀内热源项。
In addition, the conception of parallel network resistance heat generation has been applied to deal with the non-uniform internal heat source item.
地表的非均匀性是普遍存在的，对不同的地表通量参数化方案来说，地面非均匀性对对网格区面积平均通量计算的影响程度可能不同。
The appearance of heterogeneity can be observed widely in nature. The surface heterogeneities have different impacts on the estimation of area-averaged flux for different parameterization schemes.
提出一种新的三维空间不规则网格有限差分方法，模拟具有地形构造的非均匀各向异性介质中弹性波传播过程。
This paper presents a new 3d finite-difference (FD) method using spatially irregular grids to simulate elastic wave propagation in heterogeneous anisotropic media with topographic structures.
本文应用空间理想非均匀线性弹性力学平衡关系生成三维贴体与边界正交网格。
Three-dimensional body-fitted grids perpendicular to the boundary are generated in this paper by applying equilibrium relation of forces acting on the ideal non-uniform linear elastic lines.
分析了时域有限差分(FDTD)网格的生成原理，提出了一种新型非均匀FDTD网格生成算法。
The principle of generating FDTD (Finite Difference Time Domain) grid is analysed, and an improved arithmetic for generating nonuniform FDTD grid is presented.
该文提出了由自适应三维网格和固定矩形网格组合的“双网格”方法来模拟非均匀边界条件控制下河道演变的思路。
A dual grid, consisted of an adaptive 3-d grid and a stationary 2-d rectangular grid, is employed to model the fluvial processes under the control of non-uniform boundary conditions.
该文提出了由自适应三维网格和固定矩形网格组合的“双网格”方法来模拟非均匀边界条件控制下河道演变的思路。
A dual grid, consisted of an adaptive 3-d grid and a stationary 2-d rectangular grid, is employed to model the fluvial processes under the control of non-uniform boundary conditions.
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