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TRAINING ON SURFACE EXPLORATION STUDIES FOR GEOTHERMAL RESOURCES AND DEVELOPMENT
OF CONCEPTUAL MODELS
UNDER THE AUSPICES OF INTERIM PROJECT COORDINATION UNIT OF THE AFRICA GEOTHERMAL
CENTER OF EXCELLENCE
ASMARA ERITREA 8-17 APRIL 2019
An overview of Geothermal Exploration Methods andProject Development
Gylfi Páll Hersir, Iceland GeoSurvey
Monday April 8th 2019
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Classification according to Temperature
High-temperature if reservoir temperature at 1 km depth is
above 200°C
Medium-temperature if reservoir temperature at 1 km depth
is between 150-200°C
Low-temperature if reservoir temperature at 1 km depth is
below 150°C
Also on the basis of energy content [high- or low-enthalpy],
physical state [liquid-dominated, two-phase or vapour-
dominated] or their nature and geological setting
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Introduction to Surface Exploration
The objective is to obtain information about the properties of the geothermal system prior to drilling
Successful surface exploration will reduce the cost of later stages in the development and thus save a lot of money in the end
Geothermal surface exploration is a multidisciplinary task
Exploration strategy depends on many factors, including geological setting and temperature in the system
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Surface exploration can provide information on:
Temperature in the geothermal reservoir
Permeability (fractures) of the reservoir
Areal extent of the thermal anomaly
Depth to useful temperatures
Location of the up-flow zone
Chemical composition of fluid
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Conceptual model of a high temperature field
Figure: Kristján Sæmundsson, ÍSOR ©© ICELAND GEOSURVEY
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We need careful exploration:
• A deep exploration borehole in a high temperature field can cost several million USD.
• The total cost of geo-scientific exploration is only a part of the cost of one such well.
• However, exploration requires considerable up-front cost prior to exploration drilling. Therefore:
– Exploration methods must be selected with respect to the site
– Exploration must be carried out in professional manner
– Stepwise approach is recommended, i.e. the strategy must be revised as the results appear.
© ICELAND GEOSURVEY
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Scales of Exploration:
• Regional exploration: Exploration covering large area in order to identify possible geothermal resources and roughly assess their size.
• Local exploration: Exploration that concentrates on the interior of a known geothermal field in order to identify the best production sites and target for drilling to obtain maximum energy output with minimum cost.
© ICELAND GEOSURVEY
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The selection of exploration methods
• The geology of geothermal fields are quite variable from one place to another.
• There is no single exploration procedure that can be applied universally to all geothermal fields.
• The selection of exploration methods must be tailor-made for each field.
• But we have guidelines to form suitable exploration strategy for each field.
© ICELAND GEOSURVEY
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Regional exploration – the first steps of geothermal development
1. Review of existing data
2. Reconnaissance
3. Geological Exploration
4. Geochemical Exploration
5. Geophysical Exploration
6. Exploration Drilling
7. Preliminary Resource Estimate
These studies end in a pre-feasibility report
© ICELAND GEOSURVEY
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Step 1. Review and study available data
© ICELAND GEOSURVEY
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Step 2: Reconnaissance
• Desktop study of all available data• Field studies:
• Visual studies, maps, photographs (infra red)• Mapping of the manifestations• Temperatures and flow rate• Mapping of soil temperatures• Fluid sampling and analyses (geo-thermometers, fluid chemistry)• Historical data on activity and utilization
• Ownership and rights (licensing)• Environmental aspects (EIA)• Social aspects• Market possibilities
Are there market opportunities in developing the area?
© ICELAND GEOSURVEY
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Components of geothermal surface exploration
• Geological mapping
• Geophysical exploration
• Geochemical exploration
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Step 3: GeologicalExploration
• Geological mapping (lithology).
• Structural geology
(faults, fractures, dykes).
• Volcanology and volcanic history.
• Hydrogeology.
• Geo-hazards and environmental geology.
Does the surface activity relate to geological structures ?
© ICELAND GEOSURVEY
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ICELAND GEOSURVEY
A simplified geological map of SW-Iceland showing fissures.Hengill cv bisected by a fissure swarm: 3-5 km wide and 40 km long.Triple junction: WVZ, RP and SISZ.Swarm was active in 1789 with extensive rifting and subsidence.
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ICELAND GEOSURVEY
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ICELAND GEOSURVEY
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ICELAND GEOSURVEY
A geological map of the Hengill area, yellow dots denote surface manifestations, black curves the three volcanic centres Graendalur (0.3-0.5 My), Hrómundartindur (erupted 11 t.y.a.); Hengill 2 & 5 t.y.a.)
Mapping of
geological units
Type of units
Chemical analyses
Volume of volcanic products
Age volcanic activity
Volcanic hazard?
