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相关概念视频

Conditions on Early Earth02:06

Conditions on Early Earth

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.
Vapor Pressure02:34

Vapor Pressure

When a liquid vaporizes in a closed container, gas molecules cannot escape. As these gas phase molecules move randomly about, they will occasionally collide with the surface of the condensed phase, and in some cases, these collisions will result in the molecules re-entering the condensed phase. The change from the gas phase to the liquid is called condensation. When the rate of condensation becomes equal to the rate of vaporization, neither the amount of the liquid nor the amount of the vapor...
Vapor Pressure Lowering03:28

Vapor Pressure Lowering

The equilibrium vapor pressure of a liquid is the pressure exerted by its gaseous phase when vaporization and condensation are occurring at equal rates: Dissolving a nonvolatile substance in volatile liquid results in a lowering of the liquid’s vapor pressure. This phenomenon can be explained by considering the effect of added solute molecules on the liquid's vaporization and condensation processes. To vaporize, solvent molecules must be present at the surface of the solution. The presence of...
Conditions on Early Earth02:06

Conditions on Early Earth

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.
Distillation: Vapor–Liquid Equilibria01:01

Distillation: Vapor–Liquid Equilibria

Distillation is a separation technique that takes advantage of the boiling point properties of disparate elements in a mixture. To perform distillation, we begin by heating a miscible mixture of two liquids with a significant difference in boiling points (at least 20°C). As the solution heats up and reaches the bubble point of the more volatile component, some molecules of the more volatile component transition into the gas phase and travel upward into the condenser, which is a glass tube with...
Volatilization01:10

Volatilization

Volatilization gravimetry is an analytical technique that measures the mass lost due to the volatilization of the substance. This technique is used to estimate the amount of volatile material in a sample. To perform this method, heat a known amount of the sample to a high temperature in a crucible or other suitable vessel. The volatile substance in the sample evaporates, and the vapor is completely expelled from the crucible either by heating the sample or bubbling a stream of inert gas through...

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相关实验视频

Updated: Jul 10, 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

原始的中海基岩中的蒸汽不和和地球上层地幔的挥发性含量.

Alberto E Saal1, Erik H Hauri, Charles H Langmuir

  • 1Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA. asaal@ldeo.columbia.edu

Nature
|October 9, 2002
PubMed
概括
此摘要是机器生成的。

这项研究分析了中海基岩中爆发前的挥发性物质含量,揭示了对地球的新见解.

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相关实验视频

Last Updated: Jul 10, 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

Atom Probe Tomography Analysis of Exsolved Mineral Phases
08:14

Atom Probe Tomography Analysis of Exsolved Mineral Phases

Published on: October 25, 2019

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
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Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment

Published on: February 27, 2021

科学领域:

  • 地质化学 地质化学
  • 火山学 火山学是一门学科.
  • 地球科学 地球科学 地球科学

背景情况:

  • 岩系统中的挥发性分析告诉地球地幔的组成和岩脱气对海洋和大气化学的影响.
  • 大多数喷发的岩在大气压下脱气,由于岩溶解度低,失去了主要的挥发性特征.

研究的目的:

  • 为了确定来自Siqueiros内部转变传播中心的中海基岩的低和爆发前挥发性物质含量.
  • 在上层地幔内建立对挥发性丰度和行为的新约束.

主要方法:

  • 在一系列中海基岩中对挥发性物质含量的分析.
  • 调查低和岩石中挥发性和耐火性微量元素之间的相关性.

主要成果:

  • 报告的低和的爆发前挥发性物质含量对于Siqueiros中海基岩.
  • 在普通的中海基岩源中对二氧化碳,水,,硫和的丰度建立了新的约束.
  • 利用二氧化碳行为和CO2 / Nb和CO2 / Cl比率来估计原始的二氧化碳和.

结论:

  • 在爆发前的岩石中,低和使得主要的挥发性特征得以保留.
  • 数据为地幔挥发性含量和行为提供了改进的估计.
  • 通过挥发性分析,对中洋山脊的受约束脱气和污染历史.