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Diffusion01:12

Diffusion

Diffusion is the passive movement of substances down their concentration gradients—requiring no expenditure of cellular energy. Substances, such as molecules or ions, diffuse from an area of high concentration to an area of low concentration in the cytosol or across membranes. Eventually, the concentration will even out, with the substance moving randomly but causing no net change in concentration. Such a state is called dynamic equilibrium, which is essential for maintaining overall...
Gas Exchange and Transport01:20

Gas Exchange and Transport

Gas exchange, the intake of molecular oxygen (O2) from the environment and the outflow of carbon dioxide (CO2) into the environment, is necessary for cellular function. Gas exchange during respiration occurs largely via the movement of gas molecules along pressure gradients. Gas travels from areas of higher partial pressure to areas of lower partial pressure. In mammals, gas exchange occurs in the alveoli of the lungs, which are adjacent to capillaries and share a membrane with them.
Behavior of Gas Molecules: Molecular Diffusion, Mean Free Path, and Effusion03:48

Behavior of Gas Molecules: Molecular Diffusion, Mean Free Path, and Effusion

Although gaseous molecules travel at tremendous speeds (hundreds of meters per second), they collide with other gaseous molecules and travel in many different directions before reaching the desired target. At room temperature, a gaseous molecule will experience billions of collisions per second. The mean free path is the average distance a molecule travels between collisions. The mean free path increases with decreasing pressure; in general, the mean free path for a gaseous molecule will be...
Diffusion01:21

Diffusion

Diffusion is a type of passive transport. In passive transport, a substance tends to move from an area of high concentration to an area of low concentration until the concentration is equal across the space. For example, take the diffusion of substances through the air. When someone opens a perfume bottle in a room filled with people, the perfume is at its highest concentration in the bottle and is at its lowest at the edges of the room. The perfume vapor will diffuse, or spread away, from the...
Diffusion on Chromatography Columns01:07

Diffusion on Chromatography Columns

In column chromatography, when an analyte is introduced as a narrow band at the top of the column, the solutes begin to separate and broaden, developing a Gaussian profile. This broadening occurs due to various factors, such as longitudinal diffusion.
Longitudinal diffusion occurs when the solute molecules in the mobile phase diffuse from the more concentrated center of the chromatographic band to the more dilute regions on either side, both towards and against the flow direction. This...
External and Internal Respiration01:24

External and Internal Respiration

External respiration occurs in the lungs, and it is the first step in the journey of oxygen inside the body. When we inhale, oxygen enters our lungs and diffuses across the thin alveolar membrane. The alveoli are tiny, air-filled sacs that provide a vast surface area for gas exchange. Oxygen in the alveoli has a higher partial pressure (105 mmHg) than in the adjacent pulmonary capillaries (40 mmHg), establishing a pressure gradient. As a result, oxygen molecules move from the alveoli into the...

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Updated: Jul 7, 2026

Whole-Body Nanoparticle Aerosol Inhalation Exposures
10:11

Whole-Body Nanoparticle Aerosol Inhalation Exposures

Published on: May 7, 2013

下層大気の拡散による分離.

Yosuke Adachi1, Kenji Kawamura, Laurence Armi

  • 1Scripps Institution of Oceanography, 9500 Gilman Drive, La Jolla, CA 92093-0244, USA.

Science (New York, N.Y.)
|March 11, 2006
PubMed
まとめ

大気中のガスは重力によって分離され,この現象は,以前は低気圏では,乱流によって検出できなかった. 研究者らは,主に熱の影響によって引き起こされる,地表近くの空気のこの重力分離を検出しました.

科学分野:

  • 大気科学 大気科学
  • 地質物理学 地質物理学とは地質物理学です.
  • 物理化学 物理化学

背景:

  • 大気中のガスの重力分離は,200年近く前から理論化されてきました.
  • 下層大気中の乱れ混合は,歴史的に,この現象の経験的検出を妨げています.
  • 強い夜間逆転は,微妙な効果を観察するのに有利な安定した大気条件を生み出します.

研究 の 目的:

  • 大気成分の重力分離を実験的に検出し,定量化する.
  • 地表近くの層におけるガス分離に対する熱的および重力測定的要因の影響を調査する.
  • 観測された分離に対する熱と重力測定の貢献の相対的重要性を決定する.

主な方法:

  • 強烈な夜間逆転時に地表近くの層から空気のサンプルを採取した.
  • 採取した空気サンプルにおけるアルゴン/窒素 (Ar/N2) の比率の正確な測定を用いた.
  • 分離に起因する大気成分比の変動を特定し,定量化するために分析されたデータ.

主要な成果:

  • 地表近くの空気中の大気成分の重力分離を成功裏に検出しました.
  • 観測された分離は,熱力と重力力の結合効果と一致しています.

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Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions
05:45

Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions

Published on: January 7, 2019

関連する実験動画

Last Updated: Jul 7, 2026

Whole-Body Nanoparticle Aerosol Inhalation Exposures
10:11

Whole-Body Nanoparticle Aerosol Inhalation Exposures

Published on: May 7, 2013

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions
05:45

Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions

Published on: January 7, 2019

  • 分離効果への熱的貢献は,重力測定的貢献よりも重要であることが判明しました.
  • 結論:

    • 大気ガスの重力分離は,強い夜間逆転などの特定の条件下で検出できます.
    • 熱グラディエントは,地表近くの大気中のガス分離を推進する上で主要な役割を果たします.
    • この発見は,長年にわたる理論を検証し,大気組成の研究のための新しい道を開きます.