Open access peer-reviewed chapter

Thermodynamics of ABO3-Type Perovskite Surfaces

By Eugene Heifets, Eugene A. Kotomin, Yuri A. Mastrikov, Sergej Piskunov and Joachim Maier

Submitted: November 6th 2010Reviewed: May 23rd 2011Published: November 2nd 2011

DOI: 10.5772/20114

Downloaded: 3841

1. Introduction

The ABO3-type perovskite manganites, cobaltates, and ferrates (A= La, Sr, Ca; B=Mn, Co, Fe) are important functional materials which have numerous high-tech applications due to their outstanding magnetic and electrical properties, such as colossal magnetoresistance, half-metallic behavior, and composition-dependent metal-insulator transition (Coey et al., 1999; Haghiri-Gosnet & Renard, 2003). Owing to high electronic and ionic conductivities. these materials show also excellent electrochemical performance, thermal and chemical stability, as well as compatibility with widely used electrolyte based on yttrium-stabilized zirconia (YSZ). Therefore they are among the most promising materials as cathodes in solid oxide fuel Cells (SOFCs) (Fleig et al., 2003) and gas-permeation membranes (Zhou, 2009). Many of the above-mentioned applications require understanding and control of surface properties. An important example is LaMnO3 (LMO). Pure LMO has a cubic structure above 750 K, whereas below this temperature the crystalline structure is orthorhombic, with four formula units in a primitive cell. Doping of LMO with Sr allows one to increase both the ionic and electronic conductivity as well as to stabilize the cubic structure down to room temperatures - necessary conditions for improving catalytic performance of LMO in electrochemical devices, e.g. cathodes for SOFCs. In optimal compositions of La1-xbSrxbMnO3(LSM) solid solution the bulk concentration of Sr reaches xb0.2.

Understanding of LMO and LSM basic properties (first of all, energetic stability and reactivity) for pure and adsorbate-covered surfaces is important for both the low-temperature applications (e.g., spintronics) and for high-temperature electrochemical processes where understanding the mechanism of oxygen reduction on the surfaces is a key issue in improving the performance of SOFC cathodes and gas-permeation membranes at relatively high (~800°C) temperatures. First of all, it is necessary to determine which LMO/LSM surfaces are the most stable under operational conditions and which terminations are the energetically preferential? For example, the results of our simulations described below show that the [001] surfaces are the most stable ones in the case of LMO (as compared to [011] and others). However, the [001] surfaces have, in turn, two different terminations: LaO or MnO2. We will compare stabilities of these terminations under different environmental conditions (temperature and partial pressure of oxygen gas). Another important question to be addressed is, how Sr doping affects relative stabilities of the LMO surfaces? These issues directly influence the SOFC cathode performance. Answering these questions requires a thermodynamic analysis of surfaces under realistic SOFC operational conditions which is in the main focus of this Chapter. Such a thermodynamic analysis is becoming quite common in investigating structure and stability of various crystal surfaces (Examples of thermodynamic analyses of binary and ternary compounds can be found in Reuter & Scheffler, 2001a, 2001b; Bottin et al., 2003; Heifets et al., 2007a, 2007b, Johnson et al., 2004).

The thermodynamic analysis requires careful calculations of energies for two-dimensional slabs terminated by surfaces with various orientations and terminations. The required energies could be calculated using ab initio methods of the atomic and electronic structure based on density functional theory (DFT). In this Chapter, we present the results obtained using two complementary ab initio DFT approaches employing two different types of basis sets (BS) representing the electronic density distribution: plane waves (PW) and linear combination of atomic orbitals (LCAO). Both techniques were used to calculate the atomic and electronic structures of a pure LMO whereas investigation of the Sr influence on the stability of different (001) surfaces was performed within LCAO approach.

After studying the stabilities of various surfaces, the next step is investigating the relevant electrochemical processes on the most stable surfaces. For this purpose, we have to evaluate the adsorption energies for O2 molecules, O atoms, the formation energies of O vacancies in the bulk and at the stable perovskite surfaces. These energies, together with calculated diffusion barriers of these species and reactions between them, allow us to determine the mechanism of incorporation of O atoms into the cathode materials. However, such mechanistic and kinetic analyses lie beyond the scope of this Chapter (for more details see e.g. Mastrikov et al., 2010). Therefore, we limit ourselves here only to the thermodynamic characterization of the initial stages of the oxygen incorporation reaction, which include formation of stable adsorbed species (adsorbed O atoms, O2 molecules) and formation of oxygen vacancies. The data for formation of both oxygen vacancies and adsorbed oxygen atoms and molecules have been collected using plane wave based DFT.

2. Computational details

The employed thermodynamic analysis relies on the energies obtained by DFT computations of the electronic structure of slabs terminated by given surfaces using the above-mentioned two types of basis sets. All calculations are performed with spin-polarized electronic densities, complete neglect of spin polarization results in considerable errors in material properties (Kotomin et al, 2008)).

The plane wave calculations were performed with VASP 4.6.19 code (Kresse & Hafner, 1993; Kresse & Furthmüller, 1996; Kresse et al., 2011), which implements projector augmented wave (PAW) technique (Bloechl, 1994; Kresse & Joubert, 1999), and generalized gradient approximation (GGA) exchange-correlation functional proposed by Perdew and Wang (PW91) (Perdew et al., 1992). Calculations were done with the cut-off energy of 400 eV. The core orbitals on all atoms were described by PAW pseudopotentials, while electronic wavefunctions of valence electrons on O atoms and valence and core-valence electrons on metal atoms were explicitly evaluated in our calculations.

