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相关概念视频

Errors in Taping01:18

Errors in Taping

446
Errors in taping arise from multiple factors that can significantly impact measurement accuracy in surveying. Misalignment of the tape, often due to human error, is one primary source. A skilled rear tapeman, using a telescope, can help correct alignment by guiding the head tapeman; however, human limitations still lead to small inaccuracies. These errors may include misplacement of pins or inaccurate tape readings due to common visual confusions, such as mistaking a six for a nine. Such...
446
Common Leveling Mistakes and Errors01:17

Common Leveling Mistakes and Errors

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A survey team is tasked with determining the elevation difference between points Point A and Point B, separated by uneven terrain. They use a leveling instrument and a leveling rod.Common MistakesMisreading the Rod: During a backsight reading at Point A, the instrumentman observes the rod partially obscured by tall grass. Instead of reading 1.135 m, they mistakenly record 1.735 m due to the misalignment of the crosshair with the wrong graduation. This error adds 0.600 m to all subsequent...
601
Rolling With Slipping01:14

Rolling With Slipping

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Rolling with slipping is a physical phenomenon that occurs when a rolling object experiences both rotational and linear motion but also experiences frictional forces that cause slipping. This phenomenon can occur in various situations, such as when a tire rolls on a wet road or a ball rolls on a rough surface.
An object's rolling motion is characterized by its rotation around its axis, while linear motion refers to the object's translational motion along a surface. Frictional forces can...
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Friction: Problem Solving01:21

Friction: Problem Solving

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Friction is an essential force that influences the motion of objects in daily life. Depending on the situation, it can be either beneficial or problematic. Consider a bus with a mass of three megagrams and its center of mass at a specific point, moving along a banked road at a constant speed. The coefficient of static friction between the tires and the road is 0.5. Find the maximum angle of the banked road at which the bus would not slip or tip.
Initially, a visual representation of the...
603
Rolling Resistance01:21

Rolling Resistance

746
When a solid cylinder rolls steadily on a rigid surface, the normal force applied by the surface on the cylinder is perpendicular to the tangent at the contact point. However, since no materials are entirely rigid, the surface's reaction to the cylinder involves a range of normal pressures.
For instance, imagine a hard cylinder rolling on a comparatively soft surface. The cylinder's weight compresses the surface beneath it. As the cylinder moves, the material in front of it slows down due to...
746
Free-body Diagrams: Problem Solving01:30

Free-body Diagrams: Problem Solving

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Free-body diagrams are essential tools for physicists and engineers studying the motion of objects. Free-body diagrams are graphical representations of the object or system under consideration, and they focus solely on the essential forces acting on the object. This tool helps break down complex problems into simpler models that are easier to understand and solve.
For example, consider a block with a mass of 10 kg released on an inclined plane at an angle of 30° to the horizontal, where...
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相关实验视频

Updated: Mar 30, 2026

The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults
07:39

The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults

Published on: November 6, 2021

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地测证据表明,阿尔廷塔赫断层系统的滑动率较低.

Bendick1, Bilham, Freymueller

  • 1CIRES & Department of Geological Sciences, University of Colorado, Boulder 80309-0399, USA.

Nature
|March 15, 2000
PubMed
概括

地测数据揭示了阿尔廷塔赫断层系统的存在.

科学领域:

  • 地质物理学 地质物理学
  • 构造学 构造学 构造学 构造学
  • 地质测量是指地质测量.

背景情况:

  • 印度-亚洲碰撞驱动整个东亚的变形.
  • 阿尔廷塔格断层系统的活动受到争论,地质估计范围广泛.
  • 之前的模型与其在适应印度-亚洲融合中的作用存在冲突.

研究的目的:

  • 为了量化整个阿尔廷塔赫断层系统的滑动率和收缩.
  • 将地质测量测量与地质和动态模型预测进行比较.
  • 评估阿尔廷塔赫断层系统对亚洲变形的贡献.

主要方法:

  • 在Altyn Tagh断层系统 (89-91°E) 进行地质测量.
  • 分析左侧剪切和南北收缩.
  • 与现有的地质滑坡率估计和动态模型进行比较.

主要成果:

  • 在Altyn Tagh断层系统中,左侧切割幅度为9 ± 5 mm yr-1.
  • 在Altyn Tagh断层系统中收缩3 ± 1mm yr−1.
  • 西藏的南北收缩在90°E的9 ± 1毫米年−1.

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相关实验视频

Last Updated: Mar 30, 2026

The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults
07:39

The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults

Published on: November 6, 2021

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Image-based Lagrangian Particle Tracking in Bed-load Experiments
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Image-based Lagrangian Particle Tracking in Bed-load Experiments

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Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

Published on: August 5, 2016

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结论:

  • 地测数据表明,阿尔廷塔赫断层系统的滑动率低于一些地质估计.
  • 测量的变形支持来自亚洲构造学动态模型的预测.
  • 阿尔廷塔格断层系统容纳的印度-亚洲汇合的部分比以前的一些研究所建议的要小.