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Tectonic Mapping
•Map faults and fissures
•Determine throw
on faults
•Determine age of
faults and fissures
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Volcanology
•Map volcanic craters
and fissures
•Determine their age
•Determine the type of
lava erupted
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Surface manifestations
Extensive mapping of:
•Fumaroles
•Hot springs
•Warm ground
•Altered ground
•Characteristic vegetation
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Geological model
• Tectonic setting and history
• Vulcanological history
• Likely locations and types of heat sources
• Likely permeability structure
• Geological risk assessment
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Geochemistry is:
• studies of soil chemical anomalies• measurement of soil diffuse degassing• sampling of hot springs and fumaroles• sampling of cold springs• analyses of chemical species in water; and gas in steam• geothermometers for water and steam• stable isotope analyses
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Objectives of geochemical surveys are:
To obtain information about:
– temperature in the reservoir
– chemical composition of fluids
– source of fluids
– evaluate corrosion potential of the fluid
– evaluate scaling potential
– evaluate the origin of the fluid
– evaluate active upflow zones with I the area
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Mapping of manifestations, temperature and
flow rate.
Mapping of soil temperatures
Chemical analysis of springs and gas from
steam vents gives information on reservoir
temperatures.© ICELAND GEOSURVEY
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Chemical geothermometers
• Temperature sensitive reactions control concentrations and concentration ratios of chemical components in water solutions and gases
• This allows evaluation of subsurface temperatures based on fluid and gas compositions
• Chemical geothermometers implicitly assume that equilibrium was attained in the reservoir and no reactions occurred during the upflow
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Chemical geothermometers
• Best to use as many geothermometers as possible (complete analyses)
• Discrepancies between results of different geothermometers may provide important information about the nature of the system
– e.g. extent and distribution of condensation and interactions with cold groundwater
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CO2-temperature map of Torfajökull geothermal system, Central Iceland
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Surface Geophysics is:
Measuring different physical attributes of the earth crust from the surface:
We distinguish between:
Direct methods: thermal, electrical, passive seismicsIndirect or structural methods: gravity, magnetics andactive seismic methods
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Main Geophysical Methods in Geothermal
• Thermal methods (soil temperature, heat-flow)
• Electrical methods (resistivity)
• Gravity methods (rock density)
• Magnetic methods (rock magnetization)
• Seismic methods (sound velocity, seismicity,geological structure)
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Resistivity and Electrical methods
Resistivity is the most diagnostic parameter for geothermal activity that can be measured from the surface - Ωm
Elevated temperature and geothermal alteration produce distinctive resistivity structure
However, care must be taken. Fossil alteration preserves the resistivity structure
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• DC-methods (Schlumberger, Dipole-Dipole) < 1 km
• TEM-methods (TEM) < 1 km
• Magneto-Tellurics (MT, AMT) several km
Electrical Methods
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32Schlumberger method
TEM
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The setup of a MT sounding: Electrodes for measuringthe electric field, coils for the magnetic field; aquisitionunit for digital recording and GPS for syncronizing data
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m a.s.l.400 -
200 -
- 200 -
- 400 -
- 600 -
0 -
0 500 1000 1500 2000 m
ResistivityTemperature°C
Alteration
Unaltered rocks
Smectite - zeolite zone
Mixed layered clay zone
Chlorite zone
Chlorite-epidote zone
> 25 m
10 - 25 m
2 - 10 m low resistivity cap
High resistivity core
250
200
200
150
100
50
NJ-1
1
NG
-7
NG
-10
Nesjavellir
Resistivity cross-section from Nesjavellir geothermal field, SW-Iceland, alteration zoning and temperature
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MSc Defense – Andemariam Teklesenbet-13/01/12
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1D inversion of resistivitydata from Alid byAndemariam
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ICELAND GEOSURVEY
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Aeromagnetic map of the Hengill area, SWIceland. Flying altitude 800 m a.s.l.; 1549stations
Positive anomaly NE-SW, due to normalmagnetization of lavas from the Brunhesgeomagnetic epoch (<0.8 My)Matuyama epoch (0.8-2.5 My)was reversed.
Magnetic low coincides with surfacemanifestations (black dots),demagnetisation due to alteration
Magnetics
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Result of relative location of
earthquakes from a high
temperature field in Iceland. The
red lines are known faults on the
surface. The dots are epicenters,
their color show the year of the
quakes. The upper map shows the
epicenters but the lower one
shows a blow up of the upper one.
The maps show clearly how the
epicenters are bound to just one
of the faults and this fault is known
to be a flow path for geothermal
water. The upper cross section
shows a north-south cross section
of the hypocenters while the lower
one shows a east-west section.
Note the westward dip of the fault
and the deepest earthquakes are
at 6 km depth suggesting
temperature close to 700°C (taken
from Flóvenz et al., 2012; modified
from Hjaltadóttir and Vogfjörð,
2011)
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A cross section showing seismic hypocenters across the Menengai caldera
and geothermal field in the East-African Rift Valley in Kenya. The lower
boundary of the seismic activity defines the brittle –ductile boundary in the
crust, possibly the 450°C isotherm (taken from Flóvenz et al., 2012;
modified from Simiyu, 2008)
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Joint interpretation
During the progress of exploration, the geologists, geochemists and geophysicists develop individual ideas about the geothermal prospect.
