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5/16/2018

Chapter 10: Properties of : The Air We Breathe

Sept, 2006 Sept, 2016

http://ozonewatch.gsfc.nasa.gov

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Chapter Outline

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric . 10.4 Relating P,T, and V: The Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 of Gases and Henry’s Law . 10.11 Gas Effusion and : Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

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The Properties of Gases

Neither definite shape nor definite

The Properties of Gases

Gases can be compressed.

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The Properties of Gases

All gases are miscible with all other gases.

http://catalog.flatworldknowledge.com/bookhub/4309?e=averill_1.0-ch13_s01

Chapter Outline

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 . 10.4 Relating P,T, and V: The . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

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Kinetic Molecular Theory of Gases

1. Gas particles have tiny volumes compared with their container’s volume

Kinetic Molecular Theory of Gases

2. They don’t interact with other gas molecules, e.g. no intermolecular .

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Kinetic Molecular Theory of Gases

3. They move randomly and constantly

Kinetic Molecular Theory of Gases

4. Elastic collisions with walls of container and other gas molecules

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Kinetic Molecular Theory of Gases

5. Have average kinetic energy that is proportional to 2 absolute Kelvin : KE = ½ mu rms

A = B since both at the same temperature

2 2 ½ mAu rms,A = ½ mBu rms,B 푢푟푚푠,퐴 푚퐵 2 2 = mAu rms,A = mBu rms,B 푢푟푚푠,퐵 푚퐴 2 2 u rms,B u rms,B

m u2 = m MM = A rms,A B 푢푟푚푠,퐴 푀푀퐵 2 = molar u rms,B 푢푟푚푠,퐵 푀푀퐴 mass 2 mA u rms,A = mB 2 mA u rms,B mA Graham’s Law of Effusion: We will return to this in Section 10.11 2 u rms,A = mB 2 u rms,B mA 푟푎푡푒 푒푓푓푢푠푖표푛,퐴 푀푀 = 퐵 푢 푚 푟푎푡푒 푒푓푓푢푠푖표푛,퐵 푀푀퐴 푟푚푠,퐴 = 퐵 푢푟푚푠,퐵 푚퐴

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rms velocity inversely proportional to the Molar Mass

= 32 g/mol

= 28

= 18

= 4

Chapter Outline

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric Pressure . 10.4 Relating P,T, and V: The Gas Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

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Pressure = /unit area

Molecules collide with the inside surface of the container. The force of the collision is measured as pressure.

Pressure at Level

Pounds/in2 (psi) 14.7 psi

Atmospheres (atm) 1 atm

Pascals (N/m2) 101.325 X 103 Pa

Torr (mmHg) 760 mmHg

Torricelli’s Barometer

The pressure of the Column of atmosphere on the surface mercury of the mercury in the dish is balanced by the 760 mm Hg downward pressure exerted by the mercury in Atmospheric the column. pressure

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Elevation and Atmospheric Pressure

0.35 atm

0.62 atm

0.83 atm

Chapter Outline

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric Pressure . 10.4 Relating P,T, and V: The Gas Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

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State Variables for a Gas P = pressure V = volume T = temperature n = number of moles

Some math before continuing - y = mx + b 60

50 m

40

30 yaxis 20

10 b 0 0 5 10 15 20 25 xaxis

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Boyle’s Law: P and V (n and T held constant) • P and V are inversely proportional - • P  then V  • If you plot P vs. 1/V the result is a straight line • P = mx + b = m(1/V) + b • so P = m/V and PV = m

• P1V1 = m and P2V2 = m, so

• P1V1 = P2V2

Boyle’s Law and

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Applying Boyle’s Law Example

A bubble of at the bottom of a lake floats up to the surface. The pressure at the bottom of the lake is 4.75 atm and the volume is 5.65 mL. At the surface, the new pressure is 0.985 atm. Assuming that the temperature and number of moles remained constant, what is the final volume of the bubble?

P1 = 4.75 atm P2 = 0.985 atm V1 = 5.65 mL V2 = ? mL

Explaining Boyle’s Law Using Kinetic Molecular Theory

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Charles’s Law: V and T (n and P held constant) • T and V are directly proportional - • T  then V  • If you plot V vs. T the result is a straight line • V = mT + b = mT • so V = mT and V/T = m

• V1/T1 = m and V2/T2 = m V V 1  2 Volume of a gas extrapolates to zero at T1 T2 absolute zero (0 K = −273°C) so you MUST use the Kelvin temperature.

