_CarbonCycleSE
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Villanova University *
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Course
1050
Subject
Geography
Date
Dec 6, 2023
Type
Pages
8
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Date:
Student Exploration: Carbon Cycle
Directions: Follow the instructions to go through the simulation. Respond to the questions and
prompts in the orange boxes.
Vocabulary:
atmosphere, biomass, biosphere, carbon reservoir, carbon sink, fossil fuel, geosphere,
greenhouse gas, hydrosphere, lithosphere, photosynthesis
Prior Knowledge Questions
(Do these BEFORE using the Gizmo.)
In the process of
photosynthesis
, plants take in carbon dioxide (CO
2
) from the atmosphere and water (H
2
O)
from the soil. Using the energy of sunlight, plants build molecules of glucose (C
6
H
12
O
6
) and oxygen (O
2
).
1.
How do plants on Earth affect the amount of carbon in Earth’s atmosphere?
The oceanic CO2, exposed rocks, and land plants.
2.
Animals eat plants and produce carbon dioxide and water. How do animals affect the amount of carbon in
Earth’s atmosphere?
They eat plants that process carbon dioxide and when they eat the plants there are fewer
plants producing the carbon dioxide.
Gizmo Warm-up
The
Carbon Cycle
Gizmo allows you to follow the many paths an atom of
carbon can take through Earth’s systems. To begin, notice the black carbon
atom in the
Atmospheric CO
2
area, highlighted in yellow. The glowing blue
areas represent possible locations the carbon atom could go next.
1.
From Earth’s atmosphere, where can the carbon atom go next?
The oceanic CO2, exposed rocks, and land plants.
2.
Click on
Land plants
and read the description. How did the carbon atom get from the atmosphere to a
plant?
Through photosynthesis, plants use energy from the sun
to turn carbon dioxide into oxygen.
3.
Select
Land animals
. How did the carbon atom get from land plants into the animal?
Animals consume plants.
4.
Select
Atmospheric CO
2
. How did the carbon atom get from land animals back to the atmosphere?
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Through cellular respiration, land animals release carbon
back into the atmosphere.
Activity A:
Carbon pathways
Get the Gizmo ready:
●
Click
Reset
.
Introduction:
Earth can be divided into four systems.
The
atmosphere
is the air above Earth’s surface. The
hydrosphere
is composed of all of Earth’s water. The
geosphere
is the rocky, non-living part of Earth. The
biosphere
consists of all living things, including people. Some scientists use the term “anthroposphere” to
describe everything made or modified by humans.
Question: How does carbon move between the atmosphere, hydrosphere, biosphere, and geosphere?
1.
Explore: Use the Gizmo to create a path for carbon that begins and ends in the atmosphere. Fill in the
steps in the path below. Then, label each location with the system it represents. Finally, summarize very
briefly how the carbon atom got to that location.
Carbon path
System
How it got there
Atmospheric CO
2
Atmosphere
Atmospheric CO
2
comes from volcanoes,
burning fossil fuels, and other sources.
Oceanic CO
2
Hydrosphere
Coldwater dissolves more carbon dioxide.
Marine Plants/Algae
Biosphere
Through photosynthesis, marine algae
remove carbon dioxide from the ocean.
Sediments
Geosphere
Sediments are where large amounts of
carbon are stored.
Lithosphere
Geosphere
The lithosphere has carbon-containing
rocks.
Volcano
Geosphere
Rocks are heated to high temps and are
melted and carbon dioxide forms.
Atmospheric CO
2
Atmosphere
Atmospheric CO2 comes from volcanoes,
burning fossil fuels, and other sources.
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2.
Create: Click
Reset
. Use the Gizmo to create a path in which the carbon atom goes from the atmosphere
to the hydrosphere, biosphere and geosphere. Describe each transition briefly.
Atmosphere
Hydrosphere
Biosphere
Geosphere
Atmospheric CO
2
Oceanic CO
2
Marine Algae
Sediments
Volcanoes, burning fossil
fuels, and other sources.
Coldwater dissolves
CO
2
Through
photosynthesis the
plants remove CO
2
Uneaten plants sink to
the bottom and become
marine sediments.
3.
Explore: Use the Gizmo to create three more carbon paths, each starting and ending in the atmosphere.
