| Title | Comparison of U-tube boreholes and a thermosiphon on heat pump performance in an aquifer |
| Publication Type | thesis |
| School or College | College of Engineering |
| Department | Mechanical Engineering |
| Author | Workman, Christopher B. |
| Date | 2011-05 |
| Description | Reducing our energy consumption and dependence on fossil fuels has become a common social, political and engineering goal. Heating and cooling of buildings account for a large percentage of the energy consumption in the United States. Improving HVAC efficiency in buildings can play a major role in reducing energy use. Small scale geothermal systems that utilize low-grade heat have gained popu-larity as a way to reduce HVAC energy consumption. U-tubes and thermosiphons are two di fferent technologies designed to transfer heat to and from the ground in order to provide building heating and cooling. This thesis presents a short and long term experimental analysis. The short term analysis compares the performance of these technologies. The long term analysis focuses on the U-tubes, looking at the COP of the overall system during the course of a heating season and comparing temperatures for a theoretical air source heat pump system. |
| Type | Text |
| Publisher | University of Utah |
| Subject | borehole; heat pump; thermosiphon; U-tube; geothermal systems |
| Dissertation Institution | University of Utah |
| Dissertation Name | Master of Science |
| Language | eng |
| Rights Management | © Christopher B. Workman |
| Format | application/pdf |
| Format Medium | application/pdf |
| Format Extent | 75,639,368 bytes |
| Identifier | us-etd3,31734 |
| Source | Original housed in Marriott Library Special Collections, TH7.5 2011 .W67 |
| ARK | ark:/87278/s6tq6g99 |
| DOI | https://doi.org/doi:10.26053/0H-MPMR-JZ00 |
| Setname | ir_etd |
| ID | 194752 |
| OCR Text | Show COMPARISON OF U-TUBE BOREHOLES AND A THERMOSIPHON ON HEAT PUMP PERFORMANCE IN AN AQUIFER by Christopher B. Workman A thesis submitted to the faculty of The University of Utah in partial ful llment of the requirements for the degree of Master of Science Department of Mechanical Engineering The University of Utah May 2011 Copyright c Christopher B. Workman 2011 All Rights Reserved The U n i v e r s i t y o f Utah Graduate School STATEMENT OF THESIS APPROVAL The thesis of has been approved by the following supervisory committee members: , Chair Date Approved , Member Date Approved , Member Date Approved and by , Chair of the Department of and by Charles A. Wight, Dean of The Graduate School. ABSTRACT Reducing our energy consumption and dependence on fossil fuels has become a common social, political and engineering goal. Heating and cooling of buildings account for a large percentage of the energy consumption in the United States. Improving HVAC e ciency in buildings can play a major role in reducing energy use. Small scale geothermal systems that utilize low-grade heat have gained popu- larity as a way to reduce HVAC energy consumption. U-tubes and thermosiphons are two di erent technologies designed to transfer heat to and from the ground in order to provide building heating and cooling. This thesis presents a short and long term experimental analysis. The short term analysis compares the performance of these technologies. The long term analysis focuses on the U-tubes, looking at the COP of the overall system during the course of a heating season and comparing temperatures for a theoretical air source heat pump system. CONTENTS ABSTRACT : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : iii LIST OF FIGURES: : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : vi NOMENCLATURE: : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : viii CHAPTERS 1. INTRODUCTION : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : 1 1.1 Project Background . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 1.2 Motivation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 1.3 Novelty . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2 1.4 Hypotheses . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2 1.5 Ground Source Heat Pumps . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 1.5.1 Description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 1.5.2 Types . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4 1.5.3 Advantages . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4 1.5.4 Disadvantages . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 1.5.5 Current Research . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 1.6 Thermosiphon . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8 1.6.1 Description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8 1.6.2 Advantages . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8 1.6.3 Disadvantages . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 1.6.4 Current Research . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 2. METHODS : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : 12 2.1 Testing Methodology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 2.1.1 Short Term Comparison . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 2.1.2 Long Term U-tube Analysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 2.1.3 Energy Balance . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 2.1.3.1 Thermocouples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 2.1.3.2 Flowmeter . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 2.1.3.3 Powermeter . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17 2.1.3.4 Data Logger . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17 2.2 Design . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17 2.2.1 Thermosiphon System . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17 2.2.1.1 Thermosiphon Boiling Enhancement . . . . . . . . . . . . . . . . . 17 2.2.1.2 Thermosiphon Heat Exchanger . . . . . . . . . . . . . . . . . . . . . 20 2.2.1.3 Three-way Valves . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20 2.2.2 Thermocouple Junctions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20 2.3 Manufacturing . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26 2.3.1 Thermosiphon . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26 2.3.2 Thermocouples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 30 2.4 Installation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 30 2.4.1 U-tube System . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 30 2.4.2 Thermosiphon System . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 37 2.5 Challenges . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 38 2.5.1 Field experiment vs. controlled lab environment . . . . . . . . . . . . 38 2.5.2 Human factors . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 38 2.5.3 Weather . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 39 2.5.4 Inexperience . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 40 3. U-TUBE HEAT TRANSFER : : : : : : : : : : : : : : : : : : : : : : : : : : : : : 41 3.1 Short Term Analysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41 3.1.1 U-tube Inlet and Outlet Temperatures . . . . . . . . . . . . . . . . . . . 41 3.1.2 U-tube Instrumentation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41 3.1.3 Temperature vs. Time for the Heavily Monitored U-tube . . . . . 43 3.1.4 Immersed compared to surface mounted thermocouple temper- atures . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 46 4. THERMOSIPHON HEAT TRANSFER : : : : : : : : : : : : : : : : : : : : 48 4.1 Short Term Analysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 48 4.1.1 Temperature vs. time at multiple locations . . . . . . . . . . . . . . . . 48 4.1.2 Immersed compared to surface mounted thermocouple temper- atures . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 49 5. THERMAL EXTRACTION AND HEAT PUMP ANALYSIS : 52 5.1 Heat absorbed by the heat pump . . . . . . . . . . . . . . . . . . . . . . . . . . . . 52 5.2 Heat absorbed by the heat pump per unit length of borehole . . . . . . 52 5.3 COP . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 53 5.3.1 Comparison of U-tube to Thermosiphon COP . . . . . . . . . . . . . 53 5.3.2 Seasonal U-tube COP . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 53 5.4 Comparison of ground source to an air source heat pump . . . . . . . . . 56 6. CONCLUSIONS : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : 59 6.1 Findings . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 59 6.2 Challenges . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 59 6.3 Recommendations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 59 REFERENCES: : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : 61 v LIST OF FIGURES 1.1 Interfering Heat Transfer in U-tubes . . . . . . . . . . . . . . . . . . . . . . . . . . 3 1.2 U-tube Operating Principle . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5 1.3 Thermosiphon Operating Principle . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 2.1 Schematic Drawing of the Overall Experimental Set-up . . . . . . . . . . . . 14 2.2 Immersed Thermocouples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16 2.3 Flowmeter . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16 2.4 Powermeters . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18 2.5 Current Transformers . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18 2.6 WattNodes . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 2.7 Data Logger . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 2.8 Thermosiphon Heat Exchanger . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 21 2.9 Sprinkler Box for H.X. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 21 2.10 Three-way Valves . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 22 2.11 Heat Exchanger and Three-way Valve Enclosure . . . . . . . . . . . . . . . . . 22 2.12 Valve Enclosure . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 23 2.13 Valve Enclosure Access . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 23 2.14 Thermocouple Enclosure: Step 1 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 24 2.15 Thermocouple Enclosure: Step 2 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25 2.16 Thermocouple Enclosure: Step 3 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25 2.17 Thermocouple Enclosure: Final Product . . . . . . . . . . . . . . . . . . . . . . . 26 2.18 Thermosiphon Manufacturing: Step 1 . . . . . . . . . . . . . . . . . . . . . . . . . 27 2.19 Thermosiphon Manufacturing: Step 2 . . . . . . . . . . . . . . . . . . . . . . . . . 27 2.20 Thermosiphon Manufacturing: Step 3 . . . . . . . . . . . . . . . . . . . . . . . . . 28 2.21 Thermosiphon Manufacturing: Step 4 . . . . . . . . . . . . . . . . . . . . . . . . . 28 2.22 Thermosiphon Manufacturing: Step 5 . . . . . . . . . . . . . . . . . . . . . . . . . 29 2.23 Thermocouple Manufacturing: Step 1 . . . . . . . . . . . . . . . . . . . . . . . . . 30 2.24 Thermocouple Manufacturing: Step 2 . . . . . . . . . . . . . . . . . . . . . . . . . 31 2.25 Thermocouple Manufacturing: Step 3 . . . . . . . . . . . . . . . . . . . . . . . . . 31 2.26 Thermocouple Manufacturing: Step 4 . . . . . . . . . . . . . . . . . . . . . . . . . 32 2.27 Thermocouple Manufacturing: Step 5 . . . . . . . . . . . . . . . . . . . . . . . . . 32 2.28 The Borehole Drilling Rig: View 1 . . . . . . . . . . . . . . . . . . . . . . . . . . . . 33 2.29 The Borehole Drilling Rig: View 2 . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34 2.30 Drill Bits . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34 2.31 U-tube Insertion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35 2.32 Vertical U-tube After Installation . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35 2.33 Heat Pump and Inline Pump . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36 2.34 Bottom of a U-tube . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36 2.35 Thermosiphon Coupling . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 37 2.36 Snow During Construction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 39 3.1 U-tube Inlet and Outlet Temperatures . . . . . . . . . . . . . . . . . . . . . . . . . 42 3.2 U-tube Borehole 1 Vertical Section View . . . . . . . . . . . . . . . . . . . . . . . 44 3.3 U-tube Temperatures vs. Time . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 45 3.4 Immersed vs. Surface Temperatures for the U-tube System . . . . . . . . . 47 4.1 Thermosiphon Temperatures vs. Time . . . . . . . . . . . . . . . . . . . . . . . . . 50 4.2 Immersed vs. Surface Temperatures for the Thermosiphon System . . . 51 5.1 Q-low per Foot of Borehole Comparison . . . . . . . . . . . . . . . . . . . . . . . 54 5.2 COP Comparison . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 55 5.3 Average Daily COP . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 57 5.4 Comparison of U-tube System Temperatures to Ambient Air Temper- atures . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 58 vii NOMENCLATURE COP coe cient of performance COPHP;rev reversible COP of a heat pump, COPHP;rev = TH THTL TH temperature of the high-temperature reservoir TL temperature of the low-temperature reservoir _Q L the rate of heat absorbed by the heat pump from the geothermal system m_ the mass ow rate of the glycol mixture cp speci c heat of the glycol mixture T the temperature di erence of the glycol mixture between the heat pump inlet and outlet _V the volumetric ow rate of the glycol mixture the density of the glycol mixture _Q L;normalized the rate of heat absorbed by the heat pump from the geothermal system per unit length of borehole, _Q L;normalized = _Q L Total Borehole Length COPHP coe cient of performance of any heat pump, COPHP = QH Wnet QH the amount of heat rejected from the heat pump Wnet the electrical work input to the heat pump QL the amount of heat absorbed by the heat pump from the geothermal system _W net the rate of electrical work input to the heat pump CHAPTER 1 INTRODUCTION 1.1 Project Background This experiment was part of a whole house energy monitoring project. The project was a joint e ort between the University of Utah Mechanical Engineering Department and ConSol. It was funded by a grant from Building America, a branch of the Department of Energy. The goal of the project to quantify the energy savings from a variety of new, `green' technologies in the residential construction industry. These technologies were implemented in a new housing development in Park City, UT. The system of particular interest for this study was the ground source heat pump system which utilized vertical U-tubes as the ground loop heat exchanger. Another type of ground heat exchanger called a thermosiphon was integrated into the heat pump system so that it could be compared to the U-tube system. English units are used throughout this document due to the requirements of these other parties. 1.2 Motivation Reducing our energy consumption and dependence on fossil fuels has become a common social, political and engineering goal. Motivations for this goal range from concerns about anthropogenic climate change to improving air quality to reducing energy costs to decreasing dependence on foreign energy sources. Growing energy demands and increasing concerns about the environmental impact of generating energy from fossil fuels continue to drive the pursuit of clean, carbon free energy generation on the production side and increasing e ciency on the demand side. According to DR International (2009), buildings consumed 39% of the U.S. primary energy in 2006. Therefore improved e ciency in this area can play a major role in 2 reducing energy use. No matter the motivation, reducing the energy consumption of buildings is one of the best ways to achieve these goals. One of the systems that is growing increasingly popular to reduce building energy usage is the Ground Source Heat Pump (GSHP) system. Another emerging technology is the thermosiphon. The motivation for this thesis is to better understand the characteristics of these systems in order to better integrate them into building designs and further re ne sizing procedures. This improved understanding will help to further re ne system sizing and design techniques so that energy e ciency can be improved. 1.3 Novelty The majority of research on GSHP systems has been focused on mathematical models simulating the subsurface heat transfer occurring. There has been little experimental veri cation of the simulation results from these mathematical models. The novelty of this experiment is that while there have been thousands of GSHP installations around the world (Florides and Kalogirou, 2007), there have been very little experimental data gathered on these systems. One of the only documented experiments was conducted in China on a large cylindrical piling that had U-tubes and instrumentation installed (Nam et al., 2008). 1.4 Hypotheses The major design aw with U-tube boreholes is the close proximity of the inlet uid pipe to outlet uid pipe within the borehole (Figure 1.1.) This con guration dramatically reduces the heat transfer potential of the system because the uid on its way down the borehole is not only in uenced by the temperature of the surrounding soil, but also by the temperature of the uid in heading back up the opposite side of the U-tube. The thermosiphon transfers heat based on a phase change in a single pipe. The hypothesis is that the thermosiphon will yield higher heat transfer rates per foot of drilling because it will not su er from the \cancellation" of the GSHP system. COP, coe cient of performance, is a term used to quantify of the e ciency of a heat pump system. The thermodynamic de nition of the reversible COP of a 3 Figure 1.1: Interfering Heat Transfer in U-tubes. When the cool uid enters the U-tube it not only extracts heat from the surrounding grout and soil, but also from the warmer uid exiting the other side of the U-tube. Extracting heat from the warmer, exiting side of the U-tube lowers the exiting uid temperature which decreases the e ectiveness of U-tube as a heat exchanger. heat pump is, COPHP;rev = TH THTL . As heat is removed from the ground during the heating season, it is predicted that the ground temperature, TL, will decrease, causing the COP to decrease. The energy monitoring equipment on this system allows for the actual measurement of these temperature changes, not just predicted based on a mathematical model. 