Seabed mineral resources, an alternative for the future of renewable energy: A critical review
Graphical abstract
Introduction
Several types of minerals are found in the deep sea, including marine nodules, ferromanganese crusts, and massive polymetallic sulphides (Schriever and Thiel, 2013). Fe and Mn oxides (crusts and nodules) are formed by direct precipitation in seawater. They are mainly deposited on the flat parts and on the flanks of seamounts, where ocean currents prevent sedimentation (Konstantinova et al., 2017). These deposits are located in all oceans around the world (Marino et al., 2017a, Marino et al., 2017b). While polymetallic sulphides have been observed in a wide variety of volcanic and tectonic environments, at depths that vary between 3700 and 1500 m (Herzig and Hannington, 1995), they mostly occur in an oceanic ridge system that is almost 60,000 km long (Pandey, 2013). These are formed when seawater interacts with the heat of magma in the subsoil region (Hannington et al., 2011).
Diverse authors have highlighted the need to generate new options to overcome an eventual stagnation of the growth capacity in mining (ICSG., 2017, Toro et al., 2019a, Toro et al., 2019b), considering the significant challenges faced by the industry. The grade of the terrestrial deposits is continuously decreasing, for example, in the year 1900 the average of copper contained in the rocks was approximately 4%, while currently, the grades are close to 0.5% Cu (Mudd, 2009, Toro, 2020), with some cases reaching 0.26% (mch, 2012). In comparison, subsea polymetallic sulphide deposits have grades between 1 and 12% Cu, while manganese nodules also contain grades of 1% Cu (Hein et al., 2013). Land mining is exploited three-dimensionally, where significant amounts of surcharges are eliminated to find the mineral deposits. In contrast, the deposits of marine nodules and ferromanganese crusts are strictly two-dimensional, being on the seabed without overloading. On the other hand, massive polymetallic sulphides are three-dimensional and can be tens of meters thick; however, they are not exposed to overload (Hein et al., 2013).
The constant growth of technological advances is causing an expansion in the requirements for critical metals (Ros, 2018). Base metals are called “critical metals”, which are indispensable for the manufacturing of advanced technology, green technology, and emerging industries (Graedel et al., 2015, Pak et al., 2019). Researchers estimated that the largest reserves of many of these elements are located on the seabed, where the largest reserves of cobalt, nickel, and manganese are found in submarine deposits (mch, 2018), in addition to a considerable amount of rare earth (Pak et al., 2019).
Global warming is one of the primary concerns for industrial development, with carbon dioxide being the most significant contributor to climate change (Hofer et al., 2018, Lacis et al., 2010, Ming et al., 2014, Murakami et al., 2020). The energy sector produces substantial amounts of CO2; hence, it is imperative to move toward decarbonisation (Greenpeace. , 2019, Lacis et al., 2010). This creates financial opportunities for mining due to the metal boom that decarbonization involves, and the large-scale deployment of generating renewable energy (West et al., 2019). Interestingly, Rietveld et al., (2019) projected a decrease in energy demands; however, the authors highlighted a reduction in the use of fossil fuels. Fig. 1 exhibits a prediction on the market of energy from different sources, where we highlighted how the consumption of electricity, biomass, and waste will grow, with a notable lessening of the use of oil.
Critical metals generate a positive perception for the development of technological advances, though their production causes controversy. An example is the effectively monopolistic status of China in the mining, refining, and technical knowledge for the production of rare earth elements (Jaroni et al., 2019). This has generated conflicts with the European Union, the USA and Japan due to their dependence on these raw materials (Rietveld et al., 2019). Another example is Cobalt production, as its supply is dominated by only one country, the Democratic Republic of the Congo. They produce nearly 60% of the world’s Cobalt, while no other country offers more than 6%. Despite this, the Democratic Republic of the Congo is one of the poorest countries in the world (Banza et al., 2018).
For the reasons previously stated, the mineral resources of the seabed are an interesting alternative that would allow the expansion in the supply of critical metals. They would also diversify the exploitation of reserves to avoid monopolistic concentrations in the production of these strategic elements.
Section snippets
Mineral resources on the seabed
The oceans and other saline waters are the largest water resource on the planet, representing 97.4% of global water (Cisternas and Gálvez, 2018). The ocean covers 71% of the planet's surface (Kirk Cochran, 2014) and is the habitat of 97% of living things (González et al., 2012, Toro et al., 2018). Due to its great depth, distance, and extent, exploration and mapping is a highly challenging process, and only a small fraction of the ocean floor has been bathymetrically mapped (Mayer et al., 2018,
Metals present
The increasing increase in technological advances has increased the demand for critical metals, which raises concerns regarding the sustainability of resources (Habib et al., 2020, Ros, 2018, Wall et al., 2017, Watari et al., 2020). The world population is expected to increase by 2 billion people in the next 30 years, from the current 7.700 billion to the 9.700 billion in 2050, reaching a peak of about 11.000 billion by 2100 (UN, 2019). More than 2.5 billion inhabitants live in countries with
The current project for the exploitation of underwater deposits
Since marine nodules were discovered on the HMS Challenger journey (1872–1876) (Toro et al., 2020), humanity has progressed in economically exploiting these resources (Sharma, 2017). The first mining pilot tests were performed in the Pacific Ocean by the IMO of the USA, Japan, Canada, and Germany in 1978. In these exploitation tests, 800 tons of marine nodules were extracted, at 5500 m from the sea, where they concluded that it would be feasible to exploit marine resources. However, this
Conclusions (Summary)
Approximately a third of the population lives in countries with expanding economies, which require resources to continue their growth and respond to the need for a sustainable energy future. While recycling may appear to be an excellent alternative to recover metals, along with other options to replace the critical minerals, it has not been possible to satisfy the current demand. This has been primarily due to the increase in technological advances, which are associated with a high demand for
Declaration of Competing Interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgements
Ricardo I. Jeldres is grateful for the support of Centro CRHIAM Project Anid/Fondap/15130015. Pedro Robles thanks the Pontificia Universidad Católica de Valparaíso for the support provided.
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