Fluids and Thermodynamics

Fluids and Thermodynamics

Fluids Fluids are substances that can flow, such as liquids and gases, and even a few solids. In Physics B, we will limit our discussion of fluids to substances that can easily flow, such as liquids and gases. D = m/V D: density (kg/m3) m: mass (kg) V: volume (m3) You should remember how to do density calculations from chemistry! Density can also be represented by - ρ ρ= m/V ρ: density (kg/m3)

Pressure P = F/A P : pressure (Pa) F: force (N) A: area (m2)
Pressure unit: Pascal ( 1 Pa = 1 N/m2) The force on a surface caused by pressure is always normal (or perpendicular) to the surface. This means that the pressure of a fluid is exerted in all directions, and is perpendicular to the surface at every location.

Atmospheric Pressure Atmospheric pressure is normally about 100,000 Pascals. Differences in atmospheric pressure cause winds to blow. Low atmospheric pressure inside a hurricane’s eye contributes to the severe winds and the evelopment of the storm surge..

Calculate the net force on an airplane window if cabin pressure is 90% of the pressure at sea level, and the external pressure is only 50% of that at sea level. Assume the window is 0.43 m tall and 0.30 m wide. Atmospheric pressure = Pa Pcabin = Pa Poutside = Pa Cabin Outside P = F/A P = 90000Pa – 50000Pa = 40000Pa A = lw A = 0.3m · 0.43m = 0.129m2 F = AP F = 0.129m2 · 40000Pa = 5160N

The Pressure of a Liquid
P = ρgh P: pressure (Pa) ρ : density (kg/m3) g: acceleration constant (9.8 m/s2) h: height of liquid column (m) This type of pressure is often called gauge pressure. Why? The gauges we use to measure pressure do not take into account the atmospheric pressure which is very large! If the liquid is water, this is referred to as hydrostatic pressure. Why? Hydro – water + static - stationary

Absolute Pressure Absolute pressure is obtained by adding the atmospheric pressure to the hydrostatic pressure. Pabs = Patm + ρgh Hydrostatic Pressure in Dam Design The depth of Lake Mead at the Hoover Dam is 180 m. What is the hydrostatic pressure and what is the absolute pressure at the base of the dam?

Hydrostatic Pressure in Dam Design
The depth of Lake Mead at the Hoover Dam is 180 m. What is the hydrostatic pressure and what is the absolute pressure at the base of the dam? ρfresh water = 1000 kg / m3 P = ρgh P = 1000 kg / m3 · 9.8m/s2 · 180 m = Pa Pabs = Patm + ρgh Pabs = Pa Pa = Pa

Hydrostatic Pressure in Levee Design
Hurricane Katrina August 2005 A hurricane’s storm surge can overtop levees, but a bigger problem can be increasing the hydrostatic pressure at the base of the levee.

New Orleans Elevation Map
New Orleans is largely below sea level, and relies upon a system of levees to keep the lake and the river at bay Max ht of the levee 17.5 ft Surge elevation set at 11.5 ft Normal lake level at 1.0ft

Calculate the increase in hydrostatic pressure experienced by the levee base for an expected (SPH Design) storm surge. How does this compare to the increase that occurred during Hurricane Katrina, where the water rose to the top of the levee? Not to mention there is atmospheric changes during hurricanes which effect the absolute pressure 16.5ft = 12in / 1ft · 2.54 cm / 1 in · 1 m / 100 cm = 5.03m hlevee = 16.5ft ρsalt water = 1025 kg /m3 P = ρgh P = 1025 kg /m3 ·9.8m/s2 · 5.03m = Pa

Pascal’s Principle Applies when a pressure is applied to a container holding a fluid Applies to closed systems Pascal’s principle applies in hydraulic systems F1 / A1 = F2 / A2

A person stands on a piston. The system is full of hydraulic fluid
A person stands on a piston. The system is full of hydraulic fluid. The car with a mass of 1500 kg is sitting on a piston that has a radius of 3.1 m. A person is standing on the other piston that has a radius of 0.40 m. What must the weight of the person be to cause the car to rise? mc = 1500kg rc = 3.1m rp = 0.40m Fp = ? Ac =πr2 = π(3.1m)2 = 30.19m2 Ac =πr2 = π(0.40m)2 = 0.50m2 Fc / Ac = Fp / Ap Fp = FcAp / Ac Fp = (1500· 9.8m/s2) · 0.50m2 / 30.19m2 = 243N This is equal to 54 lbs, so a child could stand on the piston and make the car move!!!

