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Impact of enhanced oxide reducibility on rates of solar-driven thermochemical fuel production

Published online by Cambridge University Press:  09 October 2017

Michael J. Ignatowich
Affiliation:
Department of Chemical Engineering, California Institute of Technology, Pasadena, CA 91125, USA
Alexander H. Bork
Affiliation:
ETH Zürich, Zürich 8093, Switzerland
Timothy C. Davenport
Affiliation:
Department of Materials Science, Northwestern University, Evanston, IL 60208, USA
Jennifer L. M. Rupp
Affiliation:
Department of Materials Science and Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
Chih-kai Yang
Affiliation:
Materials Science, California Institute of Technology, Pasadena, CA 91125, USA
Yoshihiro Yamazaki
Affiliation:
INAMORI Frontier Research Center, Kyushu University, Fukuoka 819-0395, Japan
Sossina M. Haile*
Affiliation:
Department of Materials Science, Northwestern University, Evanston, IL 60208, USA Materials Science, California Institute of Technology, Pasadena, CA 91125, USA
*
Address all correspondence to S. M. Haile at sossina.haile@northwestern.edu

Abstract

Two-step, solar-driven thermochemical fuel production offers the potential of efficient conversion of solar energy into dispatchable chemical fuel. Success relies on the availability of materials that readily undergo redox reactions in response to changes in environmental conditions. Those with a low enthalpy of reduction can typically be reduced at moderate temperatures, important for practical operation. However, easy reducibility has often been accompanied by surprisingly poor fuel production kinetics. Using the La1−x Srx MnO3 series of perovskites as an example, we show that poor fuel production rates are a direct consequence of the diminished enthalpy. Thus, material development efforts will need to balance the countering thermodynamic influences of reduction enthalpy on fuel production capacity and fuel production rate.

Information

Type
Research Letters
Copyright
Copyright © Materials Research Society 2017 
Figure 0

Figure 1. A thermochemical cycle that converts H2O to H2 by cyclic reduction and oxidation of a lanthanum strontium manganite oxide at respective temperatures TTR (thermal reduction temperature) and TFP (fuel production temperature) using solar-derived thermal energy as the input.

Figure 1

Figure 2. CALPHAD derived (a) enthalpy and (b) entropy of reduction of La1−xSrxMnO3−δ (LSM) compounds with strontium content from x = 0.1 (LSM91) to x = 0.4 (LSM64) each as a function of oxygen nonstoichiometry.

Figure 2

Figure 3. Oxygen content in LSM compounds as a function of oxygen partial pressure at (a) 1400 °C and (b) 800 °C. Reduction under 10−5 atm O2 is indicated by the vertical line in (a). Upon quenching from the reduction condition to 800 °C, the materials retain the δ attained at high temperature, implying an internal chemical potential corresponding to the intersection of the horizontal δi lines in (b) with the 800 °C curves. The vertical line in (b) is the equilibrium oxygen partial pressure resulting from thermolysis of 20% H2O in Ar, used experimentally for the fuel production half-cycle. The thermodynamic driving force for the initiation of the oxidation reaction is determined by the distance between the vertical line in (b) and the nonstoichiometry curve at δi.

Figure 3

Figure 4. Hydrogen production calculated by the thermo-kinetic (quasi-equilibrium) model compared to experimental data for two temperature cycling of LSM compounds: (a) LSM91, (b) LSM82, (c) LSM73, and (d) LSM64. Reduction performed nominally at 1400 °C under 10 ppm O2, and oxidation nominally at 800 °C under 20% steam at 200 mL/min. The inset in (a) additionally shows the computed behavior of ceria in the thermokinetic limit. Experimental data have been reported previously and reflect the hydrogen detected by mass spectrometry in the evolved gas stream.[9]

Figure 4

Table I. Process parameters for the computation of thermo-kinetic hydrogen production profiles.