Underground pumped hydroelectric energy storage (UGPHES) is a similar energy storage concept to conventional pumped hydroelectric energy storage (PHES), with the major difference that the lower reservoir is located in an underground cavern system. This study examines several existing energy storage systems, introducing the UGPHES as an alternative bulk energy storage technology in South Africa to contribute to the limited electricity grid with environmental and economic benefits.
Purpose and scope of research
Pumped Hydroelectric Energy Storage (PHES) is a conventional energy storage method used around the world. This dissertation report presents a new adaptation of the pumped hydroelectric method of storing energy, known as underground pumped hydroelectric energy storage (UGPHES).
Methodology
However, although there are many energy storage methods available and with the development of renewable energy sources, the real challenge lies in being able to store large amounts of energy in an efficient and cost-effective manner. In the recent past, existing energy storage technologies have been improved and many new storage technologies have been developed.
Compressed air energy storage (CAES)
One of the main reasons behind energy storage is the fast response time required during peak demand, which the conventional coal and nuclear power plants cannot efficiently handle, resulting in energy waste [3]. Another existing CAES plant that has been in operation since 1991 is the McIntosh 110 MW plant built in southwest Alabama on the McIntosh salt dome.
Battery energy storage
The battery has a lifetime of 2500 cycles and is more environmentally friendly than lead batteries due to the use of less toxic electrolytes [28]. Lead-acid batteries have a very low energy density of around 30 Wh/kg with a power density of around 180 W/kg [34].
Thermal energy storage (TES)
Testing of the two-tank molten salt storage system using molten salt as a heat transfer fluid was conducted in the “Solar Two” Central Receiver Solar Power Plant demonstration project in California [24]. Trough and tower storage facilities are two methods of transferring heat to the molten salt.
Hydrogen energy storage
Large amounts of renewable energy, such as wind power and photovoltaics, can also be stored and transported using a hydrocarbon-based energy storage system (CHES). This allows excess energy from renewable sources to be stored for longer periods of time and used at times when demand exceeds supply [50].
Superconducting magnetic energy storage
Performance does not degrade over the life of the system, including controllability and reliability. One of the biggest technical challenges to consider in system design is the potential to generate large magnetic fields due to the fact that SMES system cryostats become rapidly pressurized when the coils become non-superconducting [53].
Ocean renewable energy storage (ORES)
The European Organization for Nuclear Research, CERN, is home to one of the largest superconducting magnets built for a liquid hydrogen bubble chamber with a stored energy of about 0.2 MWh [56]. The total charging capacity of the storage cylinder (in megawatt hours) can be related to the internal volume of the sphere, the depth and the efficiency of the pump/turbine unit.
Flywheel energy storage
The stored kinetic energy is converted into electrical energy and vice versa, by the electrical machine that drives the flywheel. Compact and self-contained, allowing the flywheel system to be placed in areas with limited space.
Supercapacitor energy storage
With the advancement in the use of nanotube technology to increase the surface area of the capacitor, the energy density of the supercapacitor is comparable to that of a lithium-ion battery. The permittivity of the dielectric, the surface area of the plates and the distance between the plates determine the capacitance.
Pumped hydroelectric energy storage (PHES)
For most surface water systems as in the case of the upper reservoir of a PHES system, the flow is considered to be turbulent [70]. The upper (front) tank is constructed in the same manner as the conventional PHES scheme and is usually located directly above the lower tank as shown in Figure 3-1.
Cost of UGPHES
The one-stage UGPHES system is a system where there is a single vertical drop or hydroelectric plant and a single underground power plant between the upper and lower reservoir. In a double-stage UGPHES scheme, there are two vertical falls or hydroelectric power plants and two underground power plants between the upper and lower reservoir.
UGPHES site requirements
The most frequent problems that arise are the disposal of waste generated from the excavation of the lower reservoir and the gradual temperature increase of circulated water [77]. The spoil from the excavation of the lower reservoir could be used in the construction of the upper reservoir, while the gradual increase in water temperature is not seen as a serious problem [77].
UGPHES performance and modelling
The location of the pump in the well and the hydraulic conductivity of the material create the limits of the yield of the well [3]. When water is injected into a well, as shown in Figure 3-2, a dike forms due to the hydraulic conductivity of the aquifer material.
Existing installations of UGPHES systems
The water will be pumped back into the upper reservoir using low-cost off-peak energy. The facility will be located near existing power transmission lines and an industrial substation.
