Chemistry: Atoms First 2e

# 8.3Stoichiometry of Gaseous Substances, Mixtures, and Reactions

Chemistry: Atoms First 2e8.3 Stoichiometry of Gaseous Substances, Mixtures, and Reactions
By the end of this section, you will be able to:
• Use the ideal gas law to compute gas densities and molar masses
• Perform stoichiometric calculations involving gaseous substances
• State Dalton’s law of partial pressures and use it in calculations involving gaseous mixtures

The study of the chemical behavior of gases was part of the basis of perhaps the most fundamental chemical revolution in history. French nobleman Antoine Lavoisier, widely regarded as the “father of modern chemistry,” changed chemistry from a qualitative to a quantitative science through his work with gases. He discovered the law of conservation of matter, discovered the role of oxygen in combustion reactions, determined the composition of air, explained respiration in terms of chemical reactions, and more. He was a casualty of the French Revolution, guillotined in 1794. Of his death, mathematician and astronomer Joseph-Louis Lagrange said, “It took the mob only a moment to remove his head; a century will not suffice to reproduce it.”2

As described in an earlier chapter of this text, we can turn to chemical stoichiometry for answers to many of the questions that ask “How much?” The essential property involved in such use of stoichiometry is the amount of substance, typically measured in moles (n). For gases, molar amount can be derived from convenient experimental measurements of pressure, temperature, and volume. Therefore, these measurements are useful in assessing the stoichiometry of pure gases, gas mixtures, and chemical reactions involving gases. This section will not introduce any new material or ideas, but will provide examples of applications and ways to integrate concepts we have already discussed.

### Gas Density and Molar Mass

The ideal gas law described previously in this chapter relates the properties of pressure P, volume V, temperature T, and molar amount n. This law is universal, relating these properties in identical fashion regardless of the chemical identity of the gas:

$PV=nRT PV=nRT$

The density d of a gas, on the other hand, is determined by its identity. As described in another chapter of this text, the density of a substance is a characteristic property that may be used to identify the substance.

$d= m V d= m V$

Rearranging the ideal gas equation to isolate V and substituting into the density equation yields

$d= mP nRT =( m n ) P RT d= mP nRT =( m n ) P RT$

The ratio m/n is the definition of molar mass, :

$ℳ= m n ℳ= m n$

The density equation can then be written

$d= ℳP RT d= ℳP RT$

This relation may be used for calculating the densities of gases of known identities at specified values of pressure and temperature as demonstrated in Example 8.11.

### Example 8.11

Measuring Gas Density What is the density of molecular nitrogen gas at STP?

Solution The molar mass of molecular nitrogen, N2, is 28.01 g/mol. Substituting this value along with standard temperature and pressure into the gas density equation yields

$d= ℳP RT = (28.01g/mol)(1.00atm) (0.0821Latm mol −1 K −1 )(273K) =1.25g/L d= ℳP RT = (28.01g/mol)(1.00atm) (0.0821Latm mol −1 K −1 )(273K) =1.25g/L$

Check Your Learning What is the density of molecular hydrogen gas at 17.0 °C and a pressure of 760 torr?

d = 0.0847 g/L

When the identity of a gas is unknown, measurements of the mass, pressure, volume, and temperature of a sample can be used to calculate the molar mass of the gas (a useful property for identification purposes). Combining the ideal gas equation

$PV=nRT PV=nRT$

and the definition of molarity

$ℳ= m n ℳ= m n$

yields the following equation:

$ℳ= mRT PV ℳ= mRT PV$

Determining the molar mass of a gas via this approach is demonstrated in Example 8.12.

### Example 8.12

Determining the Molecular Formula of a Gas from its Molar Mass and Empirical Formula Cyclopropane, a gas once used with oxygen as a general anesthetic, is composed of 85.7% carbon and 14.3% hydrogen by mass. Find the empirical formula. If 1.56 g of cyclopropane occupies a volume of 1.00 L at 0.984 atm and 50 °C, what is the molecular formula for cyclopropane?

