physical paper 1- carbon Flashcards

1
Q

What is organic carbon

A

Form found in living organisms such as plants and trees

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2
Q

What is inorganic carbon

A

Carbon extracted from ores and minerals

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3
Q

What is anthropogenic co2

A

Carbon dioxide generated by human activity

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4
Q

What happens in a simple carbon cycle

A

Sunlight releases c02 which plants take in for photoysynthesis. Plant may die and decay- atmosphere. Or be eated by an animal which takes in the co2, animals release to atmosphere by respiration, they eventually die and waste/bones get buried in the rock. Those fossil fuels then get burnt for energy and co2 emitted.

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5
Q

What is the primary store of carbon on the earth and how it can release carbon

A

In the earths mantle- it escapes by constructive and destructive plate margins
Much released at destructive plate margins from metamorphism

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6
Q

What are different carbon compounds and where are they found

A

CO2- atmosphere, soils and oceans
CH4 (methane)- atmosphere, soils and sedimentary rocks
CaCO3 (calcium carbonate)- calcareous rocks, oceans, skeletons, shells
Hydrocarbons- solids, liquids, gasses- sedimentary rocks
Bio-molecules- living things- proteins, carbs, fat, oil and DNA

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7
Q

What is the fast/short term carbon cycle and processes

A

Moves carbon much faster, instead of millions of years it happens over years. The increased speed is because the fast carbon cycle moves carbon through living things. Moves 1000x more carbon per year than a slow.
Photosynthesis, respiration, decomposition

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8
Q

What is the slow/long term carbon cycle and processes

A

Moves carbon between the atmosphere, lithosphere and oceans. 10-10m tonnes of carbon per year and takes 100-200m years for carbon to move through. Carbon is removed into long term storage by burial of sedimentary rock layers e.g. coal
Compression, burial, volcanic eruptions

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9
Q

What do the different flows of carbon move through

A

Photosynthesis
Respiration
Combustion
Decomposition
Diffusion
Weathering and erosion
Burial and compaction
Carbon sequestration

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10
Q

Flows of carbon between the atmosphere and lithosphere

A

Combustion- burning of FF
Erupting volcano

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11
Q

Flows of carbon between the atmosphere and biosphere

A

Combustion- wildfires
Respiration
Photosynthesis

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12
Q

Flows of carbon between the atmosphere and hydrosphere

A

Diffusion

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13
Q

Flows of carbon between the lithosphere and hydrosphere

A

Erosion/weathering

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14
Q

Flows of carbon between the lithosphere and biosphere

A

Sequestration
Decomposition

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15
Q

Flows of carbon between the hydrosphere and biosphere

A

Crustations take carbon to build shells
Marine plant take in co2- phytoplankton

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16
Q

What are the measures of carbon

A

Giggatone (GTG)
Gigatonne per year (CTCy-1)

17
Q

What is carbon stored as in the lithosphere

A

Stored in both organic and inorganic forms
Inorganic- fossil fuels- coal, oil, gas- 4100 GTG
Organic- litter, organic matter and humus in soil- 1500-1600 GTG
Stored in: mantle, marine sediments and rocks- 100m GTG
Peat- 250GTG

18
Q

What is carbon stored as in the hydrosphere

A

Oceanic stores:
Surface layer: sunlight penetrates so photosynthesis can take place- 900GTG
Intermediate layer: deep layer of water- 37100 GTG
Living organic matter and dissolved organic matter
Oceanic carbon in total is 40 000 GTG

19
Q

How does carbon get into the intermediate layer of oceans with no sunlight

A

When organisms die their dead cells, shells and other parts sink into deep water. Decay releases co2 into deep water and form layers of carbon rich sediment.
Over millions of years chemical and physical processes turn these sediments into rocks

20
Q

What is atmospheric carbon like

A

Very high millions of years ago and the lowest concentration has been the past 2 millions years suggesting It changes over time. Makes up 0.04% the earths atmosphere.

21
Q

Where is atmospheric carbon measured and why

A

Mauna Loa observatory as the air is undisturbed and in a remote location and limited influence from vegetation and human activity

22
Q

Why has atmospheric increased over the past 60 years

A

Increased 100ppm
Due to human activity such as deforestation farming and burning of fossil fuels

23
Q

Where is carbon stored in the biosphere

A

In the tropics due to high biodiversity and nutrient rich soils containing carbon. Lots of farming can take place which increases co2.

24
Q

What is the net carbon sink and net carbon source

A

If more carbon enters a store than leaves this is known as the net carbon sink. If more carbon leaves it then it’s known as a net carbon source.