Technological adaptation of UGPHES
There is also a proposed UGPHES project for the Port of Estonia – Muuga, where the sea will be used as the upper reservoir and the lower reservoir will be located underground [77]. Seawater extracted from the Baltic Sea will be used due to its marginal salinity of only 4-6%.
Aquifers in South Africa
Aquifer consumption in South Africa contributes only about 15% of the total amount of water used in the country [93]. The withdrawal of the maximum volume (m3) of groundwater per unit area per year without further long-term decline in the water table is known as the Groundwater Resource Potential (GRP).
Aquifer under seabed
Aquifers in Namibia
This is partly due to the fact that South Africa supplies almost half of Namibia's electricity [109]. However, the use of the Ohangwena II vast aquifer for a UGPHES scheme could benefit both Namibia and South Africa in the long term.
Transboundary aquifers shared by South Africa
It should be noted that there is no indication that the potential of this aquifer has been fully explored. The aquifer characteristics of this area include the Burgersdorp Formation, the Molteno Formation and the Elliot Formation [2].
Cost estimate of an aquifer UGPHES system
One such parameter is the head height which is directly proportional to the power output. The ever-increasing demand for energy storage coupled with the pressure of environmental concerns due to the required urban or suburban space development has led to the use of underground space for the large-scale storage of energy in the form of CAES and UGPHES technologies.
Viability of using abandoned mines and quarries for UGPHES
These technologies, which require the excavation of underground rock to depths of up to 1,500 m [80], are being developed in conjunction with the development of underground excavation technology, which makes the use of underground space an attractive option for energy storage. An additional consideration for underground space is the use of existing infrastructure in the form of abandoned mines and quarries [80].
Challenges and possible solutions for using abandoned mines and quarries for UGPHES
Upper reservoir
Lower reservoir
The Longwall method allows all the coal to be completely removed, allowing the roof of the mine to collapse into the void. The rocks overlying the coal seam are blasted and removed, allowing the coal to be extracted.
Head and energy quantity
While individual sections of deposits can be reused, new deposits will also need to be constructed [115]. The associated costs of achieving storage capacity for each unique case of an abandoned mine or quarry will need to be assessed to understand the feasibility of such an option.
Feasibility of mining engineering
It is clear that the water mass and head are directly proportional to the storage capacity. The full development of drift is a form of effective mitigation as it minimizes the amount of intruding mine water and sediment [115].
Assembly and structure
This water must be pumped to the surface as it reduces the available pumping volume and ultimately reduces the efficiency of the plant with the added risk of sediment infiltration into the system posing a hazard to the plant. Adequate drainage and a combination of cement and chemical grouts will allow the construction of a grout curtain capable of cutting off a large percentage of water entering the mine [80].
Cost of electricity generation for a UGPHES scheme
The maintenance and operating costs can be divided into fixed maintenance costs and variable maintenance costs. 87 is the replacement cost coefficient for the major parts that need to be replaced. B7 is the replacement times for the major parts being replaced.
Cost assessment of UGPHES in an abandoned mine
This is an opportunity for the low-cost construction of a lake or a reservoir, independent of the UGPHES plant project. Significantly higher specific costs can be expected for the machine and generator cavern in the case of the UGPHES plant in an abandoned mine due to unfavorable conditions in the existing cavern.
Abandoned mines in South Africa
Groundwater contamination is also the result of the ingress of polluted surface water into underground groundwater layers. The UGPHES technology will first need to be adopted as a viable option for energy storage in South Africa and will require extensive research into the technology.
Thermal extraction from mine water
Existing installations of UGPHES using abandoned mines or quarries
The upper reservoir will be formed underground between the existing +122 m and +305 m elevations of the mine with an estimated surface area of 50 acres and 732 acre-meter volume. The concrete power station structure next to the mine, approximately 625 meters below the upper reservoir, will be 21 meters wide, 85 meters long and 12 meters high [134].
UGPHES design for the abandoned Ohio limestone mine
The power station was designed to be located 81 meters below the bottom of the mine so that the pumps could be submerged to prevent cavitation [80]. The seepage analysis was carried out to determine the impact of the high-pressure brine on the potential seepage in the power station.
16] Hadjipaschalis, I., Poullikkas, A., and Efthimiou, V., "Overview of Current and Future Energy Storage Technologies for Electric Power Applications," Journal of Renewable. 112] Hobbs, P.J., and Esterhuyse, C.J., "A Preliminary Evaluation of the Groundwater Resources of the Upper Limpopo River Valley, North West Transvaal," Department of Water Affairs and Forestry Report Gh Pretoria, South Africa.