Label each location with A for atmosphere, B for biosphere, G for geosphere, or H for hydrosphere. (You
can also use P for the anthroposphere if you like, or just include it in the biosphere.)
Path 1:
Atmosphere A and Oceanic Co2 H
Path 2:
Atmosphere A, Land Plants B, C Atmosphere A
Path 3:
Atmosphere A and Land Plants B
4.
Explain: Based on the Gizmo, explain how the following transitions might take place:
A.
Describe at least two ways that carbon can get from a land plant to the atmosphere.
1.
Through the process of photosynthesis, taking carbon and turning it into
oxygen and that oxygen getting into the atmosphere.
2.
Forest fire producing carbon dioxide and it getting into the atmosphere.
B.
Describe at least two ways that carbon can get from the atmosphere to the hydrosphere.
1.
Carbon dissolving into rai water weakening rocks but then the minerals in
rocks, as well as the carbon, is being released into the sea. (hydrosphere).
2.
Carbo dissolving into cold water heading direction to the hydrosphere.
C.
Can you find two ways that carbon can get from the ocean to the
lithosphere
? (The lithosphere is
the rigid layer of the Earth, including the crust and part of the mantle.)
1.
Trees being turned into coal then being in the lithosphere and heated up and
turned into carbon.
2.
Shells and coral being weakened by the carbon and turned into limestone
and limestone being a part of the lithosphere.
D.
Describe at least two ways that carbon can get from seashells to the atmosphere.
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1.
When seashells are turned into limestone and are now becoming exposed
rocks they are then exposed to the atmosphere.
2.
Seashells turning into limestone then becoming a part of cement plants in
which carbon is being released into the atmosphere.
Activity B:
Human activities
Get the Gizmo ready:
●
Click
Reset
.
Introduction: Fossil fuels
, such as coal, oil, and natural gas, formed over millions of years from the remains
of ancient plants and animals. The burning of fossil fuels, as well as other human activities, increases the
amount of carbon dioxide in the atmosphere.
Question: How does human activity affect the carbon cycle?
1.
Describe: Using the Gizmo, determine how coal and petroleum (oil) are formed. Describe the steps
required to form each fuel from atmospheric CO
2
.
Coal:
Land plants that accumulate in swaps can turned into coal.
Petroleum:
Uneaten plants become a part of sediment.
2.
Explore: Natural gas is a mixture of methane (CH
4
), ethane (C
2
H
6
), and other gases. Find two ways that
natural gas forms. List the steps of the two carbon pathways below:
Path 1:
Land plants that are compressed from swap coal and as a result, create natural
gas.
Path 2:
Uneaten marine plants as animals pile up on time petroleum and natural gas is
created.
How is the formation of natural gas related to the formation of coal and petroleum?
Everything used to make petroleum and coal are compressed and heated so that proess
helps release the air that was in the various resources.
3.
Describe: Fossil fuels are used in many ways. Using the Gizmo, describe the main use for each fuel.
Coal:
Coal is used to generate electricity.
Petroleum:
Petroleum is used for gasoline.
Natural Gas:
Natural gas is used for generating electricity.
In each case, what is the end product of burning the fossil fuel, and where does it go?
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Its released into the atmosphere.
4.
Explore: Another major contribution to atmospheric carbon dioxide is the cement industry. Using the Gizmo,
find a carbon atom path from the atmosphere to the cement plant. (Hint: One of the ingredients in cement is
limestone.)
Path
Atmosphere, Oceanic, Shells/corals, Limest, Cement Plant
How is carbon dioxide produced in a cement plant?
Limestone is heated releasing it into the atmosphere.
5.
Analyze: Click
Reset
, then navigate to the
Land animals
. Select
Atmospheric CH
4
.
A.
How do land animals create methane?
Bacteria break down and undigested
materials.
B.
Humans raise large numbers of cattle for
food. How will these herds of cows affect
Earth’s atmosphere?
The cattle will be producing immense
amounts of methane so there would be
lots of carbon dioxide in the air.
6.
Analyze: In many tropical rainforests, people clear land by cutting down trees and burning them. After a few
years, the soil runs out of nutrients and cannot be farmed any longer. How does this practice of “slash and
burn agriculture” affect Earth’s atmosphere?
