The Processes Of Thecarbon Cycle 1C Flashcards
Weathering
Driven by atmosphere, rain and groundwater
Breakdown rocks on the surface
Small particles are combined with with plant and soil particles and then are carried by the ocean.
Large particles are deposited on the shore
Sediment accumulates
Layers build up and shale rock is formed due to surface pressure.
Dissolved sediments mix with seawater and are used by marine organisms to make skeletons and shells contains calcium carbonate.
When these organisms die, the carbonate collects at the bottom of the ocean and sedimentary rocks form.
Carbon sequestration - oceanic carbon pump ( vertical circulation)
Co2 moves from the atmosphere to the ocean by diffusion
Warm water absorbs co2 a low latitudes
High latitudes the cold water sinks and carbon is transferred dear into the ocean
When the cold water heats and rises to the surface the carbon is released into the atmosphere
Therefore a constant exchange between the atmosphere and the ocean
Carbon sequestration - biological pump
Phytoplankton fixes co2 through photosynthesis and carbon passes through the oceanic food web
Carbonate is removed from the ocean by shell-building organisms
Organisms die and the shells sink into deep water
Layers of carbon-rich sediments are formed and turn to rocks over millions of years.
Combustion
Fossil fuels contain carbon captured by living organisms over millions of years and stored in the earths crust
These fuels are mined for a primary energy source and release a by-product of a greenhouse gas co2
Decomposition
Occurs by microbes such as bacteria and fungi
Releases co2 into the atmosphere
Decomposition produces organic compounds which dissolve in run-off from land surface.
Greenhouse gases are released as a by-product
Respiration
Plants release co2 into the atmosphere - 1/2 terrestrial portion
Microscopic organisms release co2 by respiration from the soil.
Photosynthesis
Energy from sunlight and combine co2 from the atmosphere with water from the soil to produce carbohydrates
Trees are a large carbon store as trees live for many years and have resistant structures with wood taking a while to decompose.
Precipitation
Co2 from the atmosphere dissolves in rainwater to form weak carbonic acid
Increasing co2 conc from anthropogenic emissions increase the acidity of rainfall leading to more acidic ocean waters