GCSE

Chemistry

  1. Introduction to GCSE Chemistry (AQA) Coming soon
  2. 1. Atomic Structure and the Periodic Table

  3. 1.1 Atomic Structure, Elements, Compounds, and Mixtures
  4. 1.2 The Periodic Table Coming soon
  5. 2. Bonding, Structure, and the Properties of Matter
  6. 2.1 Chemical Bonds, Ionic, Covalent and Metallic Coming soon
  7. 2.2 How Bonding and Structure are Related to the Properties of Substances Coming soon
  8. 2.3 Structure and Bonding of Carbon Coming soon
  9. 2.4 Bulk and Surface Properties of Matter including Nanoparticles Coming soon
  10. 3. Quantitative Chemistry
  11. 3.1 Chemical Measurements, Conservation of Mass and the Quantitative Interpretation of Chemical Equations Coming soon
  12. 3.2 Use of Amount of Substance in Relation to Masses of Pure Substances Coming soon
  13. 3.3 Yield and Atom Economy of Chemical Reactions Coming soon
  14. 3.4 Using Concentrations of Solutions in mol/dm³ [HT] Coming soon
  15. 3.5 Use of Amount of Substance in Relation to Volumes of Gases [HT] Coming soon
  16. 4. Chemical Changes
  17. 4.1 Reactivity of Metals Coming soon
  18. 4.2 Reactions of Acids Coming soon
  19. 4.3 Electrolysis Coming soon
  20. 5. Energy Changes
  21. 5.1 Exothermic and Endothermic Reactions Coming soon
  22. 5.2 Chemical Cells and Fuel Cells Coming soon
  23. 6. The Rate and Extent of Chemical Change
  24. 6.1 Rate of Reaction Coming soon
  25. 6.2 Reversible Reactions and Dynamic Equilibrium Coming soon
  26. 7. Organic Chemistry
  27. 7.1 Carbon Compounds as Fuels and Feedstock Coming soon
  28. 7.2 Reactions of Alkenes and Alcohols Coming soon
  29. 7.3 Synthetic and Naturally Occurring Polymers Coming soon
  30. 8. Chemical Analysis
  31. 8.1 Purity, Formulations and Chromatography Coming soon
  32. 8.2 Identification of Common Gases Coming soon
  33. 8.3 Identification of Ions by Chemical and Spectroscopic Means Coming soon
  34. 9. Chemistry of the Atmosphere
  35. 9.1 The Composition and Evolution of the Earth's Atmosphere Coming soon
  36. 9.2 Carbon Dioxide and Methane as Greenhouse Gases Coming soon
  37. 9.3 Common Atmospheric Pollutants and their Sources Coming soon
  38. 10. Using Resources
  39. 10.1 Using the Earth's Resources and Obtaining Potable Water Coming soon
  40. 10.2 Life Cycle Assessment and Recycling Coming soon
  41. 10.3 Using Materials Coming soon
  42. 10.4 The Haber Process and the use of NPK Fertilisers Coming soon
Module Progress
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Learning

The oxygen that is present in the Earth's atmosphere today is primarily a result of the process of photosynthesis carried out by algae and plants. During photosynthesis, carbon dioxide and water are converted into glucose (a type of sugar) and oxygen. This process can be represented by the equation:

6CO2 + 6H2O → C6H12O6 + 6O2

carbon dioxide + water –light→ glucose + oxygen

Approximately 2.7 billion years ago, algae in the Earth's oceans began producing oxygen through photosynthesis. Initially, the oxygen produced by algae did not accumulate in the atmosphere as it reacted with various elements, such as iron, in the Earth's crust and dissolved in the oceans.

However, over time, the oxygen produced by algae gradually accumulated in the atmosphere. This increase in atmospheric oxygen was a significant event in Earth's history and is known as the Great Oxygenation Event. As oxygen levels increased, it had a profound impact on the evolution of life on Earth.

The presence of oxygen in the atmosphere enabled the evolution of more complex organisms, including plants. These plants further contributed to the production of oxygen through photosynthesis. Over the next billion years, as plants evolved and spread across the Earth, the percentage of oxygen in the atmosphere gradually increased.

The gradual increase in atmospheric oxygen provided a critical environment for the evolution of animals. Oxygen is essential for aerobic respiration, the process by which animals extract energy from food. As oxygen levels increased, more complex animals with more energy-demanding lifestyles could evolve.

Today, oxygen makes up approximately 21% of the Earth's atmosphere, allowing for the survival and thriving of a diverse range of organisms.

Conclusion

The increase in atmospheric oxygen is attributed to the photosynthetic activities of algae and plants. Over billions of years, the production of oxygen through photosynthesis gradually led to an increase in atmospheric oxygen levels. This increase in oxygen played a crucial role in the evolution of life on Earth, enabling the development of more complex organisms, including animals.

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