Pre-congress course on
Geothermal Energy Resources for Developing Countries
Environmental aspects of geothermal energy resources utilization
M. J. Heath
Camborne School of Mines, University of Exeter, Redruth, UK.
ABSTRACT: Geothermal energy is often advocated as one of a number of 'green', 'renewable' alternatives to fossil fuels for the supply of clean energy for the future. Geothermal energy is not without its environmental impacts, however, particularly on air, water, land use and the aesthetic qualities of the landscape in regions with geothermal energy potential. A range of socioeconomic impacts are also important. Geothermal energy is not always renewable, except over very long timescales, and geothermal energy exploitation often takes the form of heat mining with long term implications for site rehabilitation. These environmental factors can be addressed at different stages in the development of geothermal energy resources through environmental impact assessment (EIA) in advance of any development and through the implementation of an environmental management system (EMS) during the operation of a geothermal energy scheme. Approaches to optimizing environmental impacts are also considered.
Reference: HEATH, M. J., 2002. Environmental aspects of
geothermal energy resources utilization. In: Chandrasekharam, D. and
Bundschuh, J. (Eds). Geothermal Energy (Resources)
for Developing Countries. A. A. Balkema, Rotterdam.
1 INTRODUCTION
1.1 Geothermal energy - general features
Geothermal energy is energy derived from heat from the Earth's interior. This heat can be held in hot water or steam or in the rocks themselves and represents a potentially vast energy resource, estimated by Armstead & Tester (1987) to be more than 300 times the energy held in fossil fuels. Although sometimes included in lists of 'renewable' energies, most sources of geothermal energy are non-renewable, at least over human time scales, and the utilization of geothermal energy is sometimes referred to at 'heat mining', a useful term that serves as a reminder of the non-renewable nature of these resources. In view of the greatly reduced emissions of CO2 that are associated with geothermal energy when compared with the use of fossil fuels, geothermal energy is often described as a 'clean energy' (Department of Energy, 1994) but there are still environmental impacts to consider in relation to its utilization. Geothermal energy associated with hot water or pressurized steam held in aquifers or with hot dry rocks requires different approaches to its exploitation.
1.2 Geothermal aquifer systems
In the case of geothermal aquifer systems, heat can be held as pressurized steam or in hot water in deep aquifers and can be exploited directly by drilling into the aquifer. In 'high enthalpy' geothermal systems, such as those of Iceland, New Zealand and California, pressurized steam or superheated water can be used to drive a turbine, either passing the steam directly into the turbine in 'direct cycle' systems, or using a heat exchanger in a 'binary cycle'. In 'flash cycle' systems, energy is extracted from hot water by passing it through a low pressure vessel to produce steam to drive the low pressure stages of a turbine. Waste steam from these systems can either be vented directly to the atmosphere (non-condensing systems) or can be condensed prior to reinjection into wells (condensing systems), both of which have potential environmental impacts.
In 'low enthalpy' geothermal systems, hot water aquifers at temperatures below boiling point can be used directly by pumping to district heating schemes, for horticultural and agricultural use (Rinehart, 1994) or for industrial purposes or to preheat water for electricity generation. Geothermal district heating schemes have been successfully developed in Southampton, UK (ETSU, 1994), for example, and at Melun, France (Armstead, 1878).
1.3 Hot dry rock systems
In hot dry rock (HDR) geothermal systems, heat is extracted from dry rocks rather than aquifers. In this case, water must be introduced into the dry system in order to transfer heat to the surface where it can be used to generate electricity or for space heating or other purposes. The extraction of heat from an HDR geothermal energy resource is essentially non-renewable as the rock is cooled in the process, but HDR resources are extremely large (Armstead & Tester, 1987). Research into HDR systems is currently taking place in Europe, the USA and Japan but none are as yet in production.
1.4 Geothermal energy in developing countries
Geothermal energy generally makes a small contribution to the energy needs of the major developed countries but makes a significant contribution in a number of developing countries, including the Philippines, Mexico, Indonesia, El Salvador and Kenya (Reed & Renner, 2002).