We found that seven- and eight-plane slabs infinite in two (x-y) directions are thick enough to show convergence of the main properties. The periodically repeated slabs were separated along the z-axis by a large vacuum gap of 15.8 Å. All atomic coordinates in slabs were allowed to relax. To avoid problems with a slab dipole moment and to ensure having identical surfaces on both sides of slabs, we employed the symmetrical seven-layer slab MnO2(LaO-MnO2)3 in our plane-wave simulations, even though it has a Mn excess relative to La and a higher oxygen content. Such a choice of the slab structure however only slightly changes the calculated energies. For example, the energy for dissociative oxygen adsorption on the [001] MnO2-terminated surface

O2+2MnMnx2Oad-+2MnMnE1

is -2.7 eV for eight-layers (LaO-MnO2)4 slab and -2.2 eV for the symmetrical seven-layer MnO2-(LaO-MnO2)3 slab. The use of symmetrical slabs also allows decoupling the effects of different surface terminations and saving computational time due to the possibility to exploit higher symmetry of the slabs. The simulations were done using an extended 2√2 × 2√2 surface unit cell and a 2 × 2 Monkhorst-Pack k-point mesh in the Brillouin zone (Monkhorst & Pack, 1976). Such a unit cell corresponds to 12.5% concentration (coverage) of the surface defects in calculations of vacancies and adsorbed atoms and molecules.

The choice of the magnetic configuration only weakly affects the calculated surface relaxation and surface energies (Evarestov, et. al., 2005; Kotomin et al, 2008; Mastrikov et al., 2009). Relevant magnetic effects are sufficiently small (≈0.1eV) as do not affect noticeably relative stabilities of different surfaces; these values are much smaller than considered adsorption energies and vacancy formation energies. As for slabs the ferromagnetic (FM) configuration has the lowest energy, we performed all further plane-wave calculations with FM ordering of atomic spins.

The quality of plane-wave calculations can be illustrated by the results for the bulk properties (Evarestov, et. al., 2005; Mastrikov et al., 2009). In particular, for the low-temperature orthorhombic structure the A-type antiferromagnetic (A-AFM) configuration (in which spins point in the same direction within each [001] plane, but opposite in the neighbor planes) is the energetically most favorable one, in agreement with experiment. The lattice constant of both the cubic and orthorhombic phase exceeds the experimental value only by 0.5%. The calculated cohesive energy of 30.7 eV is also close to the experimental value (31 eV).

In our ab initio LCAO calculations we use DFT-HF (i.e., density functional theory and Hartree-Fock) hybrid exchange-correlation functional which gave very good results for the electronic structure in our previous studies of both LMO and LSM (Evarestov et al., 2005; Piskunov et al., 2007). We employ here the hybrid B3LYP exchange-correlation functional (Becke, 1993). The simulations were carried out with the CRYSTAL06 computer code (Dovesi, et. al., 2007), employing BS of the atom-centered Gaussian-type functions. For Mn and O, all electrons are explicitly included into calculations. The inner core electrons of Sr and La are described by small-core Hay-Wadt effective pseudopotentials (Hay & Wadt, 1984) and by the nonrelativistic pseudopotential (Dolg et al., 1989), respectively. BSs for Sr and O in the form of 311d1G and 8–411d1G, respectively, were optimized by Piskunov et al., 2004. BS for Mn was taken from (Towler et al., 1994) in the form of 86–411d41G, BS for La is provided in the CRYSTAL code’s homepage (Dovesi, et. al., 2007) in form 311-31d3f1, to which we added an f-type polarization Gaussian function with exponent optimized in LMO (α=0.475). The reciprocal space integration was performed by sampling the Brillouin zone with the 4×4 Monkhorst-Pack mesh (Monkhorst & Pack, 1976). In our LCAO calculations, nine-layer symmetrical slabs (terminated on both sides by either [001] MnO2 or La(Sr)O surfaces) were used. The calculations were carried out for cubic phases and for A-AFM magnetic ordering of spins on Mn atoms. All atoms have been allowed to relax to the minimum of the total energy. This approach was initially tested on bulk properties as well, the experimentally measured atomic, electronic, and low-temperature magnetic structure of pure LMO and LSM (xb=1/8) were very well reproduced (Piskunov et al., 2007).

3. Thermodynamic analysis of surface stability

As was mentioned above, understanding of many surface related phenomena requires preliminary investigation of the relative stabilities of various crystalline surfaces. Usually (especially for high-temperature processes such as catalysis in electrochemical devices), determining the structure with the lowest internal energy is not sufficient. The internal energy characterizes only systems with a constant chemical composition, while atomic diffusion and atomic exchange between environment and surfaces occur at high temperatures. Thus, we have to take into account the exchange of atoms between the bulk crystal, its surface, and the gas phase, into our analysis of surface stability. Such processes are included into the Gibbs free energies at the thermodynamic level of description. Therefore, we have to calculate the surface Gibbs free energy (SGFE) Ωi for the LMO and LSM surfaces of various orientations and terminations. The SGFE is a measure of the excess energy of a semi-infinite crystal in contact with matter reservoirs with respect to the bulk crystal (Bottin et al., 2003; Heifets et al., 2007a, 2007b; Johnston et al., 2004 ; Mastrikov et al., 2009; Padilla & Vanderbilt, 1997, 1998; Pikunov et al., 2008; Pojani et al., 1999; Reuter & Scheffler, 2001b, 2004). The SGFEs are functions of chemical potentials of different atomic species. The most stable surface has a structure, orientation and composition with the lowest SGFE among all possible surfaces.