Jacques Alexandre Charles (1796-1823) The French chemist Charles was most famous in his lifetime for his experiments in ballooning. The first such flights were made by the Montgollier brothers in June 1783, using a large spherical balloon made of linen and paper and filled with hot air. In August 1783, however, a different group. supervised by Jacques Charles, tried a different approach. Exploiting his recent discoveries in the study of gases, Charles decided to inflate the balloon with hydrogen gas. Because hydrogen would escape easily from a paper bag, Charles made a bag of silk coaled with a rubber . Inflating the bag to its final diameter took several days and required nearly 500 pounds of acid and 1000 pounds of iron to generate the hydrogen gas. A huge crowd watched the ascent on August 27, 1783. The balloon stayed aloft for almost 45 minutes and travelled about 15 miles. When it landed in a village, however, the people were so terrified they tore if to shreds.

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Sample Exercise 10.4: Applying Charles’ Law

Several students at a northern New England campus are hosting a party celebrating the mid-January start of “spring” semester classes. They decide to decorate the front door of their apartment building with party balloons. The air in the inflated balloons is initially 70 oF. After an hour outside, the temperature of the balloons is -12 oF. Assuming no air leaks from the balloons and the pressure in them does not change significantly, how much does their volume change? Express your answer as a percentage of the initial volume.

Explaining Charles’ Law Using Kinetic Molecular Theory

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Avogadro’s Law: V and n (T and P held constant) • V and n are directly proportional • n  then V  • If you plot V vs. n the result is a straight line • V = mn + b = mn • so V = mn and V/n = m

• V1/n1 = m and V2/n2 = m V V 1  2 n1 n2

Avogadro’s Law Problem (none given in text, p. 427)

V1 = 3.5 L V2 = 10.1 L n1 = 0.140 mol n2 = ? mol

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Chapter Outline Note: we are skipping ahead to Sec. 10.6, then back to Sec. 10.5 . 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric Pressure . 10.4 Relating P,T, and V: The Gas Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

Ideal Gas Equation

Boyle’s law: V a 1 (at constant n and T) P Charles’ law: V a T (at constant n and P) Avogadro’s law: V a n (at constant P and T)

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Standard Temperature and Pressure (STP).

Experiments show that at STP, 1 mole of an ideal gas occupies 22.414 L.

PV = nRT

Sample Exercise 10.7: Applying the Ideal Gas Law

Bottles of compressed O2 carried by climbers ascending Mt. Everest are designed to hold one kilogram of the gas. What volume of O2 can one bottle deliver to a climber at an where the temperature is -38 oC and the atmospheric pressure is 0.35 atm? Assume that each bottle contains 1.00 kg of O2.

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Chapter Outline Note: we are now back to Sec. 10.5

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric Pressure . 10.4 Relating P,T, and V: The Gas Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

Deriving the Combined Gas Law P, V, T, and n

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Sample Exercise 10.6: Applying the Combined Gas Law

The pressure inside a weather balloon as it is released is 798 mmHg. If the volume and temperature of the balloon are 131 L and 20 oC, what is the volume of the balloon when it reaches an altitude where its internal pressure is 235 mmHg and T = -52 oC?

Chapter Outline

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric Pressure . 10.4 Relating P,T, and V: The Gas Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

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Densities and Molecular of Gases Using PV = nRT

Sample Exercise 10.8: Calculating the Density of a Gas

According to the U.S National Weather Service, the air temperature in Phoenix, AZ reached 25.56 oC on January 1, 2012, when the atmospheric pressure was 1.0106 atm. What is the density of the air? Assume the average molar mass of air is 28.8 g/mol, which is the weighted average of the molar masses of the various gases in dry air.

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Example: Calculating the Molecular from PV = nRT

1.018 g of Freon-113 gas is trapped in a 145 mL container at 760 mmHg and 50.0°C. What is the molar mass of Freon-113?

Chapter Outline

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric Pressure . 10.4 Relating P,T, and V: The Gas Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

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Gas Laws & Stoichiometry

Example: Combining Stoichiometry and the Ideal Gas Law

Chlorine gas can be prepared in the laboratory by the reaction of manganese dioxide with hydrochloric acid:

MnO2(s) + 4 HCl(aq)  MnCl2(aq) + 2 H2O(l) + Cl2(g)

How many grams of MnO2 should be added to excess HCl to obtain 275 mL of chlorine gas at 5.0°C and 650 mmHg?

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Chapter Outline

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric Pressure . 10.4 Relating P,T, and V: The Gas Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

Dalton’s Law of Partial

. For a mixture of gases in a container:

• Ptotal = P1 + P2 + P3 + . . .

Total pressure depends only on total number moles of gas, not on their identities

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Mole Fraction &

. Mole Fraction: • Ratio of the # of moles of a given component in a mixture to the total # of moles in a mixture: nn 11 x1  ntotal n 1 n 2  n 3  ... . Mole Fraction in Terms of Pressure:

• When V and T are constant, P  n

Mole Fraction & Partial Pressure

Since P  n nP11 x1  nPtotal total

P And: x  1 1 P total

Then… P1 x 1 P total

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Sample Exercise 10.11: Calculating Mole Fractions and Partial Pressures

Scuba divers who dive to depths below 50 meters may breathe a gas mixture called during the deepest parts of their dives. One formulation of the mixture, called Trimix 10/70, is 10% oxygen, 70% helium, and 20% nitrogen by volume. What is the mole fraction of each gas in this mixture, and what is the partial pressure of oxygen in the lungs of a diver at a depth of 60 meters (where the ambient pressure is 7.0 atm)?

