Carbon Flashcards
Define “biogeochemical” carbon cycle
- Biological cycle: fast, sequestration between atmosphere, ocean, sediment etc.
- Geological cycle: organic matter buried in sediments + takes millions of years to form fossil fuels, carbon from volcanic emission, erosion/formation of sediment on seafloor
- Chemical: carbon is a non-metal element, can be part of human life, 4th most abundant in world
What are the three carbon stores?
- Terrestrial: in the lithosphere (sedimentary rocks), biosphere (organisms +biomass broken down by micro-organisms into CO2, organic storage)
- Atmosphere: rapid interchange with terrestrial
- Ocean: hydrosphere, dissolve in deep ocean and at surface
How do annual fluxes of carbon vary in rate?
- Stable when outputs/inputs are not beyond threshold, equilibrium
- Small change = shift and amplify feedback loops
How does carbon form sedimentary carbonate rocks?
- Limestone = calcium carbonate
- Carbon extracted from ocean by phytoplankton/marine creatures through photosynthesis
- Shells/skeletons cement w heat + pressure to form limestone on ocean floor
How is carbon biologically derived in shale and coal?
- Remains of non-skeletal organic material decay in anaerobic conditions, forming hydrocarbon chains, crude oil stored in pores of shale
- Coal formed from remains of trees and plants
- Organic material from swamps become peat, converted to coal w heat/pressure
How are phytoplankton part of the biological pump?
- They sequester CO2 during photosynthesis which becomes organic matter
- Dead cells sink, carbon transported to deep ocean and decay releases CO2 there
What is the carbonate pump?
- Sediment that sinks to the seabed gradually transforms into rock which remains there for geological epochs
(Ocean stores more carbon)
What is the thermohaline circulation?
- Cold water holds more gas
- Warm tropic water moving towards poles evaporates, leaving cold/salty water
- It’s dense/heavy so sinks to bottom of ocean
- Carbon pump = sinks and pushes the deep water away (forms N Atlantic deep water)
- Cold water recharged by Antarctic water (big carbon sink)
What do terrestrial primary producers do?
- Land based absorption of carbon
- Stores in leaves, roots, bark until needed
- Converts carbon into carbs during photosynthesis
How is biological carbon stored as dead organic matter in soils?
- Vegetation accumulates and compresses (partially degraded), trapping carbon
- Held in anaerobic conditions as it’s locked in (waterlogged) peatlands
- Drying up = aerobic conditions, soil biota decompose veg and respire carbon into atmosphere
- Burning = release methane, traps more carbon in atmosphere
What is the concentration of atmospheric carbon like?
- Natural carbon release after Ice Age
- More phytoplankton growth increases CO2 sequestration
- Permafrost melt = methane release, trap light waves, increase temp (+ve feedback)
How does natural GHG effect determine temperature and precipitation distribution?
- GHGs increase temp, increasing precipitation and clouds
- Leads to albedo effect with increase in reflection, decreasing temp
What is Net Primary Productivity?
- The rate of generation of biomass
- Linked to growth and how many nutrients are stored in the biosphere
How does terrestrial photosynthesis and storage of carbon vary between biomes?
- Depends on latitude due to temp and precip
- Tropical: large biomass, high decomposition + instant nutrient uptake = less carbon in litter+soil
- Temperate: more organic matter in soil = higher capacity to store carbon (biota respire through decomposition)
- Taiga: Slow decomposition + frozen upper soil so soil biota cannot respire much
How does ocean photosynthesis regulate carbon in the atmosphere?
- Tropic water is stratified so surface water is nutrient poor due to evaporation
- Polar regions have mixed surface/deep water so nutrients available all year
- Light for photosynthesis decreases with depth (less sequestration)
- Coastal estuaries = most production (shallow + carbon from erosion)
- Open ocean also high due to size
How is soil health influenced by stored carbon?
- Stores 30% of global carbon but local conditions determine sequestration and emission
- Clay-rich soils hold more as it protects carbon from decomposition by biota
- Soil erosion removes carbon from active surface layer
- Depends on weathering and decomposition
How has fossil fuel combustion altered the balance of carbon pathways?
- Anthropogenic climate change
- Carbon transferred from fossil stores to atmosphere, accelerated carbon exchanges
- Combined with natural changes (albedo effect, Milankovitch cycle etc)
What is energy consumption?
- Total energy use
- Industrialisation/urbanisation = power grids, increased population, increase household wealth
- Consumption decreases due to env concerns + efficient appliances
What is an energy mix?
- Proportion of each type of primary resource that the country utilises within a year
- More than 80% is fossil fuels
What is energy transition?
- Changes from pre-industrialised, industrialising, industrialised, post-industrial
- Causes change in energy mix
- Slow due to geopolitical tensions
What is domestic vs foreign energy?
- Internally produced
- Imported, dependency
What is primary and secondary energy?
- Primary = original source of energy (coal, oil, wind)
- Secondary is converted from primary energy into a form that energy can be consumed in (electricity)
What is renewable and non-renewable energy?
- Renewable is when the source is not depleted when used (wind, water, sun)
- Non-renewable is when the source is finite, the resource is not replenished at the rate of consumption (biomass, fossil fuels)