physics 207: lecture 23, pg 1 lecture 23 goals: chapter 16 chapter 16 use the ideal-gas law. use...
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Physics 207: Lecture 23, Pg 1
Lecture 23Goals:Goals:
• Chapter 16Chapter 16 Use the ideal-gas law. Use pV diagrams for ideal-gas processes.
• Chapter 17Chapter 17 Employ energy conservation in terms of 1st law of TD Understand the concept of heat. Relate heat to temperature change Apply heat and energy transfer processes in real situations Recognize adiabatic processes.
• AssignmentAssignment HW9, Due Wednesday, Apr. 14th HW10, Due Wednesday, Apr. 21st (9 AM)
Exam 3 on Wednesday, Apr. 21 at 7:15 PM (Statics, Ang. Mom., Ch.14 through 17)
Physics 207: Lecture 23, Pg 2
Thermodynamics: A macroscopic description of matter
Recall “3” Phases of matter: Solid, liquid & gas All 3 phases exist at different p,T conditions Phase diagram
Triple point of water:
p = 0.06 atm
T = 0.01°C
Triple point of CO2:
p = 5 atm
T = -56°C
Physics 207: Lecture 23, Pg 3
Modern Definition of Kelvin Scale
Water’s triple point on the Kelvin scale is 273.16 K One degrees Kelvin is defined to be 1/273.16 of the
temperature at the triple point of water
Triple point
Accurate water phase diagram
Physics 207: Lecture 23, Pg 4
Changes due to Heat or Thermal Energy Transfer
Change the temperature (it gets hotter) Change the state of matter (solidliquid, liquidgas)
Accurate water phase diagram
Path onheating
Physics 207: Lecture 23, Pg 5
Energy Transfer to a solid (ice)1. Temperature increase or
2. State Change
If a gas, then V, p and T are interrelated….equation of state
Physics 207: Lecture 23, Pg 8
Defining a temperature scale
Three main scales
212
Farenheit
100
Celsius
32 0 273.15
373.15
Kelvin
Water boils
Water freezes
0-273.15-459.67Absolute Zero
Physics 207: Lecture 23, Pg 9
Some interesting facts In 1724, Gabriel Fahrenheit made thermometers
using mercury. The zero point of his scale is attained by mixing equal parts of water, ice, and salt. A second point was obtained when pure water froze (originally set at 30oF), and a third (set at 96°F) “when placing the thermometer in the mouth of a healthy man”. On that scale, water boiled at 212. Later, Fahrenheit moved the freezing point of
water to 32 (so that the scale had 180 increments).
In 1745, Carolus Linnaeus of Upsula, Sweden, described a scale in which the freezing point of water was zero, and the boiling point 100, making it a centigrade (one hundred steps) scale. Anders Celsius (1701-1744) used the reverse scale in which 100 represented the freezing point and zero the boiling point of water, still, of course, with 100 degrees between the two defining points.
T (K)
108
107
106
105
104
103
100
10
1
0.1
Hydrogen bomb
Sun’s interior
Solar corona
Sun’s surface
Copper melts
Water freezes
Liquid nitrogen
Liquid hydrogenLiquid helium
Lowest T~ 10-9K
Physics 207: Lecture 23, Pg 10
Ideal gas: Macroscopic description Consider a gas in a container of volume V, at
pressure p, and at temperature T Equation of state
Links these quantities Generally very complicated: but not for ideal gas
Physics 207: Lecture 23, Pg 11
Ideal gas: Macroscopic description
pV = nRT R is called the universal gas constant
In SI units, R =8.315 J / mol·K
n ≡ number of moles
Equation of state for an “ideal gas” Collection of atoms/molecules moving randomly No long-range forces
Their size (volume) is negligible Density is low Temperature is well above the condensation point
Physics 207: Lecture 23, Pg 12
Boltzmann’s constant
In terms of the total number of particles N
p, V, and T are thermodynamic variables
pV = nRT = (N/NA ) RT
kB is called the Boltzmann’s constant
kB = R/NA = 1.38 X 10-23 J/K
pV = N kB T
Number of moles: n = m/M
One mole contains NA=6.022 X 1023 particles :
Avogadro’s number = number of carbon atoms in 12 g of carbon
m = mass (kg)M= mass of one mole (kg/mol)
Physics 207: Lecture 23, Pg 13
What is the volume of 1 mol of gas at STP ?T = 0 °C = 273 Kp = 1 atm = 1.01 x 105 Pa
nRTpV
4.22m0224.0
Pa1001.1K 273Kmol/J31.8
3
5
p
nRTV
The Ideal Gas Law
Physics 207: Lecture 23, Pg 14
There are four things that can vary: p, V, n & T
Typically, two of these are held constant and the relationship between the remaining two is studied
nRTpV
The Ideal Gas Law
Physics 207: Lecture 23, Pg 15
Example
A spray can containing a propellant gas at twice atmospheric pressure (202 kPa) and having a volume of 125.00 cm3 is at 27oC. It is then tossed into an open fire. When the temperature of the gas in the can reaches 327oC, what is the pressure inside the can?
