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One mystery in environmental science is the imbalance in the "carbon dioxide budget." Considering only human activities, scientists have estimated that 1.6 billion metric tons of \(\mathrm{CO}_{2}\) is added to the atmosphere every year because of deforestation (plants use \(\mathrm{CO}_{2},\) and fewer plants will leave more \(\mathrm{CO}_{2}\) in the atmosphere). Another 5.5 billion tons per year is put into the atmosphere because of burning fossil fuels. It is further estimated (again, considering only human activities) that the atmosphere actually takes up about 3.3 billion tons of this \(\mathrm{CO}_{2}\) per year, while the oceans take up 2 billion tons per year, leaving about 1.8 billion tons of \(\mathrm{CO}_{2}\) per year unaccounted for. Describe a mechanism by which \(\mathrm{CO}_{2}\) is removed from the atmosphere and ultimately ends up below the surface (Hint: What is the source of the fossil fuels?) [Sections \(18.1-18.3 ]\)

Short Answer

Expert verified
The unaccounted-for 1.8 billion metric tons of COâ‚‚ per year may be sequestered through a mechanism involving photosynthesis and the carbon cycle. Plants and other photosynthetic organisms remove COâ‚‚ from the atmosphere and convert it into organic compounds. As these plants die and are buried under sediment, they become part of the fossil fuel formation process over millions of years, ultimately ending up below the Earth's surface as coal, oil, or natural gas. This process helps store carbon beneath the Earth's surface; however, burning fossil fuels releases this stored carbon back into the atmosphere, contributing to the global carbon budget imbalance.

Step by step solution

01

Understand the given data

The data provided in the exercise states that human activities add: - 1.6 billion metric tons of CO2 is added to the atmosphere yearly because of deforestation - 5.5 billion metric tons of CO2 due to burning fossil fuels Additionally, the atmosphere takes up 3.3 billion metric tons of COâ‚‚ per year, the ocean takes up about 2 billion metric tons per year, leaving 1.8 billion metric tons of COâ‚‚ per year unaccounted for.
02

Identify the source of fossil fuels

Fossil fuels, such as coal, oil, and natural gas, are formed from the remains of ancient plants and animals that have been subjected to heat and pressure over millions of years. They are primarily composed of carbon and hydrogen, and when burned as a fuel, they release CO2 into the atmosphere.
03

Understand the carbon cycle

The carbon cycle is a natural process through which carbon atoms circulate between the Earth's surface, atmosphere, and oceans. It includes key processes such as photosynthesis, respiration, and decomposition, and plays a significant role in determining the levels of CO2 in the atmosphere.
04

Describe a mechanism by which CO2 is removed from the atmosphere

One mechanism by which CO2 is removed from the atmosphere is through photosynthesis. Plants take in COâ‚‚ from the atmosphere and, using sunlight, convert it into glucose and oxygen. This glucose can then be used by the plants for growth and is transformed into more complex organic molecules, such as cellulose and lignin. As these plants die and are buried under layers of sediment, they can become part of the fossil fuel formation process over millions of years, ultimately ending up below the Earth's surface in the form of coal, oil, or natural gas.
05