3.1. Method of analysis for LMO surfaces

Introducing the chemical potentials La, Mn, and O for the La, Mn, and O atomic species, respectively, the SGFE per unit cell area i corresponding to the i termination is defined as

Ωi=12[Gslabi-NLaiμLa-NMniμMn-NOiμO],E2

whereis the Gibbs free energy for the slab terminated by surface i, NiLa, NiMn, and NiO denote numbers of La, Mn, and O atoms in the slab. Here we assume that the slab is symmetrical and has the same orientation, composition, and structure on both sides. The SGFE per unit area is represented by

ωi=ΩiAE3

The thermodynamic part of the description below follows the well known chemical thermodynamics formalism developed originally by Gibbs in 1875 (see Gibbs, 1948) for perfect bulk and surfaces and extended by Wagner & Schottky, 1930 (also Wagner, 1936) for point defects.

The chemical potential LaMnO3 of LMO (in the considered orthorhombic or cubic phase) is equal to the sum of the chemical potentials of each atomic component in the LMO crystal:

μLaMnO3=μLa+μMn+3μOE4

Owing to the requirement for the surface of each slab to be in equilibrium with the bulk LMO, the chemical potential is equal to the specific bulk crystal Gibbs free energy accordingly to

μLaMnO3=gLaMnO3bulkE5

Eq. (4) imposes restrictions on μLa, μMn, and μO, leaving only two of them as independent variables. We use in following μO as one of the independent variables because we consider oxygen exchange between the LaMnO3 crystal and gas phase and have to account for strong dependence of this chemical potential on T and pO2. As another independent variable, we use μMn. We will simplify the equation for the SGFE and eliminate the chemical potentials La and LaMnO3 by substituting this expression for the LMO bulk chemical potential:

Ωi=12[GslabiNAigLaMnO3bulk]ΓA,MniμMnΓA,OiμO,E6

where ΓiA,a are the Gibbs excesses in the i-terminated surface of components a with respect to the number of ions in A type sites (for ABO3 perovskites) of the slabs (Gibbs,1948; Johnston et al., 2004) :

ΓA,ai=12(NaiNAiNabulkNAbulk)E7

Here A type of sites are occupied solely by La atoms in LMO, so NA=NLa for LMO. This will become somewhat more complicated in solid solutions such as LSM (see the next subsection). NAbulkis the number of A-sites in unit cell in the bulk. Nabulkis the number of a atoms in unit cell in the bulk.

The Gibbs free energies per unit cell for crystals and slabs are defined as

gj=Ej+EjvibrTsj+pvjE8

where Ej is the static component of the crystal energy, Ejvibr is the vibrational contribution to the crystal energy, vj volume, and sj entropy. All these values are given per formula unit in j-type (=La,Mn, LMO…) crystals. We can reasonably assume that the applied pressure is not higher than ~100 atm. in practical cases. The volume per lattice molecule in LaMnO3 is ~64 Å3. Then the largest pvj term in Eq.(13) can be estimated as ~ 5 meV. This value is much smaller than the amount of uncertainty in our DFT computations and, therefore, can be safely neglected. As it is commonly practiced, we will neglect the very small vibration contributions to gj, including contributions from zero-point oscillations to the vibrational part of the total energy. This rough estimate is usually valid, but can be broken if the studied material has soft modes. The same consideration is valid for slabs used in the present simulations. While it might be important to check vibrational contributions in some cases, here we will neglect it. Besides, facilities in computer codes for calculations of vibrational spectra of crystals and slabs appeared only within a few last years and such calculations are still very demanding and practically possible only for relatively small unit cells. Therefore, we approximate the Gibbs free energies with the total energies obtained from DFT calculations:

gjEjE9

Then, replacing the chemical potentials of La and Mn atoms by their deviations from chemical potentials in the most stable phases of respective elementary crystals,

ΔμLa=μLagLabulkμLaELabulkE10

and

ΔμMn=μMngMnbulkμMnEMnbulkE11

and chemical potential of O atoms by its deviation from the energy of an oxygen atom in a free, isolated O2 molecule (EO2total/2),

ΔμO=μOEO2total2E12

we can determine the surface Gibbs free energy from

Ωi=ϕiΓA,MniΔμMnΓA,OiΔμO.E13

We can express the constant ϕi in Eq. (13) as

ϕi=12[GslabiNAigLaMnO3bulk]ΓA,MnigMnbulk12ΓA,OiEO212[EslabiNAiELaMnO3bulk]ΓA,MniEMnbulk12ΓA,OiEO2,E14

what resembles the expression for the Gibbs free energy of surface formation. Here Eslab stands for the total energy of a slab and replaces the Gibbs free energy of the slab.

The equilibrium condition (5) can be rewritten as

ΔμLa+ΔμMn+3ΔμO=Δgfbulk(LaMnO3)E15

where

Δgfbulk(LaMnO3)=gLaMnO3bulkgLabulkgMnbulk32EO2ELaMnO3bulkELabulkEMnbulk32EO2.E16

Here Δgfbulk(LaMnO3)has meaning of the Gibbs free energy of LaMnO3 formation from La, Mn and O2 in their standard states.

