OCR A Level ELSS - 5. OCR A Level ELSS 4.1b Systems and Global Water & Carbon Cycles Flashcards

1
Q

What is an isolated system?

A

a system that has no interactions with its surroundings

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2
Q

What is a closed system?

A

Linked processes where there are no inputs or outputs of matter. Energy still moves into and out of the network.

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3
Q

What is an input?

A

the addition of energy or matter into a system

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4
Q

What is a store or sink in a system?

A

The part of a system where water or carbon is retained for a period of time.

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5
Q

What is a flow/process/pathway in a system?

A

The mechanism by which water or carbon moves from one store to another.

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6
Q

What is an open system?

A

A cycle or process where inputs and outputs can add or remove material or energy

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7
Q

What is dynamic equilibrium?

A

a state of balance between continuing processes in a system

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8
Q

What is the cryosphere?

A

All frozen water on earth

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9
Q

What is the lithosphere?

A

the rigid outer part of the earth, consisting of the crust and upper mantle.

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10
Q

What is the atmosphere?

A

the layer of gases that surrounds Earth

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11
Q

What is the biosphere?

A

all life on earth

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12
Q

What is the hydrosphere?

A

All the water on earth

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13
Q

What is the Natural World?

A

Biomes and ecosystems, for example, not the human or built environment.

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14
Q

What does the term Flora mean?

A

The plants living in a defined are at a defined time

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15
Q

What does the term Fauna mean?

A

The animals living in a defined area at a defined time.

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16
Q

What is Carbon?

A

A black (when solid), non-metallic element with the atomic number 6, the basis of life on Earth, many rocks and fossil fuels.

17
Q

What is the global carbon cycle?

A

A representation of the movement of carbon between different stores including: Soil (pedosphere), Terrestrial biomass (biosphere), Atmosphere Oceans Sea floor sediments and Sedimentary rocks (lithosphere). Through a series of flows including: Photosynthesis Respiration Decomposition Combustion Oxidation Weathering and Volcanic Activity

18
Q

What is the global water cycle?

A

A representation of the global movement of water between: 3 major stores (oceans, land and atmosphere) and Through a series of flows (precipitation, evaporation, evapotranspiration and run-off/groundwater flow)

19
Q

How much water is there on earth?

A

1.4 billion km3

20
Q

How much water is stored in the oceans?

A

1.3 billion km3 (~ 97%)

21
Q

How much water is stored in the atmosphere?

A

13,000 km3 (~ 0.001%)

22
Q

How much water is stored on land?

A

39 million km3 (~ 2.8%)

23
Q

How much water and carbon and for how long does water and carbon stay in the Ocean?

A

a very large expanse of sea It stores 1.3 billion km3 of WATER (about 97% of global water) Residence time of ~3600 years It stores 38 billion tonnes of CARBON (around 0.038% or global carbon),

24
Q

How much water and carbon and for how long does water and carbon stay in the Atmosphere?

A

A thin layer of gases surrounding Earth. It stores 13,000 km3 (about 0.001% of Global Water) Residence time of 10 days for water (FAST) It stores 600 billion tonnes of CARBON FAST Carbon Cycle

25
Q

How much water and carbon and for how long does water and carbon stay in the Pedosphere?

A

the soil layers of Earth. Stores 65 km3 of WATER (about 0.005% of Global Water) Residence time of 2-50 Weeks (FAST) It stores 2,300 billion tonnes of CARBON. FAST Carbon Cycle

26
Q

How much water and carbon and for how long does water and carbon stay in the Biosphere?

A

Consists of all life on Earth. Any organic material. Stores 0.6km3 of WATER (around 0.00004% of global water) Residence time of 2-50weeks. It stores 560 billion tonnes of CARBON. FAST Carbon Cycle.

27
Q

How much water and carbon and for how long does water and carbon stay in the Cryosphere?

A

The component of the hydrological cycle where water is locked up as ice and snow. Stores 29,000km3 of Water (around 2% of global water. Residence time of 15,000years Snow and Glacial Ice store insignificant quantities of CARBON. However the trapped CO2 can be used to help understand past climates.

28
Q

How much water and carbon and for how long does water and carbon stay in the Lithosphere?

A

The rigid outer part of the earth, consisting of the crust and upper mantle (Rock). Stores 9,500km3 of WATER (around 0.7% of global water) in aquifers. Residence time up to 10,000 years. Stores 60,000 - 100 million billion tonnes of CARBON. SLOW Carbon Cycle (~150 million years)

29
Q

What is the slow carbon cycle?

A

The parts of the carbon cycle that take between 100-200million years to complete. It starts in the Atmosphere - where CO2 + Water vapour combine to form carbonic acid making rainfall slightly acidic. This means that chemical weathering (carbonation) takes place on carbonate rocks (like limestone and chalk) which releases some CO2 back to the atmosphere, but the rest is dissolved in water and enters the Hydrosphere, flowing from rivers into the oceans. Oceans are also able to absorb CO2 directly from the atmosphere through direct ocean uptake (diffusion). Marine organisms fix this ocean carbon with calcium to form calcium carbonate as part of their shells and skeletons. When these organisms die they sink to the ocean floor (sedimentation). Over millions of years, heat and pressure convert these shells and skeletons back into carbon-rich sedimentary rocks (Lithosphere). Again, over 100s of millions of years, tectonic plate movement takes these ocean sediments to destructive plate boundaries where, through subduction, the carbon is then released back into the atmosphere in volcanic eruptions. The SLOW CARBON CYCLE moves between 10 and 100 million metric tons of carbon each year.

30
Q

What is the fast carbon cycle?

A

The parts of the carbon cycle that are between 10 and 1,000 times faster than the slow carbon cycle. It is unique to Earth as it moves carbon through the biosphere. Atmosphere to Biosphere - Land plants (primary producer organisms) and phytoplankton in the oceans absorb CO2 from the atmosphere through photosynthesis and combine it with water to form carbohydrates (sugar/glucose). Biosphere to Atmosphere - Respiration converts sugar and glucose back into CO2. Decomposition and waste gases also releases CO2 and CH4 (methane) back into the atmosphere. Combustion (burning) also releases carbon back to the atmosphere. Biosphere to Pedosphere - Decomposition can release organic carbon into the soils in the form of humus Atmosphere to Oceans through the Biological (organic) pump and Oceans to Atmosphere through diffusion. The FAST CARBON CYCLE moves between 1 billion and 100 billion metric tons of carbon each year.

31
Q

What are phytoplankton?

A

these are similar to terrestrial plants in that they contain chlorophyll and require sunlight in order to live and grow. Most phytoplankton are buoyant and float in the upper part of the ocean, where sunlight penetrates the water.

32
Q

How much carbon is added to the atmosphere, oceans and biosphere each year through the combustion of fossil fuels?

A

10 Gigatons per year