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Article

The Suitability of the Pacific Islands for Harnessing Ocean Thermal Energy and the Feasibility of OTEC Plants for Onshore or Offshore Processing

by
Hyeon-Ju Kim
1,*,
Ho-Saeng Lee
1,
Seung-Taek Lim
1 and
Michael Petterson
2
1
Seawater Energy Plant Research Center, Korea Research Institute of Ships & Ocean Engineering, Daejeon 34103, Korea
2
School of Science, Auckland University of Technology, Auckland 1010, New Zealand
*
Author to whom correspondence should be addressed.
Geosciences 2021, 11(10), 407; https://doi.org/10.3390/geosciences11100407
Submission received: 18 July 2021 / Revised: 20 August 2021 / Accepted: 21 August 2021 / Published: 27 September 2021
(This article belongs to the Special Issue The Geoscience of the Pacific Islands Region: Theory and Practice)
Browse Figures
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Abstract

:
Ocean Thermal Energy Conversion (OTEC) relies on the thermal differences between ocean surface waters and cooler waters at c. 1000 m depth. The highest and most reliable thermal differentials are in the low latitudes, 20° either side of the equator, including the Pacific Islands region. Whilst in theory OTEC can utilize an inexhaustible amount of stored energy within the oceans, in practice the industry remains in its technical infancy, but with an increasing relevance to a post-fossil-fuel, environmentally conscious world. OTEC does not only produce electricity. OTEC-seawater utilization technologies produce high demand ocean minerals, desalination, a range of waters for aquaculture and hydroponics, and have the potential to produce large quantities of green hydrogen. OTEC is a green energy and could revolutionize the energy and economic landscape of Pacific island countries, providing reliable low-C electricity and a basis for a range of industry. This paper analyses the economics of using OTEC in combination with existing and potential future industries of importance to the Pacific (and other oceanic) regions, including tuna fisheries, seabed minerals and green hydrogen. The conclusions of these analyses suggest that OTEC has the potential to minimize carbon emissions, increase efficiencies, and create new high-quality green-technology industries and livelihoods.

1. Introduction

Fossil fuels have been the mainstay of energy requirements for most of the global community from the earliest to the most recent industrial revolutions. However, the release of carbon, and other greenhouse gases, in significant abundance, has caused global environmental changes that require urgent solutions. Climate change caused by anthropogenically-induced global warming requires the establishment of efficient and effective counter-measures. Response and adaptation to climate change is being sought through the more efficient use of existing energy resources, the supply of new and renewable energy resources, and the reduction and absorption of carbon dioxide and other Greenhouse Gas Emissions [1].
Some of the Pacific Island Countries and Territories, particularly low-lying atolls, act as ‘early warning systems’ for environmental change impacts, such as sea level rise, variable and less predictable rainfall patterns, and higher average land temperatures. Countries such as Kiribati and Tuvalu, which are low-lying atoll nations, have produced an infinitesimal share of global greenhouse production, and yet may face the most adverse consequences of climate change, even perhaps the loss of their countries to sea-level rise [2]. The aspirations of the United Nations Sustainable Development Goals (SDGs) [3] for food <SDG#2>, water <SDG#6>, and energy <SDG#7> is an existential goal for the survival and development of the Pacific Islands, as well as the public prosperity of mankind [4].
Within the global tropical belts, situated between 20 degrees latitudes, north and south of the equator, warm sea-surface water temperatures (20–30 °C) are present throughout the year, whilst the deeper ocean waters (at depths =/> 1000 m) are at a constant temperature of c. 5 °C. This thermal gradient between surface and deeper seawaters provides the physical background for ocean thermal energy conversion (OTEC). An engineering principle, termed Rankine cycle power generation, can use the thermal gradient to generate power. Whilst at the moment OTEC is not a large-scale commercial reality, a number of organizations are developing small-scale OTEC plants, both land and sea-based, with the vision that, one day, the plants will become large enough to attract commercial interest. Ocean Thermal Energy Conversion (OTEC) power generation has been evaluated as being particularly appropriate to the equatorial Pacific Island countries, due to the excellent temperature conditions, and the existence of small island developing states with more limited energy options compared to large contiguous continental settings. OTEC can continuously generate electricity, day and night, all year round [5].
OTEC plants are flexible systems that can provide a lot of outputs, beyond only electricity. For example, OTEC plants can provide regional cooling and heating systems, desalinate seawater, extract seawater minerals, assist with aquaculture through the provision of waters at variable temperatures, and hydroponic cultivation using discharged water, as well as generating green-clean electricity responsible for country-base-load requirements. The Pacific Islands region is also attractive globally to the fishing industry for tuna in particular, and to the mining industry for the development of seabed mining industries [1]. Currently, tuna caught in the tropical belt fishing grounds are being transported directly to the large Asian and European/North American markets, or overseas processing plants. Whilst Pacific Island states will explore all options available for economic development, we argue that the provision of electricity from OTEC plants, alongside seawater-utilisation technologies, such as seawater-minerals for the cosmetics industry, and aquaculture, offer other opportunities for the diversification of livelihoods. The realisation of OTEC technologies could significantly improve livelihoods and the economy, whilst minimizing carbon footprints [2].
This paper introduces the Research and Development status from the principle of OTEC, and examines the social acceptance of power generation cost based upon the current status of local electricity supply and rates. Scenarios where OTEC can assist with industries such as seabed deep-sea minerals, aquatic product manufacture, and the provision of freshwater from desalination is reviewed.