The geothermal electric power industry in the USA is the
largest in the world, with an electrical generating capacity of over 2100
MW (megawatts of electricity), a little over half of which (1100 MW) is
in The Geysers geothermal field in California. Generating capacity in the
Philippines is currently around 890 MW and in Mexico is 700 MW; other developed
countries with major geothermal capacity include Italy with 545 MW, and
New Zealand with 460 MW (Reed & Renner, 2002). Interestingly, in Iceland,
which has an overabundance of both hydroelectric and geothermal energy
potential, most geothermal energy is used for space heating and hot water
rather than electrical generation (Reed & Renner, 2002).
2 ENVIRONMENTAL IMPACT ASSESSMENT FOR GEOTHERMAL ENERGY UTILIZATION
2.1 Scope of Environmental Impact Assessments
An Environmental Impact Assessment (EIA) is a formal procedure carried out as part of the planning process prior to any development. Its purpose is to assess the future impact of a proposed development on both the natural and human environments. For large projects with potentially significant environmental impacts, such as a major geothermal energy scheme, the EIA might be compulsory. For smaller projects, such a geothermal heat pump installations, the EIA might be optional but might be produced in support of a planning application to demonstrate that the environmental impacts have been considered.
The EIA will take into account any plans within the proposed development to address environmental impacts. Thus, the possible creation of water pollution problems, for example, might not be considered problematic if water treatment and monitoring procedures are also part of the plan. Similarly, plans for the restoration and aftercare of abandoned sites would be taken into account in the overall EIA.
The scope of an EIA is necessarily very broad and will vary from project to project. It will include impacts on both the natural environment (in terms of physical, chemical or biological impacts) and the human environment (in terms of economic development, employment, health implications, cultural aspects etc.).
An EIA will address the impacts of both the construction and operational phases of the proposed development. Indeed, the impacts associated with these different phases of the project might be significantly different. An EIA should include, short-, medium- and long-term impacts, local and global impacts, direct, indirect, secondary, cumulative, permanent and temporary, positive and negative effects of the project. Clearly, for a major geothermal energy development, the impacts are likely to be many, with local and global implications for the physical/chemical/biological and human environments.
2.2 Framework for Environmental Impact Assessment (EIA)
A framework for EIA is provided by the European Community's Council Directive on the assessment of the effects of certain public and private projects on the environment (85/337/EEC) which states that an EIA shall identify, describe and assess in an appropriate manner, in the light of each individual case ... the direct and indirect effects of a project on the following factors:
— human beings, fauna and flora;
— soil, water, air, climate and the landscape;
— material assets and the cultural heritage;
— the interaction between [these] factors (European
Community, 1985).
Geothermal energy schemes are covered by Annex II of the
Directive (proposed developments which may require EIA following
a case-by-case examination or thresholds or criteria set by Member States).
Here, there is specific reference to "Deep drillings, in particular: geothermal
drilling", "Industrial installations for the production of electricity,
steam and hot water" and "Industrial installations for carrying gas, steam
and hot water; transmission of electrical energy by overhead cables". "Construction
of overhead electrical powerlines with a voltage of 220 kV or more and
a length of more than 5 km" is included in Annex I (where EIAs are always
required). Annex IV of the Directive provides a detailed list of the information
requirements of an EIA, which, for a geothermal energy development, should
include the information outlined in Table 1.
3 ENVIRONMENTAL IMPACTS OF GEOTHERMAL ENERGY UTILIZATION
3.1 Global environmental factors
With increasing concern about climate change associated
with increasing atmospheric CO2 concentrations that are due,
at least in part, to the burning of fossil fuels, geothermal energy, along
with other 'renewable' energy resources, is considered to offer global
benefits through the provision of clean energy with low associated CO2
emissions (International Energy Agency, 1998).
| Table 1. Scope of an EIA: information required under EC Directive 85/337/EEC (based on European Community, 1985) |
1 A description of the project
itself, including in particular:
3. A description of the aspects of the environment itself that are likely to be significantly affected by the proposed scheme, including the human population, fauna and flora, soil, water, air, micro- and macro-climatic factors, material assets, including the architectural, archaeological and cultural heritage, landscape and the interrelationship between these factors; here, questions relating to the development in an area of outstanding natural beauty or of special scientific interest (common features of geothermal fields) would be addressed. This description should include the direct effects of the proposed scheme and any indirect, secondary, cumulative, short-, medium- and long-term, permanent and temporary, positive and negative effects of the project. 4. A description of the likely significant effects of the proposed project on the environment resulting from:
5. A description of the measures envisaged to prevent, reduce and where possible offset any significant adverse effects on the environment; here, the planned environmental protection and management methods would be described with special reference to the special problems likely to be encountered at a geothermal energy plant. 6. A non-technical summary of the information provided under the above headings (allowing non-technical decision-makers to reach their conclusion as to whether or not the scheme should go ahead). 7. An indication of any difficulties (such as technical deficiencies or lack of know-how) encountered by the developer in compiling the required information. |
These global benefits are shown in Table 2 and 3, in which
life cycle emissions of carbon dioxide (CO2), sulphur dioxide
(SO2) and nitrogen oxides (NOX) associated with a
range of renewable energies and with conventional fossil-fuelled electricity
generation, are compared with emissions from geothermal electricity generation.