Calculate the pressure exerted on the bottom of a glass that moves upward in elevator with constant acceleration, increasing from rest to 1.2 m/s in 2.7 s. The height of the water is 15 cm. The radius of the cup is 2 cm. The glass is filled with water which has a density of 1000 kg /m3.Do not include atmospheric contribution in your answer. V = Acircle · h = m2 · 0.15m = m3 ΣF = ma h FN - mg= ma m = Vρ = m3 · 1000 kg / m3 = Kg a = (vf – vi) / t FN = ma + mg a = (1.2 m/s – 0m/si) / 2.7s = 0.44m/s2 A FN = Kg(0.44m/s m/s2) = N A = πr2 A = π(0.02m)2 = m2 FN = ma + mg

Calculate the pressure exerted on the bottom of a glass that moves upward in elevator with constant acceleration, increasing from rest to 1.2 m/s in 2.7 s. The height of the water is 15 cm. The radius of the cup is 2 cm. The glass is filled with water which has a density of 1000 kg /m3.Do not include atmospheric contribution in your answer. P1 = FN / A h P2 = ρgh P = ρgh + FN / A A P = 1000kg/m3 · 9.8m/s2 · 0.15m N / m2 = 3006Pa

Buoyancy

Floating is a type of equilibrium
An upward force counteracts the force of gravity for these objects. This upward force is called the buoyant force Fbuoyancy mg

Archimedes Principle Archimedes’ Principle: a body immersed in a fluid is buoyed up by a force that is equal to the weight of the fluid it displaces. The Buoyant Force Fbuoy = ρVg Fbuoy: the buoyant force exerted on a submerged or partially submerged object. V: the volume of displaced liquid. ρ : the density of the displaced liquid. When an object floats, the upward buoyant force equals the downward pull of gravity. The buoyant force can float very heavy objects, and acts upon objects in the water whether they are floating, submerged, or even sitting on the bottom.

Buoyant force on submerged object
A sharks body is not neutrally buoyant, so a shark must swim continuously or he will sink deeper. Fbuoy = ρVg mg Fbouy ≠ mg

SCUBA divers use a buoyancy control system to maintain neutral buoyancy (equilibrium!). Fbuoy = ρVg mg Fbouy = mg

If the diver wants to rise, he inflates his vest, which increases the amount of water he displaces, and he accelerates upward Fbuoy = ρVg mg Fbouy = mg

Buoyant force on floating object
If the object floats on the surface, we know for a fact Fbuoy = mg! The volume of displaced water equals the volume of the submerged portion of the ship. Fbuoy = ρVg mg Fbouy = mg

The height above the water is 0.02m
Assume a wooden raft has 80.0% of the density of water. The dimensions of the raft are 6.0 meters long by 3.0 meters wide by 0.10 meter tall. How much of the raft rises above the level of the water when it floats? Fbuoy = ρVg h y w l mg ΣF: Fbouy – mg = 0 We also know that the volume of displacement is equal to the volume of water displaced ρglwy = (0.8ρ)glwh ρgVsub – (0.8ρ)gVtotal = 0 y = (0.8) h y = 0.8 · 0.1m = 0.08m The height above the water is 0.02m

Buoyant Force The buoyant force can be extremely strong.
Incredibly massive objects can float, even when they are not intended to…

Moving Fluids

When a Fluid Flows… …mass is conserved. Provided there are no inlets our outlets in a stream of flowing fluid, the same mass per unit time must flow everywhere in the stream. Fluid Flow Continuity The volume per unit time of a liquid flowing in a pipe is constant throughout the pipe. We can say this because liquids are not compressible, so mass conservation is also volume conservation for a liquid.

