Chapter 7. Gases We are surrounded by an atmosphere composed of a mixture of gases that we refer to as air. The behavior of air determines our weather, and the oxygen, O2, in air supports our life. We also encounter gases in countless other situations. For example, chlorine gas, Cl2, is used to purify drinking water. Acetylene gas, C2H2, is used in welding. Nitrous oxide gas, N2O, sometimes called laughing gas, is used as anesthetic in dentistry. Our goal in this chapter is to develop a deeper understanding of the physical properties of gases. 1. Properties of gases Under appropriate conditions, substances that are ordinarily liquids or solids can also exist in the gaseous state, where they are often referred to as vapors. The substance H2O, for example, can exist as solid ice, liquid water, or water vapor. Frequently, a substance exists in all three states of matter. The characteristic properties of gases arise because the individual molecules are relatively far apart. ① A gas expands to fill its container. Consequently, the volume of the gas is equal to the volume of the container in which it is held. ② Gases form homogeneous mixtures with one another regardless of the identities or relative proportions of the component gases. 7–1 2. Gas pressure Gases exert a pressure on any surface with which they are in contact. For example, the gas in an inflated balloon exerts a pressure on the inside surface of the balloon. 1) Pressure: P = F/A P: pressure, F: force, A: area Unit: Pa (pascal), 1 Pa = 1 N/m2 2) Liquid pressure P = F/A = mg/A = Vg/A = Ahg/A = gh ( = density) h A 3) Measurement of atmospheric pressure The force experienced by any area exposed to Earth’s atmosphere is equal to the weight of the column of air above it. It is the pressure exerted by this column of air that we refer to as atmospheric pressure. The actual value of atmospheric pressure depends on location, temperature, and weather. a) In 1643, Torricelli constructed a device to measure the pressure of atmosphere. mercury (Hg) barometer vacuum air pressure 76 cm Hg (a) (b) Figure. Measurement of atmospheric pressure with a mercury barometer. (a) The mercury levels are equal inside and outside the open-tube. (b) A column of mercury 76 cm high is maintained in the closed-end tube. 7–2 b) Units of pressure 1 atm = 760 mmHg = 760 torr = 14.7 lb/in2 (psi) = 1.0333 kg/cm2 = 101,325 N/m2 (Pa) = 101.324 kPa What is the height of a water column, in meters, that could be maintained by standard atmospheric pressure? ((Hg) = 13.6 g/cm3) Solution: 1 atm = (H2O)·g·h(H2O) = (Hg)·g·h(Hg) h(H2O) = (Hg)·h(Hg)/(H2O) = [13.6 g/cm3 × 76 cm]/[1.0 g/cm3] = 1.03 × 103 cm = 10.3 m c) Manometer We use various devices to measure the pressure of enclosed gas. i) An open-end manometer: An open-end manometer is usually employed to measure gas pressures that are near atmospheric pressure. Patm Pgas Patm Pgas PHg Hg Patm Pgas Hg (a) Pgas = Patm (b) Pgas = Patm + PHg 7–3 (c) Pgas = Patm - PHg ii) A closed-end manometer: A closed-end manometer is usually employed to measure gas pressures below atmospheric pressure (5–300 mmHg). The pressure is just the difference in the heights of the liquid levels in the two arms. vacuum P=0 PHg Gas AIr (a) (b) Pgas = PHg 3. Ideal gas equation Experiments with a large number of gases reveal that the four variables, pressure (P), volume (V), temperature (T), and the quantity of matter (n) in the gaseous samples are usually sufficient to define the state, or condition, of a gas. 1) V 1/P (at constant n and T) V T (at constant n and P) V n (at constant P and T) Boyle's law: Charle's law: Avogadro's law: V nT/P ∴ V = RnT/P or PV = nRT (Ideal gas equation) An ideal gas is a hypothetical gas whose pressure–volume– temperature behavior can be completely explained by the ideal gas equation. The molecules of an ideal gas do not attract or repel one another, and their volume is negligible compared with the volume of the container. 7–4 2) Some remarks a) STP (Standard Temperature and Pressure) i) For an ideal gas: 0 ℃ and 1 atm ii) Volume of 1 mol of gas at STP = 22.4 L) b) R (gas constant) = 0.082 (L·atm)/(K·mol) = 1.987 cal/(K·mol) = 8.314 J/(K·mol) c) K (Kelvin temperature or absolute temperature) K = ℃ + 273.15 d) Molecular weight (Mw) determination: PV = nRT = (m/Mw)RT e) At constant n, P1V1/T1 = P2V2/T2 P1V1 = nRT1, P2V2 = nRT2 A glass vessel weighs 40.1305 g when clean, dry, and evacuated; 138.2410 g when filled with water at 25 ℃ (density of water = 0.9970 g/cm3); and 40.2959 g when filled with propylene gas (C3H6) at 740.4 mmHg and 25 ℃. What is the molecular weight of propylene? 