The range of values of the chemical potentials which consistent with existence and stability of the crystal (LMO here) itself is determined by the set of the following conditions. To prevent La and Mn metals from leaving LMO and forming precipitates, their chemical potentials must be lower in LMO than in corresponding bulk metals. These conditions mean:

μMn<gMnbulkE17
and
μLa<gLabulkE18

Similarly, precipitation of oxides does not occur, if the chemical potentials of atoms in LMO are smaller than in the oxides:

2μLa+3μO<gLa2O3bulkE19
μMn+μO<gMnObulkE20
3μMn+4μO<gMn3O4bulkE21
2μMn+3μO<gMn2O3bulkE22
and
μMn+2μO<gMnO2bulkE23

Exclusion of La chemical potential and expressing of these conditions through the deviations of the chemical potentials (10-12) transform the conditions to

ΔμMn<0E24
ΔμMn+3ΔμO>Δgfbulk(LaMnO3)E25
xΔμMn+yΔμO<Δgfbulk(MnxOy)E26
and
2ΔμMn+3ΔμO>2Δgfbulk(LaMnO3)Δgfbulk(La2O3)E27

where the formation energies of oxides are defined by

Δgfbulk(MxOy)=gMxOybulkxgMbulky2EO2EMxOybulkxEMbulky2EO2.E28

Note, however, that sometimes compositions are fixed by bringing the multinary crystals into coexistence with less complex sub-phases.

If the SGFE becomes negative, surface formation becomes energetically favorable and the crystal will be destroyed. Therefore, the condition for sustaining a crystal structure is for SGFE to be positive for all potential surface terminations. Therefore, one more set of conditions on the chemical potentials of the crystal components can be written as

Ωi>0E29

where i corresponds to the surface with the lowest SGFE.

3.2. Method of analysis for LSM surfaces

In LSM we have to re-define the SGFEs, because there are now four components in this material (instead of three in LMO) with Sr atoms substituting a fraction of La atoms in the perovskite A sub-lattice. The SGFE definition for LSM can be written as

Ωi=12[GslabiNLaiμLaNSriμSrNMniμMnNOiμO]E30

Let us denote concentration of Sr atoms in the bulk of LSM as

xb=NSrbulkNAbulkE31

where NSrbulkis the average number of Sr atoms per crystal unit cell in the bulk. Then for LSM

NLabulk=(1xb)NAbulkE32

becomes the average number of La atoms per LSM unit cell in the bulk.

The chemical potential of a LSM formula unit is

μLSM=(1xb)μLa+xbμSr+μMn+3μOE33

Equilibrium between LSM surface and its bulk means that

μLSM=gLSMbulkE34

We will continue using approximation (9) in the following, replacing the Gibbs free energies of bulk and slab unit cells by their total energies. The conditions (32, 33) impose restrictions on four chemical potentials of all LSM components and reduces the number of independent components to three. We have chosen to keep the chemical potentials of O, Mn and La as independent variables. Then the chemical potential of the Sr atom can be expressed as

μSr=1xb(ELSM(1xb)μLaμMn3μO)E35

and its deviation (analogous to eqs. (10-12) and keeping in mind approximation (9)) as

ΔμSr=μSrgSrbulkμSrESrbulkE36

The expressions for the excesses ΓA,Oiand ΓA,Mnido not change with respect to LMO. We still have to remember only that NA does not coincide any more with NLa in LSM. NA refers only to the number of A-sites in the perovskite unit cell, but not to the number of La atoms. Since we excluded chemical potential for Sr, only the excesses for La atoms will be required.

For the calculation of excesses of La atoms we have to account for mixing of La and Sr atoms in A-site of the perovskite lattice. Using eqs.(7,31), the excess of La atoms for surface i can be expressed as:

ΓA,Lai=12(NLaiNLabulkNAbulkNAi)=12(NLai(1xb)NAi)E37

Then SGFEs for LSM reads

Ωi=ϕiΓA,LaiΔμLaΓA,MniΔμMnΓA,OiΔμOE38

where

ϕi=12(GslabiNAiELSMbulk)ΓA,LaiELabulkΓA,MniEMnbulkΓA,OiEO22E39

The conditions of LSM crystal stability include the same bounds which work for LMO. However, we have to add conditions preventing precipitations of several new materials and express all conditions through three chemical potentials for La, Mn and O atoms. Precipitation of Mn, La, and Sr metals will be avoided if

ΔμMn<0E40
ΔμLa<0E41

and

(1xb)ΔμLa+ΔμMn+3ΔμO>Δgfbulk(LSM)E42

where Gibbs free energy of LSM formation is

Δgfbulk(LSM)=ELSMbulkxbESrbulk(1xb)ELabulkEMnbulk32EO2E43

Precipitation of oxides is avoided, if

xΔμMn+yΔμO<Δgfbulk(MnxOy)E44
2ΔμLa+3ΔμO<Δgfbulk(La2O3)E45
(1xb)ΔμLa+ΔμMn+(3xb)ΔμO>Δgfbulk(LSM)xbΔgfbulk(SrO)E46

where

Δgfbulk(SrO)=ESrObulkESrbulkEO22E47

Similarly, precipitation of LaMnO3 and SrMnO3 perovskites will be prevented, if

11xbΔgfbulk(LSM)xb1xbΔgfbulk(SrMnO3)<<ΔμMn+ΔμLa+3ΔμO<Δgfbulk(LaMnO3).E48

Here the Gibbs free energy of SrMnO3 formation is defined as

Δgfbulk(SrMnO3)=ESrMnO3bulkESrbulkEMnbulk32EO2.E49

Lastly, spontaneous formation of surfaces does not occur, if condition (29) is satisfied as well.