2. Principles and Types of Ocean Thermal Energy Conversion

Ocean Thermal Energy Conversion (OTEC) generates power through closed cycle (CC-OTEC) and open cycle (OC-OTEC) processes (Figure 1 [6]). CC-OTEC, also called Anderson OTEC, evaporates low-temperature boiling working fluids (organic refrigerants) such as ammonia and the synthesized compound R32 (difluroromethylene), into warm surface water within a closed circulatory system. Fluid-steam flow turns the turbine, and generates power, with the working fluid vapor passing through the turbine being condensed by the colder deep seawater, and circulated via a pump. OC-OTEC, also called Claude OTEC, uses surface seawater as both a heat source, and a working fluid [7]. Surface seawater evaporates under reduced pressure, and then rotates a low-pressure steam turbine to generate electric power. Water vapor is liquefied to obtain fresh water. Another hybrid system (HC-OTEC), which uses aspects of CC and OC-OTEC to simultaneously conduct closed-circulation power generation and open-circulation desalination. For the production of green hydrogen using marine renewable power, a seawater electrolyzer or a water electrolyzer can be used. As the seawater electrolyzer linked with CC-OTEC cycle is in the basic stage, the HC-OTEC cycle that can produce fresh water as well as electricity will be more promising to apply the water electrolyzer. Research to improve the efficiency of each cycle is being conducted in various countries around the world, and systems and core parts and devices for realizing this are being developed [7,8].
The degree and duration of the temperature difference is an important influencing factor for the performance of OTEC. In low latitudes, it is possible to operate year-round with higher efficiencies, whereas in mid-latitudes, it is possible to operate only in summer (late spring to early autumn) with variable to lower efficiencies.

3. Distribution and Capacity of Ocean Thermal Energy

The minimum differential temperature between the surface and deeper ocean waters that can operate an OTEC plant is 17–18 °C. OTEC plants operate to maximum efficiency when located in regions that can sustain a 17–18 °C minimum temperature differential for all or most of the year. The average temperature of the upper part of the ocean that can be used as a seawater heat source is 12.6 °C. The middle ocean depths are maintained at a temperature of around 3.8 °C, and the deepest ocean temperatures are around 1 °C or less. Whilst there is relatively little change in water temperatures in the middle and deep layers of the ocean throughout the year, the upper layers are strongly influenced by ocean currents, solar insolation, and energy flows. Average sea surface temperatures can be higher than 28 °C at the equator, and as low as 0 °C in the polar regions. In the mid-latitude waters around Korea, sea-temperatures at depths of 200 m or more are constant throughout the year, but the upper layer fluctuates between 8 and 26 °C due to seasonal changes [9]. Therefore, in the case of the Korean sea area, it is estimated that the utilization rate of OTEC (the percentage of time throughout the year whereby OTEC is technically possible) will reach about 38%, based on a temperature difference of 18 °C or more. However, in tropical and subtropical seas (between 20 degrees south latitude and 20 degrees north latitude, Figure 2) the annual operation rate is judged to be close to 100%.
The annual available capacity of OTEC is estimated to be 80,000 TWh [10], or more than three times the current global electricity demand (24,000 TWh). OTEC resources are fully renewable, and, in theory, inexhaustible. They can continuously produce electricity and do not require electricity storage devices.
As the change of convection due to global warming has mutual influence with the change of output of OTEC plant as long as the background of thermohaline circulation (THC) is strong enough (e.g., 15.6 Sv at its present-day value), large OTEC flows will not significantly disturb it [11]. In addition, conditions that can increase the output of OTEC plant occur depending on various variables such as the temperature and change period of global warming, and the intensity of the Atlantic THC [12].
Traditional OTEC technologies use the temperature difference between deep ocean water and surface seawater (17–24 °C) [13], and, if it is possible, can additionally utilize other locally available heat resources (e.g., solar energy, geothermal energy, hot water resources, incineration heat, etc.) where deep ocean water is available. OTEC technology efficiencies can be significantly increased by the thermal addition of additional energies (solar, geothermal etc.) as this increases the thermal gradient of the power plant (to 30–80 °C, rather than the c. 18–25 °C from ocean temperature differentials alone) [14].

