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The decomposition of ozone into oxygen gas is a fascinating chemical reaction that takes place in our environment. Ozone, which is represented chemically as \(\mathrm{O}_3(g)\), is a form of oxygen that plays a crucial role in protecting life on Earth by absorbing most of the sun's harmful ultraviolet radiation. However, under certain conditions, such as at room temperature and standard atmospheric pressure, ozone is not very stable and can decompose into oxygen gas \(\mathrm{O}_2(g)\). This reaction can be represented as \(2 \mathrm{O}_3(g) \longrightarrow 3 \mathrm{O}_2(g)\).
Understanding this decomposition process is important because it helps explain how ozone's protective layer is maintained and balanced in the atmosphere. As ozone decomposes, it releases energy, indicating the transformation from a less stable form (ozone) to a more stable form (oxygen gas). This natural process is part of a complex cycle involving the creation and destruction of ozone, which is crucial for the atmospheric equilibrium.

An exothermic reaction is one in which energy is released, usually in the form of heat, into the surroundings. In this context, the decomposition of ozone to form oxygen gas is an exothermic process. The reaction's enthalpy change \(\Delta H\) is given as \(-284.6 \mathrm{~kJ}\). This negative value tells us that the reaction releases energy. For every 2 moles of ozone that decompose, 284.6 kJ of energy is liberated.
To determine the energy released per mole of ozone, simply divide the total energy change by 2, which gives \(-142.3 \mathrm{kJ/mol}\) of \(\mathrm{O}_3(g)\). This energy release is a sign that the reactants, in this case, ozone molecules, possess higher energy compared to the products, which are oxygen molecules. An exothermic reaction like this suggests that after the reaction, the system and surroundings are in a lower energy state, contributing to the stability of \(\mathrm{O}_2(g)\) over \(\mathrm{O}_3(g)\).

Ozone's critical environmental function is its ability to absorb ultraviolet (UV) radiation from the sun. In the stratosphere, a region of the Earth's atmosphere, ozone plays a key protective role by blocking harmful UV rays that could otherwise reach the Earth’s surface, causing damage to living organisms. This process is essential for life on Earth, as UV radiation can lead to health issues like skin cancer and cataracts, as well as adversely affecting ecosystems.
The UV absorption process involves the energy from UV radiation splitting ozone molecules into oxygen molecules and a singlet oxygen atom, which can quickly recombine to form ozone again. This cyclical process of ozone formation and decomposition maintains ozone levels and continues to provide a shield against UV radiation. Understanding the absorption properties of ozone is crucial for environmental science, as it helps us comprehend the effects of pollutants that can diminish the ozone layer, emphasizing the importance of ozone in our atmosphere.