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Embracing the Future: The Ball State University Geothermal Project

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Universities and Climate Change

Part of the book series: Climate Change Management ((CCM))

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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Correspondence to James W. Lowe .

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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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