Example Of Dalton's Law Of Partial Pressure

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Nov 25, 2025 · 12 min read

Example Of Dalton's Law Of Partial Pressure
Example Of Dalton's Law Of Partial Pressure

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    The concept of Dalton's Law of Partial Pressures is fundamental to understanding the behavior of gas mixtures. It provides a simple yet powerful way to calculate the total pressure exerted by a mixture of gases based on the individual pressures of each gas component. In essence, Dalton's Law states that the total pressure exerted by a mixture of non-reacting gases is equal to the sum of the partial pressures of each individual gas. Let's delve into the depths of this principle through various examples.

    Understanding Dalton's Law: A Detailed Look

    Before jumping into examples, it's crucial to solidify our understanding of the key terms and the law itself.

    • Partial Pressure: The pressure that each gas in a mixture would exert if it occupied the entire volume alone. It's essentially the "individual contribution" of each gas to the total pressure.
    • Total Pressure: The sum of all the partial pressures in a gas mixture.
    • Dalton's Law Formula: P<sub>total</sub> = P<sub>1</sub> + P<sub>2</sub> + P<sub>3</sub> + ... + P<sub>n</sub>, where P<sub>total</sub> is the total pressure and P<sub>1</sub>, P<sub>2</sub>, P<sub>3</sub>, ..., P<sub>n</sub> are the partial pressures of each individual gas.

    The underlying assumption of Dalton's Law is that the gases in the mixture do not react with each other. If a chemical reaction occurs, the number of moles of each gas changes, and the law no longer accurately predicts the total pressure.

    Real-World Examples of Dalton's Law

    Dalton's Law isn't just a theoretical concept; it has practical applications in various fields, from medicine to scuba diving.

    1. Air Composition and Atmospheric Pressure

    The air we breathe is a mixture of gases, primarily nitrogen (N<sub>2</sub>), oxygen (O<sub>2</sub>), argon (Ar), and trace amounts of other gases like carbon dioxide (CO<sub>2</sub>) and neon (Ne). At sea level, the atmospheric pressure is approximately 1 atmosphere (atm), which is equal to 760 mmHg (millimeters of mercury) or 101.325 kPa (kilopascals).

    Let's break down the partial pressures of the major components:

    • Nitrogen (N<sub>2</sub>): Approximately 78% of air. Therefore, P<sub>N2</sub> = 0.78 * 1 atm = 0.78 atm (or 592.8 mmHg)
    • Oxygen (O<sub>2</sub>): Approximately 21% of air. Therefore, P<sub>O2</sub> = 0.21 * 1 atm = 0.21 atm (or 159.6 mmHg)
    • Argon (Ar): Approximately 0.9% of air. Therefore, P<sub>Ar</sub> = 0.009 * 1 atm = 0.009 atm (or 6.84 mmHg)

    According to Dalton's Law, the total pressure of the air should be the sum of these partial pressures:

    P<sub>total</sub> = P<sub>N2</sub> + P<sub>O2</sub> + P<sub>Ar</sub> + ...

    P<sub>total</sub> = 0.78 atm + 0.21 atm + 0.009 atm + ... ≈ 1 atm

    This example demonstrates how Dalton's Law accurately describes the composition of air and its contribution to atmospheric pressure. The small amounts of other trace gasses contribute to reaching the exact value of 1 atm.

    2. Scuba Diving and Partial Pressure of Oxygen

    Scuba divers need to understand Dalton's Law to avoid oxygen toxicity and nitrogen narcosis. As a diver descends, the pressure increases dramatically. At a depth of 10 meters (approximately 33 feet), the total pressure is about 2 atmospheres. At 20 meters (approximately 66 feet), it's about 3 atmospheres, and so on.

    The partial pressure of each gas in the breathing mix increases proportionally to the total pressure. If a diver is breathing compressed air (21% oxygen), the partial pressure of oxygen at 30 meters (4 atmospheres total pressure) would be:

    P<sub>O2</sub> = 0.21 * 4 atm = 0.84 atm

    While this level of oxygen is generally safe, exceeding certain partial pressure limits of oxygen (typically around 1.4 atm to 1.6 atm) can lead to oxygen toxicity, causing seizures and potentially drowning.

    Similarly, the partial pressure of nitrogen also increases. At higher partial pressures, nitrogen can have a narcotic effect, impairing judgment and coordination – a condition known as nitrogen narcosis or "rapture of the deep."

    Divers use gas mixtures like Nitrox (enriched oxygen mixes) or Trimix (helium, oxygen, and nitrogen) to manage the partial pressures of oxygen and nitrogen at different depths, mitigating the risks of oxygen toxicity and nitrogen narcosis. By adjusting the percentage of each gas, divers can maintain safe and comfortable breathing conditions.

