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  • Rainwater pH: Understanding Atmospheric Equilibrium & Acidity
    The pH of rainwater in equilibrium with the atmosphere is approximately 5.6.

    Here's why:

    * Carbon dioxide (CO2) in the atmosphere: Rainwater is naturally acidic due to the presence of dissolved carbon dioxide (CO2) from the atmosphere.

    * Carbonic acid formation: When CO2 dissolves in water, it forms carbonic acid (H2CO3), which then dissociates into hydrogen ions (H+) and bicarbonate ions (HCO3-).

    * Equilibrium: The pH of rainwater reaches an equilibrium point where the rate of CO2 dissolving into water equals the rate of CO2 escaping from the water.

    * pH 5.6: This equilibrium point results in a pH of approximately 5.6, which is considered slightly acidic.

    Important Note: The actual pH of rainwater can vary depending on factors like:

    * Pollution: Industrial emissions, such as sulfur dioxide (SO2) and nitrogen oxides (NOx), can increase the acidity of rainwater.

    * Location: Rainwater in areas with high levels of pollution may have a lower pH than rainwater in pristine environments.

    * Other atmospheric gases: Other gases like ozone and ammonia can also influence the pH of rainwater.

    While a pH of 5.6 is considered normal for rainwater, any pH lower than this indicates acid rain, which can have negative impacts on the environment and human health.

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