4. Technology Development and Industrial Trend of OTEC

OTEC is one of the marine energy technologies that has not been commercialized in spite of the fact that it has had a long history (Figure 3). Jules Verne’s marine science novel ‘20,000 Leagues Under the Sea’ published in 1870, brought the existence of ocean thermal gradients to the world. In 1881, the theoretical basis for OTEC was developed by D’Arsonval, with the first electricity generated through OTEC technologies, in 1930, by George Claude. Hydrocarbons, particularly cheap and abundant oil supplies, inhibited further development of OTEC until the global petroleum oil crisis of 1973, which encouraged further research and development in the United States and Japan. In 1978, the U.S. succeeded in the operational realisation of OTEC through its ‘Mini-OTEC’ project (Figure 4a): a 50 kW offshore closed-cycle OTEC power plant, based in Hawaii, using ammonia as a working fluid [14].
An additional 210 kW onshore open-cycle OTEC power generation plant (Figure 4b) was developed in 1983, and tested for long-term operation. Japan conducted a number of demonstration experiments by the Tokyo Electric Power (100 kW plant (Figure 4c), in Nauru), and Kyushu Electric Power Companies (50 kW plant), and Saga University (75 kW plant). India installed a 1 MW class offshore closed-cycle OTEC power plant (Figure 4d) using ammonia, in the Indian Ocean, but the plant ceased operation due to the breakage of a key connection part between the plant barge and riser (intake pipe) [15].
Since 2008, the United States, Japan, and France have resumed research and development for seawater temperature thermal gradient OTEC generation, and additionally, in 2011, Korea, developed a 100 W class land-based proto-type OTEC plant (Figure 5a), followed by a 20 kW class pilot OTEC plant (Figure 5b) in 2012–2013 [13], by the Korea Research Institute of Ships and Ocean Engineering (KRISO) with affiliated clean ships and offshore plants developed from 2011. The hybrid OTEC system to produce about 200 kW (Figure 5c) was fabricated and demonstrated in 2014, that used deep ocean water as a heat sink (5 °C) and waste heat from a wood gasification generator as a heat source (75 °C) [16]. Based on this, in 2019, a 1000 kW class OTEC demonstration plant (Figure 6) was produced, and a performance evaluation field test was successfully conducted in the south eastern sea, of the East Sea of Korea, demonstrating the production of 338 kW of electricity, with a relatively small temperature difference [17]. If this plant is installed and operated in the equatorial ocean latitudes with local temperature differences of 24 °C or higher, it is estimated that about 1000 kW will be produced.
The OTEC industry can be thought of as both a plant manufacturing, and a power generation business. Plant manufacturing is the manufacturing of systems, parts and devices, and consists of turbines, generators, evaporators, condensers, refrigerant pumps, seawater pumps, water intake pipes (risers), power control devices, and plant monitoring and control devices. The seawater temperature difference power plant can be built onshore or installed offshore. When installed within the ocean, a constant position should be maintained, so that the plant does not drift or fluctuate with the waves or ocean currents, and the design of a platform, as well as an appropriate mooring/anchoring system is developed. As an example of the OTEC platform, we introduced a Sevan-type platform (Figure 7) that acquired AIP from BV [19]. It aims to manufacture platforms, systems, parts, and devices with high performance, a long life, low cost, and at minimal environmental impact.
The current status of OTEC-potential for various countries around the world, including research and development, is being investigated and analysed, every three-months, under the commission of IEA-OES [20,21]. Currently, planning, installation, and operation of OTEC are in progress at about 20 locations around the world (Figure 8). The results of on-line surveys of global OTEC status are summarized with respect to type, project stage, generation capacity, heat exchange, working fluid requirements, and so forth (Figure 9). OTEC Plants can be onshore or offshore, or combinations of both.

5. Economic Feasibility of OTEC and Applicability of Pacific Island Countries

It is imperative that a robust economic case is designed for the development of OTEC at any specific site, within a particular market. An economic analysis requires consideration of the quality of resources and economies of scale, alongside market place supply and demand conditions. The IEA-OES (2015 [22]) presented the power generation cost (LCOE) of OTEC, by comparing it with wave power generation, and tidal power generation (Table 1). The power generation cost of a 10–20 MW class commercialization demonstration plant is estimated to reach US-cents 35~65/kWh, and US-cents 15~28/kWh for larger 100 MW class commercialization plants. Vega, Oh, and others, estimate that when 100–400 MW class commercial plants begin to be deployed, at around 2030, and potential carbon credits are taken into account ($2/t CO2), the power generation cost will decrease to US-cents 8–15/kWh [23,24]. Solar and wind power generation is expected to decrease to US-cents 7–8/kWh around 2020, but these power types require electricity storage, which adds cost.
Pacific Island countries tend to have high electricity rates, with relatively small markets, and volatile demand. According to the current status of electricity rates in the Pacific Islands (Table 2), it is estimated that the costs of modern day OTEC plants will be competitive with respect to present day electricity prices for countries such as Tonga, Vanuatu, and Solomon Islands. Improvements in OTEC plant efficiencies will make OTEC highly competitive for many small islands developing states, including Pacific Island countries [25].
Therefore, the power generation cost of OTEC will not only be cheaper than the local electricity rates, but also will realize energy welfare through stable supply. In addition, since it is possible to reduce greenhouse gases, it is expected that it can be put into practical use as an energy source for establishing a carbon-neutral eco-friendly clean foundation [2].