Solution First determine the empirical formula of the gas. Assume 100 g and convert the percentage of each element into grams. Determine the number of moles of carbon and hydrogen in the 100-g sample of cyclopropane. Divide by the smallest number of moles to relate the number of moles of carbon to the number of moles of hydrogen. In the last step, realize that the smallest whole number ratio is the empirical formula:

$85.7 g C×1 mol C12.01 g C=7.136 mol C7.1367.136=1.00 mol C85.7 g C×1 mol C12.01 g C=7.136 mol C7.1367.136=1.00 mol C$
$14.3 g H×1 mol H1.01 g H=14.158 mol H14.1587.136=1.98 mol H14.3 g H×1 mol H1.01 g H=14.158 mol H14.1587.136=1.98 mol H$

Empirical formula is CH2 [empirical mass (EM) of 14.03 g/empirical unit].

Next, use the provided values for mass, pressure, temperature and volume to compute the molar mass of the gas:

$ℳ= mRT PV = (1.56g)(0.0821Latm mol −1 K −1 )(323K) (0.984atm)(1.00L) =42.0g/mol ℳ= mRT PV = (1.56g)(0.0821Latm mol −1 K −1 )(323K) (0.984atm)(1.00L) =42.0g/mol$

Comparing the molar mass to the empirical formula mass shows how many empirical formula units make up a molecule:

$ℳ EM = 42.0g/mol 14.0g/mol =3 ℳ EM = 42.0g/mol 14.0g/mol =3$

The molecular formula is thus derived from the empirical formula by multiplying each of its subscripts by three:

$( CH 2 ) 3 = C 3 H 6 ( CH 2 ) 3 = C 3 H 6$

Check Your LearningAcetylene, a fuel used welding torches, is composed of 92.3% C and 7.7% H by mass. Find the empirical formula. If 1.10 g of acetylene occupies of volume of 1.00 L at 1.15 atm and 59.5 °C, what is the molecular formula for acetylene?

Empirical formula, CH; Molecular formula, C2H2

### Example 8.13

Determining the Molar Mass of a Volatile Liquid The approximate molar mass of a volatile liquid can be determined by:

1. Heating a sample of the liquid in a flask with a tiny hole at the top, which converts the liquid into gas that may escape through the hole
2. Removing the flask from heat at the instant when the last bit of liquid becomes gas, at which time the flask will be filled with only gaseous sample at ambient pressure
3. Sealing the flask and permitting the gaseous sample to condense to liquid, and then weighing the flask to determine the sample’s mass (see Figure 8.19)
Figure 8.19 When the volatile liquid in the flask is heated past its boiling point, it becomes gas and drives air out of the flask. At $tl⟶g,tl⟶g,$ the flask is filled with volatile liquid gas at the same pressure as the atmosphere. If the flask is then cooled to room temperature, the gas condenses and the mass of the gas that filled the flask, and is now liquid, can be measured. (credit: modification of work by Mark Ott)

Using this procedure, a sample of chloroform gas weighing 0.494 g is collected in a flask with a volume of 129 cm3 at 99.6 °C when the atmospheric pressure is 742.1 mm Hg. What is the approximate molar mass of chloroform?

Solution Since $ℳ=mnℳ=mn$ and $n=PVRT,n=PVRT,$ substituting and rearranging gives $ℳ=mRTPV,ℳ=mRTPV,$

then

$ℳ=mRTPV=(0.494 g)×0.08206 L·atm/mol K×372.8 K0.976 atm×0.129 L=120g/mol.ℳ=mRTPV=(0.494 g)×0.08206 L·atm/mol K×372.8 K0.976 atm×0.129 L=120g/mol.$

Check Your Learning A sample of phosphorus that weighs 3.243 $××$ 10−2 g exerts a pressure of 31.89 kPa in a 56.0-mL bulb at 550 °C. What are the molar mass and molecular formula of phosphorus vapor?

124 g/mol P4

### The Pressure of a Mixture of Gases: Dalton’s Law

Unless they chemically react with each other, the individual gases in a mixture of gases do not affect each other’s pressure. Each individual gas in a mixture exerts the same pressure that it would exert if it were present alone in the container (Figure 8.20). The pressure exerted by each individual gas in a mixture is called its partial pressure. This observation is summarized by Dalton’s law of partial pressures: The total pressure of a mixture of ideal gases is equal to the sum of the partial pressures of the component gases:

$PTotal=PA+PB+PC+...=ΣiPiPTotal=PA+PB+PC+...=ΣiPi$

In the equation PTotal is the total pressure of a mixture of gases, PA is the partial pressure of gas A; PB is the partial pressure of gas B; PC is the partial pressure of gas C; and so on.

