Carbon Flashcards
What is the carbon cycle?
The movement of carbon in fluxes between different stores. It has been developing for billions of years and achieved its present balance around 290 million years ago, although human activities in the last 200 years have upset it
What are the 3 processes within the carbon cycle?
Biological processes
Geological processes
Chemical processes
What are biological processes?
Living plants and animals
What are geological processes?
Erosion, deposition and rock formation
What are chemical processes?
Reactions under heat and pressure
What is the terrestrial carbon store?
Sedimentary rocks have high concentrations of carbon (limestone is 42%)
Geological processes have also trapped carbon in the form of coal, oil and natural gas
The terrestrial store is the largest
What’s the largest carbon store?
Terrestrial
What is the atmospherics carbon store?
Volcanic activity, respiration, wildfires and out gassing emit carbon dioxide into the atmospheric store
> this store is very small compared to others
Small changes in concentration affect global temperatures and between 2012 and 2017 the average CO2 atmospheric concentration increased by 3% mostly due to humans
What is the ocean carbon store?
Carbon dioxide is dissolved by oceans from the atmosphere but it only makes up a tiny proportion of sea water mass
Most CO2 is stores in intermediate and deep sea water with only about 2.5% in surface waters
Which kind of rocks contain the most carbon?
Sedimentary
Metamorphic and igneous contain much less
How are sedimentary carbon rocks formed?
Shells and skeletons that collect at the bottom of the ocean as well as from calcareous ooze
Marine creatures and phytoplankton absorb carbon from sea water and when their remains collect on the sea bed the calcium carbonate is compacted by the weight of new layers above them and cemented together to form limestone
Calcerous oozes are not found where the ocean is too deep (over 6000m) becasue the pressure causes calcium carbonate to dissolve
What are biologically derived carbon rocks?
These are formed from the remains of living organisms deposited in layers within sedimentary rocks such as shale
Organic carbon from tropical coastal swamps is buried to produce coal, the hardness of which depends on the amount of pressure and heat when squashed during rock formation
Anaerobic reactions may convert organic carbon layers into a liquid - this is oil- that can move between the layers
A by product of coal and oil creation is methane which also becomes trapped between the rocks
What’s 2 ways carbon can be released?
Volcanic out gassing
Chemical weathering of rocks
What is volcanic outgassing? How does this release carbon?
Tectonic forces may bring limestone rocks into contact with extreme heat which causes chemical reactions and releases co2 into the atmosphere
Volcanic activity at plate boundaries or intra plate hotspots may release co2 into the atmosphere
Geothermal areas also release CO2 through hot springs
Degassing occurs because CO2 is not dissolved easily and so is released early in eruptions
What is chemical weathering of rocks? How does this release carbon?
Limestone rocks are very easily weathered by rain becasue it becomes a weak carbonic acid as it falls through the air and absorbs some CO2. This acid then dissolves the calcium carbonate of the rock and dissolved carbon is then carried away by the water to be deposited on the sea bed (calcium carbonate) or released as gas (carbon dioxide).
How is coal formed?
- Formation of Coal
Coal is formed primarily from the remains of plant material that accumulated in swampy, forested environments 300-400 million years ago (Carboniferous period).
Stages of Coal Formation:
1. Peat Formation – Dead plants accumulate in waterlogged, oxygen-poor environments (e.g., swamps).
2. Lignite (Brown Coal) – Over time, peat is buried and compressed by sediments, starting to lose moisture.
3. Bituminous Coal – Further heat and pressure drive out volatile compounds, increasing carbon content.
4. Anthracite (Hard Coal) – The highest-grade coal, formed under extreme heat and pressure, with a very high carbon content and energy value.
Key Processes:
• Anaerobic decomposition (low oxygen) prevents complete decay.
• Compaction and lithification due to sediment accumulation.
• Increased pressure and temperature transform peat into coal.
How is oil and natural gas formed?
- Formation of Oil and Natural Gas
Oil and natural gas are formed from the remains of marine microorganisms (plankton, algae) that lived in ancient seas 50-500 million years ago.
Stages of Oil and Gas Formation:
1. Organic Sediment Deposition – Plankton die and sink to the seafloor, mixing with mud.
2. Kerogen Formation – Over millions of years, layers of sediment build up, and heat and pressure transform organic material into a waxy substance called kerogen.
3. Cracking Process – At 50-100°C (oil window), kerogen breaks down into crude oil. At 100-200°C (gas window), it further breaks down into natural gas.
4. Migration and Trapping – Oil and gas migrate through porous rocks until trapped by impermeable rock layers (cap rocks), forming reservoirs.
Key Processes:
• Sedimentation and burial under anoxic conditions (low oxygen).
• Thermal maturation (heat and pressure convert organic matter into hydrocarbons).
• Migration through porous rock and accumulation in reservoirs.
What is the geographical importance of coal oil and gas? Where are they found?
Geographical Importance
• Coal is found in continental landmasses (e.g., USA, China, Russia).
• Oil and gas are primarily found in marine sedimentary basins (e.g., Middle East, Gulf of Mexico, North Sea).
• Fossil fuel extraction has led to economic growth, geopolitical tensions, and environmental concerns such as carbon emissions and climate change.
What are phytoplankton and why are they useful?
Microscopic single celled plants found in the warm surface waters of the ocean
They consume carbon dioxide from the atmosphere and photosynthesise, storing it in their body as a carbohydrate
When they die they transfer carbon deeper into the ocean (forming calcium carbonate layers when they sink to the sea bed) or are eaten by zooplankton
This is a biological carbon pump
What is the marine carbonate pump?
The marine food web extends from phytoplankton to zoo plankton and then to other organisms like corals, oysters and crabs which consume carbon and also use it to make their shells and skeletons
These creatures return some carbon dioxide to the atmosphere via respiration but also use enough to create room for the sea to absorb more from the atmosphere
In a short time period, carbon is taken from the atmosphere into the ocean and then chemically transferred to the sea bed to become sedimentary rocks
This is the marine carbonate pump
What kind of sea water sinks and what does this allow?
Colder denser sea water sinks to deep ocean areas where slow moving currents enable CO2 to be stored
What is the thermohaline circulatory system?
- Warm salty ocean currents transfer energy heat from tropical areas towards the poles, and cold less salty currents transfer colder water towards the equator. The temperature and salinity differences cause the large scale circulation of sea water
- Warmer water travel nearer to the surface because heat rises, while large volumes of cold water move at depths of 3km or below. This moves sea water around the world between oceans: warm surface currents and cold deep currents
- Parts of the thermohaline circulatory system help to transfer CO2 from oceans around to equator to polar ocean sinks. Currents that push water up and downwards (upwelling and down welling) move dissolved CO2
This is the physical carbon pump
What is the physical carbon pump
The thermohaline circulatory system