6. OTEC-Based Processing Plant and Applicability in Pacific Island Countries

The prescient risks posed by anthropogenically caused climate change are requiring urgent actions to reduce greenhouse gas emissions. The irony in the Pacific region is that the very existence of countries that have produced a tiny proportion of global cumulative greenhouse gases could be threatened by sea level rise (e.g., COP21). Assisting Pacific Island Countries to develop greener economies is part of the global response to CO2 emission reductions, and helps the region develop future-looking economies [2,26]. Whilst there are a variety of solutions (solar, wind, etc.) that are possible within the Pacific region, OTEC offers the opportunity to access huge amounts of stored ocean energy, and develop a range of future-looking seawater utilisation industries (aquaculture, seawater minerals, drinking water, hydrogen-generation) that can generate high quality livelihoods [1].
Various useful mineral resources exist on the ocean floor (seabed minerals) (Figure 10, [27]). These include polymetallic nodules, polymetallic or seafloor massive sulfides, and cobalt-rich ferromanganese crusts. Manganese nodules (Figure 11, [27]) are gravel-potato-sized mineral aggregations that contain manganese, nickel, copper, titanium, cobalt, and rare earth elements. They are situated on the oceanic abyssal plains, at depths of 4000 to 6000 m. There are a range of estimates of metal resources contained within manganese nodules: around 1.7 trillion t of manganese nodules exist in the Pacific Ocean alone. Around 15% of the world’s ocean floors contain manganese nodules, with an average of 15 kg/m2 [28]. It is estimated that the global mineable quantity of manganese nodules is around 500 billion t [29].
It will be useful to consider the energy requirements of ocean floor mining operations (Figure 12). The greener energy options will be particularly attractive. The operation of deep-sea mines generates CO2 through: (1) the operation of ships used to transport ore to the destination port; (2) transportation of personnel and goods through supply lines; and (3) the generation of electricity (Figure 13). External costs associated with increased CO2 emissions from shipping and mining operations are based on estimates of total annual fuel use (in tons). Fuel use includes the following activities: (1) submarine mining tools and power supply of production support vessels; (2) barge activities; and (3) crew boats.
The feasibility of manganese nodules mining within the Pacific Ocean has been reviewed by the Secretariat of the Pacific Community (Cardno, 2016 [30]). The Penrhyn Basin, Cook Islands, is an example of a Pacific region containing high concentrations of nodules, and an abundant resource of nodules (Hein et al., 2015 [31]). There is a high nodular abundance (>25 kg/m2) and area of 124,000 km2, and an estimate mineral resource of 3.6 billion t (Hein et al., 2015 [31]). The generally accepted economic nodule density cut-off grade for commercial mining, is around 5 kg/m2, with the nodule density range within the Cook Islands Exclusive Economic Zone ranging from 5 kg/m2 to over 50 kg/m2 (Cronan, 2013 [32]).
Mining operations are varied and complex, from exploration, to extraction, to refining and final metal production (Figure 14, Figure 15 and Figure 16).
Manganese nodule processing, mineral beneficiation, and smelting plants required for manganese nodules would treat 2.5 million t of manganese nodules per year [30]. If it is installed on land, a high pressure/high temperature acid leaching facility covering an area of about 180 acres will be required. Refining plants would include processing and support facilities, as well as long-term waste containment areas, with possible separate processing buildings for copper and nickel end-product development, nodule grinding and leaching, pH adjustment and neutralization, and ammonia recovery (Dames and Moore, 1977 [34]). There would be a boiler-house/power-house and several cooling towers located adjacent to the chemical process areas, alongside offices, laboratories, maintenance shops, warehouses, worker-cafeteria, and other facilities.
The plants in total could occupy an area of 20–40 acres (8.1~16.2 ha), while an additional 20 acres (8.1 ha) would be needed for raw ore storage, settling ponds for treating wastewater, and storage for various other inputs that feed into the process [34].
In addition to raw nodules and waste, about 5500 t of fuel and process materials would enter the facility, and about 240 t of waste products would be emitted per day [34].
The current marine fisheries industry within the Pacific is an extensive large-volume industry. The distribution of Pacific tuna fisheries is shown in Figure 17 and Figure 18. This is also the region where OTEC plants can operate most efficiently and effectively.
Mining and smelting 2.5 million t of manganese nodules per year requires 1.6 billion gallons (6,056,658 m3) of water and 149 GWh of electricity per year [30]. Assuming that the electricity demand for seawater desalination is 5 kWh per m3, some 30.3 GWh of energy will be required. The power demand could be met by installing an OTEC power plant with a net output of 24 MW (total output 40 MW) or more, to supply 179.3 GWh annually to the mineral refining plant, as well as all fresh water requirements from seawater desalination. OTEC plants would prevent the emission of 82,370 t of CO2 per year. Hydrogen could also be produced by the OTEC plant: this fuel could be used to power ships and transportation related to mining at sea.
The caught tuna is transported directly to the market through a carrier, or transported to a treatment facility, for processing and sale. Processing is rarely undertaken within the Pacific region itself, for a range of reasons including electricity capacity, water resource availability, and distance from international market. There is scope for increasing the number of fish processing plants within the Pacific region. The case of fish production in Kiribati is considered here from the viewpoint of OTEC assisting this area of economic development.
Kiribati Fish Ltd. [36] was established in 2010 and completed in 2012. It is located at Betio Port, South Tarawa Island. Fiji and China have invested US $8 million, contributing to the revitalization of the local economy and job creation. The core businesses of the Kiribati Fisheries Company are tuna fishing, local fisheries, fish processing, and export packaging and transport (Figure 19 and Figure 20). This industry has created jobs for 200 people.
Electricity and fresh water are essential for processing tuna (Figure 20) and other fish products. At the present time, diesel generators and seawater desalination systems are installed for plant operation purposes. Fuel costs are an important consideration for business such as this, as are carbon emissions, and water costs. The power generation cost of diesel generators depends on the fuel cost: these are relatively expensive in Kiribati, with the resulting power being supplied at rates of AU$0.55/kWh for commercial and AU$0.70/kwh for industrial use. Water is also scarce, and expensive at AU$2/KL, if the monthly usage is less than 2.5 t, and AU$15.00/KL if it is more than 10 t [37].
The Kiribati Fisheries Company is operating two 200 kW class diesel generators and two 50 t/day reverse osmosis seawater desalination systems, as shown in Figure 21 and Figure 22. It was not easy to estimate the unit cost of power generation and desalination, but when one 200 kW diesel generator is operated for one hour, 59.5 L of diesel is consumed, so the fuel cost is about AU$73.6. Including depreciation and maintenance costs, it is estimated to be equivalent to commercial electricity rates (AU$0.55/kWh). To this end, if an OTEC plant with a net output of 0.6 MW (total output of 1 MW) were deployed, the annual carbon emission reduction is estimated to reach 2294 t CO2.
In South Tarawa, Kiribati, the annual temperature of the sea surface water is c. 28~30 °C, and the deep seawater at a depth of 1000 m is c. 5 °C, which makes OTEC plants located in South Tarawa particularly efficient and able to produce 24/7 year-round power. Assuming that the annual operating cost is 5% of the production cost, based on the production cost of the 1 MW OTEC plant, and experiences within Korea to date for OTEC technologies, (Figure 23 [17,18]), the life cycle power generation cost (LCOE) is estimated to be less than US$0.39/kWh (Table 3 [23]). Based on this, it is estimated that the power generation cost of 10 MW and 100 MW commercial plants will decrease to less than US$0.18/kWh and US$0.09/kWh respectively, with efficiency improvements and capacity increase progress [38]. Therefore, within the oceans of equatorial island countries such as Tarawa, it will be possible to establish a low-carbon, clean production base, through power-generation and desalination, using an appropriately scaled OTEC plant.
Hydrogen generation from OTEC plants is increasingly becoming a realistic proposition, with 100 MW plants generating (Figure 24 [39]), 10 MW (83,220 MWh/year) for electricity, and 50 MW (416,100 MWh/year) used for desalination and hydrogen production. Some 19 t of hydrogen could be produced per day (about 7000 t/year).
Makai Ocean Engineering. Inc. has estimated the production cost of OTEC power for hydrogen production and transporting it to a demand site, based on a range of scenarios. For the case of using all of the electricity of an OTEC plant, capable of producing 25 to 200 t/day hydrogen, the supply cost, including transportation, was estimated at US$8 to US$3/kg H2 (Figure 25, [39]). This accounted for an interest rate on initial investment of 10%. If a discounted c. 4% interest rate were applied, costs reduce to c. US$4.5–2/kg H2 (Figure 26, [39]). Interest rates of 4–6%, on initial investment costs, could achieve a price for green hydrogen of $3/kg.
Therefore, if the current OTEC technologies become successful and further improved, the generation of green hydrogen is a distinct technical and economic possibility (Figure 27, [40]). A very large floating structure (VLFS) is required for processing of deep-sea mineral resources and pelagic aquatic resources, and hydrogen production in the open sea. VLFS can be fabricated by connecting multiple Octagonal Sevan platforms centering on the OTEC platform, and basic studies were carried out through numerical analysis and Ocean Engineering basin experiments in KRISO [41,42].