Figure 8.20 If equal-volume cylinders containing gas A at a pressure of 300 kPa, gas B at a pressure of 600 kPa, and gas C at a pressure of 450 kPa are all combined in the same-size cylinder, the total pressure of the mixture is 1350 kPa.

The partial pressure of gas A is related to the total pressure of the gas mixture via its mole fraction (X), a unit of concentration defined as the number of moles of a component of a solution divided by the total number of moles of all components:

$PA=XA×PTotalwhereXA=nAnTotalPA=XA×PTotalwhereXA=nAnTotal$

where PA, XA, and nA are the partial pressure, mole fraction, and number of moles of gas A, respectively, and nTotal is the number of moles of all components in the mixture.

### Example 8.14

The Pressure of a Mixture of Gases A 10.0-L vessel contains 2.50 $××$ 10−3 mol of H2, 1.00 $××$ 10−3 mol of He, and 3.00 $××$ 10−4 mol of Ne at 35 °C.

(a) What are the partial pressures of each of the gases?

(b) What is the total pressure in atmospheres?

SolutionThe gases behave independently, so the partial pressure of each gas can be determined from the ideal gas equation, using $P=nRTVP=nRTV$:

$PH2=(2.50×10−3mol)(0.08206Latmmol−1K−1)(308K)10.0L=6.32×10−3atmPH2=(2.50×10−3mol)(0.08206Latmmol−1K−1)(308K)10.0L=6.32×10−3atm$
$PHe=(1.00×10−3mol)(0.08206Latmmol−1K−1)(308K)10.0L=2.53×10−3atmPHe=(1.00×10−3mol)(0.08206Latmmol−1K−1)(308K)10.0L=2.53×10−3atm$
$PNe=(3.00×10−4mol)(0.08206Latmmol−1K−1)(308K)10.0L=7.58×10−4atmPNe=(3.00×10−4mol)(0.08206Latmmol−1K−1)(308K)10.0L=7.58×10−4atm$

The total pressure is given by the sum of the partial pressures:

$PT=PH2+PHe+PNe=(0.00632+0.00253+0.00076)atm=9.61×10−3atmPT=PH2+PHe+PNe=(0.00632+0.00253+0.00076)atm=9.61×10−3atm$

Check Your Learning A 5.73-L flask at 25 °C contains 0.0388 mol of N2, 0.147 mol of CO, and 0.0803 mol of H2. What is the total pressure in the flask in atmospheres?

1.137 atm

Here is another example of this concept, but dealing with mole fraction calculations.

### Example 8.15

The Pressure of a Mixture of Gases A gas mixture used for anesthesia contains 2.83 mol oxygen, O2, and 8.41 mol nitrous oxide, N2O. The total pressure of the mixture is 192 kPa.

(a) What are the mole fractions of O2 and N2O?

(b) What are the partial pressures of O2 and N2O?

Solution The mole fraction is given by $XA=nAnTotalXA=nAnTotal$ and the partial pressure is PA = XA $××$ PTotal.

For O2,

$XO2=nO2nTotal=2.83 mol(2.83+8.41)mol=0.252XO2=nO2nTotal=2.83 mol(2.83+8.41)mol=0.252$

and $PO2=XO2×PTotal=0.252×192 kPa=48.4 kPaPO2=XO2×PTotal=0.252×192 kPa=48.4 kPa$

For N2O,

$XN2=nN2nTotal=8.41 mol(2.83+8.41)mol=0.748XN2=nN2nTotal=8.41 mol(2.83+8.41)mol=0.748$

and

$PN2=XN2×PTotal=0.748×192 kPa=143.6 kPaPN2=XN2×PTotal=0.748×192 kPa=143.6 kPa$

Check Your Learning What is the pressure of a mixture of 0.200 g of H2, 1.00 g of N2, and 0.820 g of Ar in a container with a volume of 2.00 L at 20 °C?

