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

Minerals01:26

Minerals

1.4K
Minerals are essential nutrients that the human body needs in small amounts to work properly. They play a vital role in many bodily functions, such as building strong bones and transmitting nerve impulses. Some minerals are needed for hormone production or to maintain a normal heartbeat. Major minerals include calcium, phosphorus, potassium, sulfur, sodium, chlorine, and magnesium, while trace minerals include iron, manganese, copper, iodine, zinc, cobalt, fluoride, and selenium.
 
Major...
1.4K
Porosity in Cement Paste01:18

Porosity in Cement Paste

490
The porosity of concrete is a measure of the void spaces within its structure. These spaces impact its strength and durability significantly. When water and cement interact, a chemical reaction called hydration creates a semi-solid paste. This paste includes combined water, making up approximately 23% of the cement's dry mass, and gel water, which fills minuscule voids known as gel pores, accounting for about 28% of the cement gel volume.
The balance of water to cement in the mix is...
490
Magnetic Susceptibility and Permeability01:31

Magnetic Susceptibility and Permeability

2.5K
In linear magnetic materials, like paramagnets and diamagnets, magnetization is proportional to the magnetic field intensity. The constant of proportionality, a dimensionless number, is called magnetic susceptibility. The value of the susceptibility depends on the type of material.
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...
2.5K
Conditions on Early Earth02:06

Conditions on Early Earth

102.1K
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
102.1K
Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

20.4K
Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
20.4K
Crystal Field Theory - Octahedral Complexes02:58

Crystal Field Theory - Octahedral Complexes

31.1K
Crystal Field Theory
To explain the observed behavior of transition metal complexes (such as colors), a model involving electrostatic interactions between the electrons from the ligands and the electrons in the unhybridized d orbitals of the central metal atom has been developed. This electrostatic model is crystal field theory (CFT). It helps to understand, interpret, and predict the colors, magnetic behavior, and some structures of coordination compounds of transition metals.
CFT focuses on...
31.1K

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

Origin of Earth's hydrogen and carbon constrained by their core-mantle partitioning and bulk Earth abundance.

Nature communications·2025
Same author

Trace element partitioning in a deep magma ocean and the origin of the Hf-Nd mantle array.

Science advances·2024
Same author

Novel non-Joule heating technique: Externally laser-heated diamond anvil cell.

The Review of scientific instruments·2023
Same author

Stratification in planetary cores by liquid immiscibility in Fe-S-H.

Nature communications·2022
Same author

The Fe-FeSi phase diagram at Mercury's core conditions.

Nature communications·2022
Same author

Experimental evidence for hydrogen incorporation into Earth's core.

Nature communications·2021

相关实验视频

Updated: Feb 19, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

13.0K

在地球深处的矿

Kei Hirose1,2, Ryosuke Sinmyo3,2, John Hernlund3

  • 1Earth-Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo 152-8550, Japan. kei@elsi.jp.

Science (New York, N.Y.)
|November 11, 2017
PubMed
概括

酸矿是地球深层的关键矿物,影响着行星的进化. 了解它们的特性对于理解地幔动态和岩石行星的发展至关重要.

科学领域:

  • 地质学
  • 矿物物理
  • 星球科学

背景情况:

  • 酸矿在地球的下层地幔中很丰富 (>660公里深).
  • 富含的矿在核心-地幔边界转变为后矿.
  • 富含的矿,虽然很小,但记录了化学差异化.

研究的目的:

  • 阐明地幔矿在地球结构和进化中的重要性.
  • 突出佩洛夫斯基特在理解地球发展中的作用.

主要方法:

  • 分析矿物质的物理性质.
  • 在矿中微量元素的地化学解释.

主要成果:

  • 矿的特性决定了下层地幔岩石的运输.
  • 这些矿物质对于理解地球的动态演变至关重要.
  • 在火星之外的岩石行星中, 岩石是重要的组成部分.

结论:

  • 层矿对地球的内部动力学有着根本性的作用.
  • 他们的研究为整个宇宙的陆地行星的演变提供了洞察力.

更多相关视频

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

12.1K
Atom Probe Tomography Analysis of Exsolved Mineral Phases
08:14

Atom Probe Tomography Analysis of Exsolved Mineral Phases

Published on: October 25, 2019

7.8K

相关实验视频

Last Updated: Feb 19, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

13.0K
Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

12.1K
Atom Probe Tomography Analysis of Exsolved Mineral Phases
08:14

Atom Probe Tomography Analysis of Exsolved Mineral Phases

Published on: October 25, 2019

7.8K