Geothermal Potential of Jamaica
Geothermal Potential of Jamaica
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.