    3. Collecting Gas Over Water

    A common laboratory technique involves collecting a gas produced in a chemical reaction over water. In this scenario, the collected gas is saturated with water vapor. Therefore, the total pressure of the collected gas is the sum of the partial pressure of the gas you're interested in and the partial pressure of water vapor.

    P<sub>total</sub> = P<sub>gas</sub> + P<sub>H2O</sub>

    The partial pressure of water vapor (also known as the vapor pressure of water) depends on the temperature. You can find the vapor pressure of water at different temperatures in standard reference tables.

    Example:

    Suppose you collect hydrogen gas (H<sub>2</sub>) over water at 25°C. The total pressure of the collected gas is measured to be 750 mmHg. The vapor pressure of water at 25°C is 23.8 mmHg. What is the partial pressure of the hydrogen gas?

    Using Dalton's Law:

    P<sub>total</sub> = P<sub>H2</sub> + P<sub>H2O</sub>

    750 mmHg = P<sub>H2</sub> + 23.8 mmHg

    P<sub>H2</sub> = 750 mmHg - 23.8 mmHg = 726.2 mmHg

    Therefore, the partial pressure of the hydrogen gas is 726.2 mmHg. This value is crucial for accurately calculating the amount of hydrogen gas produced in the reaction using the ideal gas law.

    4. Respiration and Gas Exchange in the Lungs

    Dalton's Law plays a vital role in understanding gas exchange in the lungs. The air in the alveoli (tiny air sacs in the lungs) is a mixture of gases, including oxygen, carbon dioxide, nitrogen, and water vapor. The partial pressures of oxygen and carbon dioxide in the alveoli are different from those in the inhaled air due to gas exchange with the blood.

    • Inhaled Air: As mentioned earlier, the partial pressure of oxygen in inhaled air is approximately 0.21 atm (159.6 mmHg). The partial pressure of carbon dioxide is very low, close to 0 mmHg.
    • Alveolar Air: In the alveoli, oxygen is constantly being absorbed into the blood, and carbon dioxide is being released from the blood. This results in:
      • A lower partial pressure of oxygen (approximately 104 mmHg) compared to inhaled air.
      • A higher partial pressure of carbon dioxide (approximately 40 mmHg) compared to inhaled air.

    The differences in partial pressures drive the diffusion of oxygen from the alveoli into the blood and carbon dioxide from the blood into the alveoli. Oxygen then binds to hemoglobin in red blood cells and is transported to the tissues, while carbon dioxide is exhaled.

    5. Industrial Processes: Gas Mixing and Reactions

    Many industrial processes involve mixing gases to achieve specific compositions for chemical reactions or other applications. Dalton's Law is essential for calculating the required partial pressures of each gas to achieve the desired mixture.

    Example:

    Suppose a chemical company wants to create a gas mixture containing 50% nitrogen, 30% hydrogen, and 20% methane at a total pressure of 10 atm. What should the partial pressures of each gas be?

    Using Dalton's Law and the given percentages:

    • P<sub>N2</sub> = 0.50 * 10 atm = 5 atm
    • P<sub>H2</sub> = 0.30 * 10 atm = 3 atm
    • P<sub>CH4</sub> = 0.20 * 10 atm = 2 atm

    The company would need to carefully control the flow rates of each gas to ensure that the partial pressures match these calculated values. This ensures the correct composition for the intended chemical reaction.

    6. Weather Forecasting and Atmospheric Modeling

    Meteorologists use Dalton's Law in atmospheric models to predict weather patterns. The atmosphere is a complex mixture of gases, and the partial pressure of water vapor plays a crucial role in determining humidity and the likelihood of precipitation.

    • Humidity: Humidity is a measure of the amount of water vapor in the air. The higher the partial pressure of water vapor, the higher the humidity.
    • Dew Point: The dew point is the temperature at which water vapor in the air will condense into liquid water. When the air temperature cools to the dew point, the air becomes saturated with water vapor, and condensation occurs, leading to fog, dew, or clouds.

    By understanding the partial pressure of water vapor and its relationship to temperature and humidity, meteorologists can develop more accurate weather forecasts.

    7. Medical Applications: Blood Gas Analysis

    In medicine, blood gas analysis is a critical diagnostic tool used to assess a patient's respiratory function. Blood gas analyzers measure the partial pressures of oxygen (PaO<sub>2</sub>) and carbon dioxide (PaCO<sub>2</sub>) in arterial blood.

