Problem 149
Question
One method of preparing elemental mercury involves roasting cinnabar (HgS) in quicklime (CaO) at 600.^ C followed by condensation of the mercury vapor. Given the heat of vaporization of mercury (296 J/g) and the vapor pressure of mercury at \(25.0^{\circ} \mathrm{C}\left(2.56 \times 10^{-3} \text {torr }\right),\) what is the vapor pressure of the condensed mercury at \(300 .^{\circ} \mathrm{C} ?\) How many atoms of mercury are present in the mercury vapor at \(300 .^{\circ} \mathrm{C}\) if the reaction is conducted in a closed 15.0 -L container?
Step-by-Step Solution
Verified Answer
The vapor pressure of the condensed mercury at 300°C is 171.27 torr. There are 3.27 x 10²² atoms of mercury in the vapor phase at 300°C in a 15.0-L container.
1Step 1: Convert temperatures to Kelvin
We need to work with temperatures in Kelvin for these calculations. To do this, add 273.15 to the Celsius temperature:
Temperature 1 (T₁):
25.0°C + 273.15 = 298.15 K
Temperature 2 (T₂):
300.0°C + 273.15 = 573.15 K
2Step 2: Use the Clausius-Clapeyron equation
The Clausius-Clapeyron equation relates the vapor pressure, temperature, and heat of vaporization of a substance:
\( \ln\left(\frac{P_2}{P_1}\right) = \frac{-\Delta H_\text{vap}}{R} \left( \frac{1}{T_2} - \frac{1}{T_1} \right) \)
where \(P_1\) is the initial vapor pressure (2.56 x 10⁻³ torr), \(P_2\) is the final vapor pressure, \( \Delta H_\text{vap}\) is the heat of vaporization (296 J/g), R is the ideal gas constant (8.314 J/mol K), T₁ is the initial temperature (298.15 K), and T₂ is the final temperature (573.15 K). We will solve for \(P_2\).
3Step 3: Calculate the vapor pressure at 300°C
Rearrange the Clausius-Clapeyron equation to solve for \(P_2\):
\( P_2 = P_1 \cdot \exp\left( \frac{-\Delta H_\text{vap}}{R} \left( \frac{1}{T_2} - \frac{1}{T_1} \right) \right) \)
Plug in the given values and calculate the vapor pressure at 300°C:
\( P_2 = (2.56 \times 10^{-3}\, \text{torr}) \exp\left( \frac{-(296\,\text{J/g})}{(8.314\, \text{J/mol K})} \left( \frac{1}{573.15\, \text{K}} - \frac{1}{298.15\, \text{K}} \right) \right) \)
\( P_2 = 171.27\, \text{torr} \)
The vapor pressure of the condensed mercury at 300°C is 171.27 torr.
4Step 4: Use the ideal gas law
Now, we will use the ideal gas law to find the number of atoms in the vapor phase in a 15.0-L container:
\(P * V = n * R * T\)
where P is the pressure, V is the volume, n is the number of moles, R is the ideal gas constant, and T is the temperature.
First, convert the pressure to atm and R = (0.0821 L atm/mol K):
\(P_{\text{atm}} = \frac{171.27\, \text{torr}}{760\, \text{torr/atm}} = 0.2253\, \text{atm}\)
Next, plug in the values, and solve for the number of moles (n):
\(n = \frac{P * V}{R * T} = \frac{0.2253\, \text{atm} * 15.0\, \text{L}}{0.0821\, \text{L atm/mol K} * 573.15\, \text{K}}\)
\(n = 0.0544\, \text{moles} \)
5Step 5: Determine the number of atoms
To find the number of atoms, multiply the number of moles by Avogadro's number (6.022 x 10²³ atoms per mole):
Number of Mercury atoms = 0.0544 moles * 6.022 x 10²³ atoms/mol = 3.27 x 10²² atoms
There are 3.27 x 10²² atoms of mercury in the vapor phase at 300°C in a 15.0-L container.
Key Concepts
Clausius-Clapeyron EquationHeat of VaporizationIdeal Gas LawAvogadro's NumberVapor Pressure
Clausius-Clapeyron Equation
The Clausius-Clapeyron equation is a vital formula in thermodynamics that describes the relationship between the vapor pressure and temperature of a substance. It illustrates how vapor pressure increases with temperature for a given substance. Specifically, it connects the change in vapor pressure due to a change in temperature to the substance's heat of vaporization.
Mathematically, the equation is expressed as:
\[ \ln\left(\frac{P_2}{P_1}\right) = \frac{-\Delta H_{\text{vap}}}{R} \left( \frac{1}{T_2} - \frac{1}{T_1} \right) \]
where \(P_1\) and \(P_2\) are the initial and final vapor pressures, \(\Delta H_{\text{vap}}\) is the heat of vaporization, R is the ideal gas constant, and \(T_1\) and \(T_2\) are the initial and final temperatures in Kelvin. This formula can predict the vapor pressure at a new temperature if the vapor pressure is known at some initial condition, making it invaluable in many fields including meteorology, engineering, and material science.
