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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.
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.
Gravimetry: Inorganic And Organic Precipitating Agents00:49

Gravimetry: Inorganic And Organic Precipitating Agents

In gravimetry, the precipitant is chosen carefully to obtain a pure solid that can be easily filtered. Common inorganic precipitants can be used to determine several cations and anions. In some cases, the formation of the same precipitate can be used to determine the cation and the anion. For example, the reaction of barium and chromate ions to give barium chromate is used to determine both barium and chromate. However, precipitates such as hydroxides, oxalates, and metal ammonium phosphates...
X-ray Crystallography02:18

X-ray Crystallography

The size of the unit cell and the arrangement of atoms in a crystal may be determined from measurements of the diffraction of X-rays by the crystal, termed X-ray crystallography.
Diffraction
Diffraction is the change in the direction of travel experienced by an electromagnetic wave when it encounters a physical barrier whose dimensions are comparable to those of the wavelength of the light. X-rays are electromagnetic radiation with wavelengths about as long as the distance between neighboring...
X-ray Diffraction of Biological Samples01:10

X-ray Diffraction of Biological Samples

X-ray diffraction or XRD is an analytical tool that utilizes X-rays to study ordered structures such as crystalline organic and inorganic samples, polycrystalline materials, proteins, carbohydrates, and drugs.
According to Bragg's law, when X-rays strike the sample positioned on a stage, the rays are  scattered by the electron clouds around the sample atoms. The  X-ray diffraction or scattering is caused by constructive interference of the X-ray waves that reflect off the internal crystal...
Crystal Growth: Principles of Crystallization01:25

Crystal Growth: Principles of Crystallization

Crystallization is a phase transformation process in which crystals are precipitated from a supersaturated solution or formed from other sources. During crystallization, atoms or molecules arrange themselves into a well-defined, rigid crystal lattice to minimize energy.
Initiating crystallization involves manipulating the concentration of the solute and the temperature of the solution. Since crystal growth occurs when the ratio of concentration and solubility of the solute in the solvent – the...

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相关实验视频

Updated: Jul 12, 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

阿波罗12号水晶岩石的主要元素变化和可能的来源材料

I Kushiro, H Haramura

    Science (New York, N.Y.)
    |March 26, 1971
    PubMed
    概括

    阿波罗12号月球岩石揭示了岩石的分化. 分析表明,大多数岩石起源于一个单一的分化岩体,可能是岩,橄结晶起着关键作用.

    科学领域:

    • 月球地质学 月球地质学
    • 石化学 石化学是一门学科.
    • 地质化学 地质化学

    背景情况:

    • 阿波罗12号任务提供了各种各样的月球岩石样本.
    • 了解月球岩石的组成对于破译月球的地质历史至关重要.

    研究的目的:

    • 为了化学分析阿波罗12号水晶岩石.
    • 为了确定这些月球样本的起源和差异化过程.

    主要方法:

    • 传统的化学岩石分析.
    • 石化分析用于识别规范性矿物质 (石英,橄,高).
    • 氧化物变化图来说明组成趋势.

    主要成果:

    • 九个阿波罗12号水晶岩石的分析.
    • 五块岩石含有规范石英;其他岩石含有规范橄和高.
    • 观察到铁与的比率存在很大差异.
    • 在氧化物变化图中在光滑曲线上绘制的组成.

    结论:

    • 大多数分析的岩石可能代表一个单一的差异化岩体.

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    Atom Probe Tomography Analysis of Exsolved Mineral Phases

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    相关实验视频

    Last Updated: Jul 12, 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

    Synchrotron X-ray Microdiffraction and Fluorescence Imaging of Mineral and Rock Samples
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    Synchrotron X-ray Microdiffraction and Fluorescence Imaging of Mineral and Rock Samples

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    Atom Probe Tomography Analysis of Exsolved Mineral Phases

    Published on: October 25, 2019

  • 通过橄石结晶和沉积的岩石分化是一个主要的过程.
  • 原始的岩可能起源于不同深度的岩.