These emissions values are based on life cycle analysis of the different
energy sources and include emissions associated not only with energy generation
itself but with the construction of plant and manufacture and transport
of machinery and components, which can be greater for renewables than the
energy expended in producing the plant and machinery for conventional electricity
generation because renewables generally harness energy sources that are
more 'dispersed' or 'dilute' (in contrast to the 'concentrated' energy
represented by, say, coal or oil).
| Table 2. Life cycle emissions (g/kWh) of key pollutant gases for electricity generated from renewable energy sources (adapted from International Energy Agency, 1998). | ||||||||
| Energy crops
(current
|
Energy crops
(future
|
Hydro (small) | Hydro (large) | Solar (photo-
voltaic) |
Solar (thermal) | Wind | Geo-
thermal |
|
| CO2 | 17-27 | 15-18 | 9 | 3.6-11.6 | 98-167 | 26-38 | 7-9 | 79 |
| SO2 | 0.07-0.16 | 0.06-0.08 | 0.03 | 0.009-
0.024 |
0.20-0.34 | 0.13-0.27 | 0.02-0.09 | 0.02 |
| NOX | 1.1-2.5 | 0.35-0.51 | 0.07 | 0.003-
0.006 |
0.18-0.30 | 0.06-0.13 | 0.02-0.06 | 0.28 |
| Table 3. Life cycle emissions (g/kWh) of key pollutant gases for electricity generated from fossil fuels and geothermal energy (adapted from International Energy Agency, 1998). | ||||||
| Coal
(best practice) |
Coal
(FGD and
|
Oil
(best practice) |
Gas
(CCGT) |
Diesel
(embedded) |
Geo-
thermal |
|
| CO2 | 955 | 987 | 818 | 430 | 772 | 79 |
| SO2 | 11.8 | 1.5 | 14.2 | - | 1.6 | 0.02 |
| NOX | 4.3 | 2.9 | 4 | 0.5 | 12.3 | 0.28 |
| CCGT: combined cycle gas turbines; FGD: flue gas desulphurization. | ||||||
It is clear from these comparisons that geothermal energy offers significant reductions in emissions of CO2, the main greenhouse gas, and of SO2 and NOX, both of which are toxic gases and major contributors to acid rain. These reductions represent the main argument offered in support of the further development of such energy sources. Locally, however, the balance of environmental costs and benefits is sometimes less clear.
3.2 Local environmental factors
Despite the emissions reductions that can be achieved by utilizing geothermal as opposed to conventional (fossil) energy sources, the local environmental impacts can sometimes be significant, especially with regard to air and water pollution, land use, and impacts on the aesthetic qualities of the landscape. The socioeconomic impacts on the local environment must also be considered.
Other gaseous pollutants include traces of ammonia, hydrogen, nitrogen, methane, radon and the volatile species of boron, arsenic and mercury, though generally in very low concentrations (International Energy Agency, 1998). Silica is also sometimes problematic, as at Wairakei in New Zealand, where forest damage has been attributed to silica deposition (Armstead, 1978).
In addition to gaseous emissions, dust can be associated with the construction of the plant, with drilling and with the clearance of the land for site development. More visible are the plumes of steam which contribute to the overall visual impact of the site during its operation.
Chloride brines of Na and Ca are particularly important as they can have very high concentrations of metals (Mattigod & Page, 1983). Of particular interest here are Fe, Mn, Pb, Zn, Ba and B. Other contaminants can include I, Sb, Li, H2S, Hg, Rb, bicarbonate, fluoride, silicate and ammonia (Nicholson, 1992). Contamination of shallow groundwater reservoirs can also be caused by drilling fluids and as a result of well casing failure, which might also affect groundwater levels (Hunt & Brown, 1996).