7. Direction of Use of OTEC to Strengthen Regional Resilience

The climate crisis facing Pacific island nations not only relates to the possible shrinking of island boundaries with sea level rise but, also relates to a number of aspects of life quality and livelihoods. These may relate to the shortage and cost of energy supply, impacts on food and water security, and ecosystem degradation, as well as increasing risks related to coastal erosion, heat waves, cyclone frequency and intensity, drought length and frequency, and other environmental impacts. OTEC technologies can have a place in assisting with more optimistic future scenarios [43]. These include 24/7 production of green energy from a practically inexhaustible energy source, the provision of fresh water from desalination, opportunities for cooling, refrigeration and heating, contributions to aquaculture and hydroponic agriculture, the potential development of seawater mineral industries (e.g., salt, lithium, sodium, potassium, calcium, strontium, chlorine, etc.), and the generation of hydrogen.
An economically sized OTEC plant will enable the sustainable development of related projects that require a large amount of seawater. For example, the 100 MW class OTEC plant has to take in more than about 10 million t of deep seawater per day, and drain it to about 10 °C with clean seawater quality. This will enable a large scale aquaculture complex that produces more than 50,000 t of salmon per year, or desalination or facility agriculture, microalgae culture, and so on. In addition to green power and fuel supply, district cooling is capable of establishing carbon-neutral communities along Pacific Islands Countries.
This paper focuses on small island developing states (SIDS) that have a number of advantages for small scale to medium scale OTEC plants. However, the return on economic investment is not anticipated to be large, as markets are small. SIDS have an urgent need for reliable green energy and they are excellent ‘testing grounds’ for the further development of OTEC technologies. It is probable that if the proof on concept for OTEC plants in SIDS is realized, there would be a natural progression to larger scale OTEC plants (100 MW to GWs), which would require larger markets and bigger populations. Countries such as Indonesia, Malaysia, Philippines and Mexico, etc. are candidates for the development of large OTEC plants.
OTEC can assist with a range of industries including fisheries, shipping, and seabed mining. These are an impressive combination of potential outputs from one generic technology. These environments, materials, and energy can be used to promote health and improve economic regeneration. In other words, the use of seawater energy and resources could contribute to achieving a range of UN Sustainable Development Goals (SDGs) for the local community (Figure 28 and Figure 29).
If seawater energy and onshore energy are combined, a range of eco-friendly blue-green infrastructures can be assembled encompassing industry, residences, recreational areas, on and off-shore. OTEC and offshore solar power generation, sea water air conditioning (SWAC) and freezing or refrigeration, seawater desalination and extraction of useful substances, aquaculture and plant factories, and land and sea forest development could be created in urban and rural areas alongside infrastructure such as ports and airports (blue ports), universities, and public institutions. Furthermore, features (Figure 29) such as the Blue campus, sports, and cultural facilities (Blue arena) [44], and energy-independent villages and islands, can be created alongside the OTEC and seawater utilization technologies.

