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相关概念视频

Average Velocity01:12

Average Velocity

To calculate the other physical quantities in kinematics, we must introduce the time variable. The time variable allows us not only to state the position of the object during its motion, but also how fast it is moving. The speed at which an object is moving is given by the rate at which the position changes with time. For each position xi, we assign a particular time ti. If the details of the motion at each instant are not important, the rate is usually expressed as the average velocity. This...
Average Acceleration01:30

Average Acceleration

The importance of understanding acceleration spans our day-to-day experiences, as well as the vast reaches of outer space and the tiny world of subatomic physics. In everyday conversation, to accelerate means to speed up. For instance, we are familiar with the acceleration of our car; the harder we apply our foot to the gas pedal, the faster we accelerate. The greater the acceleration, the greater the change in velocity over a given time. Acceleration is widely seen in experimental physics. In...
Instantaneous Acceleration01:16

Instantaneous Acceleration

Acceleration is in the direction of the change in velocity, but it is not always in the direction of motion. When an object slows down, its acceleration is opposite to the direction of its motion. Although commonly referred to as deceleration, this causes confusion in our analysis as deceleration is not a vector, and does not point to a specific direction with respect to a coordinate system. Therefore, the term deceleration is not used. For example, when a subway train slows down, it...
Acceleration Vectors01:30

Acceleration Vectors

In everyday conversation, accelerating means speeding up. Acceleration is a vector in the same direction as the change in velocity, Δv, therefore the greater the acceleration, the greater the change in velocity over a given time. Since velocity is a vector, it can change in magnitude, direction, or both. Thus acceleration is a change in speed or direction, or both. For example, if a runner traveling at 10 km/h due east slows to a stop, reverses direction, and continues their run at 10 km/h due...
Central-Force Motion01:17

Central-Force Motion

The central force system operates by exerting a force on an object directed towards a fixed point, typically the origin, with the force magnitude determined by the object's distance from this fixed point. In the context of an object with mass 'm,' polar coordinates are employed to express the equation of motion. Notably, the azimuthal component of force is nonexistent in this system. A comprehensive rewrite and integration of this equation reveal that the product of the squared radial distance...
Velocity of an Object01:18

Velocity of an Object

Understanding how an object moves along a path requires distinguishing between motion over a time span and motion at a precise moment. A useful example is a vehicle traveling along a straight and level path, where its position at any given time is known. The initial step in analyzing this motion is to measure how far the vehicle travels over a fixed time period. This measurement, called average velocity, is computed by dividing the total change in position by the duration over which the change...

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相关实验视频

Updated: Jul 8, 2026

Single Wavelength Shadow Imaging of Caenorhabditis elegans Locomotion Including Force Estimates
08:41

Single Wavelength Shadow Imaging of Caenorhabditis elegans Locomotion Including Force Estimates

Published on: April 18, 2014

在加利福尼亚州文图拉附近,垂直地运动的高速率.

R S Yeats

    Science (New York, N.Y.)
    |April 15, 1977
    PubMed
    概括

    海洋沉积岩揭示了文图拉盆地迅速消退,直到60万年前. 从那时起,它的北部边缘以每年10毫米的速度上升,相当于地质测量速率,但低于圣安德烈亚斯断层.

    科学领域:

    • 地质地质地质地质地质地
    • 地质物理学 地质物理学
    • 构造学 构造学 构造学 构造学

    背景情况:

    • 文图拉盆地的地质历史和构造活动对于理解区域地动态至关重要.
    • 之前的研究提供了长时间垂直移位率的有限量化数据.

    研究的目的:

    • 量化过去200万年来在文图拉盆地垂直移位的速度.
    • 为了比较四分期的垂直运动与最近的地质测量和其他主要断层系统.

    主要方法:

    • 海洋沉积岩的裂变轨道测年.
    • 射线测年技术. 射线测年技术.
    • 古磁分析以确定年龄限制.

    主要成果:

    • 文图拉盆地经历了高达9.5±2.5毫米/年速度的显著沉降,直到大约60万年前.
    • 大约60万年前沉降停止,随后北方盆地边缘升起.
    • 自60万年前以来,北边缘以每年10 ± 2毫米的平均速度上升.

    结论:

    • 沉降的停止和随后的升起表明,文图拉盆地的构造体制发生了重大变化.
    • 最近的升起速度与地质数据一致,但明显低于在圣安德烈亚斯断层沿线观察到的升起速度.

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    Last Updated: Jul 8, 2026

    Single Wavelength Shadow Imaging of Caenorhabditis elegans Locomotion Including Force Estimates
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    Single Wavelength Shadow Imaging of Caenorhabditis elegans Locomotion Including Force Estimates

    Published on: April 18, 2014

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    Visualization of High Speed Liquid Jet Impaction on a Moving Surface

    Published on: April 17, 2015

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