Assume any change in the volume of the can is negligible.
Steps
1. Convert to Kelvin (From 300 K to 600 K)
2. Use P/T = nR/V = constant P1/T1 = P2/T2
3. Solve for final pressure P2 = P1 T2/T1
WD40 foolishness
Physics 207: Lecture 23, Pg 16
Example problem: Air bubble rising A diver produces an air bubble underwater, where the absolute
pressure is p1 = 3.5 atm. The bubble rises to the surface, where the pressure is p2 = 1.0 atm. The water temperatures at the bottom and the surface are, respectively, T1 = 4°C, T2 = 23°C
What is the ratio of the volume,V2 , of the bubble just as it reaches the surface to its volume at the bottom, V1?
Is it safe for the diver to ascend while holding his breath?
No! Air in the lungs would expand, and the lung could rupture.
Physics 207: Lecture 23, Pg 18
Example problem: Air bubble rising
A diver produces an air bubble underwater, where the absolute pressure is p1 = 3.5 atm. The bubble rises to the surface, where the pressure is p2 = 1 atm. The water temperatures at the bottom and the surface are, respectively, T1 = 4°C, T2 = 23°C
What is the ratio of the volume of the bubble as it reaches the surface,V2, to its volume at the bottom, V1? (Ans.V2/V1 = 3.74)
pV=nRT pV/T = const so p1V1/T1 = p2V2/T2
V2/V1 = p1T2/ (T1 p2)
= 3.5 296 / (277 1)
If thermal transfer is efficient.
[More than likely the expansion will be “adiabatic” and, for a diatomic gas, PV = const. where = 7/5, see Ch. 17 & 18]
Physics 207: Lecture 23, Pg 19
Buoyancy and the Ideal Gas Law
A typical 5 passenger hot air balloon has approximately 700 kg of total mass and the balloon itself can be thought as spherical with a radius of 10.0 m. If the balloon is launched on a day with conditions of 1.0 atm and 273 K, how hot would you have to heat the air inside (assuming the density of the surrounding air is 1.2 kg/m3 and the air behaves and as an ideal gas) in order to keep the balloon at a constant altitude?
Hint: Remember the weight of the air inside the balloon.
p, V and R do not change!
Balloon weight = Buoyant force – Weight of hot air
Ideal gas law: pV = nRT nT= pV/R = const.
or T = const. = 1.2 x 273 kg K/m3
Physics 207: Lecture 23, Pg 20
Buoyancy and the Ideal Gas Law
mballoon g = air at 273 K V g – air at T V g
mballoon = air at 273 K V – air at T V
mballoon = (1.2 – 330 / T) V
700 / 4200 = 1.2 – 330 / T
330 / T = (1.2 - 0.2)
T = 330 K 57 C
Physics 207: Lecture 23, Pg 21
pV diagrams: Important processes
Isochoric process: V = const (aka isovolumetric) Isobaric process: p = const Isothermal process: T = const constant
TpV
Volume
Pre
ssur
e
2
2
1
1 T
p
T
p
1
2Isochoric
Volume
Pre
ssur
e
2
2
1
1 T
V
T
V
1 2
Isobaric
Volume
Pre
ssur
e
2211 VpVp 1
2
Isothermal
Physics 207: Lecture 23, Pg 22
pV vs. Fx diagrams
Work (on the system) remains the area under the curve
dW = F dx
or
dW = F/A (A dx) = P dVworld = -p dVsystem
constant TpV
Volume
Pre
ssur
e
2211 VpVp 1
2
Isothermal
Position
For
ce
1
2
Physics 207: Lecture 23, Pg 23
Work and Energy Transfer (Ch. 17)
K reflects the kinetic energy of the system
ΔK =Wconservative + Wdissipative + Wexternal
Wconservative = - ΔU (e.g., gravity)
Wdissipative = - ΔEThermal
Wexternal Typically, work done by contact forces
ΔK + ΔU + ΔETh = Wexternal= ΔEsys
Physics 207: Lecture 23, Pg 24
Work and Energy Transfer
ΔK + ΔU + ΔETh = Wexternal= ΔEsys
But we can transfer energy without doing work
Q ≡ thermal energy transfer
ΔK + ΔU + ΔETh = W + Q = ΔEsys
If ΔK + ΔU = ΔEMech = 0 ΔETh = W + Q
Physics 207: Lecture 23, Pg 25
1st Law of Thermodynamics
Thermal energy Eth : Microscopic energy of moving molecules and stretching molecular bonds. ΔEth depends on the initial and final states but is independent of the process.
Work W : Energy transferred to the system by forces in a mechanical interaction.
Heat Q : Energy transferred to the system via atomic-level collisions when there is a temperature difference.
ΔEth =W + Q
W & Q with respect to the system
Physics 207: Lecture 23, Pg 26
Lecture 23
• AssignmentAssignment HW9, Due Wednesday, Apr. 14th HW10, Due Wednesday, Apr. 21st (9 AM)
Exam 3 on Wednesday, Apr. 21 at 7:15 PM (Statics, Ang. Mom., Ch.14 through 17)