Fluid Flow Continuity (cont.) V = Avt V: volume of fluid (m3)
A: cross sectional areas at a point in the pipe (m2) v: speed of fluid flow at a point in the pipe (m/s) t: time (s) A1v1 = A2v2 A1, A2: cross sectional areas at points 1 and 2 v1, v2: speed of fluid flow at points 1 and 2

A pipe of diameter 6. 0 cm has fluid flowing through it at 1. 6 m/s
A pipe of diameter 6.0 cm has fluid flowing through it at 1.6 m/s. How fast is the fluid flowing in an area of the pipe in which the diameter is 3.0 cm? How much water per second flows through the pipe? A1v1 = A2v2 πr21 v1 = πr22 v2 Apipe = πr2 v2 = πr21 v1 / πr22 v2 = π(0.06m)2 · (1.6 m/s) / π(0.03m)2 = 6.4 m/s

The water in a canal flows 0
The water in a canal flows 0.10 m/s where the canal is 12 meters deep and 10 meters across. If the depth of the canal is reduced to 6.5 meters at an area where the canal narrows to 5.0 meters, how fast will the water be moving through this narrower region? What will happen to the water in an open waterway if it cannot flow as fast as it wants to through a narrow region in a channel? It will rise and flow out of the channel V2 = l1w1v1 / l2w2 V2 = A1v1 / A2 A1v1 = A2v2 V2 =(12m · 10m · 0.1 m/s) / (6.5m · 5m) = 0.37 m/s

Natural Waterways Flash flooding can be explained by fluid flow continuity

Artificial Waterways Flooding from the Mississippi River Gulf Outlet was responsible for catastrophic flooding in eastern New Orleans and St. Bernard during Hurricane Katrina.

Fluid Flow Continuity in Waterways
Mississippi River Gulf Outlet levees are overtopped by Katrina’s storm surge. A hurricane’s storm surge can be “amplified” by waterways that become narrower or shallower as they move inland.

Moving Fluids and Bernoulli Effect

Bernoulli’s Theorem The sum of the pressure, the potential energy per unit volume, and the kinetic energy per unit volume at any one location in the fluid is equal to the sum of the pressure, the potential energy per unit volume, and the kinetic energy per unit volume at any other location in the fluid for a non-viscous incompressible fluid in streamline flow. All other considerations being equal, when fluid moves faster, the pressure drops.

Bernoulli’s Theorem p + ρgh + ½ ρv2 = Constant p : pressure (Pa)
ρ : density of fluid (kg/m3) g: gravitational acceleration constant (9.8 m/s2) h: height above lowest point (m) v: speed of fluid flow at a point in the pipe (m/s)

Knowing what you know about Bernoulli's principle, design an airplane wing that you think will keep an airplane aloft. Draw a cross section of the wing. Longer d, higher v, lower p Flift Fthurst Fdrag Flift = ΔPA mg

Problem: An above-ground swimming pool has a hole of radius 0
Problem: An above-ground swimming pool has a hole of radius 0.10 cm in the side 2.0 meters below the surface of the water. How fast is the water flowing out of the hole? How much water flows out each second? po + ρgh + ½ ρv2 = Constant h1 = 2m po + ρgh1 + ½ ρv12 = po + ρgh2 + ½ ρv22 ρgh1 + ½ ρv12 = ρgh2 + ½ ρv22 h2 = 0 m v1 = 0 m/s ρgh1 + = ½ ρv22 gh1 = ½v22 What about energy mgh = ½ mv2 v2 = √(2gh1) gh = ½ v2 v2 = √(2·9.8 m/s2 · 2.0m) = 6.26 m/s v2 = √(2gh1) Same equation!!! Bernoulli’s principle

Problem: An above-ground swimming pool has a hole of radius 0
Problem: An above-ground swimming pool has a hole of radius 0.10 cm in the side 2.0 meters below the surface of the water. How fast is the water flowing out of the hole? How much water flows out each second? v2 = 6.26 m/s h1 = 2m V = Avt V/t = Av V/t = πr2v V/t = π(0.001 m)2 · (6.26m/s) = 1.97 x 10-5 m3/s