1.5 Ground Source Heat Pumps 1.5.1 Description GSHP systems couple a heat pump to an in ground heat exchanger in order to exploit the relatively constant soil temperatures that occur underground below a depth of about 5 meters (Florides and Kalogirou, 2007). The idea is that the ground temperature is thermodynamically favorable to the ambient air temperature, lead- ing to a higher COP. In many geographic locations, this constant temperature is 4 a more favorable thermal energy source for heating than air if the air temperature is cooler and for cooling if the air is warmer (Omer, 2008). A diagram explaining the operating principle of a vertical U-tube heat exchanger can be seen in Figure 1.2. There are four major components in a GSHP system. The rst component is a subterranean heat exchanger, which is typically a closed loop network of high- density polyethylene pipe. The piping network lled with a working uid, typically a mixture of water with ethylene glycol or methanol. The second component is a heat pump, which uses a refrigeration cycle, to supplement the heating or cooling from the subterranean heat exchanger. The third component is an inline pump to circulate the working uid between the subterranean heat exchanger and the heat pump. The fourth component is a system to distribute the intended space conditioning, which could be a forced air or radiant heating system. 1.5.2 Types There are many di erent types of GSHP systems. The two most general cat- egories are open and closed loop systems, each having their own advantages and disadvantages. Open systems could consist of air passing through tubes buried in the ground or water injection/recovery wells. Closed systems consist of horizontal or vertical networks of piping buried underground (Florides and Kalogirou, 2007; Omer, 2008; Rawlings and Sykulski, 1999). There is not one best type of GSHP system, design choices are made based on site, budget, and installation factors. 1.5.3 Advantages GSHPs are a more mature technology than thermosiphons. This maturity is the greatest advantage of GSHPs compared to thermosiphons. Well established installation procedures, design parameters and materials/tools speci c to building these systems already exist. All of these factors result in more durable, easier to design systems. 5 Figure 1.2: U-tube Operating Principle. The U-tube extracts heat from the ground by using a long pipe as a heat exchanger in the ground. A uid, cooler than the ground enters the U-tube. As it travels the length of the U-tube, it extracts heat from the warmer ground and exits the U-tube at a warmer temperature than when it entered. 6 Ambient Air Temperature = T_air Ground surfac7 Exiting Fluid ........ - at Tflpjd ..... Heat- Heat- Heat- Heat- Heat- Heat- ---:::::s ........- Entering Fluid , at TfIuid,iDIoI -Heat -Heat -Heat -Heat Surrounding Ground Temperature = T JIl'01ID'i Relations in an ideal scenario- T ........ > TfIufd, ...... > TfIufd,_ T ........ > TfIufd, ...... > T_air U-tube 7 1.5.4 Disadvantages The inline pump and heat pump increase the initial capital investment and operating cost compared to a passive technology where this equipment is not necessary, such as thermosiphons. The other primary disadvantage of closed loop GSHPs is that it is very di cult to design a system where the inlet and outlet ows of the system do not thermally interfere with one another. Figure 1.1 shows the performance robbing heat transfer that occurs in the U-tube borehole. 1.5.5 Current Research There has been a substantial amount of research involving GSHPs in recent years. Most of the current research has been focused on numerical models of the underground heat transfer (Nam et al., 2008; Yavuzturk et al., 1999). Short term behavior modeling is important in order to determine system energy consumption on a given day or on an hour-by-hour basis (Yavuzturk and Spitler, 1999; Xu and Spitler, 2006). Long term models are important because they evaluate the e ect of heat rejection and extraction on ground temperature over the period of years, in order to mitigate thermal saturation of the surrounding ground, while with the goal of minimizing the system borehole length for cost control (Nam et al., 2008; Yavuzturk et al., 1999). This is by no means the full extent of the published modeling research, but represents the general direction of current research in this area. Another pertinant research area in GSHPs has been borehole thermal conduc- tivity testing. In-situ thermal conductivity is one of the most important design parameters, but also the most di cult to ascertain. This research is particularly relevant because thermal conductivity for this experimental site was abnormally high as a result of ground water ow. This arti cially high, measured, thermal conductivity does not represent the actual value, but is in ated due to advection. This measured value of thermal conductivity only represents an apparent thermal conductivity, which will a ect system performance for better or worse, according to Chiasson et al. (2000). To the author's knowledge, the major hole in low grade geothermal research 8 is the lack of experimental data. The novelty of this experiment is that it gives greater insight into the underground heat transfer. Better understanding of the underground formation temperature response to heat extraction will re ne sizing practices, resulting in reduced initial capital and operating costs for GSHP systems. 1.6 Thermosiphon 1.6.1 Description A thermosiphon is a superconducting device that transfers heat with a theoret- ical temperature di erence of zero. A thermosiphon is a pipe that is evacuated and charged with a refrigerant. When it is positioned at a slope, with a heat source on the bottom and a heat sink at the top, the thermosiphon begins to function as a superconductor. The heat source at the bottom induces vaporization of collected liquid, the density di erence of this vapor to the surrounding liquid causes it to rise in the pipe, until it reaches the heat sink at the top of the tube. The heat sink induces condensation, the resulting liquid is now denser than the surrounding vapor causing it to sink in the tube, returning to the bottom of the tube for the cycle to repeat. A diagram of the thermosiphon operating principle can be seen in Figure 1.3. 1.6.2 Advantages The biggest advantage of thermosiphons is that they passively extract heat from the ground in the con guration shown in Figure 1.3. There is no need for a pump to circulate the working uid in order for heat transfer to occur in this application of thermosiphons. Another advantage of the thermosiphon is a higher heat transfer rate per foot of drilling (Udell et al., 2011). The single pipe design of a thermosiphon means that it is not susceptible to the ine cient, cancellation that occurs in U-tube boreholes. It also has as an extremely high apparent thermal conductivity, due to the phase change nature of the design (Dunn and Reay, 1994). 9 Figure 1.3: Thermosiphon Operating Principle. Thermosiphon operation is driven by a phase change process. As heat moves from the warm ground to the cool air reservoir, liquid refrigerant in the bottom thermosiphon, the refrigerant undergoes a phase change, vaporization, and is converted from a liquid to a vapor. Once refrigerant starts to vaporize it becomes less dense than the surrounding liquid, causing it to rise. As it rises to the top of the thermosiphon, heat is extracted from the top of the thermosiphon to the cooler heat exchanger. This loss of heat caused the refrigerant to undergo a phase change, condensation, and is converted from a vapor to a liquid. The liquid, now denser than surrounding vapor, falls back down the walls of the thermosiphon to repeat the process. 10 -Heat Heat- -Heat Heat- Heat- -Heat Heat- -Heat Heat Exchanger Thermosiphon Ambient Air Temperature = T_air und Surface Surrounding Ground Temperature = T gmmuI Relations in an ideal scenarioTgmmuI > TIOf > TIIX > T_air 11 1.6.3 Disadvantages The immaturity of thermosiphons in HVAC applications makes installation much more challenging. There are no established installation procedures or mate- rials. There are no contractors who are experienced in installing these systems. All of these factors increase the potential for issues with proper installation, durability and serviceability which ultimately means unforeseen expense of the system. The other disadvantage of the thermosiphon is that this passive extraction con guration is limited to heating applications. The thermosiphon is essentially a pipe lled with a gas that is above atmospheric pressure. This means that the thermosiphon poses a slight danger because it is a form of pressure vessel. If there is a small leak a thermosiphon system is more susceptible to stop functioning than a GSHP system, because the refrigerant vapor can escape very quickly causing a pressure drop. This creates a challenge because it demands an absolutely leak proof system for operation. 