GCSE
Chemistry
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Introduction to GCSE Chemistry (AQA) Coming soon
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1.1 Atomic Structure, Elements, Compounds, and Mixtures
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1.2 The Periodic Table Coming soon
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2.1 Chemical Bonds, Ionic, Covalent and Metallic Coming soon
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2.2 How Bonding and Structure are Related to the Properties of Substances Coming soon
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2.3 Structure and Bonding of Carbon Coming soon
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2.4 Bulk and Surface Properties of Matter including Nanoparticles Coming soon
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3.1 Chemical Measurements, Conservation of Mass and the Quantitative Interpretation of Chemical Equations Coming soon
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3.2 Use of Amount of Substance in Relation to Masses of Pure Substances Coming soon
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3.3 Yield and Atom Economy of Chemical Reactions Coming soon
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3.4 Using Concentrations of Solutions in mol/dm³ [HT] Coming soon
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3.5 Use of Amount of Substance in Relation to Volumes of Gases [HT] Coming soon
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4.1 Reactivity of Metals Coming soon
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4.2 Reactions of Acids Coming soon
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4.3 Electrolysis Coming soon
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5.1 Exothermic and Endothermic Reactions Coming soon
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5.2 Chemical Cells and Fuel Cells Coming soon
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6.1 Rate of Reaction Coming soon
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6.2 Reversible Reactions and Dynamic Equilibrium Coming soon
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6.2.1 Reversible Reactions
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6.2.2 Energy Changes and Reversible Reactions
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6.2.3 Equilibrium
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6.2.4 The Effect of Changing Conditions on Equilibrium (HT only)
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6.2.5 The Effect of Changing Concentration (HT only)
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6.2.6 The Effect of Temperature Changes on Equilibrium (HT only)
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6.2.7 The Effect of Pressure Changes on Equilibrium (HT only)
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6.2.1 Reversible Reactions
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7.1 Carbon Compounds as Fuels and Feedstock Coming soon
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7.2 Reactions of Alkenes and Alcohols Coming soon
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7.3 Synthetic and Naturally Occurring Polymers Coming soon
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8.1 Purity, Formulations and Chromatography Coming soon
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8.2 Identification of Common Gases Coming soon
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8.3 Identification of Ions by Chemical and Spectroscopic Means Coming soon
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9.1 The Composition and Evolution of the Earth's Atmosphere Coming soon
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9.2 Carbon Dioxide and Methane as Greenhouse Gases Coming soon
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9.3 Common Atmospheric Pollutants and their Sources Coming soon
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10.1 Using the Earth's Resources and Obtaining Potable Water Coming soon
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10.2 Life Cycle Assessment and Recycling Coming soon
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10.3 Using Materials Coming soon
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10.4 The Haber Process and the use of NPK Fertilisers Coming soon
1. Atomic Structure and the Periodic Table
9.1.3 How Oxygen Increased
The oxygen that is present in the Earth's atmosphere today is primarily a result of the process of photosynthesisThe process by which plants use light energy to produce glucose. 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 respirationA chemical process that releases energy from glucose using oxygen, occurring in mitochondria., 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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