25
Explanation of how the different types of rock are formed.
Sedimentary rocks are formed by different rocks in the ocean due to erosion/weathering and being compacted and buried over a long period of time. This can form into metamorphic rock due to the burial of rock leading to high pressures and high temperatures so the layers distort/melt together. Igneous rocks are formed by the high temperatures and melting of rock to produce magma and also magma from molten crust and mantle which cools and hardens to form igneous rocks.
26
The movement of carbon- factors driving change in magnitude of stores over time- lithosphere
1. In water, carbon is removed from the atmosphere by dissolving to form carbonic acid. As this acidic water reaches the surface as rain it reacts with minerals on earths surface, dissolving their component ions through weathering. 2.these component ions are carried in rivers and get back to oceans where they settle as minerals e.g. calcite, a form of calcium carbonate. 3. Coral and other shell builders extract this from water and they eventually die, build up on ocean floor and become buried and stored in layers of limestone 4. Tectonic forces cause plate movement to push the sea floor under continental Margins- subduction and the carbon sea floor is pushed deep into ground and melt. 5. Molten rock rises back to surface through volcanic eruptions or hot springs and returns back to atmosphere.
27
Where is carbon stored in the terrestrial biosphere
Living vegetation Plant litter Soil humus Peat Animals soil is the largest store, animals is the smallest
28
the movement of carbon- atmospheric factors driving change in magnitude over time
photosynthesis respiration decomposition combustion
29
the movement of carbon- hydrological factors driving change in magnitude over time
oceanic carbon pump: physical (inorganic) pump biological (ORGANIC) PUMP
30
what are the two types of carbon sequestration in the ocean
physical (inorganic) pump biological (organic) pump
31
Physical INorganic pump
Involved in mixing of surface and deep oceans by vertical currents creating a more even distribution of carbon. Initially co2 enters oceans from difussion Water and so the carbon move from low latitude to high latitude where cold water sinks (down welling) this takes co2 to the depths of the ocean and moves back to high latitude where warm water rises (upwelling) so moves co2 to the surface The cold carbon rich water rises to surface and diffuses back to atmosphere
32
Biological organic pump
Living things in the ocean move carbon from the atmosphere into the surface water and then down into deeper oceans, and eventually into rocks: Carbon is incorporated into marine organisms by photosynthesis or shell builders, when the organisms die structural carbon e.g. shells sink to the bottom. The material lies on the floor as carbon rich sediment and over millions if years sediment will be buried to lock the carbon away where layers build p.
33
Changes in carbon over time
Carbon has been fluctuationing for hundreds and thousands of years and higher concentration of co2 is associated with higher temps, in theory co2 triggers temp change however temp change also has an impact on co2. Nowadays co2 has exceeded 400 ppm due to industrialisation
34
Impacts of cold conditions on carbon stores and transfers
-chemical weathering process more active- cold water can hold more co2 -forest coverage would be very different and effects photosynthesis and respiration. -decomposes less effective so carbon transfer reduced -less water flowed in oceans as carbon locked up as ice and so less build up on ocean floor -soil frozen
35
Impact of warm conditions on carbon stores and transfers
Melting of permafrost in tundra regions has released carbon stored. Together with other gasses such as methane is now being released into atmosphere which enhances greenhouse effect- positive feedback loop
36
Physical factors that are responsible for changed in carbon over time and scale
Wildfires- can be started naturally e.g. lightening strikes however increasingly started deliberately by people. Wildfires can turn forests from being a carbon sink into a carbon source as combustion emits to atmosphere. Plant re growth takes up emmoitted co2, carbon neural fire-re growth cycles and also produces charcoal. Scale- despite restricted to small land they can have regional impacts. Release of carbon is instant but re growth may take hundreds of years. Volcanic activity- carbon released in recent eruptions has not detected global warming because co2 emitted is very little to humans and historic eruptions may have released more. Co2 counteracted by sulfur dioxide. Scale- nearly global- short cooling effect of planets past. Not large temporal scale- humans contribute
37
Human factors that effect changes in carbon over time
Hydrocarbon extraction and combustion Farming practices Deforestation and urbanisation (land use changes)
38
How hydrocarbon extraction and combustion effect changes in carbon over time
Most of worlds gas and oil is extracted from rocks 70-100 m years old where it was previously buried Carbon has been locked in these rocks for all thus time when burned fir energy and power it is released instantly and primarily as co2 in the atmosphere, increasing cycling of carbon. 90% of anthropogenic emissions There’s an uneven distribution around the world- more in china and little in S America
39
How farming practices have lead to changed in carbon over time
-fertiliser has become more common and is one of the main source of carbon emissions -1/3 methane comes from cows which is human induced Rice yeilds increased by 25% which has resulted in 40% increase in carbon and is now one of the most widely consumed foods Temporal- as pop growing more food is required so a higher yeild and increase in technology Spactially concentrated in Asia with global impacts