The pratice of slash and burn affects the earth’s atmosphere in a negative way.
7.
Draw conclusions: In general, how do many human activities influence the carbon cycle?
It influences the carbon cycle so there is more carbon being produced than there is in the
first place.
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Activity C:
Modeling the
carbon cycle
Get the Gizmo ready:
●
Select the MODEL tab.
Introduction:
Humans have been burning fossil fuels rapidly for the past 250 years. As a result, the amount of
atmospheric CO
2
has increased by about 40% since the year 1800. By measuring how much carbon moves
into and out of the atmosphere, scientists can predict the change in the amount of atmospheric carbon dioxide
every year.
Question: How can we model changes in atmospheric carbon over time?
1.
Observe: The MODEL tab shows a simplified model of the carbon cycle. The ovals represent
carbon
reservoirs
, where carbon is stored. The unit “GtC” stands for gigatonnes of carbon, where one GtC is
equal to one trillion kilograms of carbon. The arrows represent how much carbon moves from one reservoir
to another each year, in gigatonnes per year.
A.
Look at the arrows pointing toward
atmospheric CO
2
. What are the two major
sources of atmospheric carbon?
Nature and Human activity.
B.
A
carbon sink
is a location that stores
carbon for a long period of time. Which two
carbon sinks remove carbon from the
atmosphere?
Oceans and Plants.
C.
Without changing the Gizmo, list the carbon
reservoirs from largest to smallest.
Atmosphere, Terrestrial biosphere,
Oceans, and Fossil fuels.
Note: The largest carbon reservoir is actually Earth’s lithosphere, which contains about 80,000 GtC.
However, there is not much exchange between the lithosphere and the other reservoirs on short
time scales.
2.
Experiment: If necessary, click
Return to original settings
. These settings approximate present-day
conditions, but should not be taken as exact values.
A.
What is the total amount of carbon removed
from the atmosphere each year by the
ocean and land plants?
63 = 500
2 = 38000
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B.
What is the total amount of carbon added to
the atmosphere from soil and the burning of
fossil fuels?
5000 and 2000
C.
How much will atmospheric carbon change
in one year?
1 year - 854
10 years - 8,540
100 years - 85,400
3.
Calculate: Carbon dioxide is a
greenhouse gas
that helps to trap heat in Earth’s atmosphere. We need
some CO
2
in the atmosphere to maintain a warm planet, but excess carbon can cause considerable
warming of the planet.
A.
What fossil fuel usage will result in no
change in atmospheric CO
2
each year?
Carbon Dioxide
B.
What percentage decrease in fossil fuel
usage is required to achieve this goal?
40%
4.
Experiment: Using the Gizmo model, explore the following questions:
A.
How does increasing plant
biomass
(amount of plants) affect atmospheric CO
2
?
Conceptual diagram outlining important
plant responses to higher concentrations of
Carbon dioxide(CO2) in the atmosphere.
B.
How does increasing oceanic CO
2
intake
affect atmospheric CO
2
and oceanic CO
2
?
The ocean would continue to soak up
more & more carbon dioxide(Co2)
until global warming heated the ocean
enough to slow down ocean circulation.
As carbon dioxide is absorbed by the ocean, the ocean becomes slightly more acidic. This could make it
harder for many organisms to build their shells and skeletons. The consequences of ocean acidification are
not yet fully understood.
5.
Infer: Click
Reset
and
Return to original settings
. Suppose we completely stopped burning fossil fuels
immediately. How many years would it take to return to atmospheric CO
2
levels from the year 1800, about
600 GtC? Use the Gizmo to find the answer.
50 years
6.
Think about it: Since hard-shelled organisms evolved about 550 million years ago, billions of tons of
limestone rock have been produced from their shells. Limestone is made of calcium carbonate, with the
formula CaCO
3
.
Atmospheric amount of carbon dioxide has increased in the last 550 million years which
has affected the Earth's climate via global warming.
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Based on this, how do you think the amount of atmospheric CO
2
has changed in the last 550 million years,
and how has this affected Earth’s climate? Explain your answer.
Carbon dioxide(Co2) has decreased over the last 200 million years.
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