3.3. Determination of the chemical potential of oxygen atom

As mentioned above, an exchange of O atoms between surfaces and environment occurs at all surfaces, especially at high temperatures. Moreover, such an exchange is a key factor in many electrochemical and catalytic processes. Therefore, oxygen in the studied crystal (for instance, LMO or LSM, in this Chapter) has to be considered in equilibrium with oxygen gas in atmosphere beyond the crystal surface. The equilibrium in exchange with O atoms means equality of oxygen chemical potentials in a crystal and in the atmosphere:

μO=12μO2gasE50

Chemical potentials are hardly available experimentally. It is much more convenient to operate with gas temperatures and pressures determining the oxygen chemical potential. At the same time, the Gibbs free energies of crystals are insensitive to temperature and the pressure (within approximations accepted in our present description). Therefore, we can use the dependence of oxygen gas chemical potential μO2gasto express the Gibbs free energies for surfaces through temperature and oxygen gas partial pressure.

Oxygen gas under the considered conditions can be treated (to a very good approximation) as an ideal gas. Therefore, dependence of its chemical potential from pressure can be expressed by the standard expression (as done by Johnston et al., 2004 and Reuter & Scheffler, 2001b)

μO2gas(T,p)=μO2gas(T,p0)+kTln(pp0)E51

where k is the Boltzmann constant. Here p0 is the reference pressure which we can take as the standard pressure (1 atm.). The temperature dependence of μO2gas(T,p0)includes contributions from molecular vibrations and rotations, as well as ideal-gas entropy at pressure p0. We can evaluate the temperature dependence of μO2gas(T,p0)using experimental data from the standard thermodynamic tables (Chase, 1998; Linstrom & Mallard, 2003), following Johnston et al., 2004 and Reuter & Scheffler, 2001b. These data are collected in Table 1. For this we define an isolated oxygen molecule EO2 as the reference state. Changes in the chemical potential for oxygen atom can be written as

ΔμO(T,p)=μO(T,p)12EO2==12{ΔGO2gas(T,p0)+kTln(pp0)}+δμO0E52

Here ΔGO2gas(T,p0)is the change in the oxygen gas Gibbs free energy at the pressure p0 and temperature T with respect to its Gibbs free energy at T0=298.15 K

ΔGO2gas(T,p0)=GO2gas(T,p0)GO2gas(T0,p0)==HO2gas(T,p0)HO2gas(T0,p0)TSO2gas(T,p0)+T0SO2gas(T0,p0)E53
T, KΔGO2gas (T,p0), eVT, KΔGO2gas (T,p0), eV
100-0.071000-1.10
200-0.171100-1.23
250-0.221200-1.36
298.15-0.271300-1.49
300-0.271400-1.62
400-0.381500-1.75
500-0.501600-1.88
600-0.611700-2.02
700-0.731800-2.16
800-0.851900-2.29
900-0.972000-2.43

Table 1.

Variations in the Gibbs free energy for oxygen gas at standard pressure (p0=1 atm.) with respect to its value at 0 K. Data are taken from thermodynamic tables (Chase, 1998; Linstrom & Mallard 2003).

TheδμO0in Eq. (50) is a correction which matches experimental data and the results of quantum-mechanical computations. This correction can be estimated from computations of metal oxides and metals, in a way similar to Johnston et al., 2004. Enthalpy of an MxOy oxide can be written as

hMxOy0=xhM0+y2hO20+ΔHf,MxOy0E54

Here enthalpies of the oxide, hMxOy0, and of the metal, hM0, can be approximated by the total energies for these materials calculated at 0 K on the same grounds as for approximation (9). The formation heat for La and Mn oxides under standard conditions can also be found in thermodynamic tables (Chase, 1998; Linstrom & Mallard, 2003). Equation (52) allows us to estimate the standard oxygen gas enthalpy. Since we define the total energy of an oxygen molecule as a zero for chemical potential and enthalpy calculations, the correction for the enthalpy could to be defined as

δhO20=hO20EO2E55

Using the experimental standard entropy for oxygen (Chase, 1998; Linstrom & Mallard, 2003) asSO20=205.147 J∙mol-1K-1, the correction to the oxygen chemical potential can be calculated as

δμO0=12(δhO20T0SO2gas(T0,p0))=1y(hMxOy0xhM0ΔHf,MxOy0)12(EO2+T0SO2gas(T0,p0))E56

3.4 Thermodynamic consideration of oxygen adsorption and vacancy formation

Let us consider formation of relevant oxygen species and point defects in the bulk and at the LaMnO3 surface. We use the same approximation as in the previous sections: we neglect the changes of vibrational entropy in the solid, thus only states comprising gaseous O2 exhibit the temperature-dependent Gibbs free energy contribution. In this approximation, differences between the Gibbs energies for bulk crystals or slabs (including defects and adsorbates) can be replaced with the differences in the total energy calculated from DFT, while variation of oxygen chemical potential for gaseous O2 is taken from experimental data. The Gibbs free energy of reaction for removal of a neutral O atom (1/2 O2) from the bulk (i.e. formation of one neutral VOand allocation of the left-behind two electrons mainly on two nearest Mn) is defined as