When all the different data sets are in place, they must be interpreted jointly to synthesise a conceptual model which is consistent with all the data.
The conceptual model is then used to site exploration wells.
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CONCLUSIONS
• Geothermal exploration is a multidisciplinary task (geology, geochemistry, geophysics)
• No single method is universally superior, but fracture mapping, electrical methods and chemical geothermometry are usually most important
• Integrated multi-method and dynamic approach important
• Cost-efficiency should be considered
• Successful surface exploration will save big money when project enters development phase
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Information gained from Surface Exploration(Preliminary geothermal model)
• Estimation of the size of the geothermal
resource and its exploitable thickness
• Estimation of the reservoir temperature
• Expected reservoir fluid chemistry
• Definition of drilling targets and type of
exploration wells to be drilled
• The information should be incorporated into
a preliminary conceptual model of the field.
• Volumetric assessment made to get a first
estimate of the power potential of the
resource.
© ICELAND GEOSURVEY
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© ICELAND GEOSURVEY
Step 5: Exploration Drilling (sub-surface exploration)
•Testing the results of the resistivity exploration
•Confirming/updating the conceptual model
• Confirming the temperature estimation of surface sampling
• Confirming the chemical composition of the brine
•Confirming the existence of a geothermal resource
• Flow-testing the reservoir
• Update the reservoir model
•
Is it likely that the geothermal resource is exploitable,
and what kind of power plant is viable?
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The International Financial Corporation (IFC, a member of the World Bank Group) published an analysis in June 2013 (International Financial Corporation, 2013). The IFC analysis was based on the outcome of 2613 geothermal wells in most of the countries of the world where geothermal electricity is produced. The main findings of the analysis are the following:
The average capacity of all successful wells is 7.3 MWe, while the most likely (most frequent) capacity is 3.0 MWe. The great difference in the two values reflects the skewness of the underlying statistical distribution, where a relatively few high capacity wells influence the average greatly.
Drilling success
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Resource enthalpy (resource type) causes the greatest variability in capacity, while geological conditions, well depth and well diameter have a much smaller effect.
The overall drilling success rate during the last 5 decades has been 50% during the exploration phase of a geothermal project, 74% during the development phase and 83% during the operation phase. This has improved drastically with time and analysis of wells drilled during the 2000’s shows that the success rate during the exploration phase has increased to 85%.
Drilling success - continue
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Step 6. Preliminary Resource Estimate and updating theconceptual model.
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Refined/updated Conceptual Model of the Hengill High Temperature Area
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Volumetric assessment
The first approach to evaluate the resource up on completing the surface exploration is to carry out a volumetric assessment of the resource. This assessment is improved by the information gained from the exploration drilling, often by applying Monte Carlo statistics to the volumetric assessment.
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Volumetric assessment, using the Monte Carlo method
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Regional exploration - concluding remarks
• It is our experience that the investment in executing a thorough
surface exploration program is money well spent
• One failed well due to negligence in exploration can cost
several times the cost of the surface explorations
• Surface studies should therefore have high priority in all
geothermal exploration programs
• Regional exploration and exploration drilling ends in a pre-
feasibility report, with some preliminary power plant
designs.
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Local exploration:
• If regional exploration is successful further development takes place.
• Local exploration is necessary to define drilling targets in order to maximize the energy output from new wells:
• Find the upflow zones
• Find permeable fractures
• Find fault zones and intrusions
• Find cooling magma bodies
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The first large scale Geothermal Development Project 1928-30
Utilization of a low temperature field for space heating. The field was famous for its hot springs and for centuries women carried the laundry to the hot springs (now in mid Reykjavík).
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Drilling started in 1928in Reykjavík for hot water.
14 boreholes drilled (<250 m deep)
Result about 14 l/s of 87°C water.
1928-1930
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1930 District Heating in Reykjavík- 3 km longpipeline
-Two schoolhouses, hospital, swimmingpool and 70 private housesconnected.
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The environmental benefit
From fossil fuel to geothermal
Before geothermal space heating:
Reykjavik in 1933 covered with smoke from
coal heating.
With geothermal space heating:
Reykjavik in 2008, almost same view but
without visible air pollution.
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Project Cost and Risk Profile at Various Stages of Development
58Source: ESMAP Geothermal Handbook
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What do we need to develop a geothermal resource from a hot spring to utilization?
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What do we need to develop a geothermal resource from a hot spring to utilization?
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Opportunity
+
Skills
+
Time
+
Money
+
Luck
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Thank you
The eruption of Eyjafjallajökull 2010. Photo: Ólafur G. Flóvenz