Jove
Visualize
联系我们
JoVE
x logofacebook logolinkedin logoyoutube logo
关于 JoVE
概览领导团队博客JoVE 帮助中心
作者
出版流程编辑委员会范围与政策同行评审常见问题投稿
图书馆员
用户评价订阅访问资源图书馆顾问委员会常见问题
研究
JoVE JournalMethods CollectionsJoVE Encyclopedia of Experiments存档
教育
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab Manual教师资源中心教师网站
使用条款与条件
隐私政策
政策

相关概念视频

Buoyancy and Stability for Submerged and Floating Bodies01:11

Buoyancy and Stability for Submerged and Floating Bodies

1.8K
In fluid mechanics, buoyancy and stability are key concepts for understanding the behavior of submerged and floating bodies. When a stationary body is fully or partially submerged in a fluid, the fluid exerts a force on the body known as the buoyant force. This force acts vertically upward through a point called the center of buoyancy, which is the center of the displaced fluid volume. According to Archimedes' principle, the magnitude of the buoyant force is equal to the weight of the fluid...
1.8K
Intermolecular Forces in Solutions02:28

Intermolecular Forces in Solutions

33.6K
The formation of a solution is an example of a spontaneous process, a process that occurs under specified conditions without energy from some external source.
When the strengths of the intermolecular forces of attraction between solute and solvent species in a solution are no different than those present in the separated components, the solution is formed with no accompanying energy change. Such a solution is called an ideal solution. A mixture of ideal gases (or gases such as helium and argon,...
33.6K
The Nernst Equation02:59

The Nernst Equation

40.8K
Nonstandard Reaction Conditions
The interconnection between standard cell potentials and various thermodynamic parameters such as the standard free energy change ΔG° and equilibrium constant K has been previously explored. For example, a redox reaction involving zinc(II) and tin(II) ions at 1 M concentration with Eºcell = +0.291 V and ΔG° = −56.2 kJ is spontaneous.
40.8K
Cohesion01:07

Cohesion

54.3K
Cohesion is the attraction between molecules of the same type, such as water molecules. Water molecules have an overall neutral charge but are polar molecule. An oxygen atom in one water molecule has a partial negative charge that can bind to a hydrogen atom with a partial positive charge in a second water molecule, forming a hydrogen bond. Each water molecule can form up to four hydrogen bonds with other water molecules. Hydrogen bonds are responsible for water's cohesive nature.
On a...
54.3K
Aqueous Solutions and Heats of Hydration02:42

Aqueous Solutions and Heats of Hydration

14.7K
Water and other polar molecules are attracted to ions. The electrostatic attraction between an ion and a molecule with a dipole is called an ion-dipole attraction. These attractions play an important role in the dissolution of ionic compounds in water.
When ionic compounds dissolve in water, the ions in the solid separate and disperse uniformly throughout the solution because water molecules surround and solvate the ions, reducing the strong electrostatic forces between them. This process...
14.7K
Steady, Laminar Flow Between Parallel Plates01:17

Steady, Laminar Flow Between Parallel Plates

192
Understanding steady, laminar flow between parallel plates is essential for analyzing and designing flow in narrow rectangular channels, commonly found in various water conveyance and drainage systems. The Navier-Stokes equations govern fluid motion and are generally challenging to solve due to their nonlinearity. However, simplifications are possible in certain cases, like the steady laminar flow between parallel plates. For this scenario, we assume steady, incompressible, laminar flow.
192

您也可能阅读

相关文章

通过共同作者、期刊和引用图与本文相关的文章。

排序
Same author

Probing rock rupture with naturally occurring nuclide signals.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same author

Real-rock microfluidic platform for quantifying chemical dissolution and mechanical erosion in a multiphase environment.

Lab on a chip·2025
Same author

Controls of the Nucleation Rate and Advection Rate on Barite Precipitation in Fractured Porous Media.

Langmuir : the ACS journal of surfaces and colloids·2025
Same author

Molecular Origin of Wetting Characteristics on Mineral Surfaces.

Langmuir : the ACS journal of surfaces and colloids·2023
Same author

Three-Dimensional Visualization Reveals Pore-Scale Mechanisms of Colloid Transport and Retention in Two-Phase Flow.

Environmental science & technology·2023
Same author

Pore-Scale Mechanisms of Solid Phase Emergence During DNAPL Remediation by Chemical Oxidation.

Environmental science & technology·2022

相关实验视频

Updated: Jul 3, 2025

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
08:19

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System

Published on: May 9, 2021

2.2K

在水平的Hele-Shaw细胞中,浮力驱动的溶解不稳定性.

Kai Li1,2, Ran Hu1,2, Ting Wang3

  • 1State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan 430072, China.

Langmuir : the ACS journal of surfaces and colloids
|February 15, 2024
PubMed
概括

岩石断裂中的矿物溶解由于浮力驱动的对流变得不稳定. 这项研究揭示了度边界层的临界厚度,预测了这种不稳定性在地质构造中何时发生.

更多相关视频

Magnetically Induced Rotating Rayleigh-Taylor Instability
06:42

Magnetically Induced Rotating Rayleigh-Taylor Instability

Published on: March 3, 2017

9.6K
Experimental Methods for Efficient Solar Hydrogen Production in Microgravity Environment
11:38

Experimental Methods for Efficient Solar Hydrogen Production in Microgravity Environment

Published on: December 3, 2019

7.6K

相关实验视频

Last Updated: Jul 3, 2025

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
08:19

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System

Published on: May 9, 2021

2.2K
Magnetically Induced Rotating Rayleigh-Taylor Instability
06:42

Magnetically Induced Rotating Rayleigh-Taylor Instability

Published on: March 3, 2017

9.6K
Experimental Methods for Efficient Solar Hydrogen Production in Microgravity Environment
11:38

Experimental Methods for Efficient Solar Hydrogen Production in Microgravity Environment

Published on: December 3, 2019

7.6K

科学领域:

  • 地质化学和水文地质学
  • 孔尺度反应式运输反应式运输

背景情况:

  • 岩石断裂中的矿物溶解是地质过程的关键.
  • 浮力驱动的对流可以导致溶解不稳定性,但孔尺度机制尚不清楚.
  • 实验挑战限制了对流量和度场的理解.

研究的目的:

  • 研究由浮力驱动的对流驱动的溶解不稳定性的孔尺度机制.
  • 用模拟和理论分析辐射水平几何中的溶解.
  • 开发一种关于溶解不稳定开始的预测模型.

主要方法:

  • 开发并验证了包括重力效应在内的孔尺度建模方法.
  • 采用3D孔尺度数值模拟来研究流溶动力学.
  • 进行了度边界层和时间尺度相互作用的理论分析.

主要成果:

  • 确定了浮力驱动溶解不稳定性的临界长度标准.
  • 在有限和半无限域不稳定的政权之间进行区分.
  • 证明的不稳定性来自于度边界层的重力不稳定的临界厚度.

结论:

  • 建立了一个理论模型,通过模拟和实验验证,以预测溶解不稳定性.
  • 增强对辐射水平流中的浮力驱动溶解不稳定性的理解.
  • 提供了有关岩水文和地质二氧化碳储存完整性的见解.