在地形测量中的高度波动和表面梯度
Julie Lemesle1,2, Clement Moreau3,4, Raphael Deltombe3
1U.R Concept, 59300 Valenciennes, France.
Materials (Basel, Switzerland)
|August 12, 2023
概括
地形地图中的地表高度波动与当地的地表梯度呈指数关系. 了解这些波动,可以了解各种材料类型的表面功能和完整性.
科学领域:
- 地质科学 地质科学
- 材料科学 材料科学 材料科学
- 表面计量学 表面计量学
背景情况:
- 地形地图使用 (x,y,z) 坐标表示表面.
- 高度波动代表特定表面位置的测量不确定性.
研究的目的:
- 调查地形数据中高度波动和表面梯度之间的关系.
- 为了确定表面特征如何影响测量不确定性.
主要方法:
- 对像素坐标 (x,y) 和高度样本 (z) 的分析.
- 从三角面的正常向量计算表面梯度.
- 梯度图与高度波动图的比较.
主要成果:
- 高度波动显示出对局部表面梯度的指数依赖.
- 最高的波动与特定的表面特征相关,例如翻转,喷砂或磨损的表面.
- 波动受到工具/材料相互作用和塑性变形的影响.
结论:
- 表面地形学决定了波动模式和测量不确定性.
- 波动较高的区域可以表明关键的表面功能或完整性.
- 这种关系适用于不同的表面类型,包括异质和多层材料.
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