1.4 - Carbon Cycle

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11 Terms

1
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Carbon reservoirs

Relatively stable, short-term stores of carbon on earth.

Ex: fossil fuels, soils and sediments, plant and animal biomass, and the atmosphere

<p>Relatively stable, short-term stores of carbon on earth.</p><p>Ex: fossil fuels, soils and sediments, plant and animal biomass, and the atmosphere</p>
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Carbon sinks

Relatively long-term stores that can take in more carbon dioxide than they produces

Ex: Plants, ocean, soils, sedimentary rock (can be either reservoirs or sinks, depending on their depth & time)

<p>Relatively long-term stores that can take in more carbon dioxide than they produces</p><p>Ex: Plants, ocean, soils, sedimentary rock (can be either reservoirs or sinks, depending on their depth &amp; time)</p>
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Photosynthesis

Plants use the sun's energy to convert water and carbon dioxide from the atmosphere into sugars and oxygen. Removes CO2 from atmosphere.

<p>Plants use the sun's energy to convert water and carbon dioxide from the atmosphere into sugars and oxygen. Removes CO2 from atmosphere.</p>
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Cellular respiration

Process that releases energy by breaking down glucose and releasing CO2 into atmosphere

<p>Process that releases energy by breaking down glucose and releasing CO2 into atmosphere</p>
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Decomposition

A chemical proc done by soil bacteria that breaks down organic matter and stores carbon in the soil and releases it into the atmosphere as CO2 and methane (CH4)

<p>A chemical proc done by soil bacteria that breaks down organic matter and stores carbon in the soil and releases it into the atmosphere as CO2 and methane (CH4)</p>
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Carbon sequestration (storage)

The act of removing carbon from the atmosphere and storing it. Plants sequester, or store carbon from the atmosphere.

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Direct exchange

Movement of carbon dioxide gas directly between the ocean and atmosphere.

Happens at a relatively stable rate, although excess atmospheric carbon will increase the level of CO2 in the ocean

<p>Movement of carbon dioxide gas directly between the ocean and atmosphere.</p><p>Happens at a relatively stable rate, although excess atmospheric carbon will increase the level of CO2 in the ocean</p>
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Sedimentation

The process of soil particles and decaying organic matter building up in layers on the ground or at the bottom of the ocean.

Over time, pressure from water or rock layers above compresses sediments into sedimentary rock (limestone) or FFs

<p>The process of soil particles and decaying organic matter building up in layers on the ground or at the bottom of the ocean.</p><p>Over time, pressure from water or rock layers above compresses sediments into sedimentary rock (limestone) or FFs</p>
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Burial

The formation of sedimentary rock like limestone, or fossil fuels, as layers of sediments are compressed under the ocean or overlying rock layers.

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Extraction

Removal of fossil fuels (coal, oil, natural gas) from the ground, usually by mining or drilling.

A very rapid process compared to the sedimentation and burial required to form fossil fuel

<p>Removal of fossil fuels (coal, oil, natural gas) from the ground, usually by mining or drilling.</p><p>A very rapid process compared to the sedimentation and burial required to form fossil fuel</p>
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Combustion of fossil fuels

Burning of fossil fuels (primarily in cars and power plants) to release energy

Releases carbon dioxide into the atmosphere very rapidly, acting as a carbon source

<p>Burning of fossil fuels (primarily in cars and power plants) to release energy</p><p>Releases carbon dioxide into the atmosphere very rapidly, acting as a carbon source</p>