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相关概念视频

Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

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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...
17.2K
Phase Transitions: Vaporization and Condensation02:39

Phase Transitions: Vaporization and Condensation

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The physical form of a substance changes on changing its temperature. For example, raising the temperature of a liquid causes the liquid to vaporize (convert into vapor). The process is called vaporization—a surface phenomenon. Vaporization occurs when the thermal motion of the molecules overcome the intermolecular forces, and the molecules (at the surface) escape into the gaseous state. When a liquid vaporizes in a closed container, gas molecules cannot escape. As these gas phase...
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Washing, Drying, and Ignition of Precipitates00:52

Washing, Drying, and Ignition of Precipitates

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After filtration, the precipitate is washed to remove coprecipitated impurities and any remaining mother liquor. Colloidal precipitates, such as silver chloride, are washed with an electrolyte (such as dilute nitric acid) to prevent the peptization of the precipitate. In the case of slightly soluble precipitates, the wash solution contains a common ion to reduce solubility. Lead sulfate, which is slightly soluble in water, is washed with dilute sulfuric acid. Similarly, wash solutions may be...
946
Phase Changes01:19

Phase Changes

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Phase transitions play an important theoretical and practical role in the study of heat flow. In melting or fusion, a solid turns into a liquid; the opposite process is freezing. In evaporation, a liquid turns into a gas; the opposite process is condensation.
A substance melts or freezes at a temperature called its melting point and boils or condenses at its boiling point. These temperatures depend on pressure. High pressure favors the denser form of the substance, so typically, high pressure...
4.3K
Phase Transitions02:31

Phase Transitions

19.2K
Whether solid, liquid, or gas, a substance's state depends on the order and arrangement of its particles (atoms, molecules, or ions). Particles in the solid pack closely together, generally in a pattern. The particles vibrate about their fixed positions but do not move or squeeze past their neighbors. In liquids, although the particles are closely spaced, they are randomly arranged. The position of the particles are not fixed—that is, they are free to move past their neighbors to...
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Sample Preparation for Analysis: Advanced Techniques01:08

Sample Preparation for Analysis: Advanced Techniques

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Accurate analysis of complex samples often requires advanced preparation techniques to achieve reliable and reproducible results. Samples containing inorganic or organic materials can be challenging to dissolve or decompose effectively. Standard sample preparation methods include acid digestion, fusion, dry ashing, and wet digestion.
Acid digestion with strong acids is commonly used to dissolve inorganic materials that are insoluble (do not dissolve) in water. This method can be useful for...
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相关实验视频

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Atom Probe Tomography Analysis of Exsolved Mineral Phases
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细火山灰的不同阶段

Adrian Hornby1, Esteban Gazel2, Claire Bush3

  • 1Earth and Atmospheric Sciences, Cornell University, Ithaca, NY, USA. ahornby@cornell.edu.

Scientific reports
|September 21, 2023
PubMed
概括

火山灰的组成随着颗粒大小的变化而变化,影响大气运输. 这项研究提供了一个数据集和回归,以更好地估计灰相比例和密度,以改进气候建模.

科学领域:

  • 地质化学 地质化学
  • 火山学 火山学是一门学科.
  • 大气科学 大气科学

背景情况:

  • 火山灰对气候,生态系统和健康产生影响,但其组成和尺寸依赖性属性尚不清楚.
  • 现有的数据集缺乏有关大气运输和广泛影响的灰大小的详细阶段信息.
  • 了解灰成分对于准确建模火山冲击至关重要.

研究的目的:

  • 为了表征大小分离的火山灰碎片的相位组成.
  • 为了研究相位组成如何根据粒径大小,构造学设置和散装化学变化.
  • 以有限的数据开发估计灰相比例和密度的方法.

主要方法:

  • 从VEI 2-6喷发的40个灰样本进行X射线衍射分析.
  • 灰的尺寸分离成部分.
  • 包括回归建模在内的统计分析.

主要成果:

  • 细灰 (<45微米) 显示晶体二氧化和盐的增加,玻璃和铁氧化物的减少.
  • 弧形和内板样本通过地和clinopyroxene分数进行区分.
  • 为了估计玻璃和主要晶相比例,开发了回归.
  • 无孔灰密度通过clinopyroxene + Fe-oxide 分数得到良好估计,在板内和弧形样本之间存在差异.

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结论:

  • 这项研究为了解火山灰相组成及其变异性提供了有价值的数据集.
  • 开发的回归和密度估计改善了大气和环境灰预算的限制.
  • 准确的灰表征对于完善爆炸性火山活动对地球系统影响的模型至关重要.