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Ground Temperature

Undisturbed ground temperature is best obtained from local water well logs and geological surveys. Figure 9 shows the approximate ground water temperatures in the USA. The undisturbed ground temperature will remain constant throughout the year below 30 ft. Above 30 ft., the ground temperature will change with the season. Appendix 1 – Ground Temperatures, page 36, has the ground temperatures for many locations around the world.

 

36 Application Guide AG 31-008

Appendix 1 – Ground Temperatures

State City GWT (F)

State/Country City GWT (F)

State/Country City GWT (F)

AlabamaBirmingham65

South CarolinaCharleston66

GermanyFrankfurt52

AlabamaMobile 70

South CarolinaColumbia64

GermanyHamburg51

AlabamaMontgomery67

South CarolinaGreenville62

GermanyMunich49

AlaskaAnchorage40

South DakotaSioux Falls 51

GermanyStuttgart51

AlaskaFairbanks0

TennesseeKnoxville61

GreeceAthens67

ArizonaPhoenix73

TennesseeMemphis63

HungaryBudapest53

ArkansasLittle Rock 64

TennesseeNashville60

IndonesiaJakarta83

CaliforniaFresno68

TexasAustin71

IrelandDublin52

CaliforniaLos Angeles64

TexasDallas68

IsraelJerusalem63

CaliforniaSacramento67

TexasHouston71

ItalyGenova 60

CaliforniaSan Diego64

TexasSan Antonio72

ItalyMilan57

CaliforniaSan Francisco60

UtahSaltLakeCity 53

ItalyNaples63

ColoradoDenver52

VermontBurlington46

ItalyPalermo66

ConnecticutHartford51

Virginia Norfolk 61

ItalyRome61

DelawareDover57

Virginia Richmond 60

Italy Torino58

FloridaDaytona Beach70

Virginia Roanoke 59

ItalyTrieste58

FloridaJacksonville71

DC Washington57

ItalyVenice58

FloridaMiami78

WashingtonSeattle53

JapanNagoya62

FloridaTallahassee69

WashingtonSpokane49

JapanOsaka63

FloridaTampa75

West VirginiaCharleston58

JapanSapporo51

Georgia Atlanta 62

WisconsinLa Crosse48

JapanTokyo64

Georgia Savannah 67

WisconsinMilwaukee47

KoreaInch'on 56

HawaiiHonolulu79

WyomingCheyenne48

Korea Pusan59

IdahoBoise47

AlbertaCalgary42

KoreaSeoul57

IllinoisChicago51

AlbertaEdmonton40

Kuwait KuwaitCity80

IllinoisSpringfield56

British ColumbiaVancouver53

Libyan Arab Jamahiriya Tripoli71

IndianaFort Wayne53

ManitobaWinnipeg40

MalaysiaGeorge Town84

IndianaIndianapolis55

New BrunswickMoncton42

MalaysiaKuala Lumpur83

IowaDes Moines53

Newfoundland Saint John's 43

MexicoAcapulco78

KansasWichita59

Nova ScotiaHalifax45

Mexico MexicoCity65

OhioCincinatti 57

OntarioOttawa45

Mexico Veracruz75

KentuckyLexington60

OntarioToronto48

MoroccoCasablanca66

KentuckyLouisville60

Prince Edward IslandCharlottetown42

NetherlandsAmsterdam52

LouisianaNew Orleans70

QuebecMontreal46

New ZealandAuckland56

LouisianaShreveport66

SaskatchewanRegina39

New ZealandChristchurch54

MaineCaribou 46

ArgentinaBuenos Aires64

New ZealandWellington57

MainePortland48

AustraliaAdelaide64

NorwayOslo46

MarylandBaltimore57

AustraliaBrisbane72

ParaguayAsuncion64

MassachusettsBoston50

AustraliaCanberra67

PeruLima70

MassachusettsWorchester 50

AustraliaMelbourne59

PhilippinesManila 67

MichiganDetroit50

AustraliaPerth67

PolandKrakow48

MichiganFlint49

AustraliaSydney67

PolandWarsaw49

MichiganGrand Rapids46

AustriaSalzburg51

PortugalPorto64

MinnesotaDuluth41

AustriaVienna50

Puerto RicoSan Juan84

MinnesotaMinneapolis47

BahrainManama80

QatarDoha83

MississippiJackson67

BelgiumBrussels52

RomaniaBucharest54

MissouriKansas City58

BoliviaLa Paz50

Saudi ArabiaRiyadh82

Missouri St.Louis 58

Brazil Belem82

Singapore Singapore82

MontanaBillings49

BrazilBrasilia80

SpainBarcelona62

MontanaHelena47

Brazil Recife78

SpainMadrid60

NebraskaOmaha53

BrazilSao Paulo78

SpainSevilla 67

NevadaLas Vegas69

BulgariaSofia55

SpainValencia65

NevadaReno50

ChileSantiago61

SwedenStockholm47

New HampshireConcord50

ChinaBeijing58

SwitzerlandGeneva53

New JerseyTrenton55

ChinaGuangzhou77

SyriaDamascus71