7–5 4. Mixtures of gases 1) Dalton's law ① Dalton's assumption: In a mixture of gases, each gas expands to fill the container. Each gas exerts the same pressure, called its partial pressure, that it would if it were alone in the container. ② The total pressure of a mixture of gases equals the sum of the pressures that each gas would exert if it were present alone. Ptot = Pi = (ni/V)RT (at constant V and T) i) Pi (partial pressure of the ith gas) = (ni/ntot)Ptot = XiPtot ii) Xi (mole fraction) = ni/ntot = ni/ ni Xi = 1 iii) Pi/Ptot = niRT/V = ni = Xi ntotRT/V ntot The major components of air are N2, 78.08%; O2, 20.95%; Ar, 0.93%, and CO2, 0.03% by volume. What are the partial pressures of these four gases in a sample of air at 1 atm? 2) Collecting gases over water An experiment that often comes up in the course of the laboratory work involves determining the number of moles of gas collected from a chemical reaction. Sometimes this gas is collected over water. a) Gases insoluble in H2O: N2, Ar,…(wet gas): Ptot = Pgas + PH2O = Patm Pgas + PH2O Gas Patm Patm water Figure. Collecting a gas over water. 7–6 b) Vapor pressure of water (PH2O) depends only on the temperature of water. Table. Vapor pressure of water at various temperatures T (℃) PH2O (mmHg) T (℃) PH2O (mmHg) 0 4.6 27 26.7 5 6.5 28 28.3 10 9.2 29 30.0 11 9.8 30 31.8 12 10.5 35 42.2 13 11.2 40 55.3 14 12.0 45 71.9 15 12.8 50 92.5 16 13.6 55 118.0 17 14.5 60 149.4 18 15.5 65 187.5 19 16.5 70 233.7 20 17.5 75 289.1 21 18.7 80 355.1 22 19.8 85 433.6 23 21.1 90 525.8 24 22.4 95 633.9 25 23.8 100 760.0 26 25.2 105 906.1 Suppose that 0.20 L of oxygen gas is collected over water. The temperature of the water and gas is 26 ℃, and the atmospheric pressure is 750 mmHg. a) How many moles of O2 are collected? b) What volume would the O2 gas collected occupy when dry, at the same temperature and pressure? 7–7 5. Kinetic theory of gases The ideal gas equation describes how gases behave, but it does not explain why they behave as they do. For example, why does a gas expand when heated at constant pressure? Or why does its pressure increase when the gas is compressed at constant temperature? To understand the physical properties of gases, we need a model that helps us picture what happens to the gas particles as experimental conditions such as pressure or temperature changes. Such a model is referred to as the kinetic molecular theory. 1) Assumptions ① A gas consists of a very large number of extremely small particles (atoms, molecules, or ions) in constant, straight-line motion. ② Molecules of a gas are separated by great distances. (Point mass model: it has mass but no volume.) ③ Molecules frequently collide with one another and with the wall of their container. However, these collisions occur very rapidly and most of the time molecules are not colliding. ④ Attractive and repulsive forces between gas molecules are negligible. (No intermolecular forces) ⑤ Energy can be transferred between molecules during collisions, but the average kinetic energy of the molecules does not change with time, as long as the temperature of the gas remains constant. (Due to elastic collisions between molecules, the total energy remains constant.) ⑥ The average kinetic energy of the molecules is proportional to absolute temperature. At any given temperature the molecules of all gases have the same average kinetic energy. The average kinetic energy of a molecule is EK = 1/2mv2 = CT (C: constant) v2 (the mean square speed) = (v12 + v22 + v32 + + … + vN2)/N N : the total number of molecules 7–8 2) Distribution of molecular speeds ① The absolute temperature of a gas is a measure of the average kinetic energy of its molecules. i) If two different gases are at the same temperature, the molecules have the same average kinetic energy. ii) If the temperature of a gas is doubled (say from 200 K to 400 K), the average kinetic energy of its molecules is also doubled. Thus, molecular motion increases with increasing temperature. ② Although the molecules of a gas have the average kinetic energy and hence an average speed, the individual molecules move at varying speeds. At one instant, some of them are moving rapidly, others slowly. 