Abstract
Ball State University will convert its campus from a coal-fired and natural gas-fired district heating system to a closed loop heat pump chiller district heating and cooling system serviced by more than 4,100 geothermal boreholes. It will be largest district ground source geothermal system in the United States. On May 29, 2009, an article in the The New York Times called Ball State “a pioneering university” for undertaking the initiative. The installation will include an integral programme of research designed to inform the industry – especially the owners of 65,000 other district-heated buildings in the U.S. – how to significantly reduce the “first costs” and risks associated with intensive borehole drilling, piping, and looping. These issues are cited in a 2008 Department of Energy (DOE)-sponsored study as a major impediment to the more widespread adoption of geothermal systems. The planned research will incorporate 2D resistivity programming, geological surveys of the impact of high-density boreholes on ground temperature, assessment of the role of soil and water pH, evaluation of the influence of variable system water flow, analysis of hydrological data, and verification of the claims made by new geoexchange pipe manufacturers for dramatically increased thermal transfer (40–50%) and the concomitant reduction in the number of required expensive boreholes (20–35%) to service a load.
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Appendices
Proof of Concept: Heat Pump Chillers with Geothermal Storage
Produced for Ball State University
Prepared by and Kirk T. Mescher, PE of
MEP Project No. B20.08. 01
January 28, 2009
Table of Contents
Introduction
The Concept
The Application
Conclusion
Appendix A: Heating and Cooling Loads
Appendix B: Flow Diagram
Appendix C: Borehole Design Report
Introduction
In today’s economic climate of high and rising fuel costs, many managers of large 24-hour facilities do well to examine new and creative ways to trim energy bills. One smart option is to examine the potential of a source that is already available, repurposing heat that is ordinarily discarded by the HVAC system’s condenser.
By utilizing heat pump chillers with geothermal storage instead of ordinary chillers, the temperature of this formerly waste heat can be increased until it is suitable for a wide variety of heating applications, and utilized when it is needed.
This report provides a proof of concept for heat pump chillers with geothermal storage. It will allow Ball State University to have an introductory understanding of this type of system, as well as some preliminary operational costs developed by Kirk Mescher of CM Engineering, in order for university personnel to evaluate the compatibility of this technology with their campus.
The Concept
Heat Pump Chillers
A compound centrifugal chiller is a special kind of centrifugal chiller that utilizes a combination of two (i.e. compound) compressors, instead of just one, and a component called an intercooler. The additional compressor and the intercooler allow the compound centrifugal chiller to produce condenser water at a much higher temperature than was previously possible with a standard centrifugal chiller. No longer fit only for rejection out of the cooling tower, this hot water, which can reach up to 150°F, is useful and can be utilized in a variety of heating applications that, until a few years ago, were the domain of boilers and heat pumps. Hence, this chiller is commonly called a heat pump chiller.
Although the advantages of this type of chiller are enormous, not every facility is a good fit, since not all facilities require simultaneous heating and cooling. Large facilities with 24-hour operation, such as hospitals, hotels, and universities, which have year-round demand for both heating and cooling, have tremendous potential to save energy. However, a careful examination of the loads throughout the year is prudent, in order to ensure that the heating and cooling produced by these chillers will be sufficiently utilized.
In addition, the second compressor can be turned off when the heating load is low. Although this will reduce the temperature of the condenser water leaving the chiller, it can be hot enough to meet the requirements of summer heating applications, such as reheat and domestic water, which typically do not require the high temperatures associated with winter heating. This will also allow the chillers to operate more efficiently, in the same way as a standard single compressor centrifugal chiller.
Geothermal Storage
Many facilities require simultaneous heating and cooling, but utilize only a fraction of its peak heating during the summer. In this case, a heat pump chiller can still offer tremendous benefits with the addition of a renewable technology called geothermal storage. This allows a facility to store the heat it produces in the summer and use it in the winter. This is achieved by heating the earth several hundred feet below the ground inwhat is called a loop field. This loop field is an area of land with several bores that are several hundred feet deep. Each bore houses u-shaped pipes that routes hot water and cold water down deep into the rock in the earth where it rejects or obtains load. This bedrock is an excellent thermal storage device. It can be charged with heating energy during the summer, hold this heat with minimal losses, and discharge it for utilization in the winter.
The Application
System Sizing
By examining the heating and cooling loads provided by university personnel (see Appendix A), a heat pump chiller plant with geothermal storage, including all distribution piping, was sized to meet the needs of the university’s campus. Calculated by CM Engineering, the estimated annual electrical consumption for this system will be 50 million kWh and the annual operating cost will be $2.1 million.
