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Geothermal Potential of Jamaica

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<strong>Geothermal</strong> <strong>Potential</strong><br />

<strong>of</strong><br />

<strong>Jamaica</strong><br />

- Status <strong>of</strong> Development<br />

Suresh Bhalai<br />

MINES AND GEOLOGY DIVISION<br />

Ministry <strong>of</strong> Energy and Mining<br />

Hope Gardens, Kingston 6


OUTLINE<br />

GEOTHERMAL ENERGY?<br />

<strong>Geothermal</strong> Resource vs Conventional Power Resources<br />

Current Production Methods<br />

JAMAICA - GEOTHERMAL ENVIRONMENT<br />

Geology<br />

Status <strong>of</strong> geothermal development<br />

Exploration guides<br />

Further exploration<br />

Known areas<br />

Exploitation technique<br />

Some considerations – benefits and barriers


GEOTHERMAL<br />

ENERGY?<br />

<strong>Geothermal</strong>: „geo‟ = earth; „thermal‟ = heat<br />

“heat from the earth”<br />

Earth abounds in thermal energy.<br />

Heat generated from breakdown <strong>of</strong> naturally occurring<br />

radioactive materials.<br />

Heat is present everywhere beneath the surface.<br />

Heat rises to the surface and escapes to the<br />

atmosphere.<br />

„Renewable‟ OR Sustainable?


? ? ? ?<br />

<strong>Geothermal</strong> environments:<br />

High- and moderate-temperature rocks with considerable<br />

available water and (or) steam are the only geothermal<br />

environments that can currently be developed to generate<br />

electricity.


<strong>Geothermal</strong> Energy<br />

as a<br />

Resource


<strong>Geothermal</strong> Energy as a Mineral Resource<br />

SIMILARITIES<br />

Occur everywhere,<br />

Anomalous concentrations are favourable,<br />

Have measurable GRADE and SIZE<br />

Economic deposits – those at depths accessible by<br />

current extraction technology while remaining cost<br />

efficient.<br />

80°C 180°C<br />

LOW GRADE MEDIUM GRADE HIGH GRADE


<strong>Geothermal</strong> Energy as a Mineral Resource<br />

CHARACTERISTICS MINERAL RESOURCES GEOTHERMAL ENERGY<br />

Extractive process<br />

digging, crushing and<br />

processing <strong>of</strong> large quantities<br />

<strong>of</strong> earth material<br />

Liquid<br />

(brought to surface by hot<br />

springs or wells)<br />

Extractive method<br />

Economic characteristics<br />

mine shafts, tunnels, pits and<br />

spoil heaps<br />

Size and/or grade determines<br />

pr<strong>of</strong>itability and efficiency <strong>of</strong><br />

operation<br />

Drilled wells<br />

Usable over a very wide<br />

spectrum <strong>of</strong> temperature and<br />

volume


<strong>Geothermal</strong> Energy vs Conventional Power Resources<br />

Environmentally benign – low emission<br />

• Hot water and steam plant:


<strong>Geothermal</strong> Energy vs Conventional Power Resources<br />

CO 2 EMISSIONS<br />

Similar contrasts for the emission <strong>of</strong> sulphurous gases


<strong>Geothermal</strong> Energy vs Conventional Power Resources<br />

RELIABILITY<br />

Once online geothermal power plants are very reliable<br />

Off-line ~5% (avg.) <strong>of</strong> the time.<br />

CLIMATE CHANGE<br />

<strong>Geothermal</strong> energy is an environmentally-friendly option.


Current Production Methods<br />

Hot Water<br />

Hydrothermal System<br />

Vapour-dominated<br />

Hydrothermal System<br />

Moderate Temperature<br />

Hydrothermal System


STATUS OF GEOTHERMAL<br />

DEVELOPMENT IN JAMAICA<br />

HISTORY/ STATUS OF DEVELOPMENT<br />

Late 1600s: Bath, St. Thomas,<br />

Mid-1700s: Milk River Bath<br />

1950s – Geological Survey Department<br />

1980s:<br />

• Preliminary examinations<br />

• OLADE – Latin American Energy Organization, 1982<br />

• Ittracon – 22 Springs in tourist areas<br />

• Occidental <strong>Geothermal</strong> Inc. – Blue Mountain area<br />

• Geological Survey Division<br />

OLADE Summary report available.


