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Molecules in the upper atmosphere tend to contain double and triple bonds rather than single bonds. Suggest an explanation. [Section 18.2]

Short Answer

Expert verified
Molecules in the upper atmosphere contain double and triple bonds rather than single bonds due to their greater stability under the extreme conditions of low pressure, high altitude, and high levels of UV radiation. The stronger and shorter nature of double and triple bonds makes these molecules more resistant to dissociation, allowing them to better withstand the harsh environment of the upper atmosphere.

Step by step solution

01

Understanding Single, Double, and Triple Bonds

Single bonds are the result of sharing one pair of electrons between two atoms, while double and triple bonds result from sharing two or three pairs of electrons, respectively. As a general rule, double and triple bonds are shorter and stronger than single bonds.
02

Conditions in the Upper Atmosphere

The upper atmosphere is characterized by low pressure, high altitude, and high levels of ultraviolet (UV) radiation from the sun. These conditions can influence the stability of molecules in this region.
03

Effects of UV Radiation

Ultraviolet radiation has enough energy to break the chemical bonds in molecules, leading to the dissociation of the molecules into their constituent atoms or fragments. Since double and triple bonds are stronger and require more energy to break, molecules containing such bonds tend to be more stable and less susceptible to disintegration due to UV radiation.
04

Stability of Molecules with Multiple Bonds

Molecules with double and triple bonds have stronger and shorter bonds, which makes them more stable in the upper atmosphere. The increased stability helps protect these molecules from breaking apart under the extreme conditions in the upper atmosphere.
05

Suggested Explanation

Molecules in the upper atmosphere tend to contain double and triple bonds rather than single bonds because these multiple bonds provide greater stability. The stronger and shorter nature of double and triple bonds makes these molecules more resistant to dissociation, which is an important factor considering the high levels of UV radiation in the upper atmosphere.

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Key Concepts

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

Single, Double, and Triple Bonds
The intriguing dance of electrons between atoms forms the fundamental basis of chemical bonding, and the nature of this interaction determines the strength and stability of the bond. In single bonds, one pair of electrons is shared between two atoms, creating a single shared path. However, the story grows more complex as we introduce double and triple bonds. When two pairs of electrons are shared, we get a double bond, and when three pairs come together, it results in a triple bond.

The Strength of Bonds
  • Single Bonds: Generally the longest and weakest type of covalent bonds due to fewer shared electrons. They are often found in molecules where flexibility is needed.
  • Double Bonds: These involve two shared pairs of electrons and are stronger and shorter than single bonds. The shared electron density between the two atoms holds them tighter together.
  • Triple Bonds: The strongest and shortest of the three, with three shared pairs of electrons, forming an especially robust connection between atoms.
This hierarchy of bond strength is central to understanding why certain molecules prefer certain structures in different environments, such as the upper atmosphere.
UV Radiation Effects on Molecules
When molecules ascend to the upper reaches of the atmosphere, they encounter an environment rife with ultraviolet (UV) radiation, a form of energy emanating from the sun with enough fervor to break chemical bonds. UV radiation is like a gauntlet that molecules must endure, and not all are equally prepared.Breaking BondsThe energy provided by UV radiation can cleave chemical bonds, leading to dissociation, where molecules are fragmented into atoms or smaller molecules. Double and triple bonds, with their increased electron sharing and stronger connections, demand greater energy to break compared to single bonds.

This disparity explains why UV radiation selectively affects molecules with weaker single bonds, making those with multiple bonds more likely to survive this onslaught. It highlights the relentless battle molecules face against the invisible might of UV radiation in the upper atmosphere.
Stability of Atmospheric Molecules
Stability in the chemical realm is a measure of resistance to change, and in the upper atmosphere, this attribute is a matter of survival. Here, molecules are locked in a perpetual struggle to maintain their integrity against the relentless assault of UV radiation. With the stakes so high, stability is a prized feature.

Why Multiple Bonds Win

Molecules with double and triple bonds often emerge victorious due to their shorter and stronger nature. They are less prone to dissociation, allowing them to persist where others might falter. Imagine these molecules as fortified structures in an environment wearing them down; the more robust the structure, the better its chances of enduring.It's no coincidence that such molecules are prevalent in this atmospheric layer. They represent a specialized adaptation to an extreme condition – the ability to withstand the UV radiation that would otherwise dismantle weaker bonds. This natural selection of molecular stability is a sublime example of nature's propensity for enduring through resilience.

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Most popular questions from this chapter

Explain why increasing concentrations of \(\mathrm{CO}_{2}\) in the atmosphere affect the quantity of energy leaving Earth but do not affect the quantity entering from the Sun.

Nitrogen dioxide \(\left(\mathrm{NO}_{2}\right)\) is the only important gaseous species in the lower atmosphere that absorbs visible light. (a) Write the Lewis structure(s) for \(\mathrm{NO}_{2}\). (b) How does this structure account for the fact that \(\mathrm{NO}_{2}\) dimerizes to form \(\mathrm{N}_{2} \mathrm{O}_{4} ?\) Based on what you can find about this dimerization reaction in the text, would you expect to find the \(\mathrm{NO}_{2}\) that forms in an urban environment to be in the form of dimer? Explain. (c) What would you expect as products, if any, for the reaction of \(\mathrm{NO}_{2}\) with CO? (d) Would you expect \(\mathrm{NO}_{2}\) generated in an urban environment to migrate to the stratosphere? Explain.

You are working with an artist who has been commissioned to make a sculpture for a big city in the eastern United States. The artist is wondering what material to use to make her sculpture, because she has heard that acid rain in the eastern U.S. might destroy it over time. You take samples of granite, marble, bronze, and other materials, and place them outdoors for a long time in the big city. You periodically examine the appearance and measure the mass of the samples. (a) What observations would lead you to conclude that one, or more, of the materials were well-suited for the sculpture? (b) What chemical process (or processes) is (are) the most likely responsible for any observed changes in the materials? [Section 18.4]

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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 \(2.5 \%\) 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?

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