22-Mec-B2 Environmental Control in Buildings · December 2014
Question 8 of 8: Water-source R-134a heat pump
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
Paper format. Professional Engineers of
Ontario / Engineers Canada annual examination, 07-Mec-B2 Environmental Control
in Buildings, December 2014. Three hours, open book, any non-communicating
calculator. Eight problems of 20 points each; candidates are required to solve
five. ASHRAE psychrometric charts (SI and IP) and an HFC-134a
pressure-enthalpy diagram are attached to the paper. All eight problems are
solved here.
Reference texts.
ASHRAE, Handbook — Fundamentals (Ch. 1 Psychrometrics, Ch. 16
Ventilation and Infiltration, Ch. 18 Nonresidential Cooling and Heating Load
Calculations, Ch. 19 Energy Estimating, Ch. 21 Duct Design).
McQuiston, Parker & Spitler, Heating, Ventilating and Air Conditioning:
Analysis and Design, 6th ed., Wiley.
W. P. Jones, Air Conditioning Engineering, 5th ed., Butterworth-Heinemann.
Stoecker & Jones, Refrigeration and Air Conditioning, 2nd ed., McGraw-Hill.
Carrier Air Conditioning Company, Handbook of Air Conditioning System
Design, Part 1 (the ESHF / apparatus-dew-point method used in Problem 1).
CSA B52 Mechanical Refrigeration Code; Canada's Ozone-depleting
Substances and Halocarbon Alternatives Regulations (SOR/2016-137); National
Building Code of Canada (vapour and air barriers).
Reading the numbers. Chart properties here are
computed from the ASHRAE psychrometric formulations rather than scaled off the
printed chart, so a candidate working graphically should expect agreement to about
the width of a pencil line — roughly ±0.3 °F on a dew point and
±1 % on a humidity ratio.
Given. A water-source heat pump on the R-134a cycle, with the compressor inlet and outlet states and the condenser exit temperature all specified, serving a house whose heat loss is known.
Given data — Problem 8
State / quantity
Symbol
Value
House heat loss
$q_H$
70,000 Btu/hr
Source water temperature
$t_{\mathrm{well}}$
$45^\circ\text{F}$
Compressor inlet (1)
$p_1$ / $t_1$
30 psia / $20^\circ\text{F}$
Compressor outlet (2)
$p_2$ / $t_2$
120 psia / $140^\circ\text{F}$
Condenser exit (3)
$p_3$ / $t_3$
120 psia / $90^\circ\text{F}$
House temperature (for Carnot)
$t_H$
$70^\circ\text{F}$
Find. The compressor power, the heat absorbed from the well water, the actual and Carnot coefficients of performance, a comparison with resistance heating, and a discussion of ground-source heat pumps.
Problem 8 — the cycle on the HFC-134a pressure-enthalpy diagram attached to the paper. Compression 1→2 carries the vapour into the superheat region; the condenser 2→3 rejects heat to the house; the expansion valve 3→4 is isenthalpic; and the evaporator 4→1 takes heat from the well water.
Approach. Read the three enthalpies off the attached pressure-enthalpy diagram, close the mass flow from the condenser duty (which must equal the house loss), then obtain the compressor work, the evaporator duty and the coefficients of performance in turn.
Read the enthalpies from the attached chart. At 30 psia the saturation temperature is 15.4°F, so state 1 at 20°F carries 4.6°F of superheat and $h_1 = 106.3\ \text{Btu}/\text{lb}$. At 120 psia the saturation temperature is 90.5°F; state 2 at 140°F is well into the superheat region, $h_2 = 127.4\ \text{Btu}/\text{lb}$, and state 3 at 90°F is barely subcooled, $h_3 = 41.6\ \text{Btu}/\text{lb}$. The expansion valve is isenthalpic, so $h_4 = h_3$.
Close the mass flow on the condenser. The condenser must supply the whole house load, so $$\dot m = \frac{q_H}{h_2-h_3} = \frac{70{,}000}{127.4-41.6} = 816\ \text{lb}/\text{hr}$$ rejecting 85.8 Btu per pound of refrigerant circulated.
