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(a) With respect to absorption of radiant energy, what distinguishes a greenhouse gas from a nongreenhouse gas? (b) \(\mathrm{CH}_{4}\) is a greenhouse gas, but Ar is not. How might the molecular structure of \(\mathrm{CH}_{4}\) explain why it is a greenhouse gas?

Short Answer

Expert verified
(a) A greenhouse gas absorbs and emits radiant energy within the thermal infrared range, while a non-greenhouse gas does not have significant absorption bands in the thermal infrared range. (b) Methane (\(\mathrm{CH}_{4}\)) is a greenhouse gas because of its complex and asymmetrical molecular structure, allowing it to absorb and emit infrared radiation due to the various vibrational modes. In contrast, argon (Ar) is a non-greenhouse gas because of its simple, symmetric, monatomic structure, which does not efficiently absorb or emit infrared radiation.

Step by step solution

01

Understand the concept of greenhouse gases

A greenhouse gas is a type of gas that absorbs and emits radiant energy within the thermal infrared range. The absorption of this radiant energy plays a crucial role in the greenhouse effect and global warming. In contrast, non-greenhouse gases don't have significant absorption bands in the thermal infrared range, thereby not contributing to the greenhouse effect.
02

Define the characteristics of greenhouse gases

Greenhouse gases typically share a few specific characteristics that allow them to absorb infrared radiation efficiently. These characteristics include: 1. Asymmetrical molecular structures: Greenhouse gases usually have complex and asymmetrical molecular structures, allowing for a variety of vibrational modes and the ability to absorb infrared radiation effectively. 2. Polar bonds: The presence of polar bonds within a molecule also contributes to the ability to absorb infrared radiation.
03

Analyze the molecular structure of CH4

Methane (CH4) is a greenhouse gas because it has a complex and asymmetrical molecular structure with one central carbon atom surrounded by four hydrogen atoms in a tetrahedral shape.Although the bonds in CH4 are nonpolar, the molecular structure can absorb and emit infrared radiation due to the complex vibrational modes that arise from its structure.
04

Compare the molecular structure of CH4 with Ar

Argon (Ar) is a non-greenhouse gas because it is an inert, monatomic gas with a simple, symmetric structure. It consists of only one argon atom and doesn't have any polar bonds or complex vibrational modes. As a result, argon does not efficiently absorb or emit infrared radiation, and it does not contribute to the greenhouse effect.

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Key Concepts

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

Radiant energy absorption
Greenhouse gases are unique in their ability to absorb radiant energy efficiently. These gases take in radiation from the sun, especially in the form of infrared light, and then re-emit this energy in all directions. This process is critical because it contributes to the warming of the Earth's atmosphere, a phenomenon known as the greenhouse effect.
Different gases have varying abilities to absorb this radiant energy. Greenhouse gases, like carbon dioxide and methane, have structures that enable them to absorb energy from the sun. Non-greenhouse gases, such as nitrogen and oxygen, lack this capability. This is because they don't have the necessary molecular structures to interact with infrared radiation as effectively, making them poor absorbers of radiant energy. By absorbing this energy, greenhouse gases keep Earth's temperature higher than it would be otherwise, fostering conditions essential for life.
Understanding the role of radiant energy absorption helps explain why some gases can significantly impact Earth's climate, despite being present in trace amounts.
Molecular structure of greenhouse gases
The molecular structure of a gas greatly influences whether it acts as a greenhouse gas. Greenhouse gases are usually more complex and have asymmetrical molecular structures. This complexity allows these gases to have various vibrational modes, which means they can absorb more specific frequencies of infrared radiation.
For example, methane (\(\mathrm{CH}_4\)) is a key greenhouse gas. Its self-contained, tetrahedral shape allows it to vibrate in unique ways when exposed to infrared radiation. Each type of vibration represents a different energy absorption opportunity for the gas, embedding it as an effective absorber of radiation. In contrast, a gas like argon (\(\mathrm{Ar}\)), which is a single atom, doesn't have these complex vibrational modes. Hence, it can't absorb significant amounts of infrared radiation and thus isn't considered a greenhouse gas.
In broad terms, it is the molecular structure—particularly whether it's complex and asymmetrical—that determines the capability of a gas to function as a greenhouse gas.
Infrared radiation
Infrared radiation, commonly associated with heat, plays a pivotal role in the process that underscores the greenhouse effect. The key aspect here is how this type of radiation interacts with molecules in Earth’s atmosphere. When sunlight reaches Earth, it is absorbed by the surface and then re-emitted as infrared radiation. The journey of this infrared radiation is interrupted by greenhouse gases.
Greenhouse gases absorb this energy and later re-emit it, creating a cycle that effectively traps heat closer to the Earth’s surface. This is crucial for maintaining the climate we experience every day. This trapping of heat due to infrared radiation is what keeps our planet warm enough to sustain life. Without such gases to capture infrared radiation, Earth would be frigid and unable to support complex life forms.
Some gases, due to their structural characteristics, are more capable of interacting with infrared radiation. It's this ability to absorb and re-emit infrared radiation that makes certain gases vital players in the greenhouse effect, significantly influencing global temperatures.

