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Carbon Cycle and Climate

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Carbon Cycle and Climate
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What is a diamond?

Carbon takes all sorts of forms as an element and as a compound. A diamond is just carbon, pure carbon. A diamond is good for cutting things, but it's not good for breathing or building proteins out of, yet other forms of carbon are. Carbon is essential for life on Earth and, as carbon dioxide, it is an important atmospheric gas.

The Carbon Cycle

Carbon is a very important element to living things. As the second most common element in the human body, we know that human life without carbon would not be possible. Protein, carbohydrates , and fats are all part of the body and all contain carbon. When your body breaks down food to produce energy, you break down protein, carbohydrates, and fat, and you breathe out carbon dioxide.

Carbon occurs in many forms on Earth. The element moves through organisms and then returns to the environment. When all this happens in balance, the ecosystem remains in balance too.

Short Term Cycling of Carbon

The short term cycling of carbon begins with carbon dioxide (CO 2 ) in the atmosphere.

Photosynthesis

Through photosynthesis, the inorganic carbon in carbon dioxide plus water and energy from sunlight is transformed into organic carbon (food) with oxygen given off as a waste product. The chemical equation for photosynthesis is:

Respiration

Plants and animals engage in the reverse of photosynthesis, which is respiration. In respiration, animals use oxygen to convert the organic carbon in sugar into food energy they can use. Plants also go through respiration and consume some of the sugars they produce.

The chemical reaction for respiration is:

C 6 H 12 O 6 + 6 O 2 → 6 CO 2 + 6 H 2 O + useable energy

Photosynthesis and respiration are a gas exchange process. In photosynthesis, CO 2 is converted to O 2 ; in respiration, O 2 is converted to CO 2 .

Remember that plants do not create energy. They change the energy from sunlight into chemical energy that plants and animals can use as food ( Figure below ).

The carbon cycle shows where a carbon atom might be found. The black numbers indicate how much carbon is stored in various reservoirs, in billions of tons ("GtC" stands for gigatons of carbon). The purple numbers indicate how much carbon moves between reservoirs each year. The sediments, as defined in this diagram, do not include the ~70 million GtC of carbonate rock and kerogen.

Long-Term Carbon Cycling

Carbon Sinks and Carbon Sources

Places in the ecosystem that store carbon are reservoirs. Places that supply and remove carbon are carbon sources and carbon sinks , respectively. If more carbon is provided than stored, the place is a carbon source. If more carbon dioxide is absorbed than is emitted, the reservoir is a carbon sink. What are some examples of carbon sources and sinks?

  • Carbon sinks are reservoirs where carbon is stored. Healthy living forests and the oceans act as carbon sinks.
  • Carbon sources are reservoirs from which carbon can enter the environment. The mantle is a source of carbon from volcanic gases.

A reservoir can change from a sink to a source and vice versa. A forest is a sink, but when the forest burns it becomes a source.

The amount of time that carbon stays, on average, in a reservoir is the residence time of carbon in that reservoir.

The concept of residence times is explored using the undergraduate population at UGA as an example. In this example the reservoir is the university: http://www.youtube.com/watch?v=cIuaedcVvQg (2:44).

Atmospheric Carbon Dioxide

Remember that the amount of CO 2 in the atmosphere is very low. This means that a small increase or decrease in the atmospheric CO 2 can have a large effect.

By measuring the composition of air bubbles trapped in glacial ice, scientists can learn the amount of atmospheric CO 2 at times in the past. Of particular interest is the time just before the Industrial Revolution, when society began to use fossil fuels. That value is thought to be the natural content of CO 2 for this time period; that number was 280 parts per million (ppm).

By 1958, when scientists began to directly measure CO 2 content from the atmosphere at Mauna Loa volcano in the Pacific Ocean, the amount was 316 ppm ( Figure below ). In 2011, the atmospheric CO 2 content had risen to 390 ppm.

The amount of CO 2 in the atmosphere has been measured at Mauna Loa Observatory since 1958. The blue line shows yearly averaged CO 2 . The red line shows seasonal variations in CO 2 .

This is an increase in atmospheric CO 2 of 40% since the before the Industrial Revolution. About 65% of that increase has occurred since the first CO 2 measurements were made on Mauna Loa Volcano, Hawaii, in 1958.

Human Actions Impact the Carbon Cycle

Humans have changed the natural balance of the carbon cycle because we use coal, oil, and natural gas to supply our energy demands. Fossil fuels are a sink for CO 2 when they form, but they are a source for CO 2 when they are burned.

The equation for combustion of propane, which is a simple hydrocarbon looks like this:

The equation shows that when propane burns, it uses oxygen and produces carbon dioxide and water. So when a car burns a tank of gas, the amount of CO 2 in the atmosphere increases just a little. Added over millions of tanks of gas and coal burned for electricity in power plants and all of the other sources of CO 2 , the result is the increase in atmospheric CO 2 seen in the Figure above .

The second largest source of atmospheric CO 2 is deforestation ( Figure below ). Trees naturally absorb CO 2 while they are alive. Trees that are cut down lose their ability to absorb CO 2 . If the tree is burned or decomposes, it becomes a source of CO 2 . A forest can go from being a carbon sink to being a carbon source.

This forest in Mexico has been cut down and burned to clear forested land for agriculture.

Why the Carbon Cycle is Important

Why is such a small amount of carbon dioxide in the atmosphere even important? Carbon dioxide is a greenhouse gas. Greenhouse gases trap heat energy that would otherwise radiate out into space, which warms Earth. These gases were discussed in the chapter Atmospheric Processes.

This video Keeping up with Carbon from NASA, focuses on the oceans. Topics include what will happen as temperature warms and the oceans can hold less carbon, and ocean acidification: http://www.youtube.com/watch?v=HrIr3xDhQ0E (5:39).

A very thorough but basic summary of the carbon cycle, including the effect of carbon dioxide in the atmosphere, is found in this video: http://www.youtube.com/watch?v=U3SZKJVKRxQ (4:37).

Summary

  • Carbon is essential for life as part of proteins, carbohydrates, and fats.
  • The amount of carbon dioxide in the atmosphere is extremely low, but it is extremely important since carbon dioxide is a greenhouse gas, which helps to keep Earth's climate moderate.
  • The amount of carbon dioxide in the atmosphere is rising, a fact that has been documented on Mauna Loa volcano since 1958.

Practice

Use this resource to answer the questions that follow.

1. How is carbon moved with photosynthesis?

2. How is carbon moved with respiration?

3. What process releases carbon dioxide to the atmosphere?

4. What gases does combustion produce?

5. What happens to sediment over time?

6. What occurs during weathering?

Review

1. What does it mean to say that photosynthesis and respiration are gas exchange processes?

2. How do scientists learn about carbon levels in the past?

3. How do human activities affect the carbon cycle?

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