Water travels through a 9. 6 cm diameter fire hose with a speed of 1
Water travels through a 9.6 cm diameter fire hose with a speed of 1.3 m/s. At the end of the hose, the water flows out of a nozzle whose diameter is 2.5 cm. What is the speed of the water coming out of the nozzle? If the pressure in the hose is 350 kPa, what is the pressure in the nozzle? A1v1 = A2v2 v2 = A1v1 / A2 v2 = πr21v1 / πr22 p1 = Pa v1 = 1.3 m/s p2 = ? Pa v2 = ? m/s v2 = π(0.096m)21· 1.3 m/s / π(0.025m)22 = m/s

Water travels through a 9. 6 cm diameter fire hose with a speed of 1
Water travels through a 9.6 cm diameter fire hose with a speed of 1.3 m/s. At the end of the hose, the water flows out of a nozzle whose diameter is 2.5 cm. What is the speed of the water coming out of the nozzle? If the pressure in the hose is 350 kPa, what is the pressure in the nozzle? p1 + ρgh1 + ½ ρv12 = p2 + ρgh2 + ½ ρv22 h1 = 0m h2 = 0m p1 = Pa v1 = 1.3 m/s p2 = ? Pa v2 = m/s p1 + ½ ρv12 = p2 + ½ ρv22 p2 = p1 + ½ ρv12 - ½ ρv22 p2 = p1 + ½ ρ(v12 - v22) p2 =350000Pa + ½ · kg / m3((1.3 m/s)2 – (19.17m/s)2) = Pa

Bernoulli’s Principle and Hurricanes
In a hurricane or tornado, the high winds traveling across the roof of a building can actually lift the roof off the building. +Roof&hl=en See if I can down load video

Make a device just like the above problem with a whole give them the information and they must predict where the water will hit the floor.

Thermodynamics

Thermodynamics Thermodynamics is the study of heat and thermal energy. Thermal properties (heat and temperature) are based on the motion of individual molecules, so thermodynamics is a lot like chemistry. Total energy E = U + K + Eint U: potential energy K: kinetic energy Eint: internal or thermal energy Potential and kinetic energies are specifically for “big” objects, and represent mechanical energy. Thermal energy is related to the kinetic energy of the molecules of a substance.

Temperature and Heat Temperature is a measure of the average kinetic energy of the molecules of a substance. Think of it as a measure of how fast the molecules are moving. The unit is ºC or K. Temperature is NOT heat! Heat is the internal energy that is transferred between bodies in contact. The unit is Joules (J), or sometimes calories (cal). A difference in temperature will cause heat energy to be exchanged between bodies in contact. When two bodies are at the same temperature, no heat is transferred. This is called Thermal Equilibrium.

Thermal Expansion Most substances expand when their temperature goes up. ΔL = αLo ΔT Δ L is change in length α is coefficient of linear expansion Lo is original length of substance ΔT is change in temperature

Sample problem: If the Eiffel tower is 301 m tall on a day when the temperature is 22º C, how much does it shrink when the temperature drops to 0º C? The coefficient of linear expansion is 11 x 10-6 ºC-1 for the iron the tower is made from. L0 = 301m T1 =22º C T2 =0º C α =11x10-6 /ºC ΔL = αL0 ΔT ΔL = 11x10-6 /ºC · 301m · (0 ºC - 22 ºC ) = m

Ideal Gas Law P1 V1 / T1 = P2 V2 / T2
P1, P2: initial and final pressure (any unit) V1, V2: initial and final volume (any unit) T1, T2: initial and final temperature (in Kelvin!) Temperature in K is obtained from temperature in oC by adding 273.