<strong>Jamaica</strong>n Geology


JAMAICAN GEOLOGY<br />

JAMAICA - >65 million years ago


JAMAICA - TODAY


JAMAICA - STRUCTURE


Exploration Guides


EXPLORATION GUIDES


EXPLORATION GUIDES<br />

Position on the<br />

Caribbean Plate<br />

= low –<br />

moderate<br />

resources


EXPLORATION GUIDES<br />

Hot/ warm<br />

springs<br />

<strong>Potential</strong>ly<br />

water-bearing<br />

rocks and<br />

structures<br />

GEOTHERMAL<br />

RESOURCES<br />

Subsurface<br />

temperature<br />

anomalies<br />

Seismic zones


POTENTIAL AREAS:<br />

<br />

<br />

EXPLORATION<br />

GUIDES<br />

Faulted rocks older than the White Limestone,<br />

Boundary between different older rocks,<br />

especially intrusive igneous rocks.<br />

Shale<br />

White<br />

Limestone<br />

Yellow<br />

Limestone<br />

Sandstone<br />

Dacite<br />

Conglomerate<br />

Granodiorite<br />

Andesite<br />

Marble<br />

Serpentinite


# NAME TEMP<br />

°C<br />

FLOW<br />

litres/sec<br />

EXPLORATION<br />

GUIDES<br />

1 Guava River Spring 53 0.3<br />

2 Bath Spring 54 0.3<br />

3 Mt. Felix Spring 31 0.3<br />

4 Garbrand Hall Spring 29 1.5<br />

5 Rockfort Spring 30 50<br />

7 Salt River Spring 33 100 – 200<br />

8 Milk River Springs 38 40 – 50<br />

9 Black River Spring 29 45 – 50<br />

10 Windsor Spring 36 0.5<br />

10<br />

11 Yankee River Spring 26 0.5<br />

12<br />

12 Buxton Spring 29 1.2<br />

11<br />

2<br />

9<br />

4<br />

8<br />

7<br />

3<br />

6<br />

5<br />

1<br />

4<br />

1<br />

3<br />

2


EXPLORATION GUIDES<br />

LIMITATION:<br />

Low possibility <strong>of</strong> abnormally high<br />

heat flow,<br />

Little information on geothermal<br />

gradients,<br />

Low flow rates,<br />

Contamination by seawater<br />

# NAME TEMP<br />

°C<br />

1 Guava River Spring 53 0.3<br />

2 Bath Spring 54 0.3<br />

3 Mt. Felix Spring 31 0.3<br />

4 Garbrand Hall Spring 29 1.5<br />

5 Rockfort Spring 30 50<br />

FLOW<br />

litres/sec<br />

7 Salt River Spring 33 100 – 200<br />

8 Milk River Springs 38 40 – 50<br />

9 Black River Spring 29 45 – 50<br />

10 Windsor Spring 36 0.5<br />

11 Yankee River Spring 26 0.5<br />

12 Buxton Spring 29 1.2


EXPLORATION<br />

TECHNIQUE<br />

Binary systems would be<br />

most suitable<br />

Waterbearing<br />

rocks and<br />

structures


Some Considerations


SOME<br />

CONSIDERATIONS<br />

EXPLORATION PROGRAM:<br />

Joint Government-Private coupled program,<br />

Successful in the USA,<br />

Local knowledge combined with experience,<br />

Reduces financial and discovery risks associated with<br />

exploration,<br />

Research direction: develop techniques and strategies to<br />

identify hidden systems at greater depths.


SOME<br />

CONSIDERATIONS<br />

CHALLENGES:<br />

Are our resources within economically drillable depths?<br />

What is the state <strong>of</strong> the subsurface energy system?


REFERENCES<br />

Duffield, W. A. and Sass, J. H., 2003, <strong>Geothermal</strong> Energy –<br />

Clean Power from the Earth‟s Heat. U. S. Geological Survey,<br />

Virginia, Circular 1249, 36pp.<br />

Hylton, H. A., 1987, Mineral Springs <strong>of</strong> <strong>Jamaica</strong>. Geological<br />

Survey Division, Kingston Bulletin No. II, 69pp.<br />

<strong>Jamaica</strong> Public Service, 2007, JPS – An Overview. JPS,<br />

Kingston, unpublished report, 14pp.<br />

Latin American Energy Organization, 1982, <strong>Geothermal</strong><br />

Resource Exploration, Reconnaissance, Review and<br />

Utilisation Report. Geological Survey Division, Kingston,<br />

unpublished report, 169pp.

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