8. Conclusions

The human race is facing an existential climate crisis. There is widespread agreement that greenhouse gases must be rapidly reduced to minimise the worst impacts of the climate crisis. Through COP21 and related agreements, over 120 countries have submitted long-term reduction plans (LIDS) for ‘carbon neutrality’ to the United Nations. The International Maritime Organization (IMO) is committed to reduce carbon emissions by 40% compared to 2008 figures for ships ordered after 2030, and by 50% by 2050 [45]. Shipping emissions amounts to 2.5% (about 1 billion t per year) of total global emissions.
The development of renewable energy resources and the creation of carbon-absorbing ecosystems for residential and industrial activities in Pacific island countries is an area in which OTEC technologies can significantly contribute to a greener and more sustainable future for Pacific Island countries [46]. Pacific island nations have provided miniscule amounts of global greenhouse gases, but are suffering more than most parts of the world from the negative impacts of the climate crisis. Existential threats include rising sea levels, changing rainfall distributions, increasing cyclone intensities and frequencies, and so forth. Energy and electricity costs for Pacific Island countries are amongst the highest in the world [25]. Even though all Pacific Island countries are surrounded by abundant seawater and marine resources, they are suffering chronic deficiency of drinkable water and food materials [2].
Future economic possibilities for Pacific countries include fishing, tourism, and seabed mining. OTEC provides a possibility for the further development of these industries using green energy, and greatly reducing carbon footprints [47].
Tropical oceanic regions have the highest thermal differentials in the world between surface waters and waters at depths of 1000 m. Furthermore, the Pacific equatorial waters have the advantage of not being exposed to harsh external force environments such as typhoons and high waves. This situation makes OTEC technology particularly viable in this region.
SIDS have an urgent need for reliable green energy and they are excellent ‘testing grounds’ for the further development of OTEC technologies. It is probable that if the proof on concept for OTEC plants in SIDS is realized, there would be a natural progression to larger scale OTEC plants (100 MW to GWs), which would be required larger markets and bigger populations.
OTEC can also provide a range of ancillary industries and outputs including fresh water, a range of heating, cooling and refrigeration services, aquaculture and hydroponic agriculture, green hydrogen generation, seawater mineral production, and so on [48].
Models are currently being created for a range of possible new modes of living combining OTEC technologies with on-land technologies producing a blue-green ecologically friendly environment to implement sustainable communities along the tropical belt.

Author Contributions

Conceptualization, H.-J.K. and M.P.; Methodology, H.-S.L. and S.-T.L.; Validation, H.-J.K.; Investigation, S.-T.L.; Resources, H.-J.K. and M.P.; Data curation, H.-S.L. and S.-T.L.; Writing—original draft preparation, H.-J.K. and S.-T.L.; Writing—review and editing, H.-S.L. and M.P.; Visualization, S.-T.L.; Supervision, H.-J.K. and M.P.; Project administration, H.-J.K.; Funding acquisition, H.-J.K. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by the Ministry of Oceans and Fisheries of the Republic of Korea (grant number: PMS4730).

Institutional Review Board Statement

Not applicable.

Acknowledgments

This work was financially supported by the national R&D project of “Development of 1 MW OTEC demonstration plant (6/6)” (PMS4730) funded by the Ministry of Oceans and Fisheries of the Republic of Korea.

Conflicts of Interest

The authors declare no conflict of interest.

