Boyle's, Dalton's, and Henry's Laws
Boyle's Law: The Relationship Between Pressure and Volume
Boyle's Law defines the relationship between gas pressure and volume when temperature is held constant.
Mathematical Expression: The law is expressed as .
: Initial pressure
: Initial volume
: Secondary pressure
: Secondary volume
Inverse Proportionality: Pressure varies inversely with volume.
If the volume of a container decreases, the pressure must increase to maintain the equality.
If the volume of a container increases, the pressure must decrease.
Kinetic Molecular Explanation:
At a given temperature, molecules possess a specific amount of kinetic energy and collide with the walls of their container.
In a smaller volume with a fixed number of molecules, the molecules collide with the container walls more frequently.
More collisions result in higher pressure.
Example: A container with three molecules at a constant temperature will exert more pressure if the volume is reduced because the molecules hit the walls more often.
Dalton's Law of Partial Pressures
Memory Trick: Use the full name "Dalton's Law of Partial Pressures" to distinguish it from other gas laws.
Principle of Partial Pressure: In a mixture of different gas species (e.g., Nitrogen (), Oxygen (), and Carbon Dioxide ()), each gas exerts its own pressure against the walls of the container.
Proportionality: The partial pressure of a specific gas is directly proportional to the percentage of that gas in the total mixture.
Calculation Example (6 Torr Container):
Total Pressure:
Composition: 3 molecules of , 1 molecule of , 2 molecules of .
Partial Pressure of Nitrogen (): Since makes up half of the molecules, it is responsible for half the pressure: .
Partial Pressure of Oxygen (): Since there is only one Oxygen molecule out of six, it contributes one-sixth: .
Partial Pressure of Carbon Dioxide (): Since there are two molecules of , its contribution is .
Total Pressure (): .
Atmospheric Gas Composition and Partial Pressures
The total atmospheric pressure is defined as .
Nitrogen ():
Percentage of atmosphere:
Calculation:
Nitrogen accounts for the vast majority of atmospheric pressure.
Oxygen ():
Percentage of atmosphere: approximately (specifically
Calculation:
Carbon Dioxide ():
Percentage of atmosphere:
Note: CO2 levels are very low, which is why small changes in CO2 emissions can dramatically affect atmospheric dynamics and global warming.
Partial Pressure: approximately
Water Vapor ():
Percentage of atmosphere: approximately (variable based on humidity)
Partial Pressure: approximately
Mental Calculation Techniques for Exams
To calculate partial pressures without a calculator based on a total pressure of :
1% Baseline: of is .
0.5% Threshold: Half of () is .
0.05% Threshold: One-tenth of () is .
Application to CO2: Since atmospheric is , which is slightly less than , the partial pressure is slightly less than (textbook value is ).
Application to Water Vapor: At , it is slightly less than the value (), resulting in the textbook value of .
Henry's Law of Solubility
Henry's Law of Solubility states that a gas will dissolve into a liquid (like blood plasma) in proportion to its partial pressure.
Mechanism of Movement:
Molecules move down their partial pressure gradients (from high partial pressure to low partial pressure).
Gases move between the alveoli and the bloodstream (external respiratory membrane) and between the blood and tissues (internal respiratory membrane) based on these gradients.
Fluids include both gases and liquids; gases can move into liquids, and molecules can move out of liquids back into the air.
Gas Solubility Rules and Physiological Factors
While Henry's Law dictates the pressure gradient, the actual amount of gas that dissolves is heavily influenced by specific solubility rules:
Nitrogen Solubility: Nitrogen is only half () as soluble as Oxygen in water/blood. Despite its high partial pressure, it is "hardly soluble at all" compared to other gases.
Oxygen Solubility: Oxygen is only one-twentieth () as soluble as Carbon Dioxide. Its solubility in blood is significantly enhanced by the protein hemoglobin.
Carbon Dioxide Solubility: is extremely soluble in the blood (forty times () more soluble than Nitrogen). This high solubility allows the body to retain and maintain necessary acidity levels, rather than losing it all to the atmosphere.
Nitrogen Absence in Blood: Because nitrogen lacks a specialized carrier like hemoglobin and has very low solubility, it does not dissolve well into the bloodstream despite its massive gradient in atmospheric air.
Chemical Reactivity: Carbon dioxide's high solubility is further explained by its tendency to react with water, forming a chemical equation that will be explored in later sections.