Δgfbulk(LaMnO3:VO)=Ebulk(LaMnO3:VO)+μO(T,pO2)ELaMnO3bulkE57

where Ebulk(LaMnO3:VO)is the total energy per bulk supercell with an oxygen vacancy. This definition can be re-written as

Δgfbulk(LaMnO3:VO)=ΔEfbulk(LaMnO3:VO)+ΔμO(T,pO2)E58

where

ΔEfbulk(LaMnO3:VO)=Ebulk(LaMnO3:VO)+12EO2ELaMnO3bulkE59

is the formation energy of a neutral oxygen vacancy with respect to the calculated energy 12EO2for oxygen atom in the molecule. The variation of oxygen chemical potential ΔμO(T,pO2)due to T, pO2 is described by Eq. (50). Similarly, the vacancy formation energy for the surface vacancy can be presented as

Δgfsurf(LaMnO3:VO)=ΔEfsurf(LaMnO3:VO)+ΔμO(T,pO2)E60

where

ΔEfsurf(LaMnO3:VO)=12(Eslab(LaMnO3:2VO)+EO2ELaMnO3slab)E61

Here we accounted for the fact that we use a symmetrical slab with an oxygen vacancy at each side of the slab. The total energy of such a slab is written asEslab(LaMnO3:2VO), because the slab has two vacancies.ELaMnO3slabis the total energy of the slab without defects. The Gibbs free energies of adsorption can be written in a similar way:

Δgadssurf(LaMnO3:Oads)=ΔEadssurf(LaMnO3:Oads)ΔμOE62
ΔEadssurf(LaMnO3:Oads)=12(Eslab(LaMnO3:2Oads)EO2ELaMnO3slab)E63
and
Δgadssurf(LaMnO3:O2,ads)=ΔEadssurf(LaMnO3:O2,ads)ΔμO2E64
ΔEadssurf(LaMnO3:O2,ads)=12(Eslab(LaMnO3:2O2,ads)2EO2ELaMnO3slab)E65

Here µO2=2µO, and we have to take account for two adsorbed O or O2 on the symmetrical slab. It is important to remember that the adsorption energy (60) for atomic O species is given relative to half an O2 molecule, but not with respect to gaseous O atoms.

In the present Chapter we will describe the vacancy formation energies and the adsorption energies of O atoms and O2 molecules obtained with plane wave BS and PW91 functional.

4. Results and discussions

4.1. Stability of LMO surface terminations: Plane-wave DFT simulations

Based on the results of plane-wave calculations and theoretical considerations described in Section 3, the phase diagrams characterizing stability of different LMO surfaces have been drawn in Figure 1. These diagrams were built for both low-temperature orthorhombic and high-temperature cubic phases. For O-terminated [011] and LaO+O [001] surfaces it was not possible to keep the cubic structure during lattice relaxation. Therefore, we used i values for the orthorhombic phase for both phase diagrams in Figure 1, as it was done, for instance, by Bottin et al., 2003. The calculated input data used for drawing this figure are collected in Tables 2 and 3. Optimized geometries for the slabs can be found in Mastrikov et al., 2009.

The surface stability regions in the diagrams are limited by the lines 2, 6 and 4. These lines correspond to boundaries where coexistence occurs of LMO with La2O3, MnO2 and Mn3O4, respectively. Because of the DFT deficiencies in describing the relative energies for materials

surface
ΓiLa,OΓiLa,MnØiL a
(eV/unit cell)
ØiL a
(J/m2)
orientationtermination
[001]LaO-1-0.55.38 (5.42)5.67 (5.70)
[001]LaO+O-0.875-0.54.905.16
[001]MnO210.5-3.02 (-2.93)-3.18 (-3.08)
[001]MnO2+O1.1250.5-3.16 (-3.53)-3.33 (-3.72)
[110]LaMnO-106.13 (6.05)4.56 (4.51)
[110]O210-1.16 (-1.26)-0.86 (-0.94)
[110]O001.090.81

Table 2.

Parameters defining the surface Gibbs free energies Ωi (Eq. 13) as function of O and Mn chemical potentials : excesses ΓiLa,O and ΓiLa,Mn of O and Mn atoms in the surfaces with respect to La atoms (7), and free energy of formation ØiL a (14) at ΔμO = ΔμMn = 0 eV for the LaMnO3 surfaces under consideration. These results produced with plane wave BS and PW91 functional. Values of ØiL a without brackets are for the orthorhombic phase, values in brackets are for the cubic phase. Reprinted with permission from Mastrikov et al., 2010. Copyright 2010 American Chemical Society.

CrystalCalculated δµ0O
Plane wave BS + PW91LCAO + B3LYP
La2O3-0.41-0.64
Mn2O3-0.87-0.53
MnO-0.52-0.59
MnO2-1.14-0.09
Mn3O4-0.90-0.15
average-0.77-0.40

Table 3.

The chemical potential correction (eV), Eq.(54), calculated for different oxides for both employed modeling techniques: (i) plane wave BS and PW91 functional and (ii) LCAO approach based on Gaussian-type atom-centered BS and hybrid B3LYP functional. The last line gives the average correction used in plotting the oxygen chemical potentials of the phase diagrams in Figures 1, 3, and 6.

with different degrees of oxidation, one should treat the obtained data with some precaution. Thus, we highlighted by solid lines the boundaries where metal oxides La2O3 and Mn2O3 with metals in oxidation state 3+ (lines 2 and 5) begin to precipitate in the perovskite. In these oxides, metal oxidation numbers coincide with the oxidation states for the same metals in LaMnO3. Right hand side of the diagrams in Figure 1 contains a family of chemical potentials of O atoms (50) as functions of temperature and partial pressure of oxygen gas. This part of the figures allows us to translate easily-measurable external parameters (temperature and oxygen gas pressure) into oxygen chemical potential, which is one of the variables determining explicitly the SGFE. Using this part of the figures, we can relate points on the phase diagrams with the conditions under which experiments and/or industrial processes occur. To do this, one can just to draw a vertical line for a given temperature

Figure 1.