    • PaO<sub>2</sub>: The partial pressure of oxygen in arterial blood indicates how well the lungs are transferring oxygen to the blood. A normal PaO<sub>2</sub> range is typically 80-100 mmHg. Low PaO<sub>2</sub> levels can indicate lung disease, impaired gas exchange, or other respiratory problems.
    • PaCO<sub>2</sub>: The partial pressure of carbon dioxide in arterial blood indicates how well the lungs are removing carbon dioxide from the blood. A normal PaCO<sub>2</sub> range is typically 35-45 mmHg. High PaCO<sub>2</sub> levels can indicate hypoventilation (insufficient breathing), while low PaCO<sub>2</sub> levels can indicate hyperventilation (excessive breathing).

    By analyzing these partial pressures, doctors can diagnose and manage a wide range of respiratory and metabolic disorders.

    8. Altitude and Partial Pressure

    As altitude increases, the total atmospheric pressure decreases. This means that the partial pressure of oxygen also decreases. At high altitudes, the reduced partial pressure of oxygen can lead to altitude sickness, a condition characterized by headache, fatigue, nausea, and shortness of breath.

    For example, at sea level, the partial pressure of oxygen is approximately 159.6 mmHg. At an altitude of 3,000 meters (approximately 10,000 feet), the atmospheric pressure is about 70% of that at sea level. Therefore, the partial pressure of oxygen at 3,000 meters is approximately:

    P<sub>O2</sub> = 0.21 * 0.7 atm = 0.147 atm = 111.7 mmHg

    This significantly lower partial pressure of oxygen makes it more difficult for the body to absorb oxygen, leading to the symptoms of altitude sickness. Acclimatization, or gradual exposure to higher altitudes, allows the body to adapt to the lower oxygen levels by increasing red blood cell production and improving oxygen delivery to the tissues.

    9. Controlled Atmosphere Storage

    In the food industry, controlled atmosphere (CA) storage is used to extend the shelf life of fruits and vegetables. CA storage involves carefully controlling the levels of oxygen, carbon dioxide, and nitrogen in the storage environment. By reducing the oxygen level and increasing the carbon dioxide level, respiration rates are slowed down, delaying ripening and spoilage.

    Dalton's Law is used to calculate and maintain the desired partial pressures of each gas in the storage environment. For example, apples might be stored in an atmosphere containing 3% oxygen and 3% carbon dioxide. This reduces the partial pressure of oxygen, slowing down the ripening process and extending the storage life of the apples.

    10. Leak Testing

    Dalton's Law, while not directly applied, is a principle underpinning leak testing procedures. In leak testing, pressure changes are monitored to detect leaks in sealed systems. When multiple gases are present, the overall pressure drop is reflective of the combined partial pressure changes due to the leaking of the gas mixture. By understanding the composition of the gas mixture, the effects of leaks can be more accurately interpreted.

    Key Takeaways

    • Dalton's Law of Partial Pressures is a fundamental principle for understanding gas mixtures.
    • It states that the total pressure of a gas mixture is equal to the sum of the partial pressures of each individual gas.
    • The law applies to non-reacting gases.
    • It has numerous real-world applications, including air composition, scuba diving, respiration, industrial processes, weather forecasting, and medical diagnostics.
    • Understanding Dalton's Law is crucial for safely and effectively working with gas mixtures in various fields.

    Frequently Asked Questions (FAQ)

    • What happens if the gases in the mixture react? Dalton's Law does not apply if the gases react chemically, as the number of moles of each gas will change.
    • Is Dalton's Law applicable to ideal gases only? Dalton's Law is most accurate for ideal gases, but it provides a good approximation for real gases under normal conditions.
    • How does temperature affect partial pressure? While Dalton's Law itself doesn't explicitly include temperature, the partial pressure of each gas is related to temperature through the ideal gas law (PV = nRT). Therefore, if the temperature changes, the partial pressures will also change proportionally.
    • What are the limitations of Dalton's Law? The main limitation is that it assumes the gases do not react. It also works best at relatively low pressures and high temperatures, where gases behave more ideally.
    • How is Dalton's Law used in anesthesia? Anesthesiologists use Dalton's Law to calculate the partial pressures of anesthetic gases in a patient's breathing mixture. This ensures that the patient receives the correct dose of anesthetic to maintain unconsciousness and pain relief during surgery.

    Conclusion

    Dalton's Law of Partial Pressures is a cornerstone of gas behavior understanding. From the air we breathe to the complex mixtures used in industrial processes and medical treatments, its applications are vast and impactful. By grasping the core principles and exploring the diverse examples, we can appreciate the power and relevance of this seemingly simple yet profound scientific law. Its continued use across diverse fields underscores its importance in both theoretical understanding and practical application.

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