Collecting a Gas over Water

2 KClO3(s) → 2 KCl(s) + 3 O2(g)

Gases collected:

O2(g) and H2O(g)

PPP total O22 H O

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Sample Exercise 10.12: Calculating the Quantity of a Gas Collected by Water Displacement

During the decomposition of KClO3, 92.0 mL of gas is collected by the displacement of water at 25.0 oC. If atmospheric pressure is 756 mmHg, what mass of O2 is collected?

Chapter Outline

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric Pressure . 10.4 Relating P,T, and V: The Gas Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

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Solubility of Gases

. of gases depends on T and P

Solubility ↑ as Pressure ↑

Solubility ↓ as Temperature ↑

Henry’s Law

. Henry’s Law: • The higher the partial pressure of the gas above a , the more soluble

• Cgas  Pgas

• Cgas  kH Pgas

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Sample Exercise 10.13: Calculating Gas Solubility Using Henry’s Law

Lake Titicaca is located high in the Andes Mountains between Peru and Bolivia. Its surface is 3811 m above sea level, where the average atmospheric pressure is 0.636 atm. During the summer, the average temperature of the water’s surface rarely exceeds 15 oC. What is the solubility of oxygen in Lake Titicaca at that temperature? Express your answer in molarity and in mg/L.

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Chapter Outline

. 10.1 The Properties of Gases . 10.2 The Kinetic Molecular Theory of Gases* . 10.3 Atmospheric Pressure . 10.4 Relating P,T, and V: The Gas Laws . 10.5 The Combined Gas Law (we will add moles to the equation) . 10.6 Ideal Gases and the Ideal Gas Law . 10.7 Densities of Gases . 10.8 Gases in Chemical Reactions . 10.9 Mixtures of Gases . 10.10 Solubilities of Gases and Henry’s Law . 10.11 Gas Effusion and Diffusion: Molecules Moving Rapidly . 10.12 Real Gases

*Effusion has been added to Section 10.11

Graham’s Law of Effusion, p. 415

Effusion is the process where a gas escapes through a small pore in the container wall into a region of lower pressure.

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Graham’s Law of Effusion

푢 푀푀 MM = molar mass 푟푚푠,퐴 = 퐵 푢푟푚푠,퐵 푀푀퐴

푟푎푡푒 푒푓푓푢푠푖표푛,퐴 푀푀 = 퐵 푟푎푡푒 푒푓푓푢푠푖표푛,퐵 푀푀퐴

Sample Exercise 10.1: Calculating Relative Rates of Effusion

An odorous gas emitted by a hot spring was found to effuse at 0.342 times the rate at which helium effuses. What is the molar mass of the emitted gas?

푟푎푡푒 푒푓푓푢푠푖표푛,퐴 푀푀 = 퐵 A = X (MM = ?) 푟푎푡푒 푒푓푓푢푠푖표푛,퐵 푀푀퐴 B = He (MM = 4.003 g/mol)

푟푎푡푒 푒푓푓푢푠푖표푛 푋 푀푊 = 퐻푒 푟푎푡푒 푒푓푓푢푠푖표푛,퐻푒 푀푊푋

4.003 푔/푚표푙 0.342 = 푀푀푋 4.003 푔/푚표푙 2 (0.342) = and so MMX = 34.2 g/mol or H2S 푀푀푋

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Diffusion - Same Formula as Graham’s Law of Effusion:

푈 푒푓푓푢푠푖표푛 푟푎푡푒 퐴 푑푖푓푓푢푠푖표푛 푟푎푡푒 퐴 푀 푟푚푠,퐴 = = = 퐵 푈푟푚푠,퐵 푒푓푓푢푠푖표푛 푟푎푡푒 퐵 푑푖푓푓푢푠푖표푛 푟푎푡푒 퐵 푀퐴

Problem 10.121 A flask of ammonia is connected to a flask of an unknown acid HX by a 1.00 m

glass tube. As the two gases diffuse down the tube, a white ring of NH4X forms 68.5 cm from the ammonia flask. Identify element X.

Gas Diffusion: Molecules Moving Rapidly

Maxwell’s Equation

3푅푇 푢 = 푟푚푠 푀

R = 8.314 J/mol K

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Practice Exercise 10:14 Calculating Root-Mean-Square Speeds

Calculate the root-mean-squared speed of nitrogen molecules at 25 oC.

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