References

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Figure 1. OTEC systems: closed cycle (a); and open cycle (b) [6] (Reprinted with permission from National Energy Laboratory of Hawaii Authority).
Figure 1. OTEC systems: closed cycle (a); and open cycle (b) [6] (Reprinted with permission from National Energy Laboratory of Hawaii Authority).
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Figure 2. Distribution of annual average temperature difference between 1000 m deep water and surface water (Reprinted with permission from ref. [10]. Copyright Gerard Nihous, University of Hawaiʻi at Mānoa).
Figure 2. Distribution of annual average temperature difference between 1000 m deep water and surface water (Reprinted with permission from ref. [10]. Copyright Gerard Nihous, University of Hawaiʻi at Mānoa).
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Figure 3. History of OTEC and current status.
Figure 3. History of OTEC and current status.
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Figure 4. Examples of typical OTEC power plants before 2007 [14]. (a) Mini-OTEC (USA), (b) OC-OTEC (USA), (c) Nauru OTEC (Japan), (d) NIOT OTEC (India).
Figure 4. Examples of typical OTEC power plants before 2007 [14]. (a) Mini-OTEC (USA), (b) OC-OTEC (USA), (c) Nauru OTEC (Japan), (d) NIOT OTEC (India).
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Figure 5. Research and development of OTEC systems by KRISO [13,16] (a) 100 W OTEC Mock-up, (b) 20 kW OTEC pilot plant, (c) 200 kW HOTEC(ORC) plant.
Figure 5. Research and development of OTEC systems by KRISO [13,16] (a) 100 W OTEC Mock-up, (b) 20 kW OTEC pilot plant, (c) 200 kW HOTEC(ORC) plant.
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Figure 6. 1 MW OTEC demonstration Power Plant Assembly ((a), Busan Port) and field experiment ((b), Pohang offshore) (KRISO [17,18]).
Figure 6. 1 MW OTEC demonstration Power Plant Assembly ((a), Busan Port) and field experiment ((b), Pohang offshore) (KRISO [17,18]).
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Figure 7. Aerial view of the floating type 1 MW or 10 MW OTEC power plant (KRISO, [19]).
Figure 7. Aerial view of the floating type 1 MW or 10 MW OTEC power plant (KRISO, [19]).
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Figure 8. Promising OTEC site and Project Progress (KRISO [20], IEA-OES [21]).
Figure 8. Promising OTEC site and Project Progress (KRISO [20], IEA-OES [21]).
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Figure 9. OTEC technology status survey result (KRISO [20], IEA-OES [21]).
Figure 9. OTEC technology status survey result (KRISO [20], IEA-OES [21]).
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Figure 10. Map of Manganese Nodule Rich Regions in parts of the Pacific and Indian Oceans. Pacific Island State Exclusive Economic Zones (EEZ) shown in darker blue. Nodule rich fields are bounded by brown lines. The Clarion Clipperton Zone contains the world most abundant Manganese Nodule Field [27]. Reproduced with permission, and with full acknowledgement, SPC (Pacific Community).
Figure 10. Map of Manganese Nodule Rich Regions in parts of the Pacific and Indian Oceans. Pacific Island State Exclusive Economic Zones (EEZ) shown in darker blue. Nodule rich fields are bounded by brown lines. The Clarion Clipperton Zone contains the world most abundant Manganese Nodule Field [27]. Reproduced with permission, and with full acknowledgement, SPC (Pacific Community).
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Figure 11. Examples of manganese nodule density on the seabed. (A) Small nodules of high abundance; (B) Large nodules of high abundance; (C) Small nodules of low abundance; (D) Bi-modal nodules of high abundance [27]. Reproduced with permission, and with full acknowledgement, SPC (Pacific Community).
Figure 11. Examples of manganese nodule density on the seabed. (A) Small nodules of high abundance; (B) Large nodules of high abundance; (C) Small nodules of low abundance; (D) Bi-modal nodules of high abundance [27]. Reproduced with permission, and with full acknowledgement, SPC (Pacific Community).
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Figure 12. Typical deep-sea minerals mining value chain [30]. Reprinted with permission from SPC (Pacific Community).
Figure 12. Typical deep-sea minerals mining value chain [30]. Reprinted with permission from SPC (Pacific Community).
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Figure 13. Potential range of mining activities for deep sea mining activities [30]. Reprinted with permission from SPC (Pacific Community).
Figure 13. Potential range of mining activities for deep sea mining activities [30]. Reprinted with permission from SPC (Pacific Community).
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Figure 14. Example of a Sea-floor Manganese Nodule Mining System (Credit: GRID-Arendal, https://www.grida.no/resources/7352, accessed on 18 July 2021 [33]).
Figure 14. Example of a Sea-floor Manganese Nodule Mining System (Credit: GRID-Arendal, https://www.grida.no/resources/7352, accessed on 18 July 2021 [33]).
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Figure 15. Deep Sea Mining Nodule Collector Unit (Cardno, 2013 [30]). Reprinted with permission from SPC (Pacific Community).
Figure 15. Deep Sea Mining Nodule Collector Unit (Cardno, 2013 [30]). Reprinted with permission from SPC (Pacific Community).
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Figure 16. Aerial image of the Basamuk Refinery in Papua New Guinea (Cardno, 2013 [30]). Reprinted with permission from SPC (Pacific Community). https://miningdataonline.com/property/3323/Ramu-Mine (accessed on 30 May 2021).
Figure 16. Aerial image of the Basamuk Refinery in Papua New Guinea (Cardno, 2013 [30]). Reprinted with permission from SPC (Pacific Community). https://miningdataonline.com/property/3323/Ramu-Mine (accessed on 30 May 2021).
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Figure 17. The spatial distribution of the longline catch by Tuna species in 2015–2019 in the WCPO. The size of the largest pie corresponds to the maximum value of 70,000 t (Hare et al., 2020 [35]). Reprinted with permission from SPC (Pacific Community).
Figure 17. The spatial distribution of the longline catch by Tuna species in 2015–2019 in the WCPO. The size of the largest pie corresponds to the maximum value of 70,000 t (Hare et al., 2020 [35]). Reprinted with permission from SPC (Pacific Community).
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Figure 18. Spatial distribution of the purse seine catch by Tuna species in 2015–2019 in the WCPO. The size of the largest pie corresponds to the maximum value of 1,031,000 t (Hare et al., 2020 [35]). Reprinted with permission from SPC (Pacific Community).