System Layout
Three locations are proposed for the new heat pump chillers: a new energy centre on the east side of the campus, and a new second energy center on the north side of the campus, and the third existing energy center on the south side of the campus. The new heat pump chillers can be connected directly to the existing chilled water piping system. A new hot water piping loop will need to be added to carry the hot water to the buildings. The source of the hot water, the three heat pump chiller plants, will be connected to this new hot water piping loop with branch pipes. Additional branch pipes will connect this loop to the destination of the hot water, the hot water side of the heat exchangers that currently use steam to provide hot water inside the buildings. For the buildings that do not have these heat exchangers, new air handling unit coils and terminal equipment will need to be installed, in order to accommodate the hot water. The current district heating and cooling system will remain in place and operational during the conversion.
A flow diagram of this system is shown in Appendix B. The system will provide 44°F chilled water throughout the year, and 150°F hot water in winter design conditions (with both compressors running). The hot water temperature will decrease proportionately with the outside air temperature, to a minimum of 110°F in summer design conditions (with one compressor running). This hot water will be used for domestic hot water and summer heating applications, which do not require the hotter 150°F water.
The hot water is circulated using variable frequency drive (VFD) pumps to the existing buildings until their immediate needs are met. If any heat is remaining, it is routed to a heat exchanger that deposits heat into the geothermal storage. This typically occurs during the summer. Conversely, during the winter, when an additional heat source is needed, heat is removed from the geothermal storage.
The specifics on the loop field are contained in Borehole Design Report in Appendix C. It is estimated that 3,750 bores will be needed. They will be 400 feet deep and 15 feet apart from each other. They will house two 1-inch u-bend pipes per bore. The grout thermal conductivity, which is a measure of how effectively the bedrock can hold heat, is estimated to be 0.84 Btu/hr·ft·°F.
Conclusion
It is clear that heat pump chillers with geothermal storage offer tremendous potential for energy savings for Ball State University. It is our hope that this report will offer some helpful information, as we continue to perform further analysis on this type of system to meet the heating and cooling needs of the campus.
Appendix A: Heating and Cooling Loads
Building Name | Address | Year Built | Area (ft2) | Heating Load (MBtuh) | Hot Water (gpm) | Cooling Load (tons) | Chilled Water (gpm) |
---|---|---|---|---|---|---|---|
Carmichael Hall | 1701 W. McKinley | 1967 | 22,963 | 574 | 38 | 58 | 138 |
Johnson Hall (JA Botsford-Swinford; JB Schmidt-Wilson) | 1601 N. McKinley | 1967 | 262,432 | 6,561 | 437 | 141 | 338 |
LaFollette Halls (Village Expansion) | 1515 N. McKinley | 1964 | 531,792 | 13,295 | 886 | 211 | 507 |
Lewellen Pool | 1400 N. McKinley | 1967 | 56,415 | 1,410 | 94 | 0 | |
Health/Phys Activities Building | 1740 W. Neely | 1989 | 110,710 | 2,768 | 185 | 186 | 445 |
Irving Gymnasium | 1700 W. Neely | 1962 | 135,039 | 3,376 | 225 | 186 | 445 |
Worthen Arena | 1990 | 193,267 | 4,832 | 322 | 448 | 1,075 | |
Architecture | 1212 N. McKinley | 1970 | 146,750 | 3,669 | 245 | 333 | 799 |
Subtotals | 36,484 | 2,432 | 1,562 | 3,748 | |||
Robert P. Bell Building | 1211 N. McKinley | 1982 | 106,500 | 2,663 | 178 | 141 | 338 |
David Letterman Building | 1201 N. McKinley Ave | 2005 | 86,351 | 2,159 | 144 | 128 | 307 |
Edmund F. Ball Building | 1109 N. McKinley | 1986 | 84,594 | 2,115 | 141 | 256 | 614 |