The metals content of geothermal brines from Imperial Valley, California, are shown in Table 4 where they are compared for reference with maximum admissible concentrations recommended for drinking water under the European Community drinking water directive of 1980. The higher metal concentrations observed in the Imperial Valley brines clearly exceed maximum admissible concentrations for drinking water and, therefore, represent a potentially significant environmental hazard.
Geothermal brines can not only contaminate surface and groundwaters but can also affect soils, with implications for agriculture; phytotoxic boron is particularly important in this respect (Mattigod & Page, 1983).
The pollution impacts on the water environment can be
mitigated through effluent treatment, the careful storage of waste water
and its reinjection into deep (as opposed to shallow) wells and through
careful monitoring of the condition of holding ponds and well casing (Hunt
& Brown, 1986).
| Table 4. Metal concentrations of geothermal brines from Imperial Valley, California, compared with maximum admissible concentrations for drinking water. | ||
| Metal | Concentration
Range
(ppm [1]) (Mattigod and Page, 1983) |
Maximum admissible
concentration in drinking water (ppm [2])
(From EC Directive 80/778/EEC (European Community, 1980[3])) |
| Na | 610 - 58440 | 150 (from 1987) |
| K | 70 - 23800 | 12 |
| Ca | 9 - 40000 | 100 (guide level) |
| Mg | <0.05 - 740 | 50 |
| Ba | 0.15 - 1100 | 100 (guide level) |
| Sr | 2.10 - 448 | - |
| Co | <0.0005 - <0.01 | 0.01[4] |
| Cd | <0.0005 - 2 | 0.005 |
| Cu | <0.1 - 8 | 3 |
| Fe | <0.01 - 2290 | 0.2 |
| Mn | <0.05 - 1400 | 0.05 |
| Ni | <0.01 - 4 | 0.05 |
| Pb | <0.5 - 102 | 0.05 |
| Zn | <0.01 - 600 | 5 (guide level) |
| B | 4 - 498 | 1 (guide level) |
| As | 0.025 - 12 | 0.05 |
| [1] Presented as mg
g-1 by Mattigod & Page (1983).
[2] Presented as mg l-1 in EC Directive 80/778/EEC. [3] EC Directive 80/778/EEC is being superseded by Directive 98/83/EC (European Community, 1998); the values provided by the new Directive are less comprehensive, however, and these are provided for reference only. [4] Target value for groundwater set by Netherlands Directorate General for Environmental Protection (1991) for contaminated land remediation. At the time of writing (May, 2002), EC Directives and other legislation relevant to the environment are available online through the 'EUR-Lex: Directory of Community legislation in force' at http://europa.eu.int/eur-lex/en/lif/ind/en_analytical_index_15.html. |
||
In addition to water quality impacts, the abstraction of geothermal waters can impact on groundwater levels. The most important consequence of this is ground instability and subsidence (considered below), but lowering the water table can also affect local water supplies (International Energy Agency, 1998).
As well as the major impacts that a large geothermal station might have on the aesthetic quality of the landscape, local visual impacts from buildings, plant, pipework and plumes of steam might also be considered important, especially by local residents, but this can be reduced by careful screening of the site.
Noise can be associated with the exploration, construction and production phases and can be significant in terms of occupational exposure, requiring workers to be suitably protected. Noise as an environmental impact (along with many of the visual impacts) can be reduced by the screening of the site with earth bunds and/or trees (Hunt & Brown, 1996) and through the adoption of good working practices, such as restricting working hours.
Ground subsidence occurs when geothermal fluids are withdrawn from a reservoir at a rate greater than natural inflow back into the reservoir. This causes compaction of the rock formations at the site which, in turn, leads to surface subsidence, as observed at Wairakei in New Zealand. Ground subsidence can be reduced by reinjecting waste waters into wells to maintain well pressure, though associated risks of groundwater contamination need to be considered when designing the reinjection process. Subsidence might also result from thermal contraction of rocks associated with hot dry rock geothermal utilization (Taylor, 1983).
