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The composition and evolution of the Earth's atmosphere key terms

Use these key terms for The composition and evolution of the Earth's atmosphere in AQA Chemistry 8462. The page is built from approved learning objectives for this topic and links back to the wider unit, topic hub, and related revision assets.

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key terms

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The composition and evolution of the Earth's atmosphere

AQAGCSEChemistryChemistry of the atmosphere

Key terms

  • nitrogen

    In The proportions of different gases in the atmosphere, nitrogen means a colorless, odorless gas that makes up about 80 percent of the Earth's atmosphere. This matters in The composition and evolution of the Earth's atmosphere because it supports the learning objective to recall that the Earth's atmosphere is about 80 percent nitrogen. Use nitrogen only in this subtopic-relevant sense so the definition stays concise, curriculum-specific, and useful for AQA GCSE Biology revision. Students should use this term accurately when they explain the biology, identify symptoms, or justify an answer in GCSE Biology questions.

  • atmosphere

    In The proportions of different gases in the atmosphere, atmosphere means the layer of gases surrounding the Earth, composed primarily of nitrogen and oxygen. This matters in The composition and evolution of the Earth's atmosphere because it supports the learning objective to recall that the Earth's atmosphere is about 80 percent nitrogen. Use atmosphere only in this subtopic-relevant sense so the definition stays concise, curriculum-specific, and useful for AQA GCSE Biology revision. Students should use this term accurately when they explain the biology, identify symptoms, or justify an answer in GCSE Biology questions.

  • Earth's atmosphere

    The layer of gases surrounding the Earth, composed mainly of nitrogen and oxygen.

  • oxygen

    A diatomic molecule (O2) that makes up about 20 percent of the Earth's atmosphere and is essential for respiration in living organisms.

  • carbon dioxide

    A gas present in the Earth's atmosphere in small proportions, produced by respiration and combustion.

  • water vapour

    The gaseous form of water present in the atmosphere, contributing to weather and climate.

  • atmosphere

    In The proportions of different gases in the atmosphere, atmosphere means the layer of gases surrounding the Earth, composed mainly of nitrogen and oxygen. This matters in The composition and evolution of the Earth's atmosphere because it supports the learning objective to interpret simple data showing the proportions of gases in the atmosphere. Use atmosphere only in this subtopic-relevant sense so the definition stays concise, curriculum-specific, and useful for AQA GCSE Biology revision. Students should use this term accurately when they explain the biology, identify symptoms, or justify an answer in GCSE Biology questions.

  • proportions

    In The proportions of different gases in the atmosphere, proportions means the relative amounts of different gases present in the atmosphere. This matters in The composition and evolution of the Earth's atmosphere because it supports the learning objective to interpret simple data showing the proportions of gases in the atmosphere. Use proportions only in this subtopic-relevant sense so the definition stays concise, curriculum-specific, and useful for AQA GCSE Biology revision. Students should use this term accurately when they explain the biology, identify symptoms, or justify an answer in GCSE Biology questions.

  • major gases

    The primary components of the Earth's atmosphere, including nitrogen and oxygen, that make up the bulk of the atmospheric composition.

  • trace gases

    Gases present in the atmosphere in small amounts, such as carbon dioxide, water vapour, and noble gases, which are not the major components.

  • percentage composition

    The proportion of each gas in the atmosphere expressed as a percentage of the total.

  • atmospheric gases

    Gases that make up the Earth's atmosphere, including nitrogen, oxygen, carbon dioxide, and trace gases.

  • early atmosphere

    The Earth's atmosphere in its initial state, likely composed mainly of carbon dioxide and lacking significant oxygen.

  • carbon dioxide

    A colorless gas produced by volcanic activity, significant in the early atmosphere and a key component in photosynthesis.

  • early atmosphere

    The Earth's atmosphere during its initial formation, likely composed mainly of carbon dioxide with little or no oxygen.

  • volcanic activity

    The process by which gases and materials are released from the Earth's interior, contributing to the formation of the early atmosphere.

  • carbon dioxide

    A colorless gas released by volcanoes, which was a major component of the Earth's early atmosphere.

  • water vapour

    The gaseous form of water that was released by volcanic activity and contributed to the formation of the early atmosphere.

  • water vapour

    The gaseous form of water present in the atmosphere, which can condense to form liquid water.

  • oceans

    Large bodies of saltwater that cover significant portions of the Earth's surface, formed from condensed water vapour.

  • methane

    A colorless, odorless gas that is a major component of natural gas and a possible early atmospheric gas.

  • ammonia

    A colorless gas with a pungent smell, consisting of nitrogen and hydrogen, and considered as a possible early atmospheric gas.

  • early atmosphere

    The composition of the Earth's atmosphere during its formation, primarily consisting of carbon dioxide and lacking significant oxygen.