1.87 atm

### Collection of Gases over Water

A simple way to collect gases that do not react with water is to capture them in a bottle that has been filled with water and inverted into a dish filled with water. The pressure of the gas inside the bottle can be made equal to the air pressure outside by raising or lowering the bottle. When the water level is the same both inside and outside the bottle (Figure 8.21), the pressure of the gas is equal to the atmospheric pressure, which can be measured with a barometer.

Figure 8.21 When a reaction produces a gas that is collected above water, the trapped gas is a mixture of the gas produced by the reaction and water vapor. If the collection flask is appropriately positioned to equalize the water levels both within and outside the flask, the pressure of the trapped gas mixture will equal the atmospheric pressure outside the flask (see the earlier discussion of manometers).

However, there is another factor we must consider when we measure the pressure of the gas by this method. Water evaporates and there is always gaseous water (water vapor) above a sample of liquid water. As a gas is collected over water, it becomes saturated with water vapor and the total pressure of the mixture equals the partial pressure of the gas plus the partial pressure of the water vapor. The pressure of the pure gas is therefore equal to the total pressure minus the pressure of the water vapor—this is referred to as the “dry” gas pressure, that is, the pressure of the gas only, without water vapor. The vapor pressure of water, which is the pressure exerted by water vapor in equilibrium with liquid water in a closed container, depends on the temperature (Figure 8.22); more detailed information on the temperature dependence of water vapor can be found in Table 8.2, and vapor pressure will be discussed in more detail in the chapter on liquids.

Figure 8.22 This graph shows the vapor pressure of water at sea level as a function of temperature.
Vapor Pressure of Ice and Water in Various Temperatures at Sea Level
Temperature (°C) Pressure (torr) Temperature (°C) Pressure (torr) Temperature (°C) Pressure (torr)
–10 1.95 18 15.5 30 31.8
–5 3.0 19 16.5 35 42.2
–2 3.9 20 17.5 40 55.3
0 4.6 21 18.7 50 92.5
2 5.3 22 19.8 60 149.4
4 6.1 23 21.1 70 233.7
6 7.0 24 22.4 80 355.1
8 8.0 25 23.8 90 525.8
10 9.2 26 25.2 95 633.9
12 10.5 27 26.7 99 733.2
14 12.0 28 28.3 100.0 760.0
16 13.6 29 30.0 101.0 787.6
Table 8.2

### Example 8.16

Pressure of a Gas Collected Over Water If 0.200 L of argon is collected over water at a temperature of 26 °C and a pressure of 750 torr in a system like that shown in Figure 8.21, what is the partial pressure of argon?

Solution According to Dalton’s law, the total pressure in the bottle (750 torr) is the sum of the partial pressure of argon and the partial pressure of gaseous water:

$PT=PAr+PH2OPT=PAr+PH2O$

Rearranging this equation to solve for the pressure of argon gives:

$PAr=PT−PH2OPAr=PT−PH2O$

The pressure of water vapor above a sample of liquid water at 26 °C is 25.2 torr (Appendix E), so:

$PAr=750torr−25.2torr=725torrPAr=750torr−25.2torr=725torr$

Check Your Learning A sample of oxygen collected over water at a temperature of 29.0 °C and a pressure of 764 torr has a volume of 0.560 L. What volume would the dry oxygen have under the same conditions of temperature and pressure?

0.583 L

### Chemical Stoichiometry and Gases

Chemical stoichiometry describes the quantitative relationships between reactants and products in chemical reactions.

We have previously measured quantities of reactants and products using masses for solids and volumes in conjunction with the molarity for solutions; now we can also use gas volumes to indicate quantities. If we know the volume, pressure, and temperature of a gas, we can use the ideal gas equation to calculate how many moles of the gas are present. If we know how many moles of a gas are involved, we can calculate the volume of a gas at any temperature and pressure.

Sometimes we can take advantage of a simplifying feature of the stoichiometry of gases that solids and solutions do not exhibit: All gases that show ideal behavior contain the same number of molecules in the same volume (at the same temperature and pressure). Thus, the ratios of volumes of gases involved in a chemical reaction are given by the coefficients in the equation for the reaction, provided that the gas volumes are measured at the same temperature and pressure.