Arts and Journalism Building | 1101 McKinley | 2000 | 207,141 | 5,179 | 345 | 218 | 522 |
Bracken Library | 1100 N. McKinley | 1972 | 321,800 | 8,045 | 536 | 640 | 1,536 |
University Theatre | 920 N. McKinley | 1960 | 83,667 | 2,092 | 139 | 179 | 430 |
Teachers College Building | 901 N. McKinley | 1966 | 125,650 | 3,141 | 209 | 288 | 691 |
Noyer Hall | 1601 W. Neely | 1962 | 238,320 | 5,958 | 397 | 448 | 1,075 |
Woodworth Halls | 1600 W. Riverside | 1956 | 164,626 | 4,116 | 274 | 202 | 484 |
Pruis Hall | 1000 N. McKinley | 1971 | 18,170 | 454 | 30 | 128 | 307 |
Bracken House | 2200 W. Berwyn Rd. | 1937 | 13,227 | 331 | 22 | 19 | 46 |
Whitinger Business Building | 1200 N. McKinley | 1978 | 93,763 | 2,344 | 156 | 160 | 384 |
Studebaker Halls East | 1301 W. Neely | 1965 | 97,406 | 2,435 | 162 | 51 | 123 |
Studebaker Halls West | 1401 W. Neely | 1964 | 242,080 | 6,052 | 403 | 294 | 707 |
Park Hall | 1550 Riverside | 2006 | 194,600 | 4,865 | 324 | 282 | 676 |
Music Building | 1810 W. Riverside | 1956 | 45,036 | 1,126 | 75 | 83 | 200 |
Music Instruction Building | 1809 W. Riverside | 2003 | 86,179 | 2,154 | 144 | 179 | 430 |
Emens Auditorium | 1800 W. Riverside | 1963 | 82,101 | 2,053 | 137 | 243 | 584 |
Arts and Communication Bldg. | 1701 W. Riverside | 1957 | 47,010 | 1,175 | 78 | 83 | 200 |
Health Center | 1500 W. Neely | 1962 | 19,527 | 488 | 33 | 32 | 77 |
DeHority Halls | 1500 W. Riverside | 1960 | 138,140 | 3,454 | 230 | 205 | 492 |
North Residence Hall | 1400 W. Neely | 2008 | 190,480 | 4,762 | 317 | 230 | 553 |
Subtotals | 67,159 | 4,477 | 4,490 | 10,775 | |||
North Quad | 1901 W. Riverside | 1926 | 126,543 | 3,164 | 211 | 294 | 707 |
Applied Technology | 2000 W. Riverside | 1948 | 93,274 | 2,332 | 155 | 205 | 492 |
Fine Arts Building | 2021 W. Riverside | 1935 | 74,085 | 1,852 | 123 | 198 | 476 |
Cooper Physical Sciences | 2111 W. Riverside | 1965 | 130,090 | 3,252 | 217 | 461 | 1,106 |
Cooper Nursing | 2111 W. Riverside | 1965 | 47,580 | 1,190 | 79 | 122 | 292 |
Cooper Life Sciences | 2111 W. Riverside | 1968 | 113,843 | 2,846 | 190 | 442 | 1,060 |
Ball Gymnasium | Campus Drive | 1939 | 83,197 | 2,080 | 139 | 115 | 276 |
West Quad | 2301 W. Riverside | 1936 | 57,593 | 1,440 | 96 | 109 | 261 |
Lucina Hall | 2120 W. University | 1927 | 60,014 | 1,500 | 100 | 128 | 307 |
Burris School | 2201 W. University | 1928 | 130,745 | 3,269 | 218 | 250 | 599 |
Elliott Dining | 2100 W. Gilbert | 1990 | 13,228 | 331 | 22 | 45 | 108 |
Wagoner Halls | 301 N. Talley | 1957 | 75,680 | 1,892 | 126 | 13 | 31 |
Elliott Hall | 401 N. Talley | 1937 | 51,627 | 1,291 | 86 | 32 | 77 |
Administration Building | 2000 W. University | 1912 | 54,136 | 1,353 | 90 | 96 | 230 |
Student Center | 2001 W. University | 1951 | 171,165 | 4,279 | 285 | 410 | 983 |
Burkhardt Building | 601 N. McKinley | 1924 | 61,439 | 1,536 | 102 | 70 | 169 |
Subtotals | 33,606 | 2,240 | 2,989 | 7,173 | |||
Central Chiller | West Campus Drive | 1965 | 7,909 | 198 | 13 | ||
Field Sports Building | 1720 W. Neely | 1983 | 47,736 | 1,193 | 80 | 240 | |
Greenhouses | Christy Woods | 1965 | 4,381 | 110 | 7 | ||
Heating Plant | 2331 W. Riverside | 1924 | 18,685 | 467 | 31 | ||
South Service Bldg. | Campus Drive | 1967 | 4,800 | 120 | 8 | 30 | |
Expansion | 300,000 | 7,500 | 500 | 640 | 1,500 | ||
Totals | 5,873,486 | 144,749 | 9,650 | 9,680 | 23,196 |
Appendix B: Flow Diagram
(June 30, 2009 update: One-pipe distribution system has been changed to a two-pipe distribution system)
Appendix C: Borehole Design Report
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Lowe, J.W., Koester, R.J., Sachtleben, P.J. (2010). Embracing the Future: The Ball State University Geothermal Project. In: Leal Filho, W. (eds) Universities and Climate Change. Climate Change Management. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-10751-1_17
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