Phase diagrams calculated with plane wave BS and PW91 GGA functional: The regions of stability of LaMnO3 surfaces with different terminations (LaO- and MnO2- terminated [001] surfaces without and with adsorbed O atom, O2- and O-terminated [011] surfaces) for both orthorhombic (a) and cubic (b) phases as functions of manganese and oxygen atoms chemical potential variations. Parameters for all lines on the left side of the figures are collected in Table 2. The encircled numbers point to lines, where metals or their oxides begin to precipitate: (1) metal La, (2) La2O3, (3) MnO, (4) Mn3O4, (5) Mn2O3, (6) MnO2, and (7) metal Mn. The right side of the figures contains a family of ΔμO as functions of temperature at various oxygen gas pressures according to Eq. (50) and Table 1. The labels m on the lines specifies the pressure according to: pO2 = 10m atm. Reprinted with permission from Mastrikov et al., 2010. Copyright 2010 American Chemical Society.

Figure 2.

Surface Gibbs Free Energies Ωi for LaMnO3 in (a) orthorhombic and (b) cubic phases as functions of ΔμMn at T = 1200 K and pO2 = 0.2 atm Line numbers are the same as in Figure 4.1. The red lines indicate the most stable surface in the stability window between the precipitation lines for La2O3 and Mn2O3. Reprinted with permission from Mastrikov et al., 2010. Copyright 2010 American Chemical Society.

and its crossings with lines corresponding to different gas pressures creates a pressure scale for this particular temperature. This can replace the axis for oxygen chemical potential. Alternatively, moving along the lines for chemical potential at a particular gas pressure, we can study the phase behavior with temperature. Figure 1 shows such a consideration for T=1200 K which is a typical condition for SOFC operations. We marked on these phase diagrams the most important range of oxygen gas partial pressures (between pO2 =0.2 atm. and 1 atm). Oxygen-rich conditions with a larger O chemical potential correspond to higher oxygen gas partial pressures and/or lower temperatures; in turn, oxygen-pure conditions with the lower O chemical potentials correspond to smaller oxygen gas partial pressures and/or higher temperatures.

Consistent positioning of these experimental curves with respect to our computed stability diagram requires also the correction described by Eq. (54). When drawing the right side of Figure 1, we used the correction of -0.77 eV (Table 3) calculated as average of a series of different oxides. It was calculated using the same set of oxides, which precipitation is considered in our plane-wave modeling. Both the values and the scattering (±0.37 eV) of calculated corrections are much larger than in similar studies (Heifets et al., 2007a, 2007b; Johnston et al., 2004; Reuter & Schefer, 2001a) for non-magnetic oxides (e.g. SrTiO3).

Here we consider manganese oxides which are spin-polarized solids. Besides, we included several Mn oxides with various oxidation states. This is a typical situation where DFT calculations face well known problems. The scattering of the correction magnitudes provides an estimate of uncertainty in positioning of the chemical potentials for O atoms on the right side of the phase diagrams.

Figure 2 shows cross sections of the phase diagrams at T = 1200 K and pO2 = 0.2 atm., i.e. in the range of typical SOFC operational conditions. Correspondingly, at the cross sections of the diagrams (Figure 2), the stability region lies between lines 2 and 6. This figure helps to clarify behavior of the SGFEs for surfaces with various terminations.

As it can be seen from Figures 1 and 2, under fuel cell operational conditions in both LMO phases the MnO2-terminated [001] surface is the most stable one. In the orthorhombic phase it is the clean MnO2-terminated surface, whereas in the high-temperature cubic phase the most stable surface contains adsorbed O atoms. This indicates that under identical conditions higher O adsorbate coverage is expected for the cubic LMO phase. Modeling with plane-wave BS and PW91 functional suggest that, when LMO crystal is heated, precipitation of La2O3 or Mn3O4 occurs, depending on chemical potentials variations during heating.

4.2. Stability of LMO surface terminations: LCAO simulations

Calculations performed within the LCAO approach combined with hybrid B3LYP functional were also employed in order to draw the phase diagram for stability of different LMO surface terminations (Figure 3). These calculations were carried out for a cubic phase and A-AFM magnetic ordering, where spins have the same orientations in the planes parallel to the surfaces of the slabs, but have opposite directions in neighbor planes. The comparison of stability shown in this figure includes only two primary candidates for the stable surfaces: LaO- and MnO2-terminated (001) surfaces. The stability range is limited by lines 2, 3, and 5, which correspond to precipitation of La2O3, MnO, and Mn2O3. These are substantially different oxides than suggested above in computations performed with plane-wave BS and PW91 functional. Indeed, the gap between precipitation of La2O3 and Mn2O3 shifted down significantly. Now the boundary between stability regions for LaO- and MnO2-terminated surfaces crosses the gap where LMO is stable, while PW91-GGA calculations described above and by Mastrikov et al., 2009, 2010 suggested that only the MnO2-terminated surface was stable. In calculations with hybrid B3LYP functional the MnO2-terminated surface seems to be stable, up to SOFC operational temperatures (1200 K) under ambient oxygen gas partial pressures (pO2=0.2 atm.). Above this temperature LaO-terminated surface gradually becomes more stable in the larger range in LMO crystal stability region until at ~1900 K it becomes the only stable surface. A precipitation of MnO or La2O3 has to occur while LMO crystal is heated.

