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  1. Air is a mixture of several gases, where the two most dominant components in dry air are 21 vol% oxygen and 78 vol% nitrogen . Oxygen has a molar mass of 15.9994 g/mol and nitrogen has a molar mass of 14.0067 g/mol.

    • Moist Air

      Density of Moist Air - an Air Vapor Mixture. The amount of...

    • Oxygen

      Solubility of oxygen in equilibration with air in fresh...

    • Specific Heat Ratio

      Specific Heat Ratio - Air - Composition and Molecular Weight...

    • Mole Fraction of Water Vapor

      Moist Air - Water Vapor and Saturation Pressure Saturation...

  2. en.wikipedia.org › wiki › OxygenOxygen - Wikipedia

    Oxygen gas can also be produced through electrolysis of water into molecular oxygen and hydrogen. DC electricity must be used: if AC is used, the gases in each limb consist of hydrogen and oxygen in the explosive ratio 2:1. A similar method is the electrocatalytic O 2 evolution from oxides and oxoacids.

  3. 29 lip 2024 · Nitrogen gas is the primary component of air. Nitrogen, oxygen, water vapor, argon, and carbon dioxide account for about 99% of the composition of air. Trace gases in Earth's atmosphere include neon, methane, helium, krypton, hydrogen, xenon, ozone, and many other elements and compounds.

  4. 1 lut 2021 · About 99% of the composition of air consists of nitrogen, oxygen, and argon. Water vapor (variable) and carbon dioxide are the main trace gases. There is no chemical formula for air because the Earth’s atmosphere consists of a mixture of gases.

  5. The molar mass of dry air with oxygen, nitrogen and the other components as indicated below is 28.9647 g/mol. Composition and content of each gas in air is given in the figures and the table below.

  6. Oxygen | O2 | CID 977 - structure, chemical names, physical and chemical properties, classification, patents, literature, biological activities, safety/hazards/toxicity information, supplier lists, and more.

  7. 21 sty 2023 · Structure of the atmosphere. The main divisions of the atmosphere are defined by the elevations at which the sign of the temperature gradient changes. The chemical formulas at the right show the major species of interest in the various regions.