Suppose an ideal gas occupies 4. 0 liters at 23oC and 2. 3 atm
Suppose an ideal gas occupies 4.0 liters at 23oC and 2.3 atm. What will be the volume of the gas if the temperature is lowered to 0oC and the pressure is increased to 3.1 atm. P1 = 2.3 atm V1 = 4.0 L T1 = 23ºC = 296 K P2 = 3.1 atm V2 = ? L T2 = 0ºC = 273 K P1V1/T1 = P2V2/T2 V2 = (P1V1 T2) /(T1P2) V2 = (2.3 atm · 4.0 L · 273 K) / (296 K · 3.1 atm) = L

Ideal Gas Equation P V = n R T P: pressure (in Pa) V: volume (in m3) n: number of moles R: gas law constant 8.31 J/(mol K) T: temperature (in K) PV = N/m2 · m3 = Nm = J nRT = mol · J/(mol · K) · K = J Both sides = J

Determine the number of moles of an ideal gas that occupy 10
Determine the number of moles of an ideal gas that occupy 10.0 m3 at atmospheric pressure and 25oC. 25ºC = 298K n = PV / RT PV = nRT n = Pa · 10 m3 / (8.31J/ (mol · K) · 298K) = mols

Kinetic Theory of Gases

Ideal Gas Equation PV = nRT (using moles) PV = NkBT (using molecules)
P: pressure (Pa) V: volume (m3) N: number of molecules kB: Boltzman’s constant 1.38x10-23 J/K n: Number of moles R: Universal Gas constant 8.31 J / (mol · K) T: Temperature in Kelvin

Suppose a near vacuum contains molecules of helium in one cubic meter at 0ºC. What is the pressure? PV = NkBT P = NkBT / V P = · 1.38 x J/k 273k / 1m3 = 9.42 x Pa

What is the relationship between the Universal Gas Law constant (8
What is the relationship between the Universal Gas Law constant (8.31 J / (mol K) and Boltzman’s constant kB (1.38 x J/K)? NA = 6.02 x mol-1 R = 8.31 J/(mol K) KB = R/ NA KB = 8.31 J / (mol K) / 6.02 x mol-1 = 1.38 x J/K

The kinetic theory of gases uses mechanics to describe the motion off each single molecule in a sample off an ideal gas.. When a very large number off molecules is considered,, the mechanical properties off the individual molecules are summed in a statistical way to predict the behavior off the gas sample

Gases consist of a large number of molecules that make elastic collisions with each other and the walls of the container. Molecules are separated, on average, by large distances and exert no forces on each other except when they collide. There is no preferred position for a molecule in the container, and no preferred direction for the velocity.

Simulations

Need to change this make connection PV = 3/2 N KB T
Kave = 3/2 kBT Kave: average kinetic energy (J) kB: Boltzmann’s Constant (1.38 x J/K) T: Temperature (K) The molecules have a range of kinetic energies; kave is just the average of that range Need to change this make connection PV = 3/2 N KB T PV = to work which is equal to KE we are looking at 1 molecule for N

What is the average kinetic energy and the average speed of oxygen molecules in a gas sample at 0oC?
Use atomic mass number to get the mass per mole atomic mass number = number of Neutrons + number of Protons O2 32g/mol · 1 mol / 6.02 x 1023 · 1 kg / 1000g = x kg Kave = 3/2 kBT ½ mvrms2 = 3/2 kBT vrms =√(3 kBT / m) vrms =√((3 · 1.38 x J/K · 273K) / 5.32 x 10-26kg) = m/s vrms =√( J / kg) vrms =√( J/K · K / kg) vrms =√( kg · m2/s2 / kg) vrms =√( kg · m/s2 · m / kg) vrms =√(m2/s2)

Boundary Environment System (gas) For our purposes, the system will
almost always be an ideal gas. System (gas)

The system boundary controls how the environment affects the system.
If the boundary is “closed to mass”, that means that mass can’t get in or out. If the boundary is “closed to energy”, that means energy can’t get in or out. Consider the earth as a system. What type of boundary does it have? What is the boundary? Is the boundary closed to mass? Is the boundary closed to energy? Atmosphere, crust, where gravity is negligible Yes, the increase in mass each day is negligible No, the sun adds energy to the system

Work Q W Heat ΔU ΔU = Q – W System First Law of Thermodynamics
U = Δ Total energy ΔU = Q – W

Awkward notation WARNING!
We all know that U is potential energy in mechanics. However… U is Eint (thermal energy) in thermodynamics! This means when we are in thermo, U is thermal energy, which is related to temperature. When we are in mechanics, it is potential energy, which is related to configuration or position.

