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相关概念视频

Atomic Mass01:52

Atomic Mass

Atoms — and the protons, neutrons, and electrons that compose them — are extremely small. For example, a carbon atom weighs less than 2 × 10−23 g. When describing the properties of tiny objects such as atoms, we use appropriately small units of measure, such as the atomic mass unit (amu). The amu was originally defined based on hydrogen, the lightest element, then later in terms of oxygen. Since 1961, it has been defined with regard to the most abundant isotope of carbon, atoms of which are...
Precipitation Gravimetry01:03

Precipitation Gravimetry

Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
Crystal Density01:19

Crystal Density

The crystal lattice structure of a material allows us to determine how many molecules exist in its unit cell. With this information, alongside the unit-cell parameters - three distance parameters (a, b, c) and three angular parameters (α, β, γ).Density (ρ) = (Z × M) / (a × b × c × NA)where:Z is the number of formula units per unit cellM is the molar mass of the substancea, b, and c are the edge lengths of the unit cellNA is Avogadro’s numberFor a simple cubic lattice, atoms are located only at...
Measurement of Air Content in Concrete01:23

Measurement of Air Content in Concrete

Air content measurement in concrete is critical for ensuring structural integrity and durability of concrete structures, especially in environments prone to severe weather conditions. Accurate air content analysis optimizes concrete's resistance to freeze-thaw cycles and enhances its workability and strength. Several methods are standardized under ASTM guidelines to measure the air content in fresh concrete, each suitable for different concrete types and conditions.
The pressure method,...
Measurement of Fluid Pressure01:16

Measurement of Fluid Pressure

Fluid pressure is commonly measured using devices called manometers, which rely on liquid columns to indicate pressure differences. The height of a liquid column in a manometer reflects the pressure exerted by the fluid, providing a simple yet effective means of measurement. Different types of manometers serve specific purposes based on their configurations and the type of fluids involved.
A basic form of manometer is the piezometer, a vertical tube open at the top and filled with the same...

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相关实验视频

Updated: Jul 9, 2026

Quantification of Hydrogen Concentrations in Surface and Interface Layers and Bulk Materials through Depth Profiling with Nuclear Reaction Analysis
14:11

Quantification of Hydrogen Concentrations in Surface and Interface Layers and Bulk Materials through Depth Profiling with Nuclear Reaction Analysis

Published on: March 29, 2016

测量了位于圣海伦斯山层周围的平流层中云凝聚核的测量.

C F Rogers, J G Hudson, W C Kocmond

    Science (New York, N.Y.)
    |February 20, 1981
    PubMed
    概括

    在1980年圣海伦斯山爆发后,平流层空气样本显示出云凝结核 (CCN) 的度高于预期. 这些发现凸显了火山对平流层气溶群体的影响.

    科学领域:

    • 大气科学 大气科学
    • 火山学 火山学是一门学科.
    • 气溶科学 气溶科学

    背景情况:

    • 火山爆发可以将气溶注入平流层.
    • 高层层气溶会影响气候和大气化学.
    • 云凝聚核 (CCN) 对于云的形成至关重要.

    研究的目的:

    • 在平流层测量云凝聚核 (CCN) 度.
    • 评估圣海伦斯山喷发对平流层CCN的影响.
    • 为了量化高海拔的火山中的CCN水平.

    主要方法:

    • 使用U-2飞机收集了平流层空气样本.
    • 在13至19公里的高度测量了CCN度.
    • 在1%超和下分析空气样本以检测CCN活动.

    主要成果:

    • 在平流层空气样本中观察到高于预期的CCN度.
    • 测量到的CCN度大约在每立方厘米100到1000之间.
    • 在火山羽毛内外都检测到较高的CCN水平.

    结论:

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  • 1980年圣海伦斯山喷发显著增加了平流层CCN度.
  • 火山气溶可以持续存在并影响平流层云形成.
  • 这些发现强调了火山活动对平流层气溶动态的重要性.