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用于高效精确高阶有限元可视化的粒子系统

Particle systems for efficient and accurate high-order finite element visualization.

作者信息

Meyer Miriah, Nelson Blake, Kirby Robert, Whitaker Ross

机构信息

Scientific Computing and Imaging Institute, University of Utah, Salt Lake City, UT 84103, USA.

出版信息

IEEE Trans Vis Comput Graph. 2007 Sep-Oct;13(5):1015-26. doi: 10.1109/TVCG.2007.1048.

Abstract

Visualization has become an important component of the simulation pipeline, providing scientists and engineers a visual intuition of their models. Simulations that make use of the high-order finite element method for spatial subdivision, however, present a challenge to conventional isosurface visualization techniques. High-order finite element isosurfaces are often defined by basis functions in reference space, which give rise to a world-space solution through a coordinate transformation, which does not necessarily have a closed-form inverse. Therefore, world-space isosurface rendering methods such as marching cubes and ray tracing must perform a nested root finding, which is computationally expensive. We thus propose visualizing these isosurfaces with a particle system. We present a framework that allows particles to sample an isosurface in reference space, avoiding the costly inverse mapping of positions from world space when evaluating the basis functions. The distribution of particles across the reference space isosurface is controlled by geometric information from the world-space isosurface such as the surface gradient and curvature. The resulting particle distributions can be distributed evenly or adapted to accommodate world-space surface features. This provides compact, efficient, and accurate isosurface representations of these challenging data sets.

摘要

可视化已成为模拟流程的一个重要组成部分,为科学家和工程师提供其模型的视觉直观感受。然而,利用高阶有限元方法进行空间细分的模拟,给传统的等值面可视化技术带来了挑战。高阶有限元等值面通常由参考空间中的基函数定义,通过坐标变换产生一个世界空间解,而该坐标变换不一定有闭式逆变换。因此,诸如移动立方体和光线追踪等世界空间等值面渲染方法必须执行嵌套的根查找,这在计算上是昂贵的。因此,我们建议用粒子系统来可视化这些等值面。我们提出了一个框架,允许粒子在参考空间中对等值面进行采样,在评估基函数时避免从世界空间进行昂贵的位置逆映射。粒子在参考空间等值面上的分布由来自世界空间等值面的几何信息控制,如表面梯度和曲率。由此产生的粒子分布可以均匀分布或进行调整以适应世界空间表面特征。这为这些具有挑战性的数据集提供了紧凑、高效和准确的等值面表示。

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