Because many geothermal resources are located in seismically active zones of the Earth's crust, there are sometimes problems of instability, both in the natural landscape and in association with geothermal energy utilization (DiPippo, 1991). The re-injection of fluids into the ground, for example, can enhance the seismic activity of the area affecting buildings and other structures and allowing seepage of fluids within the system, though this can be minimized by keeping reinjection pressures to a minimum. Landslide hazard might also be a feature of geothermal regions where steep slopes are susceptible to failure, perhaps leading to damage to well heads or pipes resulting in the release of steam and hot fluids. The likelihood of this can be minimized by stabilizing all slopes which may be prone to landslides (DiPippo, 1991).
Heat pollution of air and, particularly, water can represent a significant environmental impact as well as being energy inefficient. The discharge of hot water to rivers can damage aquatic wildlife (as in the Waikato River in Wairakei) and lead to unwanted growth of vegetation (Armstead, 1978). The effects of heat pollution are local, however, and the total amount of heat released in this way is negligible compared with solar radiation and does not in itself represent a significant global environmental problem (Armstead, 1978).
The tourist potential of geothermal regions and the need to protect geothermal phenomena like geysers has already been noted as a major economic consideration. At Svartsengi geothermal power station in Iceland, geothermal energy utilization has itself been used to the advantage of the tourist industry where geothermal waste waters have been used for the development of the Blue Lagoon, a spa facility developed adjacent to the plant itself (Blue lagoon Ltd., 2000).
The International Energy Agency (1998) also sees the restructuring
of energy markets as an important economic impact of renewable energy sources
which tend to take the form of many small, dispersed units rather than
the large centralized power plants that have characterized the energy markets
in recent decades. This is seen as contributing to increased competition
and greater flexibility. The ability of local schemes to meet
local demands (for heat, for example, in the case of geothermal energy)
is also noted (International Energy Agency, 1998).
4 MANAGEMENT OF OPERATIONAL ENVIRONMENTAL IMPACTS
4.1 Environmental Management Systems
4.1.1 ISO 14001
During the lifetime of a geothermal energy plant, day to day environmental impacts can be managed through the implementation of an environmental management system (EMS). The international standard for environmental management systems is the International Standards Organization's ISO 14000 series, of which ISO 14001 is the specification with guidance for use (ISO, 1996). ISO 14001 provides a structure for carrying out the following key environmental management activities:
It is of interest to note that ISO 14001, the standard for environmental management, is closely linked to the quality standard, ISO 9001 (ISO, 2000). If, therefore, an organization is already using the ISO 9000 structure (which is commonly the case in many countries), it is already well prepared to adopt an ISO 14000 environmental management system.
4.1.2 Eco-Management and Audit Scheme (EMAS)
An alternative to the ISO standard is the European Community's Eco-Management and Audit Scheme (EMAS) (European Community, 2001). The main provisions of EMAS are similar to those of ISO 14001 but there is greater emphasis on the publication of the results of environmental reviews and audits.
The purpose of EMAS, for which registration is obtained on a site-specific basis after independent (external) verification, is to help industrial (and local authority) sites to:
4.2 Optimization of the environmental impacts of geothermal energy utilization
The environmental impacts of a geothermal energy scheme can be optimized through the adoption of environmental procedures at different stages in the development of a project.
Environmental questions are addressed in advance of the development of a geothermal scheme through the implementation of an environmental impact assessment (EIA), which addresses a range of questions relating to the impacts of a proposed project on the physical, chemical, biological and human environments. During the operational phase of a geothermal scheme, day to day environmental impacts can be managed through the implementation of an environmental management system (EMS).
The environmental impacts of a geothermal development can also be optimized by paying special attention to the following aspects (International Energy Agency, 1998):
5 CONCLUSIONS
Geothermal energy offers considerable advantages over conventional fossil fuelled electricity generation through greatly reduced CO2 emissions (with global implications with regard to climate change) along with lower SO2 and NOX emissions (with implications for local air quality and the generation of acid rain). Despite the global environmental benefits that can be claimed for geothermal energy, there may be important local impacts on the atmosphere, notably through the emission of H2S and other minor gaseous pollutants, and on surface and groundwater, mainly through the disposal of contaminated waste water.
The impacts of geothermal energy utilization can be managed
and minimized through their careful consideration as an environmental impact
assessment (EIA) prior to site development and through the implementation
of an environmental management system (EMS) during the operation of the
scheme. Socioeconomic impacts are also important and can be optimized through
the involvement of local communities in the development of geothermal resources.
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