1.6.4 Current Research One of the most publicized applications of thermosiphons was the trans-Alaska oil pipeline. The pipeline uses heat pipes in the supports in order to prevent melting of the permafrost (Dunn and Reay, 1994). Heat pipes have been used by Japanese researchers to extract geothermal heat for snow melting applications (Tanaka et al., 1982). This snow melt application has had moderate success. A more recent application of the thermosiphon is thermal energy storage. This application is being studied by Dr. Kent Udell's laboratory at the University of Utah. The concept is to use thermosiphons arrays in the ground as a means of passive energy storage in the winter, in order to utilize this resource as a means for ultra-high e ciency air conditioning during the summer months (Udell et al., 2011, 2009). CHAPTER 2 METHODS 2.1 Testing Methodology The system testing consisted of a short term comparison of the U-tube system to the thermosiphon system then a long term analysis of the U-tube system. 2.1.1 Short Term Comparison The goal for the short term comparison was to run both the U-tube and ther- mosiphon systems each for at least 3 hours continuously during the same day in order to get an experimental performance comparison for the two systems in winter heating mode. This GSHP system does not typically run continuously for longer than 15 to 20 minutes while maintaining a constant interior set-point temperature during typical operation. The reasoning for running the system continuously for such a long period of time is that it takes roughly 30 minutes for the thermocouple readings to stabilize, in order to make meaningful relations. To get the heat pump system to run continuously, it was prevented from reaching its set-point temperature by opening the windows in the room where the thermostat is located and setting the desired room temperature well above the outside air temperature. It was not possible to run both the U-tube and the thermosiphon system at the same time. The U-tube system was tested rst, then the thermosiphon system was tested, each for over 3 hours on November 22nd, 2010. 2.1.2 Long Term U-tube Analysis A long term analysis was carried out on the U-tube system throughout the majority of the winter heating season. The focus was to determine temperatures along the length of the U-tube and GSHP COP trends throughout the heating season. 13 2.1.3 Energy Balance The goal of measuring temperatures, QL and COP for both a U-tube and a thermosiphon system required sensors for measuring temperature, ow and power, along with integrating a thermosiphon into a U-tube GSHP system. A diagram of the experimental system lay-out is shown in Figure 2.1 and more detailed explana- tion of the systems can be found in the following sections. The purpose of all the monitoring equipment installed is to be able to perform an energy balance on the system. This required temperature, ow rate and power measurements. Thermocouples were used to measure temperature. Turbine ow meters were used to measure the ow rate. WattNodes and Current Transformers were used to measure the electrical power consumption to nd the work input to the heat pump and uid pump. 2.1.3.1 Thermocouples T-type thermocouples were used for measuring system temperatures. They were the cheapest, easiest to wire solution. Unlike some other temperature sensors, they do not require power to take a measurement. Unfortunately, thermocouples sacri ce the precision of other technologies, like thermistors. All of the thermocouples in this experiment were mounted on the outside diameter of the pipe, except for the heat pump inlet and outlet thermocouples in the rst oor mechanical room which were immersed thermocouples (Figure 2.2.) 2.1.3.2 Flowmeter Figure 2.3 shows the turbine based owmeter used to measure the glycol ow rate which outputs a hall pulse. 14 Figure 2.1: Schematic Drawing of the Overall Experimental Set-up. This is a schematic drawing of the overall experimental set-up including the mechanical components and the monitoring equipment. Thermocouples are indicated by black dots with magenta text. The thermocouples are mounted on the outer diameter of the associated pipe unless indicated as, `immersed.' Physical locations of equipment are indicated by the dash/dot lines and blue text. 15 '------'--- '-=c.=:.:==-=; ----.-- I 1'8 SOft .. t i ::- i -t ~ t 1'875ft - ~ Heat Pump I I Heat Pump Outlet I Located in the attic, ~above the second floor I ______________ .J ---------------l • Heat Pump Outlet - (Jmmened) I Located in the moobanical i room on 1he first floor __________ J - - - -~VlThree-way Valves - - lBi12 h IBIIJ I ..... i IDld Inlet ~ BlI2Ou1k:t BID 0uIIeI t I I I I I I I I E1hy1ene Glycol ~ I and Water Mix1me I I I I I I I I I I I I I I I I I I I I I '- '- I '- ~ ~ -If § i If '" .oc 16 Figure 2.2: Immersed Thermocouples. Immersed thermocouples installed in the rst oor mechanical room Figure 2.3: Flowmeter. The owmeter installed in the rst oor mechanical room 17 2.1.3.3 Powermeter The powermeter con guration consisted of a 50 amp Current Transformer, (CTs) on one leg of the two-phase power and a Continental Controls WNA-3Y- 208-P WattNode. Pictures of these components installed in the main breaker panel for the building are shown in Figures 2.4, 2.5 and 2.6. 2.1.3.4 Data Logger The data logger used to collect and store data from the sensors was a Campbell Scienti c CR1000. Figure 2.7 shows the unit installed in its enclosure with all of the associated sensor wiring. 2.2 Design 2.2.1 Thermosiphon System The goals for the thermosiphon system were to maximize heat extraction rates and to integrate it into the GSHP system so that heat could be transferred to the heat pump. 2.2.1.1 Thermosiphon Boiling Enhancement In order to maximize heat extraction rates, nucleation sites for boiling in the inside of the pipe had to be increased. The galvanized pipe was stu ed with a wire mesh and hardware cloth in order to achieve this result. The hardware cloth, berglass screen material, was intended to increase the pipe roughness, which provides more boiling sites, therefore increasing the heat transfer rate. The wire mesh was intended to create a frame inside the pipe which forced the hardware cloth to contact the inside surface of the pipe. 18 Figure 2.4: Powermeters. CTs installed just o of the panel and WattNodes stacked below the panel Figure 2.5: Current Transformers. Split-core CTs installed around the main power feed on the breaker panel. 19 Figure 2.6: WattNodes. WattNodes installed in the panel enclosure. Figure 2.7: Data Logger. The data logger and enclosure installed on the exterior of the building. 20 2.2.1.2 Thermosiphon Heat Exchanger A problem with integrating the thermosiphon into the GSHP system was the di erence in working uids. In order to solve this problem, a shell and tube heat exchanger was used to transfer thermal energy between the refrigerant in the thermosiphon and the propylene glycol in the GSHP system. The heat exchanger was installed at an incline so that the condensing refrigerant drains out of the heat exchanger more e ectively, returning to the thermosiphon (Figure 2.8.) The heat exchanger was enclosed with a sprinkler box, so that it was still accessible once the surrounding dirt was back lled (Figure 2.9.) 2.2.1.3 Three-way Valves The other challenge with integrating the thermosiphon into the GSHP system was diverting the glycol uid ow. In order to gather meaningful data, the loop from the heat pump must operate with both the thermosiphon and U-tube system independently. This was accomplished by installing a three-way diverting ball valve in both the supply and return propylene glycol lines (Figure 2.10.) A plastic drum was used to create an enclosure around the valves so that they had some protection once they were buried (Figure 2.11 and 2.12.) ABS pipes were installed directly over the valve adjustment handles so that the position of the valves could be changed once the valves were buried (Figure 2.13.) 