New MexicoAlbuquerque59

ChinaHarbin53

TaiwanTaipei75

New YorkAlbany50

ChinaHong Kong77

ThailandBangkok85

New YorkBuffalo50

ChinaShanghai62

TunisiaTunis69

New YorkNew York City52

China Shenyang55

TurkeyAnkara52

North CarolinaAsheville59

Colombia Bogota58

TurkeyIstanbul60

North CarolinaCharlotte62

CubaHavana77

Turkey Izmir64

North CarolinaGreensboro60

CzechRepublicPrague50

United Arab EmiratesAbu Dhabi80

North CarolinaRaleigh62

DenmarkCopenhagen47

United Arab EmiratesDubai80

North DakotaBismarck44

EcuadorQuito60

United KingdomAberdeen49

North DakotaFargo42

EgyptAswan78

United KingdomBelfast51

OhioCleveland51

EgyptCairo73

United KingdomBirmingham52

OhioColumbus55

FinlandHelsinki47

United KingdomEdinburgh50

OhioDayton50

FranceBordeaux61

United KingdomLiverpool54

Oklahoma OklahomaCity62

FranceLyon57

United KingdomLondon54

OregonPortland54

FranceMarseille 59

UruguayMontevideo64

PennsylvaniaHarrisburg52

FranceNantes56

VenezuelaCaracas78

PennsylvaniaPhiladelphia55

FranceParis54

VietnamHanoi84

PennsylvaniaPittsburgh52

GermanyBerlin52

YugoslaviaBelgrade55

 

14 Application Guide AG 31-008

Figure 10 – Shallow Ground Temperature Variation with Season

 

The graph shows the variation from undisturbed ground temperature for various depths. For instance, horizontal systems usually stay within 5 ft. of the surface, which can swing by as much as 20°F from summer to winter.

 

Annual Energy Load and Balance

Key issues with Geothermal systems are the annual energy load and balance. If the building rejects more heat into the ground than it removes, then the borehole field average temperature will climb over time. Even if the heating and cooling loads are balanced, the amount of the energy rejected will affect the monthly ground temperature.

 

How fast and how much the temperature changes will depend on building usage, borehole spacing and ground water movement. Close borehole spacing will restrict the ability of the borehole to dissipate heat. On the other hand, good ground water movement will help carry away heat. If the building uses more heat then it rejects, the reverse will be true.

 

Monthly Effects and Equivalent Full Load Hours

The amount of energy transferred to or from the field will affect the ground temperature and the future performance of the field. This effect is generally considered on a monthly basis. A key factor is building use. Consider a school and a hospital, both with a 200-ton design load. Even though they have the same number of heat pump tons, the hospital operates around-the-clock and moves much more energy to and from the field than the school.

 

Most loop sizing software uses Equivalent Full Load Hours (EFLH) for heating and cooling to estimate the energy transfer effect. Equivalent full load hours are the annual heating and cooling loads divided by the installed capacity. For the hospital and school example given above, even though the installed capacity would be the same, the annual loads for the hospital will be much higher and the equivalent full load hours will be higher.

 

Estimating the equivalent full load hours requires some judgment and understanding of how the building is used. Appendix 4 – Equivalent Full Load Hours, page 39, provides Equivalent Full Load Hours for various cities and building types based on constant temperature setpoints. The following will provide the designer with some guidance on factors that affect Equivalent Full Load Hours.9

 

8 Copyright 1997, American Society Of Heating, Air-conditioning and Refrigeration Engineers Inc., www.ashrae.org. Reprinted by permission from Ground-Source Heat Pump Systems: Design of Geothermal Systems for Commercial and InstitutionalBuildings

 

9 Carlson, Steven W., Jeff W. Thornton. Development of Equivalent Full Load Heating and Cooling

Hours For GCHPs. RP-1120. ASHRAE. Atlanta, Ga.2002.

 

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