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Recharging lithium battery research with first-principles methods

Published online by Cambridge University Press:  22 March 2011

G. Ceder
Affiliation:
Massachusetts Institute of Technology; gceder@mit.edu
G. Hautier
Affiliation:
Massachusetts Institute of Technology; hautierg@mit.edu
A. Jain
Affiliation:
Massachusetts Institute of Technology; anubhavj@mit.edu
S.P. Ong
Affiliation:
Massachusetts Institute of Technology; shyue@mit.edu

Abstract

Energy storage is a critical hurdle to the success of many clean energy technologies. Batteries with high energy density, good safety, and low cost can enable more efficient vehicles with electrified drive trains, such as hybrid electric vehicles, electric vehicles, and plug-in hybrid electric vehicles. They can also provide energy storage for intermittent energy sources, such as wind and solar. Today, and for the foreseeable future, rechargeable lithium batteries deliver the highest energy per unit weight or volume at reasonable cost. Many of the important properties of battery materials can be calculated with first-principles methods, making lithium batteries fertile ground for computational materials design. In this article, we review the successes and opportunities in using first-principles computations in the battery field. We also highlight some technical challenges facing the accurate modeling of battery materials.

Information

Type
Research Article
Copyright
Copyright © Materials Research Society 2011
Figure 0

Figure 1. Diagram of a Li-ion battery. Li-ion batteries operate by shuttling Li+ ions between the cathode and anode through an electronically insulating, ion-conducting electrolyte. During discharge, lithium ions migrate from the anode, where they are at a higher chemical potential, through the electrolyte, and into the cathode, where they are at a lower chemical potential. At the same time, an electron travels through the external circuit to perform external work. The free energy change of the lithium migration process is the maximum reversible work that can be obtained. During charge, the application of an external potential forces lithium ions to migrate out of the cathode, through the electrolyte, and back into the anode.

Figure 1

Figure 2. Comparison between experimental and computed (using generalized gradient approximation [GGA]+U or Heyd-Scuseria-Ernzerhof [HSE]) voltages. As titanium does not require a U value to reproduce accurate energies, no U value was used for Li2Ti2O4 and LiTiS2. Data from Chevrier et al.6

Figure 2

Figure 3. (a) Calculated phase diagram and (b) experimental electrochemical performance of an off-stoichiometric LiFePO4. Off-stoichiometric experiments are typically performed with Li-excess or Li-deficiencies (directions B and C), but these directions do not improve electrochemical performance in LiFePO4. The calculated phase diagram shows that off-stoichiometry in an unconventional direction (mixed Li/P excess, direction A) leads to equilibrium with the highly conductive glass Li4P2O7. Li4P2O7 forms a surface coating that facilitates Li+ transfer into the cathode, thus allowing for very high rates (up to 44 C, or full discharge in less than 1.5 minutes) to be achieved in laboratory experiments (b). Adapted from Reference 37.

Figure 3

Figure 4. Comparison between the LixFePO4 experimental phase diagram from Delacourt et al.52 and Dodd et al.53 and computed phase diagrams obtained with electronic entropic contribution (middle) and without (bottom).50 The triphylite LiFePO4 is referred to by T; the fully delithiated FePO4 phase, heterosite, by H; and the solid solution region is indicated by SS. Only the introduction of the electronic entropy contribution reproduces the experimentally observed solid solution region. © 2006, American Physical Society.

Figure 4

Figure 5. Calculated thermal stabilities of delithiated MnPO4 and FePO4 (represented by MPO4 on the y-axis). The figure shows the number of moles of O2 evolved per mole of cathode material as a function of temperature. It can be seen that the onset of O2 evolution is at a much higher temperature (~700°C) for FePO4 compared to MnPO4 (~370°C), and the initial amount of O2 evolved is also much less. This difference in thermal behaviors can be explained by the fact that Fe3+ and Mn2+ both have the exchange-stabilized 3d5 electron configuration, which suggest that the decomposition of FePO4 (requiring the reduction of Fe3+ to Fe2+) would be relatively more difficult than the decomposition of MnPO4 (requiring the reduction of Mn3+ to Mn2+). Adapted from Reference 65.