We can extend Avogadro’s law (that the volume of a gas is directly proportional to the number of moles of the gas) to chemical reactions with gases: Gases combine, or react, in definite and simple proportions by volume, provided that all gas volumes are measured at the same temperature and pressure. For example, since nitrogen and hydrogen gases react to produce ammonia gas according to $N2(g)+3H2(g)⟶2NH3(g),N2(g)+3H2(g)⟶2NH3(g),$ a given volume of nitrogen gas reacts with three times that volume of hydrogen gas to produce two times that volume of ammonia gas, if pressure and temperature remain constant.

The explanation for this is illustrated in Figure 8.23. According to Avogadro’s law, equal volumes of gaseous N2, H2, and NH3, at the same temperature and pressure, contain the same number of molecules. Because one molecule of N2 reacts with three molecules of H2 to produce two molecules of NH3, the volume of H2 required is three times the volume of N2, and the volume of NH3 produced is two times the volume of N2.

Figure 8.23 One volume of N2 combines with three volumes of H2 to form two volumes of NH3.

### Example 8.17

Reaction of Gases Propane, C3H8(g), is used in gas grills to provide the heat for cooking. What volume of O2(g) measured at 25 °C and 760 torr is required to react with 2.7 L of propane measured under the same conditions of temperature and pressure? Assume that the propane undergoes complete combustion.

Solution The ratio of the volumes of C3H8 and O2 will be equal to the ratio of their coefficients in the balanced equation for the reaction:

$C3H8(g)+5O2(g) ⟶ 3CO2(g)+4H2O(l)1 volume+5 volumes3 volumes+4 volumesC3H8(g)+5O2(g) ⟶ 3CO2(g)+4H2O(l)1 volume+5 volumes3 volumes+4 volumes$

From the equation, we see that one volume of C3H8 will react with five volumes of O2:

$2.7LC3H8×5 LO21LC3H8=13.5 LO22.7LC3H8×5 LO21LC3H8=13.5 LO2$

A volume of 13.5 L of O2 will be required to react with 2.7 L of C3H8.

Check Your Learning An acetylene tank for an oxyacetylene welding torch provides 9340 L of acetylene gas, C2H2, at 0 °C and 1 atm. How many tanks of oxygen, each providing 7.00 $××$ 103 L of O2 at 0 °C and 1 atm, will be required to burn the acetylene?

$2C2H2+5O2⟶4CO2+2H2O2C2H2+5O2⟶4CO2+2H2O$

3.34 tanks (2.34 $××$ 104 L)

### Example 8.18

Volumes of Reacting Gases Ammonia is an important fertilizer and industrial chemical. Suppose that a volume of 683 billion cubic feet of gaseous ammonia, measured at 25 °C and 1 atm, was manufactured. What volume of H2(g), measured under the same conditions, was required to prepare this amount of ammonia by reaction with N2?

$N2(g)+3H2(g)⟶2NH3(g)N2(g)+3H2(g)⟶2NH3(g)$

Solution Because equal volumes of H2 and NH3 contain equal numbers of molecules and each three molecules of H2 that react produce two molecules of NH3, the ratio of the volumes of H2 and NH3 will be equal to 3:2. Two volumes of NH3, in this case in units of billion ft3, will be formed from three volumes of H2:

$683billionft3NH3×3 billionft3H22billionft3NH3=1.02×103billionft3H2683billionft3NH3×3 billionft3H22billionft3NH3=1.02×103billionft3H2$

The manufacture of 683 billion ft3 of NH3 required 1020 billion ft3 of H2. (At 25 °C and 1 atm, this is the volume of a cube with an edge length of approximately 1.9 miles.)

Check Your Learning What volume of O2(g) measured at 25 °C and 760 torr is required to react with 17.0 L of ethylene, C2H4(g), measured under the same conditions of temperature and pressure? The products are CO2 and water vapor.

51.0 L

### Example 8.19

Volume of Gaseous Product What volume of hydrogen at 27 °C and 723 torr may be prepared by the reaction of 8.88 g of gallium with an excess of hydrochloric acid?