2.2.2 Thermocouple Junctions Due to the unplanned con guration of the drill rig, it was necessary to cut the thermocouples for the heavily monitored U-tube borehole and thermosiphon short of the data logger during their installation. The wires had to be cut at the top of the boreholes at the elevation of the horizontal tubing because it was not possible to route the full length of wire, necessary to reach the data logger, through the drill rig in a con guration that made it possible to remove the drill casing. It also would have been di cult to get a wire label to stick and survive the drill casing removal process, so the wires were cut without labels. Once the drill casing was removed the location of the wires along the length of the U-tube and thermosiphon 21 Figure 2.8: Thermosiphon Heat Exchanger. The heat exchanger was mounted at an incline on top of the thermosiphon to enhance draining of condensed refrigerant to the thermosiphon. Figure 2.9: Sprinkler Box for H.X.. A sprinkler box providing access to ther- mosiphon heat exchanger and a thermocouple junction enclosure. 22 Figure 2.10: Three-way Valves. Three-way valves installed in the propylene glycol supply and return lines for the heat pump. Figure 2.11: Heat Exchanger and Three-way Valve Enclosure. The three-way valve enclosure shown with the thermosiphon heat exchanger. 23 Figure 2.12: Valve Enclosure. Hardware cloth was stapled to the valve enclosure to keep soil and debris out after the enclosure was buried. Figure 2.13: Valve Enclosure Access. A sprinkler box with ABS pipes providing access to three-way valves in the buried valve enclosure. 24 was deduced by measuring the resistance of each wire; the highest resistance wires were the longest, the lowest resistance wires being the shortest. At this point, the location of the each wire was known and the wire numbers were applied. Unplanned thermocouple junctions had to be made underground at the top of the U-tube and the thermosiphon. This required a durable, watertight connection which could be buried and weatherized the connections. Enclosures were made out of 4-inch nominal diameter ABS pipe. The pipe was cut into approximately 6-inch lengths with caps tted on each end. Holes were drilled in one of the caps, each hole being just large enough to pass one thermocouple wire through the cap (Figure 2.14). Once the wires were passed through the cap, they were stripped and standard electrical wire nuts were used to connect the corresponding wires (Figure 2.15). Epoxy was applied to the point where each wire penetrated the cap on both the inside and outside (Figure 2.16). Finally, the caps were ABS glued to the section of ABS pipe (Figure 2.17). Figure 2.14: Thermocouple Enclosure: Step 1. Thermocouples after being routed though the ABS cap at one end and connected with wire nuts. 25 Figure 2.15: Thermocouple Enclosure: Step 2. The thermocouple junction enclosure with the section of ABS pipe attached, before the second cap is attached. Figure 2.16: Thermocouple Enclosure: Step 3. The epoxy seals around where the thermocouple wires penetrate the ABS cap. 26 Figure 2.17: Thermocouple Enclosure: Final Product. The nished thermocouple junction enclosure. 2.3 Manufacturing 2.3.1 Thermosiphon To construct the thermosiphon, rst, the wire mesh and hardware cloth were cut to length and width (Figure 2.18). Second, the wire mesh was wrapped around the outside of the galvanized steel pipe it would eventually be installed in (Figure 2.19). This gave the wire mesh an initial cylindrical form. The wire mesh was then wrapped around a 1-inch diameter length of PVC pipe to give the wire mesh an even smaller diameter (Figure 2.20). The wire mesh was then laced into itself so that it formed a cylinder around the PVC pipe. Once the entire length of the wire mesh was laced into itself (Figure 2.21), the length of hardware cloth was wrapped around the wire mesh cylinder and the entire assembly was inserted into the galvanized steel pipe (Figure 2.22). Four 20-foot lengths of 1.5-inch, nominal-diameter, galvanized steel pipe were built according to the proceeding procedure. 27 Figure 2.18: Thermosiphon Manufacturing: Step 1. Wire mesh cut to length and width. Figure 2.19: Thermosiphon Manufacturing: Step 2. Wire mesh taking form around the outside of the galvanized pipe it was eventually installed inside of. 28 Figure 2.20: Thermosiphon Manufacturing: Step 3. The PVC pipe inside of the partially formed wire mesh cylinder. Figure 2.21: Thermosiphon Manufacturing: Step 4. The wire mesh cylinder once it has been formed. 29 Figure 2.22: Thermosiphon Manufacturing: Step 5. The wire mesh and hardware cloth assembly being inserted into the galvanized steel pipe. 30 2.3.2 Thermocouples O the shelf, premanufactured thermocouples were not an option for this project because the long thermocouple lengths meant exorbitant cost. Instead, 1000-foot spools of thermocouple grade wire were purchased and the thermocouples were manufactured in-house. This procedure was as follows; a length of thermocouple wire was measured and cut (Figure 2.23), an approximately 1-inch length of the outer jacket was stripped (Figure 2.24), an approximately 1-inch length of the insulation was stripped from each of the individual wires (Figure 2.25), the entire exposed length of the two individual wires was twisted together (Figure 2.26) and the exposed portion of wire was covered in two to three coats of liquid tape to weatherize (Figure 2.27). 2.4 Installation 2.4.1 U-tube System There were three U-tubes installed for the GSHP system. Each U-tube was between 80 and 100 feet long, generally shallow for a GSHP system, but deemed su cient due to an abnormally high apparent conductivity value for the soil based Figure 2.23: Thermocouple Manufacturing: Step 1. Thermocouple wire before the procedure. 31 Figure 2.24: Thermocouple Manufacturing: Step 2. Thermocouple wire with the outer jacket stripped. Figure 2.25: Thermocouple Manufacturing: Step 3. Thermocouple wire with the insulation stripped from the individual wires. 32 Figure 2.26: Thermocouple Manufacturing: Step 4. Thermocouple wire with the individual wires twisted together. Figure 2.27: Thermocouple Manufacturing: Step 5. The nished thermocouple, after being dipped in liquid tape 33 on the initial conductivity test. The boreholes were drilled using the drilling rig shown in Figures 2.28 and 2.29 with drill bits shown in Figure 2.30. The U-tubes were inserted in the casing for the drilling rig (Figure 2.31.) The boreholes were then grouted using a tremie pipe as the casing was removed. A U-tube after the vertical installation stages can be seen in Figure 2.32. At a later date, the three vertical U-tubes were connected and plumbed to the house with horizontal piping. The piping inside the house runs through the rst oor mechanical room, up to the attic above the second oor where the heat pump and inline pump are installed (Figure 2.33.) Of the three U-tubes installed for this system, only one was instrumented with thermocouples and a PEX pipe along its length. The thermocouples and PEX pipe were attached to the U-tube using duct tape every few feet (Figure 2.34.) Figure 2.28: The Borehole Drilling Rig: View 1 34 Figure 2.29: The Borehole Drilling Rig: View 2 Figure 2.30: Drill Bits. These are two types of drill bits that screw onto the end of the drill casing driven by the drilling rig. 35 Figure 2.31: U-tube Insertion. The heavily monitored U-tube during installation, showing the U-tube, pex and TCs being inserted into the drill casing. Figure 2.32: Vertical U-tube After Installation. This is the heavily monitored U-tube installed with a PEX pipe and thermocouples, before the horizontal pipes are connected. The U-tube is the two black pipes which are duct taped together and the PEX pipe is the smaller white pipe. 36 Figure 2.33: Heat Pump and Inline Pump. The heat pump and inline pump were installed in the attic above the second oor. The heat pump is the large, white device and the inline pump is the small, red device below the heat pump in the gure. Figure 2.34: Bottom of a U-tube. A more detailed view of the bottom of a U-tube pipe with thermocouples duct taped in place. In reality, it looks more like a V than a U. 37 2.4.2 Thermosiphon System The drilling contractor drilled an 80-foot well for the thermosiphon the same as if it were a U-tube. Once the well was drilled, the four 20-foot sections of galvanized pipe were connected piece by piece, with straight NPT couplings (Figure 2.35), and lowered into the drill rig casing. Once all of the pipe was lowered into the well, thermal grout was pumped into the well as the drill rig casing was pulled up. At a later date, a 1.5-inch to 1-inch adapter, 45 degree WYE elbow, and the heat exchanger assembly were screwed onto the previously installed thermosiphon pipe. PEX-pipe safe for propylene glycol mixtures and pac-joint ttings were used to plumb between the three-way valves and heat exchanger. The nal heat exchanger and thermosiphon assembly was pressure tested with air to about 120 psi, for a period of a few days, to test for leaks. After the system passed pressure testing it was charged with R-134a refrigerant to approximately 40 psi. Figure 2.35: Thermosiphon Coupling. One of the NPT couplings on the ther- mosiphon pipe during installation, shown with a PEX pipe and thermocouples. 