U is the sum of the kinetic energies of all molecules in a system (or gas).
U = N Kave U = N (3/2 kBT) U = n (3/2 R T) Since kB = R /NA

1st Law of Thermodynamics
ΔU = Q – W Δ U: change in internal energy of system (J) Q: heat added to the system (J). This heat exchange is driven by temperature difference. W: work done on the system (J). Work will be related to the change in the system’s volume. This law is sometimes paraphrased as “you can’t win”.

A system absorbs 200 J of heat energy from the environment and does 100 J of work on the environment. What is its change in internal energy? Q = 200 J U W = 100 J ΔU = Q – W ΔU = 200J – 100J = 100 J

How much work does the environment do on a system if its internal energy changes from 40,000 J to 45,000 J without the addition of heat? Q = 0 J ΔU = 45000J – 40000J = 5000J W = ? J ΔU = Q - W 5000 J = W therefore W = J

The thermodynamic state of a gas is defined by pressure, volume, and temperature.
A gas process describes how gas gets from one state to another state. Processes depend on the behavior of the boundary and the environment more than they depend on the behavior of the gas.

Isothermal Process P Constant Temperature PV = nRT V T1 T2 T3
Initial state of the gas Isothermal Process Final state of the gas V ΔT = 0 ( constant T)

Isobaric Process P Constant Pressure PV = nRT V T1 T2 T3
Isobaric Expansion Isobaric Contraction V ΔP = 0 ( constant P)

Isometric Process P Constant Volume PV = nRT V T1 T2 T3
ΔV = 0 ( constant V)

Temperature, pressure and volume all change in an adiabatic process
Insulated T1 T2 PV = nRT Isotherm Temperature, pressure and volume all change in an adiabatic process adiabat The figure compares two processes that begin with the same state and involve expansion to the same final volume. For the isothermal process, the product of P·V remains constant since T remains constant. Since the temperature must decrease for the adiabatic process, it follows that the final pressure must be less for this process. Thus the adiabat lies below the isotherm. Let's look at one more example that incorporates many of the AP points of emphasis. V Q = 0 ( No heat enters or leaves the system)

Work Calculation of work done on a system (or by a system) is an important part of thermodynamic calculations. Work depends upon volume change. Work also depends upon the pressure at which the volume change occurs.

Work Done BY gas Wgas = PΔV Positive Work Wenv = -PΔV Negative Work ΔV

Work Done ON gas Wgas = PΔV Negative since ΔV is negative Wenv = -PΔV
Positive since ΔV is negative ΔV

Calculate the work done by a gas that expands from 0. 020 m3 to 0
Calculate the work done by a gas that expands from m3 to 0.80 m3 at constant atmospheric pressure. How much work is done by the environment when the gas expands this much? V1 = m3 V2 = 0.80 m3 Wgas = PΔV Wgas = Pa·0.078m3 = 78000J Wgas = J

What is the change in volume of a cylinder operating at atmospheric pressure if its internal energy decreases by 230 J when 120 J of heat are removed from it? ΔU = -230 J Q = -120 J ΔU = Q+W W = ΔU - Q W = -230 J – (-120 J) = 110 J Wgas = PΔV ΔV = 110 J / Pa ΔV = m3

a. WAB = PVAB = P ∙ 0 = 0 J W ΔU Q -53 J A  B a. 0 J b. B  C -130 J
d. C  A e. 150 J a. WAB = PVAB = P ∙ 0 = 0 J

b. UAB = QAB - WAB = -53 - 0 = -53 J W ΔU Q -53 J A  B a. 0 J b.
B  C -130 J c. -280 J d. C  A e. 150 J b. UAB = QAB - WAB = = -53 J

c. UBC = QCB - WBC = -280 – (-130) = -150 J W ΔU Q -53 J A  B a. 0 J
d. C  A e. 150 J c. UBC = QCB - WBC = -280 – (-130) = -150 J

d. UAB + UBC + UCA = 0 UCA = - UAB – UBC = -53 – (-150) = +203 J W ΔU
Q -53 J A  B a. 0 J b. -53 J B  C -130 J c. -150 J -280 J d. +203 J C  A e. 150 J d. UAB + UBC + UCA = 0 UCA = - UAB – UBC = -53 – (-150) = +203 J

e. QCA = UCA + WCA UCA = - 203 + 150 = 353 J W ΔU Q -53 J A  B a. 0 J
B  C -130 J c. -150 J -280 J d. +203 J C  A e. +353 J 150 J e. QCA = UCA + WCA UCA = = 353 J