(a) Compressor power. The work of compression is $w = h_2-h_1 = 21.1\ \text{Btu}/\text{lb}$, so $$\dot W = \dot m\,(h_2-h_1) = 816(21.1) = 17{,}250\ \text{Btu}/\text{hr} = \boxed{5.06\ \text{kW}}$$
(b) Heat absorbed from the well water. The evaporator takes the refrigerant from state 4 to state 1, $$q_L = \dot m\,(h_1-h_4) = 816(106.3-41.6) = \boxed{52{,}750\ \text{Btu}/\text{hr}}$$ and the cycle closes: $52{,}750 + 17{,}250 = 70{,}000\ \text{Btu}/\text{hr}$, exactly the house load, which confirms the chart readings.
(c) Actual coefficient of performance. For a heat pump the useful output is the heat delivered, so $$\mathrm{COP} = \frac{q_H}{\dot W} = \frac{70{,}000}{17{,}250} = \boxed{4.06}$$
(c) Carnot coefficient of performance. Between the reservoirs the question names — well water at 45°F (504.7 R) and the house at 70°F (529.7 R) — $$\mathrm{COP}_{\mathrm{Carnot}} = \frac{T_H}{T_H-T_L} = \frac{529.7}{529.7-504.7} = 21.2$$ The actual cycle reaches only 19 % of this, which looks poor until one notices that the machine is not working between 45 and 70°F at all: it evaporates at 15.4°F and condenses at 90.5°F, and the Carnot value between those temperatures is 7.32. The real cycle achieves 55 % of that, a normal second-law efficiency. The gap between 21.2 and 7.32 is the cost of the heat-exchanger temperature differences, and it is where a designer would look first for improvement.
(d) Comparison with electric resistance heating. A resistance heater must supply the whole 70,000 Btu/hr as electricity, $$\dot W_{\mathrm{res}} = 70{,}000\ \text{Btu}/\text{hr} = \boxed{20.5\ \text{kW}}$$ against 5.06 kW for the heat pump — a factor of 4.06, the COP itself. In an average Canadian heating season the difference is on the order of 20,000 kWh for a house of this load, and it is the whole economic argument for the heat pump. Resistance heating remains attractive only for its negligible capital cost and as a supplementary source during the coldest hours.
(e) Ground-source heat pumps. This machine is a water-source heat pump using an open-loop groundwater source, and the reason it performs so much better than an air-source machine is visible in the numbers: it evaporates at 15.4°F against a 45°F source, whereas an air-source unit on the same January night would have to evaporate below a −20°C outdoor temperature, roughly halving the COP exactly when the load is greatest. Ground temperatures below about 6 m are stable at close to the local mean annual air temperature — 6 to 10°C across most of southern Canada — so the source is both warmer and steadier than the air, and the same loop provides efficient cooling in summer by rejecting heat to the ground. The costs are the ground loop itself, which typically doubles installed cost and dominates the payback; the need for adequate land or borehole depth; and, for an open-loop system like this one, groundwater quantity, quality and the provincial regulatory approvals for withdrawal and reinjection, along with fouling and corrosion risk in the evaporator. Closed vertical boreholes with a water-glycol loop avoid the water-quality problems at higher drilling cost. Long-term thermal balance also matters: a loop that is only ever used for heating gradually cools the ground around it, so in a heating-dominated Canadian climate the loop must be sized for the seasonal energy extracted, not merely for the peak load.
The cycle analysed here is a competent but unremarkable one, and the two Carnot comparisons are worth keeping side by side because they answer different questions. The reservoir-based figure of 21.2 states what a perfect machine could do with this source and this sink, and its distance from 4.06 measures everything lost in the whole installation, heat exchangers included. The cycle-temperature figure of 7.32 states what a perfect machine could do with the evaporating and condensing temperatures this equipment actually establishes, and its distance from 4.06 measures only the compressor's own irreversibility. Improving the first without improving the second means bigger heat exchangers and more pumping; improving the second means a better compressor.