38 2.5 Challenges 2.5.1 Field experiment vs. controlled lab environment The amount of e ort involved in setting up a eld experiment versus an experi- ment in a controlled lab environment cannot be understated. Everything was more di cult: travel time to the site, set-up and tear-down time, weather, coordinating with contractors, damage to installed equipment by trucks and heavy machinery. 2.5.2 Human factors The fact that this experiment was coordinated as part of a construction project and being built on an active construction site were enormous challenges. Coor- dinating with some of the trades was initially very hard for a number of reasons. They were upset because they were not made aware of our involvement when they accepted the job, and although coordinating with one more person does not sound like much, it only adds time and complication that was not factored into their original, xed bid. Being a student with classes, assignments and exams, not a full-time contractor, it was di cult to schedule work and coordinate installations with contractors. If they were working on something that I needed to be involved in, it did not matter what else was happening with school, I had to ignore all the other demands on my time and be working at the site. Unlike normal graduate projects where code, or lab experimental set-ups that are just the same as when you left them before you got pulled away for a few days, things on the construction site were rarely the same as when you left them. Being a young, inexperienced engineer was another challenge in and of itself. Having little applied experience with many of the involved trades (plumbing, elec- trical, drilling) my initial plan often had fatal aws which were glaringly obvious to veterans in the trades. With that said, I gained an enormous amount of practical knowledge from the tradesmen. The entire design and construction phase was a crash course in plumbing, electrical, drilling, excavation and HVAC. There were approximately 50 thermocouples in the eld. Many of these needed to be extended or shortened which resulted in renumbering the wires more than one 39 time. Although renumbering was done with the utmost care, checking and often double checking the numbers, it is possible that errors could have been introduced during this procedure. 2.5.3 Weather Starting installation of a eld experiment above an elevation of 6,000 feet in Utah during the fall caused a lot of major delays. Drilling was sometimes on hold until the ground thawed in the morning. Cold weather slowed the entire pace of the project. Once it got late enough in the year, snow accumulation halted work on the GSHP system (Figure 2.36.) The adhesive in duct tape loses its stickiness around freezing temperatures, which at times made it very di cult to attach thermocouples to the plastic pipe used for the GSHP. In this case, the back up solution was quick (zip) ties, but these were brittle and sometime broke at the cold temperatures. Figure 2.36: Snow During Construction. Weather drastically slowed the pace of construction. 40 2.5.4 Inexperience Choosing the right materials would have saved a lot of time and e ort, but these decisions were hard to make with little to no experience performing many of these tasks. The thermocouples running from the U-tubes and thermosiphon back to the house were run through PVC to weatherize and protect the wires. The problem was that the PVC which was chosen was irrigation PVC, the white kind, versus electrical PVC, the gray kind. This made pulling bundles of thermocouple wire through T or elbow ttings much more di cult because this was not the intended purpose of these materials. Using stranded as opposed to solid core thermocouple wire would have made installation easier. Stranded wire would have been better than solid core wire because its superior pliability would have been substantially easier to pull through the conduit. Choosing the pex pipe and associated NPT adapters connecting the thermosiphon heat exchanger to the three-way valves ended up being a process that required multiple revisions. Due to lack of experience, plain PEX and Jones ttings were installed. After consulting with the on-site plumber, oxygen-barrier PEX and pac-joint ttings were used to replace the original materials. The PEX pipe was changed because standard PEX is not compatible with glycol mixtures. The Jones ttings were replaced with pac-joint ttings because the Jones ttings are leak-prone and the pac style ttings are very dependable. These changes helped ensure that this unconventional, unrated implementation of these materials yielded the most reliable system possible in order to protect the ground water purity. CHAPTER 3 U-TUBE HEAT TRANSFER 3.1 Short Term Analysis 3.1.1 U-tube Inlet and Outlet Temperatures The three highest temperatures during the majority of the test shown in Figure 3.1 are the outlet temperatures for each borehole and the three lowest are the inlet temperatures. Overall the three inlet temperatures are well grouped together and the three outlet temperatures are well grouped together. This is as predicted because the three boreholes are connected in parallel. The temperature di erences among the inlets is more pronounced than that for the outlets. It is assumed that this greater di erence in the inlets is caused by variations in the horizontal tubing along the uid path. This includes variations in the length of the horizontal run and the variations in geology and ground temperatures in the di erent horizontal runs. 3.1.2 U-tube Instrumentation Geothermal contractors and installers do not di erentiate between an inlet or outlet during installation because it makes no di erence in terms of system performance. The thermocouples on the U-tubes were installed `blind,' without specifying the inlet or outlet side of the U-tube. The BH1 25ft, BH1 50ft - 1, BH1 50ft - 2, BH1 75ft and BH1 Bottom thermocouples were all installed on the heavily monitored U-tube during installation of the vertical borehole. The borehole inlet and outlet thermocouples were all installed during the horizontal phase. The identi cation of inlet versus outlet thermocouples was based on observing the temperatures during heat pump operation; the inlet temperature is always 42 0 50 100 150 200 250 300 34 35 36 37 38 39 40 Time (minutes) Temperature (F) BH1 Inlet BH1 Outlet BH2 Inlet BH2 Outlet BH3 Inlet BH3 Outlet Figure 3.1: U-tube Inlet and Outlet Temperatures. The solid lines indicate the U- tube borehole inlet temperatures and the dashed lines indicate the U-tube borehole outlet temperatures. 43 signi cantly lower than the outlet temperature (Figure 3.1.) Identi ying the orientation of the heavily monitored U-tube was based on the thermocouple groupings and the temperature decay rate of one thermocouple with respect to another. The potential orientations for the heavily monitored U-tube can be seen in Figure 3.2. It was deduced that the orientation of Borehole 1 is scenario two. 3.1.3 Temperature vs. Time for the Heavily Monitored U-tube Data from typical cycling of the GSHP system did not give temperatures that well represented the uid temperature at the corresponding locations in the borehole eld. During system cycling, for shorter time periods, 15 to 30 minutes, while the thermostat was trying to maintain a constant set point, it was di cult to derive any meaning from the temperatures along the length of the loop because they are so erratic. This is most likely due to the initial heat transfer rates being particularly sensitive to varying hydrological and geological conditions. The multihour endurance test results can be seen in Figure 3.3. Although the temperatures along the length of the U-tube are not as representative as expected, the inlet temperature is cooler than all of the other thermocouples on that speci c U-tube. Another important conclusion is that the outlet is warmer than the inlet for almost the entire test, representing a positive heat ux. In spite of the uncertainties related to location of the thermocouple on the U-tube, all of the temperatures except for one of the 50 foot measurements are above the temperature of the outlet, indicating that the GSHP uid cools on its path back up the U-tube. 44 Figure 3.2: U-tube Borehole 1 Vertical Section View. The U-tubes were installed `blind,' meaning that one side was not speci ed as an inlet and the other as an outlet because this does not a ect the functioning of the system. At the time of installation, it was not known by the author that the U-tubes were installed `blind' and there is some ambiguity as to which scenario the thermocouples are oriented in. Scenario 1- BHl Outlet t ~ BHl Inlet BH125ft BHI5Oft-l BHI5Oft-2 BH175ft BHIBottom Scenario 2- BH10utlet t ~ BHl Inlet BH125ft BH150ft-2 BH150ft-l BH175ft BHl Bottom 45 0 50 100 150 200 250 300 34 35 36 37 38 39 40 41 42 Time (minutes) Temperature (F) BH1 Inlet BH1 Outlet BH1 25ft BH1 50ft−1 BH1 50ft−2 BH1 75ft BH1 Bottom Figure 3.3: U-tube Temperatures