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Energies 2020, 13, 420 58 of 96 Material for hydrogen storage needs a high hydrogen capacity both gravimetric and volumetric, low dissociation temperature and pressure, low heat of formation, reversibility, low energy loss, high stability and fast charge/release rate. Among the suitable materials, light metals such as Li, Be, Na, Mg, B, Al and their complex alloys are referred as interesting for their low weight and high storage capacity [730]. Intermetallic compounds (AB2, A2B, AB, AB5) are also interesting because their properties can be tuned varying the concentration of the two elements [731]. The element A commonly is a rare earth or an alkaline earth metals and establishes a stable bond with hydrogen. The element B is normally a transition metal and establishes an unstable hydride [728]. Moreover, complex metal hydrides such as alanates, amides, imides and borohydrides are viable as solid storage materials for their low weight and high storage capacity [732]. The pressure–composition isotherms describe the thermodynamic behavior of the metal hydride formation (see Figure 26). During the charge phase, at low hydrogen content (low H/M ratio) only the metallic phase (α-phase) exists, and hydrogen is dissolved into the solid structure forming an Energies 2020, 13, x FOR PEER REVIEW 56 of 95 interstitial solid solution (physisorption). The equilibrium pressure increases with the hydrogen concentration. At higher hydrogen content (H/M > 0.1) the maximum solubility of the gas in the metal is reached. A strong hydrogen-hydrogen interaction occurs (chemisorption), leading to the is reached. A strong hydrogen-hydrogen interaction occurs (chemisorption), leading to the nucleation nucleation and growth of the hydride phase (β-phase). When the solid and the hydride phase coexist and growth of the hydride phase (β-phase). When the solid and the hydride phase coexist a plateau in a plateau in the isotherm is observed. The length of the range in which the two phases coexist the isotherm is observed. The length of the range in which the two phases coexist determines the amount determines the amount of hydrogen that can be stored at the operating temperature. At high of hydrogen that can be stored at the operating temperature. At high hydrogen concentration (H/M hydrogen concentration (H/M > 1) only the hydride phase exists, and hydrogen can be dissolved in > 1) only the hydride phase exists, and hydrogen can be dissolved in the solid structure increasing the solid structure increasing the pressure. The hydrogen desorption is an endothermal reaction that the pressure. The hydrogen desorption is an endothermal reaction that occurs at higher temperatures. Thus, external heat is required [733,734]. Figure 26. Pressure–composition isotherms. Reprinted with permission from [733]. Figure 26. Pressure–composition isotherms. Reprinted with permission from [733]. occurs at higher temperatures. Thus, external heat is required [733,734]. 5.5.4. Underground Gas Storage 5.5.4. Underground Gas Storage The natural gas network is typically connected with underground storage facilities. Underground The natural gas network is typically connected with underground storage facilities. gas storage allows a large amount of natural gas to be stored, providing a solution for short- and Underground gas storage allows a large amount of natural gas to be stored, providing a solution for long-term storage requirements. Generally, salt caverns, aquifers or depleted oil and gas fields short- and long-term storage requirements. Generally, salt caverns, aquifers or depleted oil and gas are exploited [735]. A cushion gas that remains in the reservoir is needed as base gas to provide fields are exploited [735]. A cushion gas that remains in the reservoir is needed as base gas to provide the operational capability, while the working gas is the gas that is injected and release during operating the operational capability, while the working gas is the gas that is injected and release during cycles [736]. operating cycles [736]. Natural Gas Natural Gas Salt caverns are deep caverns (300–2000 m of depth) with a volume capacity that ranges between Salt caverns are d3eep caverns (300–2000 m of depth) with a volume capacity that ranges between 5000 and 1,000,000 m , connected with the ground through a well that allows gas injection and 5000 and 1,000,000 m3, connected with the ground through a well that allows gas injection and withdrawal [737]. Salt caverns are characterized by low permeability that ensure the sealing of withdrawal [737]. Salt caverns are characterized by low permeability that ensure the sealing of the the storage, good mechanical properties that endure the pressure fluctuation safely, good solubility in storage, good mechanical properties that endure the pressure fluctuation safely, good solubility in water that enables the shape control of the cavern sides and abundant distribution of caverns with large water that enables the shape control of the cavern sides and abundant distribution of caverns with large storage capacity [738]. Drawbacks are the loss of volume and structural stability due to steady- state and transient creep provoked by constant fluid pressure or rapid pressure change, respectively [739]. The underground gas storage in aquifers is a porous gas reservoir in a low permeable rock filled with water (typically saline) and a caprock to prevent leakages [740]. The storage capacity is affected

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