Cards (14)

  • What are the proportions of the main gases in Earth's current atmosphere?
    • Nitrogen: ~4/5 (80%)
    • Oxygen: ~1/5 (20%)
    • Small proportions of other gases such as CO₂ and noble gases
  • What percentage of Earth's atmosphere is nitrogen?
    80%
  • What percentage of Earth's atmosphere is oxygen?
    20%
  • What are the other gases present in Earth's atmosphere and their characteristics?
    • Carbon dioxide (CO₂): Contributes to greenhouse effect
    • Water vapor (H₂O(g)): Influences climate and precipitation
    • Noble gases: Largely inert and unreactive
  • What does the symbol ∼ mean?
    Approximately
  • Why is evidence about Earth's early atmosphere limited?
    • Time scale of 4.6 billion years
    • Theories have changed over time
    • Limited geological records
  • What is one theory about the formation of Earth's early atmosphere?
    During the first billion years of Earth's existence:
    • Intense volcanic activity released gases
    • Early atmosphere was mainly CO₂ with little or no O₂(g)
    • Nitrogen (N₂) gradually built up
    • Small proportions of methane (CH₄) and ammonia (NH₃) were present
  • How did oceans form on early Earth?
    Water vapor condensed to form the oceans.
  • How did CO₂ levels decrease in the early atmosphere?
    • CO₂ dissolved in water
    • Carbonates precipitated, forming sediments
    • Reduced the amount of CO₂ in the atmosphere
  • What process increased oxygen levels in Earth's atmosphere?
    Photosynthesis by algae and plants.
  • Write the balanced chemical equation for photosynthesis.
    6CO₂ + 6H₂O → C₆H₁₂O₆ + 6O₂
  • When did algae first start producing oxygen in Earth's atmosphere?
    About 2.7 billion years ago
  • Over the next billion years, how did plants affect oxygen levels in the atmosphere?
    The percentage of oxygen gradually increased to a level that enabled animals to evolve.
  • How did CO₂ levels decrease in Earth's atmosphere?
    • Photosynthesis by algae and plants
    • Formation of sedimentary rocks containing carbon (e.g., limestone and coal)
    • Production of fossil fuels from decaying plant and animal remains