vs. Time. The temperatures along the length of the U-tube borehole decay over time, as heat is removed from the near- eld region. For the majority of the time, the outlet temperature is above the inlet which con rms that heat is being extracted from the ground. The outlet temperature also indicates that the uid is cooled as it returns on the outlet side of the U-tube because for the most part, it is the third coldest temperature along the length of the U-tube. 46 3.1.4 Immersed compared to surface mounted thermocouple temperatures There was an additional set of thermocouples measuring the inlet and outlet temperatures to the heat pump. In Figure 3.4, it can be seen that the surface mounted thermocouples were about 5 F warmer and have a greater temperature di erence between inlet and outlet than the immersed thermocouples. This dis- crepancy between the immersed and surface thermocouples can be attributed to warming of the uid once it enters the house. After the uid penetrates the oor in the rst oor mechanical room, it travels in uninsulated piping to the heat pump for the GSHP system, located in the attic above the second oor in the house. The immersed temperatures are measured just above the oor in the rst oor mechanical room, but the surface temperatures are measured just before the heat pump in the attic. Heat transfer between the uid in the uninsulated and the house create this temperature di erence. The immersed thermocouples represent the true performance of the geothermal system because when looking at the building from a control volume standpoint, they are the uid temperatures at the boundary of the control volume. 47 0 50 100 150 200 250 300 25 30 35 40 45 50 55 Time (minutes) Temperature (F) Heat Pump Inlet (Surface) Heat Pump Outlet (Surface) Heat Pump Inlet (Immersed) Heat Pump Outlet (Immersed) BH1 Inlet BH1 Outlet Figure 3.4: Immersed vs. Surface Temperatures for the U-tube System. The dis- crepancy between the immersed and surface mounted thermocouple temperatures is due to their di erent physical locations inside the building. Heat transfer between the pipes and the indoor environment occurs because the pipes are uninsulated on inside the house. CHAPTER 4 THERMOSIPHON HEAT TRANSFER 4.1 Short Term Analysis 4.1.1 Temperature vs. time at multiple locations Temperature histories at various depths on the outside wall of the TS pipe and the inlets and outlets of the heat exchanger are shown in Figure 4.1. The R134a temperatures at the inlet and outlet of the heat exchanger are almost identical during the period shown. This indicates that the heat transfer is occurring due to condensation. The glycol temperatures between the inlet and outlet represent a relatively constant temperature di erence meaning that the thermosiphon is extracting heat from the ground at a constant heat ux. The `shoulders,' or rapid temperature drops in the TS 50 and 75 foot ther- mocouples are caused by a delay in refrigerant reaching those locations on the thermosiphons. Starting from inactivity, once the heat exchanger has `cold' glycol uid circulating through the tube side, refrigerant starts condensing on the shell side of the heat exchanger. As this condensation occurs, the liquid refrigerant is returned to the thermosiphon due to gravity. As it travels down the walls of the thermosiphon, it saturates the mesh material, hardware cloth, as the liquid front moves down the pipe. The `shoulders' occur in the temperature pro le as the liquid refrigerant front reaches the location of a thermocouple because once the refrigerant saturates the mesh at the inside wall of the pipe, refrigerant vaporization occurs. Once refrigerant has reached the entire interior area of the pipe, the temperatures at TS 25, 50 and 75 stabilize at the same temperature, around 41 F . Unlike the TS 50 and 75 pro les, there is no `shoulder' in the TS 25 temperature pro le. The thermocouple at the TS 25 location is only 5 feet from the top of 49 the thermosiphon pipe. Therefore the response time is very short for the liquid refrigerant to reach that location once condensation starts at the heat exchanger. The immediate drop in the temperature of TS 100 at the bottom of the ther- mosiphon pipe is also observed and thus the liquid in the bottom began vaporizing as soon as the cooling of the condenser dropped the thermosiphon pipe pressure. The TS 100 thermocouple temperature stabilizes at a higher temperature than the other TS temperatures because it is located at the bottom of the thermosiphon where there is a column of liquid refrigerant in bottom of the pipe. This column creates a higher pressure at the bottom of the thermosiphon which increases the boiling temperature of the refrigerant above that at the top surface of the liquid column. 4.1.2 Immersed compared to surface mounted thermocouple temperatures The immersed versus the surface mounted thermocouple measurements in the thermosiphon test (Figure 4.2) are di erent for the same reason that they were di erent in the U-tube test, heat transfer to uninsulated pipes inside the building. 50 0 50 100 150 200 25 30 35 40 45 50 Time (minutes) Temperature (F) TS 25ft TS 50ft TS 75ft TS 100ft HX R134a Inlet HX R134a Outlet HX Glycol Inlet HX Glycol Outlet Figure 4.1: Thermosiphon Temperatures vs. Time. This gure shows the thermosiphon outside wall and heat exchanger temperatures as a function of time. The tight grouping of the HX R134a Inlet and Outlet temperatures indicates that the thermosiphon is operating as a phase change device. The temperature di erence between the HX Glycol Inlet and Outlet is relatively constant throughout the test indicating a constant heat ux into the thermosiphon. The step shaped decay of the TS 50ft and TS 75ft is caused by the delay in refrigerant saturating the mesh and inside wall of the thermosiphon pipe at those locations because a refrigerant must be at those locations for an signi cant temperature response due to vaporization. --~-- 51 0 20 40 60 80 100 120 140 160 180 200 20 25 30 35 40 45 50 Time (minutes) Temperature (F) Heat Pump Inlet (Surface) Heat Pump Outlet (Surface) Heat Pump Inlet (Immersed) Heat Pump Outlet (Immersed) HX Glycol Inlet HX Glycol Outlet Figure 4.2: Immersed vs. Surface Temperatures for the Thermosiphon System CHAPTER 5 THERMAL EXTRACTION AND HEAT PUMP ANALYSIS 5.1 Heat absorbed by the heat pump For the control volume of interest: _Q L = m_ cp T (5.1) _Q L = _V cp T (5.2) 5.2 Heat absorbed by the heat pump per unit length of borehole Figure 5.1 shows that the _Q L;normalized for the feet of borehole for the ther- mosiphon is substantially higher than that for the U-tube borehole. Based on the results from this test the thermosiphon has approximately two times the heat transfer capability per foot of borehole. The thermosiphon performs so much better because it does not have have the performance robbing cancellation that U-tubes su er from and the latent heat of vaporization yields a very low thermal resistance. This result has a signi cant impact on the initial capital cost of installing either a U-tube or a thermosiphon system. Borehole drilling costs are typically the most signi cant capital expense for a small scale geothermal system such as ground source heat pumps. For heating applications, this means that drilling costs could be cut in half through the use of thermosiphons instead of U-tube, drastically reducing rst cost of the system. One factor that could not be accounted for in the comparison is that the U- tube had already operated for a portion of the heating season on the day that the comparison testing was performed, while the thermosiphon had not been operated prior to that day. This means that ground temperatures were already slightly 53 suppressed around the U-tubes because heat had been extracted from the local soils. _Q L;normalized = _Q L Total Borehole Length (5.3) 5.3 COP 5.3.1 Comparison of U-tube to Thermosiphon COP The COP of the U-tube and thermosiphon systems during the short term tests was calculated using the following equation for COP. COPHP = QH Wnet (5.4) = Wnet + QL Wnet (5.5) COPHP = _W net + _Q L _W net (5.6) The COP of the heat pump for the U-tube borehole system is slightly better than the COP for the thermosiphon system (Figure 5.2). This calculation is in no way normalized for the di erent length of boreholes between the two systems. Therefore the U-tube system has a higher COP only due to the fact that it has three times the length of borehole. 