First Thermodynamics Examples Sheet .. and more 1. If the specific heat of water is 4.2 kJ kg-1 C-1 and the acceleration of gravity is 9.81 m s-2, estimate the temperature difference between the top and bottom of the Pistyll Rheadr waterfall in Wales (height 73 m). (Hint: consider 1 kg of water negotiating the fall). Discuss any factors which might affect the accuracy of this answer. 2. Assuming that 80% of the energy supplied to a 1.5-kw electric kettle goes to heat the water in it, how long will the kettle take to heat one litre of water from 20 C to 100 C? 3. It is found that a 60-horsepower laboratory petrol engine will only run for 15 minutes at full power on its full tank of 2 gallons of petrol whose density is 0.8 kg/litre and calorific value 42 000 kJ/kg. You are also given that 1 gallon = 4.7 litres and that 1 horsepower = 0.746 kw. Calculate (i) The thermal energy released by burning the 2 gallons of petrol. (ii) The mechanical energy delivered in the same time. (iii) The efficiency of the engine. 3. Determine the quantities Q, W and E for the following operations. You are given the following: PV = mRT, where R = 287 J kg-1 C-1 kg-1 for air Cp = 1.007 kJ kg-1 C-1 Cv = 0.72 kJ kg-1 C-1 Remember - ADIABATIC means no heat is added or removed CONSTANT VOLUME means no work is done ISOTHERMAL means no change in internal energy E (a) 1 kg of air is heated from 20 C to 45 C at constant volume. (b) As (a) but at constant pressure. [(a) Q = E = 18 kJ, W = 0; (b) Q = 25.175 kJ, E = 18 kJ, W = 7.175 kJ)] 4. 1 kg of air expands isothermally at 18 C from 100 000 Pa to 50 000 Pa. Determine its final volume, using PV = mRT (remember T is in degree ABSOLUTE) [Some useful relations (NB - all for non-flow processes) These relations all apply per kilogramme of the "working fluid" Constant volume Work E Q Zero Cv(T2 - T1) Cv(T2 - T1) Cv(T2 - T1) Cp(T2 - T1) Constant pressure R(T2 - T1) For constant-pressure, the work can also be calculated as the pressure times the change in volume. It can be calculated as pdv for all processes (which is how the polytropic expressions were calculated) but that is rather hard work! Also: PV = mRT (General Gas Equation - R = 287 J kg-1 K-1 The following two apply to any constant mass of gas: Adiabatic changes: PV = constant Isothermal changes: PV = constant An example of their use A single-cylinder engine operates on the following series of events (or cycle). 1. 2. 3. 4. 5. 250 ml of air at 20 C and atmospheric pressure (98 100 Pa) are ingested. This air is compressed adiabatically to a volume of 30 ml. It is now heated at constant volume by the addition of 0.058 kJ from the combustion of the fuel. The air is now allowed to expand adiabatically back to a volume of 30 ml. The air and spent fuel are now exhausted to atmosphere, undoubtedly polluting it.. For the compression, we need to know the mass of the air and the pressure and temperature reached. The mass is easily calculable by PV = mRT .. giving m = PV/RT. 98100 0.25 10-3 = m 287 293, so m = .292 10-3 kg We can also easily calculate the final pressure from P1V1 = P2V2 and P2 = P1(V1/V2) . It started at 250 ml and 98 100 Pa and finished at 30 ml, so... P2 = 98 100(250/30)1.4 pascal = 1.91 MPa and the temperature from PV = mRT: T2 = PV/(mR) = 1.91 106 30 10-6 / (.292 10-3 287) = 684 K so the internal energy change will be mCv(T2 - T1) = 0.72 .292 10-3 (684 - 293) = 0.082 kJ which equals the work done on the system, as no heat exchange occurred. This next section in italics calculates the work done from first principles to convince me that the answer is right. The work done is calculated by pdv given that pvn = constant ... n = 1.4 for air and we can work out the constant from 98100 (0.25 10-3)1.4 = 0.889. So p=0.889/v1.4 = 0.889v-1.4. By substitution, the integral becomes pdv = (0.889v-1.4)dv = [-0.889/0.4 v-0.4] between the two volumes 250 ml (250 10-6 m3) and 30 ml (30 10-6 m3). If we substitute these values in the usual way for definite integrals, we obtain: -0.889/0.4 [(30 10-6)-0.4 - (250 10-6)-0.4] = 82 J = 0.082 kJ (actually minus because the work was done on the system, not by it). As the compression was adiabatic, Q = 0, so U must also be 0.082 kJ. This gives a final temperature of T2, where: U = Cv(T2 - T1) = 0.72 .292 10-3 (T2 - 293) = .082 giving T2 = 682 K.} The energy is now added at constant volume by the fuel burning. Q = 0.058 kJ, so the temperature will rise by 0.058/(0.72 .292 10-3) = 276 K, giving a final temperature of 276 + 682 = 956 K. The heat from the fuel was added at constant volume, so the resulting pressure can be calculated from PV = mRT. P = .292 10-3 287 956/(30 10-6) = 2.67 MPa We can now calculate the final pressure and temperature at the end of the adiabatic expansion stage of the cycle (the 'power stroke'). The 'before and after' volumes are now 30 ml and 250 ml, so the final pressure will be: P2 = P1(V1/V2) = 2.67 106 (30/250)1.4 = 137 200 Pa and we calculate the temperature by PV = mRT: T = PV/(mR) = = 137 200 250 10-6/(.292 10-3 287) 409 K So the loss of internal energy is mCv(T1 - T2) = .292 10-3 0.72 (956-409) = 0.115 kJ, which is the work done in the expansion. We can calculate the efficiency from these figures. Heat supplied = 0.058 kJ Work done = (0.114 - .082) = 0.032 kJ (note that we had to subtract the work done on the gas during the compression!) So it looks as if the efficiency is 0.032/0.058 = 55 % ! In fact it will not be as high as this, because the engineering limitations will prevent us from using such a large heat input. We (you?) will calculate what the answer would have been if the heat from the fuel were only 0.03 kJ.