0 oC Relative number of molecules 500 oC 0 1 2 3 4 3 5 (x 10 ) Figure. Distribution of molecular speeds. The distribution of speeds of H2 molecules are shown for 0 ℃ and 500 ℃. Note that maximum in the curve increases with temperature. 7–9 3) Application to the gas law ① Gas pressure is the result of collisions between molecules and the wall of the container. ② Compressibility of gases. Because molecules of a gas are separated by great distances, gases can be compressed easily to occupy smaller volumes, ③ Boyle’s law. Decreasing the volume of a given amount of a gas increases its density and therefore increases its collision rate. ④ Charles’ law. Because the average kinetic energy of gas molecules is proportional to the sample’s absolute temperature, raising the temperature increases the average kinetic energy. Consequently, gas molecules with the wall of the container more frequently and thus the pressure increases. The volume of gas will expand until the gas pressure is balanced by the external pressure. ⑤ Dalton’s law of partial pressure. If molecules do not attract or repel one another, then the pressure exerted by one gas is not affected by another gas. Consequently, the total pressure is given by the sum of individual gas pressres. 4) Graham’s laws of diffusion and effusion ① Gas diffusion, the gradual mixing of molecules of one gas with molecules of another by virtue of their kinetic properties, provides a direct demonstration of random motion. V1/v2 = (M1/M2)1/2 V1, v2: diffusion rates of gases 1 and 2 M1, M2: molar masses ③ Effusion is a process by which a gas under pressure escapes from one compartment of a container to another by passing through a small opening. 7 – 10 6. Nonideal gases (Real gases) Although the ideal gas equation is a very useful description of gases, all real gases fail to obey this relationship to some extent. The extent to which a real gas deviates from ideal behavior may be seen by slightly rearranging the ideal gas equation. For a mole of ideal gas (n = 1), the quantity PV/(RT) equals 1 at all pressures and temperatures. PV/(RT) = n 1) The deviation from ideal behavior depends on pressure. ① At high pressures, the deviation from ideal behavior [PV/(RT)] is large and different for each gas. ② At low pressures (usually below 10 atm), however, the deviation from ideal behavior is small, and we can use the ideal gas equation without generating serious error. 2.0 1.5 H2 PV/RT 1.0 ideal gas N2 CH 4 0.5 CO 2 0 2 4 6 8 2 10 (x 10 ) Figure. PV/(RT) versus pressure for 1 mol of several gases at 300 K. The data for CO 2 pertain to a temperature of 313 K because CO 2 liquefies under high pressure at 300 K. 2) The deviation from ideal behavior also depends on temperature. ① As temperature increases, the properties of a gas more nearly approach those of the ideal gas. ② In general, gases deviate significantly from ideal behavior at temperatures near their liquefaction points; that is, the deviations 7 – 11 increase as temperature decreases, becoming significant near the temperature at which the gas is converted into a liquid. 3.0 300 K 500 K 2.0 1000 K PV/RT 1.0 ideal gas CO 2 0 3 6 9 (x 102) P (atm) Figure. PV/(RT) versus pressure for 1 mol of nitrogen gas at different temperatures. As temperature increases, the gas more closely approaches ideal behavior. Ideal gas gas Volume liquid solid 0 Real gas Temperature Figure. Volume change as a function of temperature of ideal and real gases. 7 – 12 3) We can understand the pressure and temperature effects on nonideality by considering two factors that are considered negligible in the kinetic molecular theory ① The molecules of a gas possess finite volumes. ② At short distances of approach, they exert attractive forces upon one another. (P + n2a/V2) (V – nb) = nRT i) n2a/V2: correction for intermolecular forces of attraction ii) nb: correction for the volume of gas molecules Table. Van der Waals constants for gas molecules Substance a (L2·atm/mol2) b (L/mol) Substance a (L2·atm/mol2) b (L/mol) He 0.0341 0.0237 N2 1.39 0.0391 Ne 0.211 0.0171 O2 1.36 0.0318 Ar 1.34 0.0322 Cl2 6.49 0.0562 Kr 2.32 0.0398 H2O 5.46 0.0305 Xe 4.19 0.0510 CH4 2.25 0.0428 H2 0.244 0.0266 CO2 3.59 0.0427 CCl4 20.4 0.1383 7 – 13