Figure 18. Spatial distribution of the purse seine catch by Tuna species in 2015–2019 in the WCPO. The size of the largest pie corresponds to the maximum value of 1,031,000 t (Hare et al., 2020 [35]). Reprinted with permission from SPC (Pacific Community).
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Figure 19. Unloading of tuna at Betio port (Tarawa, Kiribati, Photo: H.J. Kim).
Figure 19. Unloading of tuna at Betio port (Tarawa, Kiribati, Photo: H.J. Kim).
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Figure 20. Tuna processing work (Tarawa, Kiribati, Photo: H.J. Kim).
Figure 20. Tuna processing work (Tarawa, Kiribati, Photo: H.J. Kim).
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Figure 21. 200 kW class diesel generator (Kiribati Fish Ltd. (Tarawa, Kiribati), Photo: H.J. Kim).
Figure 21. 200 kW class diesel generator (Kiribati Fish Ltd. (Tarawa, Kiribati), Photo: H.J. Kim).
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Figure 22. 50 m3/day desalination system (Kiribati Fish Ltd. (Tarawa, Kiribati), Photo: H.J. Kim).
Figure 22. 50 m3/day desalination system (Kiribati Fish Ltd. (Tarawa, Kiribati), Photo: H.J. Kim).
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Figure 23. 1 MW OTEC demonstration plant (KRISO) [17].
Figure 23. 1 MW OTEC demonstration plant (KRISO) [17].
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Figure 24. Conceptual drawings of hybrid OTEC plants for power generation-desalination-hydrogen production (KRISO) [17].
Figure 24. Conceptual drawings of hybrid OTEC plants for power generation-desalination-hydrogen production (KRISO) [17].
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Figure 25. Hydrogen production costs according to the size of OTEC-H2 plant (Makai Ocean Eng., 2000 [39]). Reprinted with permission from Richard Argall, Makai Ocean Engineering, Inc.
Figure 25. Hydrogen production costs according to the size of OTEC-H2 plant (Makai Ocean Eng., 2000 [39]). Reprinted with permission from Richard Argall, Makai Ocean Engineering, Inc.
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Figure 26. Hydrogen production costs according to size of OTEC-H2 plant and interest rate (Makai Ocean Eng., 2000 [39]). Reprinted with permission from Richard Argall, Makai Ocean Engineering, Inc.
Figure 26. Hydrogen production costs according to size of OTEC-H2 plant and interest rate (Makai Ocean Eng., 2000 [39]). Reprinted with permission from Richard Argall, Makai Ocean Engineering, Inc.
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Figure 27. Conceptual drawing of sustainable and self-sufficient oceanic base of very large floating structure for OTEC-H2 system (KRISO, [41,42]).
Figure 27. Conceptual drawing of sustainable and self-sufficient oceanic base of very large floating structure for OTEC-H2 system (KRISO, [41,42]).
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Figure 28. Cascade use model of deep ocean water and surface water [43].
Figure 28. Cascade use model of deep ocean water and surface water [43].
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Figure 29. Blue infrastructure concepts using OTEC and SWAC systems [44].
Figure 29. Blue infrastructure concepts using OTEC and SWAC systems [44].
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Table
Table 1. Levelized Cost of Energy (LCOE) of marine energy estimated (IEA-OES) [22].
Table 1. Levelized Cost of Energy (LCOE) of marine energy estimated (IEA-OES) [22].
Deployment StageVariableWaveTidalOTEC
MinMaxMinMaxMinMax
First array/
First project		Project
Capacity (MW)		130.3100.15
CAPEX ($/kW)400018,100510014,60025,00045,000
OPEX ($/kW, year)140150016011608001440
Second array/
Second project		Project
Capacity (MW)		1100.5281020
CAPEX ($/kW)360015,3004300870015,00030,000
OPEX ($/kW, year)100500150530480950
Availability (%)85%98%85%98%95%95%
Capacity Factor (%)30%35%35%42%97%97%
LCOE($/MWh)210670210470350650
First commercial-scale projectProject
Capacity (MW)		275390100100
CAPEX ($/kW)2700910033005600700013,000
OPEX ($/kW, year)7038090400340620
Availability (%)95%98%92%98%95%95%
Capacity Factor (%)35%40%35%40%97%97%
LCOE ($/MWh)120470130280150280
Table
Table 2. Current status of electricity prices and supply in Pacific island countries (IRENA) [25].
Table 2. Current status of electricity prices and supply in Pacific island countries (IRENA) [25].
RankCountryPrice (¢/kWh)Electricity Penetration Rate (%)Renewable Energy Production Rate
(MWh)		Percentile of Renewable Energy over Total Electricity Production Population
(1000 People)		GDP per Capita
(USD)
1Vanuatu18~15927132822463335
2Solomon Islands80~85152365.33.15521517
3Cook Islands44~6599592.822410,875
4Kiribati33~589019.40.11001490
5Tuvalu31~58922002101831
6Niue41~57979031.69618
7Micronesia37~566530004.31062852
8Tonga479515.1920.031054168
9Samoa35~429528.1080.041843532
10Nauru8~411002.0570.01102071
11Palau28.2~40.59967.440.1218730
12Marshall Islands33~409016.710.03553169
13Papua New Guinea19.6~38.889.7402,4081270591845
14Fiji9~179066,593.89.18684391
www.irena.org, http://www.fea.com.fj/your-home/electricity-tariffs-and-rates (accessed on 12 May 2015).
Table
Table 3. LCOE of 1 MW OTEC power generation (KRISO) [23].
Table 3. LCOE of 1 MW OTEC power generation (KRISO) [23].
LCOE of K-OTEC (KRISO, 2018)
ConditionsEven price
Basis$0.39/kWh
CDM $20/t CO2$0.38/kWh
Reduce initial cost: 15%$0.34/kWh
Reduce initial cost: 30%$0.30/kWh
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Kim, H.-J.; Lee, H.-S.; Lim, S.-T.; Petterson, M. The Suitability of the Pacific Islands for Harnessing Ocean Thermal Energy and the Feasibility of OTEC Plants for Onshore or Offshore Processing. Geosciences 2021, 11, 407. https://doi.org/10.3390/geosciences11100407

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Kim H-J, Lee H-S, Lim S-T, Petterson M. The Suitability of the Pacific Islands for Harnessing Ocean Thermal Energy and the Feasibility of OTEC Plants for Onshore or Offshore Processing. Geosciences. 2021; 11(10):407. https://doi.org/10.3390/geosciences11100407

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Kim, Hyeon-Ju, Ho-Saeng Lee, Seung-Taek Lim, and Michael Petterson. 2021. "The Suitability of the Pacific Islands for Harnessing Ocean Thermal Energy and the Feasibility of OTEC Plants for Onshore or Offshore Processing" Geosciences 11, no. 10: 407. https://doi.org/10.3390/geosciences11100407

APA Style

Kim, H. -J., Lee, H. -S., Lim, S. -T., & Petterson, M. (2021). The Suitability of the Pacific Islands for Harnessing Ocean Thermal Energy and the Feasibility of OTEC Plants for Onshore or Offshore Processing. Geosciences, 11(10), 407. https://doi.org/10.3390/geosciences11100407

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