  • present atmosphere

    The current composition of the Earth's atmosphere, which is approximately 80% nitrogen and 20% oxygen, along with trace gases.

  • early atmosphere

    The composition of the Earth's atmosphere during its formation, likely consisting mainly of carbon dioxide and little or no oxygen.

  • volcanic activity

    The process by which gases are released from the Earth's interior, contributing to the formation of the early atmosphere.

  • early atmosphere

    The composition of the Earth's atmosphere during its initial formation, likely rich in carbon dioxide and lacking oxygen.

  • evidence

    In The Earth's early atmosphere, evidence means data or information used to support claims or theories about the Earth's early atmosphere. This matters in The composition and evolution of the Earth's atmosphere because it supports the learning objective to evaluate evidence and uncertainty when discussing the Earth's early atmosphere. Use evidence only in this subtopic-relevant sense so the definition stays concise, curriculum-specific, and useful for AQA GCSE Biology revision. Students should use this term accurately when they explain the biology, identify symptoms, or justify an answer in GCSE Biology questions.

  • photosynthesis

    The process by which algae and plants convert carbon dioxide and water into glucose and oxygen using sunlight.

  • oxygen

    A diatomic molecule (O2) produced as a byproduct of photosynthesis, essential for the respiration of most living organisms.

  • photosynthesis

    The process by which green plants and some other organisms use sunlight to synthesize foods with the help of chlorophyll, removing carbon dioxide from the atmosphere.

  • carbon dioxide removal

    The process by which carbon dioxide is taken out of the atmosphere, primarily through photosynthesis by plants and algae.

  • photosynthesis

    The process by which green plants and some other organisms use sunlight to synthesize foods with the help of chlorophyll, producing oxygen as a byproduct.

  • oxygen levels

    The concentration of oxygen in the atmosphere, which increased gradually due to the activity of photosynthetic organisms.

  • atmospheric oxygen

    The oxygen present in the Earth's atmosphere, which increased due to photosynthesis and is essential for the development of complex life.

  • photosynthesis

    The process by which algae and plants convert carbon dioxide and water into glucose and oxygen using sunlight, contributing to the increase of atmospheric oxygen.

  • atmospheric oxygen

    The amount of oxygen present in the Earth's atmosphere, which has changed over geological time.

  • photosynthesis

    The process by which algae and plants convert carbon dioxide and sunlight into oxygen and glucose.

  • carbon dioxide

    A colorless gas that is a significant component of Earth's atmosphere and is produced by respiration and combustion.

  • oceans

    Large bodies of saltwater that cover about 71% of the Earth's surface and play a crucial role in the carbon cycle.

  • carbonate precipitates

    Solid compounds formed when dissolved carbon dioxide reacts with minerals in water.

  • dissolved carbon dioxide

    Carbon dioxide that is mixed in water, contributing to the formation of carbonate precipitates.

  • carbonate precipitates

    Solid compounds formed when dissolved carbon dioxide reacts with minerals in water.

  • sedimentary rocks

    Rocks formed from the accumulation and compaction of mineral and organic particles over time.

  • carbonates

    Compounds containing the carbonate ion (CO3^2-) that marine organisms use to form shells and skeletons.

  • marine organisms

    Living organisms that inhabit the ocean and utilize carbonates to create structures such as shells and skeletons.

  • fossil fuels

    In How carbon dioxide decreased, fossil fuels means natural substances formed from the remains of dead organisms, which trap carbon. This matters in The composition and evolution of the Earth's atmosphere because it supports the learning objective to explain that some carbon was trapped in fossil fuels formed from dead organisms. Use fossil fuels only in this subtopic-relevant sense so the definition stays concise, curriculum-specific, and useful for AQA GCSE Biology revision. Students should use this term accurately when they explain the biology, identify symptoms, or justify an answer in GCSE Biology questions.

  • carbon trapping

    The process by which carbon is stored in fossil fuels, reducing atmospheric carbon dioxide levels.

  • limestone

    A sedimentary rock primarily composed of calcium carbonate, formed from the remains of marine organisms and acts as a long-term carbon store.

  • fossil fuels

    Natural substances such as coal, crude oil, and natural gas formed from the remains of dead organisms, serving as long-term carbon stores.

  • carbon dioxide

    A colorless gas that is a significant greenhouse gas and was abundant in the Earth's early atmosphere.

  • geological time

    A time scale used by geologists and other Earth scientists to describe the timing and relationships of events in Earth's history.

  • carbon cycle

    The continuous process by which carbon is exchanged between the Earth's atmosphere, land, water, and living organisms.

  • carbon dioxide removal

    The process of reducing the concentration of carbon dioxide in the atmosphere, often linked to natural processes or human activities.