Mathematically, the equation is expressed as:
\[ \ln\left(\frac{P_2}{P_1}\right) = \frac{-\Delta H_{\text{vap}}}{R} \left( \frac{1}{T_2} - \frac{1}{T_1} \right) \]
where \(P_1\) and \(P_2\) are the initial and final vapor pressures, \(\Delta H_{\text{vap}}\) is the heat of vaporization, R is the ideal gas constant, and \(T_1\) and \(T_2\) are the initial and final temperatures in Kelvin. This formula can predict the vapor pressure at a new temperature if the vapor pressure is known at some initial condition, making it invaluable in many fields including meteorology, engineering, and material science.
Heat of Vaporization
The heat of vaporization, represented by \(\Delta H_{\text{vap}}\), is the amount of energy required to convert one gram of a liquid into vapor without a change in temperature. It represents the strength of intermolecular forces within the liquid; a higher heat of vaporization indicates stronger forces that must be overcome.
For instance, mercury has a heat of vaporization of 296 joules per gram, which is a measure of the energy needed to overcome the forces holding mercury atoms together in the liquid phase. This property is crucial in calculations involving phase changes, such as converting liquid mercury to gaseous mercury, and ties directly into the Clausius-Clapeyron equation for determining vapor pressure changes.
For instance, mercury has a heat of vaporization of 296 joules per gram, which is a measure of the energy needed to overcome the forces holding mercury atoms together in the liquid phase. This property is crucial in calculations involving phase changes, such as converting liquid mercury to gaseous mercury, and ties directly into the Clausius-Clapeyron equation for determining vapor pressure changes.
Ideal Gas Law
The ideal gas law is a cornerstone in the study of gases, connecting pressure, volume, temperature, and the amount of gas present. Given by the equation:
\[ P * V = n * R * T \]
it allows us to calculate any one of these variables if the others are known. Here, P is the pressure of the gas, V is the volume it occupies, n is the number of moles of gas, R is the universal gas constant (with a value of 8.314 J/mol·K in SI units or 0.0821 L·atm/mol·K for calculations involving liters and atmospheres), and T is the temperature in Kelvin.
In the context of mercury vapor pressure, once the vapor pressure at a certain temperature is determined using the Clausius-Clapeyron equation, the ideal gas law can then be used to find out how many moles of gaseous mercury are present in a certain volume at that temperature.
\[ P * V = n * R * T \]
it allows us to calculate any one of these variables if the others are known. Here, P is the pressure of the gas, V is the volume it occupies, n is the number of moles of gas, R is the universal gas constant (with a value of 8.314 J/mol·K in SI units or 0.0821 L·atm/mol·K for calculations involving liters and atmospheres), and T is the temperature in Kelvin.
In the context of mercury vapor pressure, once the vapor pressure at a certain temperature is determined using the Clausius-Clapeyron equation, the ideal gas law can then be used to find out how many moles of gaseous mercury are present in a certain volume at that temperature.
Avogadro's Number
Avogadro's number, approximately \(6.022 \times 10^{23}\), represents the quantity of particles, typically atoms or molecules, in one mole of a substance. It's a fundamental constant that provides a link between the microscopic world of atoms and the macroscopic world of grams and liters that we interact with daily.
Understanding Avogadro's number is essential when transitioning from the amount of a substance in moles to the actual number of atoms or molecules present. This conversion is particularly crucial when quantifying the number of mercury atoms present in the vapor phase after evaporation, as demonstrated in the mercury vapor pressure calculation.
Understanding Avogadro's number is essential when transitioning from the amount of a substance in moles to the actual number of atoms or molecules present. This conversion is particularly crucial when quantifying the number of mercury atoms present in the vapor phase after evaporation, as demonstrated in the mercury vapor pressure calculation.
Vapor Pressure
Vapor pressure is the pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases (solid or liquid) at a given temperature in a closed system. It is a specific form of pressure unique to each substance and varies with temperature. A higher temperature usually results in a higher vapor pressure, as more molecules have enough kinetic energy to escape from the liquid or solid phase into the gas phase.
By understanding the vapor pressure, we gain insights into a substance's volatility and how readily it will evaporate. For mercury, knowledge of its vapor pressure at various temperatures allows for safe handling and use in applications, such as in thermometers or fluorescent lamps, where mercury's vapor state is utilized.
By understanding the vapor pressure, we gain insights into a substance's volatility and how readily it will evaporate. For mercury, knowledge of its vapor pressure at various temperatures allows for safe handling and use in applications, such as in thermometers or fluorescent lamps, where mercury's vapor state is utilized.
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