5.3.2 Seasonal U-tube COP The daily average COP of the U-tube system was calculated in order to see if there is a decline in e ciency throughout the heating season as heat is extracted from the ground. The daily average was calculated by averaging the COP on a daily basis only for times that the system is running. A least squares t was applied to the daily averages in order to determine the COP trend for the heating season. The results of this study can be seen in Figure 5.3. As predicted, the daily average COP of the U-tube system declines throughout the heating season as indicated by the negative slope of the least squares t line 54 0 50 100 150 200 250 300 −100 −80 −60 −40 −20 0 20 40 60 80 100 Time (minutes) Q−low (W/m) U−tube Thermosiphon Figure 5.1: Q-low per Foot of Borehole Comparison. The thermosiphon extracts approximately twice the heat from the ground per foot of borehole than the U-tube. The phase change nature of the thermosiphon is not susceptible to the thermal interference that a icts the U-tube design. The heat transfer per foot of borehole is important because borehole drilling is one of the most signi cant, if not the most signi cant, capital cost in a small scale geothermal system. The calculated error in this gure is on the order of 1e-11. 55 0 50 100 150 200 250 300 −1 −0.5 0 0.5 1 1.5 2 2.5 3 3.5 4 Time (minutes) COP U−tube Thermosiphon Figure 5.2: COP Comparison. The COP of the U-tube is slightly higher than the COP of the thermosiphon over the majority of the test. These data are not normalized for the length of borehole. Therefore the U-tube has a higher e ciency. The U-tube performs better only because it has three times the length of borehole. 56 in Figure 5.3. This occurs because as heat is extracted from the ground local soil temperatures around the U-tube are depressed. The depressed soil temperatures lead to a lower T in QL, and therefore a lower COP, or system heating e ciency. Another important nding is that the daily average COP is below 3 during the monitoring period. Ground source heat pump literature typically estimate system COPs to be between 4 and 5. A COP of 3 is particularly important because 3 represents the e ciency at which the operating (fuel) costs and carbon footprint are roughly equivalent to a high-e ciency natural gas furnace. Electricity is roughly 3 times more expensive than natural gas, which means that comparing a ground source heat pump to a high-e ciency furnace, with a thermal e ciency of almost 100%, the heat pump system must use less than one third the electrical energy (a COP greater than 3) in order to have a lower operating cost. A GSHP system COP of less than 3 also means that the GSHP system will likely have an in nite payback period because on average GSHP systems are more expensive than an equivalent capacity gas powered furnace. At less than 3, the carbon footprint is also greater assuming that the electricity is generated from a natural gas red power plant because the e ciency of the overall electricity, including generation and transmission, once it reaches the consumer is roughly 33%. 5.4 Comparison of ground source to an air source heat pump When considering the application of a ground source heat pump system, it is important to compare the seasonal ground temperatures to the seasonal air temperatures during the intended period of use, in this case the heating season. This comparison is important because the initial cost of a ground source heat pump system is much higher than a comparably sized air source heat pump system. A prospective GSHP system should have a more favorable source temperature than an air source system in the same location, therefore providing improved e ciency to compensates for the higher initial cost. In Figure 5.4, the heat pump inlet temperature is higher than the ambient air temperature during the majority of the analysis period. This means that the ground as a heat source is thermodynamically 57 favorable to the air as a heat source for the heat pump system. 11/18 11/23 11/28 12/03 12/08 12/13 12/18 12/23 12/28 01/02 2.1 2.2 2.3 2.4 2.5 2.6 2.7 2.8 2.9 3 Time COP Daily Avg COP Least Squares Fit Figure 5.3: Average Daily COP. The average daily COP, calculated only for time when the system was actually running, was less than 3 for the entire duration of the test. The COP declines during the heating season, as shown by the negative slope of the least squares t line. The COP had a decline of .0029 per day or roughly .086 per month. 58 11/18 11/23 11/28 12/03 12/08 12/13 12/18 12/23 12/28 01/02 −10 0 10 20 30 40 50 60 Time Temperature (F) Heat Pump Inlet (Immersed) Heat Pump Outlet (Immersed) Ambient Air Figure 5.4: Comparison of U-tube System Temperatures to Ambient Air Temper- atures. This comparison veri es that the ground is a better heat source for the heat pump than the ambient air. For 86% of the period analyzed, the heat pump inlet temperatures are above the ambient air temperatures, which makes the ground a more favorable heat source. - - - III~I' k ~ J~ ~~ II\ w N • f'J I'" v IV ~ I'" ~ V' \ ~ v 1\ CHAPTER 6 CONCLUSIONS 6.1 Findings The data indicate that the thermosiphon has roughly two times the heat ex- traction rate compared to the U-tube per foot of borehole. U-tube performance was shown to decline through the heating season. GSHP COP calculated to be less than 3, which is much lower than typically estimated values of 4 to 5. When looking at the potential of GSHP as an energy and cost saving technology, one must consider that although there is a high level of con dence in the results, that this is one GSHP installation, designed by one engineer and installed in one location with its own unique geology and hydrology. 6.2 Challenges Given the fact that this experiment was carried out on a working construction site, with deadlines and standard installation procedures, it was extremely chal- lenging to foresee all of the potential obstacles and install experiment exactly as planned. The weather slowed the planned schedule and caused major road blocks in the installation of the experiment. It is very di cult to create a realistic schedule when it comes to planning around weather during winter at high elevation. 6.3 Recommendations It would be valuable to duplicate the U-tube monitoring on another GSHP system. Comparing U-tube installations with and without spacer to separate the two pipes would be a valuable side-by-side comparison. The most important recommendations generated from this experiment are prob- ably with respect to choice of materials. If allowable, thermistors would be a 60 better choice of sensor for temperature measurement than thermocouples given their superior accuracy. No matter what type of sensor used, it is advisable to use stranded wire instead of solid core wire because the greater exibility of stranded wire will ease installation. Using electrical PVC pipe as conduit instead of standard irrigation PVC pipe will also ease the installation of wires. Due to the nonsymmetrical heat transfer in the two sides of a U-tube and the lack of contractor designation between inlet and outlet, it would be best to instrument both sides equally. Insulating around the outer diameter of the U-tube pipe where a temperature sensor is located would aid in the measurement of uid temperatures instead of a combination of uid and ground temperatures that is measured in this experiment. REFERENCES Chiasson, A., S. Rees, and J. Spitler, 2000: A Preliminary Assessment of the E ects of Ground-Water Flow on Closed-Loop Ground-Source Heat Pump Systems. ASHRAE Transactions, 106, 380{393. DR International, L., 2009: 2009 Buildings Energy Data Book. Technical report, U.S. Department of Energy. Dunn, P. and D. Reay, 1994: Heat Pipes. Elsevier Science Ltd, fourth edition. Florides, G. and S. Kalogirou, 2007: Ground heat exchangers {A review of systems, models and applications. Renewable Energy, 32, 2461{2478. Nam, Y., R. Ooka, and S. Hwang, 2008: Development of a numerical model to predict heat exchange rates for a ground-source heat pump system. Energy and Buildings, 40, 2133{2140. Omer, A., 2008: Ground-source heat pumps systems and applications. Renewable and Sustainable Energy Reviews, 12, 344{371. Rawlings, R. and J. Sykulski, 1999: Ground source heat pumps {A technology review. The Chartered Institution of Building Services Engineers, 20, 119{129. Tanaka, O., H. Yamakage, T. Ogushi, M. Murakami, and Y. Tanaka, 1982: Snow Melting Using Heat Pipes. Advances in Heat Pipe Technology, Pergamon Press Ltd, rst edition. Udell, K., P. Jankovich, and B. Kekelia, 2009: Seasonal Underground Thermal Energy Storage Using Smart Thermosiphon Technology. GRC Transactions, 33. Udell, K., B. Kekelia, and P. Jankovich, 2011: Net Zero Energy Air Conditioning Using Smart Thermosiphon Arrays. ASHRAE Transactions, 117. Xu, X. and J. Spitler, 2006: Modeling of Vertical Ground Loop Heat Exchangers with Variable Convective Resistance and Thermal Mass of the Fluid. Proceedings of the 10th International Conference on Thermal Energy Storage - Ecostock 2006 , Pomona, NJ. Yavuzturk, C. and J. Spitler, 1999: A Short Time Step Response Factor Model for Vertical Ground Loop Heat Exchangers. ASHRAE Transactions, 105, 475{485. Yavuzturk, C., J. Spitler, and S. Rees, 1999: A Transient Two-Dimensional Finite Volume Model for the Simulation of Vertical U-Tube Ground Heat Exchangers. ASHRAE Transactions, 105, 465{474. |
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