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Most popular questions from this chapter

What properties make a substance a good coagulant for water purification?

Air pollution in the Mexico City metropolitan area is among the worst in the world. The concentration of ozone in Mexico City has been measured at 441 ppb \((0.441 \mathrm{ppm})\). Mexico City sits at an altitude of 7400 feet, which means its atmospheric pressure is only \(0.67\) atm. Calculate the partial pressure of ozone at 441 ppb if the atmospheric pressure is 067 atm.

In 1986 an electrical power plant in Taylorsville, Georgia, burned \(8,376,726\) tons of coal, a national record at that time. (a) Assuming that the coal was \(83 \%\) carbon and \(25 \%\) sulfur and that combustion was complete, calculate the number of tons of carbon dioxide and sulfur dioxide produced by the plant during the year. (b) If \(55 \%\) of the \(\mathrm{SO}_{2}\) could be removed by reaction with powdered \(\mathrm{CaO}\) to form \(\mathrm{CaSO}_{3}\), how many tons of \(\mathrm{CaSO}_{3}\) would be produced?

The precipitation of \(\mathrm{A} \mathrm{L}(\mathrm{OH})_{3}\left(K_{\text {sp }}=1.3 \times 10^{-33}\right.\) ) is sometimes used to purify water. (a) Estimate the \(\mathrm{pH}\) at wh?ch precipitation of \(\mathrm{Al}(\mathrm{OH})_{3}\) will begin if \(5.0 \mathrm{lb}\) of \(\mathrm{Al}_{2}\left(\mathrm{SO}_{4}\right)_{3}\) is added to \(2000 \mathrm{gal}\) of water. (b) Approximately how many pounds of \(\mathrm{CaO}\) must be added to the water to achieve this \(\mathrm{pH}\) ?

The Henry's law constant for \(\mathrm{CO}_{2}\) in water at \(25^{\circ} \mathrm{C}\) is \(3.1 \times 10^{-2} \mathrm{M} \mathrm{atm}^{-1} .\) (a) What is the solubility of \(\mathrm{CO}_{2}\) in water at this temperature if the solution is in contact with air at normal atmospheric pressure? (b) Assume that all of this \(\mathrm{CO}_{2}\) is in the form of \(\mathrm{H}_{2} \mathrm{CO}_{3}\) produced by the reaction between \(\mathrm{CO}_{2}\) and \(\mathrm{H}_{2} \mathrm{O}\) : $$ \mathrm{CO}_{2}(a q)+\mathrm{H}_{2} \mathrm{O}(l)-\longrightarrow \mathrm{H}_{2} \mathrm{CO}_{3}(a q) $$ What is the \(\mathrm{pH}\) of this solution?

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