Conclusion

The unaccounted-for COâ‚‚ may be getting sequestered in various ways, one of which is being incorporated into the process of fossil fuel formation. Photosynthesis by plants and other photosynthetic organisms removes COâ‚‚ from the atmosphere and converts it into organic compounds. These compounds, through a series of geological processes, can eventually become fossil fuels, storing the carbon beneath the Earth's surface. However, burning fossil fuels releases this stored carbon back into the atmosphere in the form of COâ‚‚, contributing to the global carbon budget imbalance.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Carbon Dioxide Budget
The carbon dioxide budget refers to the delicate balance of carbon dioxide (\(\text{CO}_2\)) levels in Earth's atmosphere. Human activities, like deforestation and burning fossil fuels, add substantial amounts of \(\text{CO}_2\) to the atmosphere.
The exercise mentions:
  • 1.6 billion metric tons of \(\text{CO}_2\) are added due to deforestation.
  • 5.5 billion metric tons come from burning fossil fuels.
However, not all \(\text{CO}_2\) remains in the atmosphere.
The natural system, including the atmosphere and oceans, absorbs some—3.3 billion tons taken by the atmosphere and 2 billion by the oceans—but 1.8 billion tons are unaccounted for.
This discrepancy highlights the importance of understanding natural processes, like photosynthesis and fossil fuel formation, in managing atmospheric \(\text{CO}_2\) levels.
Photosynthesis
Photosynthesis is a vital process by which plants and photosynthetic organisms convert \(\text{CO}_2\) into glucose using sunlight.
Plants take in \(\text{CO}_2\) through their leaves and use it, along with water, to produce glucose and oxygen.
This process not only provides food and energy for the plant but also helps reduce atmospheric \(\text{CO}_2\) levels.- **Key Points of Photosynthesis** - **Light Energy to Chemical Energy**: Sunlight is the energy source that makes this transformation possible. - **Glucose Formation**: The carbon from \(\text{CO}_2\) becomes part of the glucose molecule, storing energy.By converting carbon into long-lasting compounds, plants help trap carbon within their bodies.
When they die, this carbon can eventually become part of fossil fuels, locking it away over millions of years.
Fossil Fuel Formation
Fossil fuel formation is a geological process that converts organic matter, derived from plants and animals, into coal, oil, and natural gas under specific conditions over millions of years.
This process is a slow form of carbon sequestration, where carbon is stored underground, reducing the amount in the atmosphere.- **Process Overview**: - **Accumulation**: Dead plants and animals pile up in sediment layers. - **Compression and Heating**: Over time, pressure and heat transform this matter. - **Forming Fossil Fuels**: Eventually, these layers turn into coal, oil, or natural gas.By sequestering carbon in the form of fossil fuels, the Earth's carbon cycle temporarily removes it from the atmosphere.
However, when these fuels are burned, the stored \(\text{CO}_2\) is released back, contributing to current global warming issues. Understanding this cycle is essential for developing strategies to maintain a balanced carbon dioxide budget.

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Most popular questions from this chapter

Why is the photodissociation of \(\mathrm{N}_{2}\) in the atmosphere relatively unimportant compared with the photodissociation of \(\mathrm{O}_{2} ?\)

(a) Explain why Mg \(\mathrm{Mg}(\mathrm{OH})_{2}\) precipitates when \(\mathrm{CO}_{3}^{2-}\) ion is added to a solution containing \(\mathrm{Mg}^{2+} .\) (b) Will Mg \((\mathrm{OH})_{2}\) precipitate when 4.0 \(\mathrm{g}\) of \(\mathrm{Na}_{2} \mathrm{CO}_{3}\) is added to 1.00 \(\mathrm{L}\) of a solution containing 125 \(\mathrm{ppm}\) of \(\mathrm{Mg}^{2+} ?\)

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As of the writing of this text, EPA standards limit atmospheric ozone levels in urban environments to 84 ppb. How many moles of ozone would there be in the air above Los Angeles County (area about 4000 square miles; consider a height of 100 \(\mathrm{m}\) above the ground) if ozone was at this concentration?

The enthalpy of fusion of water is 6.01 \(\mathrm{kJ} / \mathrm{mol} .\) Sunlight striking Earth's surface supplies 168 \(\mathrm{W}\) per square meter \((1 \mathrm{W}=1\) watt \(=1 \mathrm{J} / \mathrm{s})\) . (a) Assuming that melting of ice is due only to energy input from the Sun, calculate how many grams of ice could be melted from a 1.00 square meter patch of ice over a 12 -h day. (b) The specific heat capacity of ice is 2.032 \(\mathrm{J} / \mathrm{g}^{\circ} \mathrm{C} .\) If the initial temperature of a 1.00 square meter patch of ice is \(-5.0^{\circ} \mathrm{C},\) what is its final temperature after being in sunlight for 12 \(\mathrm{h}\) , assuming no phase changes and assuming that sunlight penetrates uniformly to a depth of 1.00 \(\mathrm{cm} ?\)

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