For the perovskite redox cycles, the heat of oxide reduction -ΔHO can vary with non-stoichometry δ [2]. To find the integrated Δhchem, the functional dependence of ΔHO with δ must be detemined. Two methods have been undertaken to explore this functional dependence: 1) combined TGA-DSC calorimetry measurements with incremental changes in δ, and 2) point-defect model fitting to equilibrium δ vs. PO2 data from TGA measurements [3,4]. The DSC measurements showed that the magnitude of ΔHO decreases to a near constant value for δ > 0.1 as illustrated for Ca0.95Sr0.05MnO3-δ in Figure 1. Similar trends were observed for the other perovskite compositions. The alternative method for finding ΔHO as a function of δ by fitting the equilibrium δ vs. PO2 involved modeling the perovskite reduction with two reversible point-defect reactions -- oxide-ion vacancy formation and Mn cation disproportionation from 4+ to 3+ and 5+ states [4]. The model fits originally assumed that these two reactions had enthalpies independent of δ but the contribution of the disproportionation reaction increased with δ thereby causing the combined ΔHO to have a minor dependence on δ as also shown in Figure 1. The point defect modeling did not show the same trends for ΔHO vs. δ but provided very similar values at high δ > 0.1. The integration of ΔHO over a change in δ (i.e. Δδ as in Table 1) provides a basis for calculating the integrated Δhchem as a function of TH. Integrated Δhchem values for CaCr0.05Mn0.95O3-δ, Ca0.95Sr0.05MnO3-δ, and Ca0.9Sr0.1MnO3-δ are shown in Table 1 along with the total energy stored which includes Δhsens derived from integration of CP with respect to T over the redox cycle heating. The higher Δhchem and associated Δhtot for Ca0.95Sr0.05MnO3-δ stems from its increase reducibility without a loss in heat of reaction and makes it a more promising material for TCES applications in these temperature ranges.
For thermal storage application, kinetic rates of TCES capture are important, particularly for concentrated solar applications where solar receiver residence times are limited. To explore kinetics, reduction and oxidation rates of porous perovskite particle beds were measured for fitting thermodynamically consistent kinetic models to the observed rates. Kinetic testing and model fitting for the Ca0.95Sr0.05MnO3-δ indicates that it achieves approximately 80% of its Δhchem thermodynamic limit in 60 s exposure of low PO2 gas for reduction at TH = 900 °C. On the other hand, at the same temperature reoxidation occurs rapidly and releases over 90% of the Δhchem limit in 30 s. The thermodynamic consistent model involving surface kinetics and ionic bulk diffusion in the perovskite particles for Ca0.95Sr0.05MnO3-δ and for CaCr0.05Mn0.95O3-δ provide a basis for designing reactors for redox cycles to be used in TCES for concentrated solar and other potential thermal energy storage applications.
References
[1] E.I. Leonidova, I.A. Leonidov, M.V. Patrakeev, and V.L. Kozhevnikov, J. Solid State Electrochem., 15 (2011) 1071-1075.
[2] J. Mizusaki, M. Yoshihiro, S. Yamauchi, K. Fueki, J. Solid State Chem., 67 (1988) 1–8.
[3] E.I. Goldyreva, E.I., I.A. Leonidov, M.V. Patrakeev, A.V.Chukin, I.I. Leonidov, V.L. Kozhevnikov, J. Alloys Comp., 638 (2015) 44-49.
[4] K.J. Albrecht, G.S. Jackson, R.J. Braun, Appl. Energy, accepted for publication (2015).