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相关概念视频

Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

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...
Phase Diagrams02:39

Phase Diagrams

A phase diagram combines plots of pressure versus temperature for the liquid-gas, solid-liquid, and solid-gas phase-transition equilibria of a substance. These diagrams indicate the physical states that exist under specific conditions of pressure and temperature and also provide the pressure dependence of the phase-transition temperatures (melting points, sublimation points, boiling points). Regions or areas labeled solid, liquid, and gas represent single phases, while lines or curves represent...
The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
States of Water01:23

States of Water

Water exists in any one of the three classical states: solid (ice), liquid (water), and gas (steam or water vapor). The state of water depends on i) the intermolecular forces that draw molecules together and ii) the kinetic energy that leads to movements that pull them apart.
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
Carbonation Shrinkage01:24

Carbonation Shrinkage

Atmospheric CO2 penetrates the concrete's pores and, in the presence of moisture, forms carbonic acid, which then reacts with calcium hydroxide in the hydrated cement, forming calcium carbonate. This process reduces the concrete's volume and is termed carbonation shrinkage.
The concrete's permeability is slightly reduced as calcium carbonate produced during the reaction fills its pores. Furthermore, its strength is slightly enhanced as the water released during the reaction facilitates the...

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相关实验视频

Updated: Jul 11, 2026

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
13:38

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

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夏季的冰雪和二氧化碳.

G Kukla, J Gavin

    Science (New York, N.Y.)
    |October 30, 1981
    PubMed
    概括

    南极海冰面积在1973-1980年间显著减少. 20世纪早期的冰状况更为严重,最近的温度与二氧化碳增加的预测一致.

    科学领域:

    • 气候学 气候学 气候学
    • 冰川学的冰川学
    • 环境科学 环境科学

    背景情况:

    • 20世纪30年代的历史数据表明,与最近的平均水平相比,南极夏季冰块状况更为严重.
    • 卫星图像显示,1973年至1980年间,南极冰块的面积大幅减少.

    研究的目的:

    • 分析南极包冰范围和北半球表面空气温度的变化.
    • 将观察到的气候变化与与大气中二氧化碳增加相关的预测进行比较.

    主要方法:

    • 对从1973年至1980年间南极包冰范围的卫星图像进行分析.
    • 从1930年代的地图集和船只报告中汇编历史气候数据.
    • 在两个不同的时期 (1934-1938年和1974-1978) 中,北半球表面空气温度的比较.

    主要成果:

    • 在1973年至1980年间,南极冰块的面积减少了250万平方公里.
    • 在北半球融化雪带的表面空气温度在1974-1978年比1934-1938年更高.
    • 观察到的温度和冰盖变化质量上与大气二氧化碳增加的预测影响保持一致.

    结论:

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  • 虽然观察到的气候趋势与二氧化碳增加的影响有定性一致,但尚未确定确切的因果关系.
  • 自然气候变化和其他未确定的过程也可能导致所观察到的雪,冰盖和温度的变化.