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Ch.16 - Acid-Base Equilibria
Chapter 16, Problem 117a

Atmospheric CO2 levels have risen by nearly 20% over the past 40 years from 320 ppm to 400 ppm. (a) Given that the average pH of clean, unpolluted rain today is 5.4, determine the pH of unpolluted rain 40 years ago. Assume that carbonic acid 1H2CO32 formed by the reaction of CO2 and water is the only factor influencing pH. CO21g2 + H2O1l2 Δ H2CO31aq2

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Key Concepts

Here are the essential concepts you must grasp in order to answer the question correctly.

pH Scale

The pH scale measures the acidity or basicity of a solution, ranging from 0 to 14. A pH of 7 is neutral, while values below 7 indicate acidity and above 7 indicate basicity. Each unit change in pH represents a tenfold change in hydrogen ion concentration, making it crucial for understanding how changes in CO2 levels can affect rainwater acidity.
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Carbonic Acid Formation

Carbonic acid (H2CO3) is formed when carbon dioxide (CO2) dissolves in water, following the reaction CO2 + H2O ⇌ H2CO3. This weak acid dissociates in water, contributing to the acidity of rainwater. Understanding this reaction is essential for determining how increased atmospheric CO2 levels influence the pH of rain.
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Acid-Base Equilibrium

Acid-base equilibrium refers to the balance between acids and bases in a solution, which affects pH. In the context of rainwater, the equilibrium between carbonic acid and its dissociated ions (H+ and HCO3-) is influenced by the concentration of CO2. An increase in CO2 leads to more carbonic acid, thus lowering the pH and increasing acidity.
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