平面的伪地质测量和完全的子多元体
Steen Markvorsen1, Matteo Raffaelli2
1Department of Applied Mathematics and Computer Science, Technical University of Denmark, Matematiktorvet, Building 303B, 2800 Kongens Lyngby, Denmark.
概括
这项研究引入了平面伪地质学来描述完全的同度沉浸. 它证明,对于三维一沉浸,具有平面外在形状的地测板是完全形的.
科学领域:
- 不同几何学微分几何学
- 里曼的几何学 里曼的几何学
背景情况:
- 完全带同度沉浸对于理解里曼的多元体的外在几何学至关重要.
- 这些沉浸的特征提供了对它们的几何性质和与周围空间的关系的洞察.
研究的目的:
- 介绍和描述一个新的曲线类别,平面伪地质学.
- 为了提供一个全同度沉浸的全同度沉浸与平行规范平均曲率向量的新特征.
- 扩展现有关于完全子沉浸的现有结果到更广泛的背景.
主要方法:
- 平面伪地质学的定义和详细研究.
- 对这些曲线的Cartan发展进行分析.
- 调查地测曲率与正常曲率之间的关系.
- 将这些概念应用于里曼的多元体之间的同度沉浸,特别是在一个共维的情况下.
主要成果:
- 使用平面伪地质学的平行正常化平均曲率向量对完全带同度沉浸的新奇特征.
- 建立平面伪地质学的本地存在和独特性.
- 证明一个同度沉浸是完全的,如果并且只有如果每一个地形都有一个平面的外在形状 (在三维-一个的情况下).
结论:
- 平面伪地质测量提供了一个强大的新工具,用于研究完全的同度沉浸.
- 该研究扩展了关于沉浸的外部几何学的经典结果.
- 这些发现有助于更深入地了解里曼系的内在和外在属性之间的关系.
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