Work (isobaric) WAB > WCD P
Where we are considering work done BY the gas A B P2 WAB = P2ΔV C D P1 WCD = P1ΔV V V1 V2

Work is path dependent P Where we are considering work done BY the gas
WABD > WACD A B P2 WABD C P1 D WACD V1 V2 V

Work done by a cycle When a gas undergoes a complete cycle, it starts and ends in the same state. The gas is identical before and after the cycle, so there is no identifiable change in the gas. DU = 0 for a complete cycle. The environment, however, has been changed.

Work done by a cycle P Work done by the gas is equal to the area circumscribed by the cycle Work done by gas is positive for clockwise cycles, negative for counterclockwise cycles. B A P2 WABCD P1 C D V1 V2 V Work done by environment is negative of work done by gas.

Second Law of Thermodynamics
No process is possible whose sole result is the complete conversion of heat from a hot reservoir into mechanical work. (Kelvin-Planck statement.) No process is possible whose sole result is the transfer of heat from a cooler to a hotter body. (Clausius statement.)

Heat Engines Heat Engines and Carnot Cycle Efficiency

Heat Engines Heat engines can convert heat into useful work.
According to the 2nd Law of Thermodynamics. Heat engines always produce some waste heat. Efficiency can be used to tell how much heat is needed to produce a given amount of work. NOTE: A heat engine is not something that produces heat. A heat engine transfers heat from hot to cold, and does mechanical work in the process.

Heat Transfer Heat Source (High Temperature) QH QH = QC QC
Heat Sink (Low Temperature) QH = input heat QC = magnitude of rejected heat

Heat Engines Heat Source (High Temperature) QH QH = QC + W QC
Heat Sink (Low Temperature)

Work and Heat Engine QH = W + QC
Heat Source (High Temperature) QH = W + QC QH: Heat that is put into the system and comes from the hot reservoir in the environment. W: Work that is done by the system on the environment. QC: Waste heat that is dumped into the cold reservoir in the environment. QH W QC Heat Sink (Low Temperature)

Efficiency of Heat Engine Efficiency = W/QH = (QH - QC)/QH
W: Work done by engine on environment QH: Heat absorbed from hot reservoir QC: Waste heat dumped to cold reservoir Efficiency is often given as percent efficiency.

A piston absorbs 3600 J of heat and dumps 1500 J of heat during a complete cycle. How much work does it do during the cycle? QH = 3600J QC = 1500J QH = W + QC W = QH - QC W = 3600 J – 1500 J = 2100J

A certain coal-fired steam plant is operating with 33% thermodynamic efficiency. If this is a 120 MW plant, at what rate is heat energy used? Eff = W/QH = (QH - QC)/QH

Carnot Cycle P Heat In QH = QC + W Eff = W / QH Work V Heat Out
Isothermal expansion Work Adiabatic compression Adiabatic expansion Isothermal compression V Heat Out

Efficiency of Carnot Cycle
For a Carnot engine, the efficiency can be calculated from the temperatures of the hot and cold reservoirs. Carnot Efficiency = (TH - TC)/TH TH: Temperature of hot reservoir (K) TC: Temperature of cold reservoir (K)

Calculate the Carnot efficiency of a heat engine operating between the temperatures of 60 and 1500 oC. TC = 60 ºC TH = 1500 ºC Efficiency = (TH - TC)/TH Efficiency = ((1500 ºC + 273) – (60 ºC + 273) )/ (1500 ºC + 273) = 0.81 or 81 %

Entropy

Entropy… Entropy is disorder, or randomness.
The entropy of the universe is increasing. Ultimately, this will lead to what is affectionately known as “Heat Death of the Universe”. Does the entropy in your room tend to increase or decrease?

Fluids and Thermodynamics

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