$2Ga(s)+6HCl(aq)⟶2GaCl3(aq)+3H2(g)2Ga(s)+6HCl(aq)⟶2GaCl3(aq)+3H2(g)$

Solution

Convert the provided mass of the limiting reactant, Ga, to moles of hydrogen produced:

$8.88g Ga×1mol Ga69.723g Ga×3 molH22mol Ga=0.191mol H28.88g Ga×1mol Ga69.723g Ga×3 molH22mol Ga=0.191mol H2$

Convert the provided temperature and pressure values to appropriate units (K and atm, respectively), and then use the molar amount of hydrogen gas and the ideal gas equation to calculate the volume of gas:

$V=(nRTP)=0.191mol×0.08206 Latmmol−1K−1×300 K0.951atm=4.94 LV=(nRTP)=0.191mol×0.08206 Latmmol−1K−1×300 K0.951atm=4.94 L$

Check Your Learning Sulfur dioxide is an intermediate in the preparation of sulfuric acid. What volume of SO2 at 343 °C and 1.21 atm is produced by burning l.00 kg of sulfur in excess oxygen?

1.30 $××$ 103 L

### How Sciences Interconnect

#### Greenhouse Gases and Climate Change

The thin skin of our atmosphere keeps the earth from being an ice planet and makes it habitable. In fact, this is due to less than 0.5% of the air molecules. Of the energy from the sun that reaches the earth, almost $1313$ is reflected back into space, with the rest absorbed by the atmosphere and the surface of the earth. Some of the energy that the earth absorbs is re-emitted as infrared (IR) radiation, a portion of which passes back out through the atmosphere into space. Most of this IR radiation, however, is absorbed by certain atmospheric gases, effectively trapping heat within the atmosphere in a phenomenon known as the greenhouse effect. This effect maintains global temperatures within the range needed to sustain life on earth. Without our atmosphere, the earth's average temperature would be lower by more than 30 °C (nearly 60 °F). The major greenhouse gases (GHGs) are water vapor, carbon dioxide, methane, and ozone. Since the Industrial Revolution, human activity has been increasing the concentrations of GHGs, which have changed the energy balance and are significantly altering the earth’s climate (Figure 8.24).

Figure 8.24 Greenhouse gases trap enough of the sun’s energy to make the planet habitable—this is known as the greenhouse effect. Human activities are increasing greenhouse gas levels, warming the planet and causing more extreme weather events.

There is strong evidence from multiple sources that higher atmospheric levels of CO2 are caused by human activity, with fossil fuel burning accounting for about $3434$ of the recent increase in CO2. Reliable data from ice cores reveals that CO2 concentration in the atmosphere is at the highest level in the past 800,000 years; other evidence indicates that it may be at its highest level in 20 million years. In recent years, the CO2 concentration has increased from preindustrial levels of ~280 ppm to more than 400 ppm today (Figure 8.25).

Figure 8.25 CO2 levels over the past 700,000 years were typically from 200–300 ppm, with a steep, unprecedented increase over the past 50 years.

### Portrait of a Chemist

#### Susan Solomon

Atmospheric and climate scientist Susan Solomon (Figure 8.26) is the author of one of The New York Times books of the year (The Coldest March, 2001), one of Time magazine’s 100 most influential people in the world (2008), and a working group leader of the Intergovernmental Panel on Climate Change (IPCC), which was the recipient of the 2007 Nobel Peace Prize. She helped determine and explain the cause of the formation of the ozone hole over Antarctica, and has authored many important papers on climate change. She has been awarded the top scientific honors in the US and France (the National Medal of Science and the Grande Medaille, respectively), and is a member of the National Academy of Sciences, the Royal Society, the French Academy of Sciences, and the European Academy of Sciences. Formerly a professor at the University of Colorado, she is now at MIT, and continues to work at NOAA.

Figure 8.26 Susan Solomon’s research focuses on climate change and has been instrumental in determining the cause of the ozone hole over Antarctica. (credit: National Oceanic and Atmospheric Administration)

### Footnotes

• 2 “Quotations by Joseph-Louis Lagrange,” last modified February 2006, accessed February 10, 2015, http://www-history.mcs.st-andrews.ac.uk/Quotations/Lagrange.html