Positioning the family of O atom chemical potential curves on the right side of Figure 3 was done in the same way as for Figure 1, but using LCAO calculations with hybrid B3LYP functional. The averaged correction δμO0(54) in this case is noticeably smaller ( -0.40 eV) than it was for PW91-GGA functional. However, deviations of this correction from its average value (±0.3 eV) is still large. This fact likely comes from the DFT difficulties, taking place even within hybrid functionals for spin-polarized systems. For diamagnetic systems, for instance SrTiO3, such deviation drops down, from ~0.25 eV in LDA calculations (Johnston et al., 2004) to ~0.03 eV in calculations (Heifets et al., 2007b) with the hybrid functional.

Figure 3.

Thermodynamic LaMnO3 [001] surface stability diagram as a function of O and Mn chemical potentials. It compares stabilities of both LaO- and MnO2-terminated [001] surfaces and accounts for precipitation conditions for (1) metal La, (2) La2O3, (3) MnO, (4) Mn3O4, (5) Mn2O3, (6) MnO2, and (7) metal Mn, the same set as at Figures 1 and 2. The stable region is shown as lightened area between precipitation lines 2,3, and 5. The right side shows a family of oxygen chemical potentials under different conditions. The label m indicates the O2 gas partial pressure: 10m atm. Red line corresponds to oxygen partial pressure p=0.2p0 as in the ambient atmosphere.

surfaceΓiLa,OΓiLa,MnØiL aØiL a
orientationtermination
[001]LaO-1-0.56.326.46
[001]MnO210.5-0.42-0.43

Table 4.

Parameters defining the surface Gibbs free energies Ωi (Eq. 13) and used to build diagram in Figure 3. The same as Table 2, but for the cubic phase of LMO only and produced with LCAO approach and hybrid B3LYP functional.

4.3. Stability of surface terminations for LSM: LCAO simulations

Since the SGFEs for LSM surfaces depend now on three variables, it is a little more complicated to draw corresponding phase diagrams. Therefore, we have drawn only several sections for the most interesting parts of the phase diagram for bulk concentration of Sr atoms xb= 1/8. Thus, Figure 4 shows the section of surface stability phase diagram under ambient oxygen gas partial pressure pO2=0.2 atm. and three various temperatures: a) 300 K - room temperature (RT), b) 1100 K, which is approximately the SOFC operational temperature, and c) 1500 K, which is close to sintering temperatures. We compared several terminations of LSM (100) surfaces: MnO2, La1-x Srx O,in the last case concentrations of Sr atoms in the surface layer were varied: xs= 0.25, 0.5, 0.75 and 1 (which simulates a segregation effect). Only three terminations appear at the shown sections: MnO2, La0,75Sr0,25O and SrO.Here we accounted for precipitation of metals (La, Mn, Sr), Mn2O3 and La2O3 oxides, and LaMnO3 and SrMnO3 perovskites. These sections of the surface phase diagram indicate that the LSM crystal can be stable only within a small quadrangle region in the presented sections. At low, room temperature two of considered terminations - MnO2 and La0.75Sr0.25O - are stable. At the higher temperatures La0.75Sr0.25O-terminated surface gradually occupies a larger portion of the stability region. Already at SOFC operational temperatures (T1100 K) this termination becomes stable in the entire stability region. Thus, Sr dopant atoms in LSM cause a relative stabilization of the

Figure 4.

Sections of surface stability diagram for LSM (001) surface structures for O2 partial pressure p=0.2p0 and temperatures of (a) 300 K (RT), (b) 1100 K (SOFC operational temperature), and (c) 1500 K (sintering temperature) (Piskunov et al., 2008). The region, where LSM (xb= 1/8 ) is stable, is the shaded area between LaMnO3, La2O3, Mn2O3, and SrO precipitation lines. The numbers from 1 to 11 in the circles indicate precipitation lines for (1) La, (2) La2O3, (3) MnO, (4) Mn3O4, (5) Mn2O3, (6) MnO2, (7) Mn, (8) Sr, (9) SrO, (10) LaMnO3, (11) SrMnO3. (Some of the mentioned oxides are not considered in this Figure, but the numbering is designed to keep consistency of notations between figures.) Hollow arrows indicate the sides from respective precipitation lines where the precipitation occurs. Insets show magnified areas with the region of LSM stability (a shaded quadrangle). Reprinted with permission from Piskunov et al., 2008. Copyright 2008 American Physical Society.

La1xsSrxsO- terminated surface with respect to the MnO2-terminated surface. However, as soon as Sr concentration xs at the La1xsSrxsO-terminated surface becomes 0.5 or larger due to Sr segregation, such a surface becomes unstable.

For better understanding changes in the surface stability with temperature, we have drawn two additional cross-sections along the precipitation lines for SrO and LaMnO3 at pO2=0.2 atm. These cross-sections are presented in Figure 5. It can be seen here that upon heating the MnO2-terminated surface leaves the stability region and becomes replaced by the La0.75Sr0.25O-terminated surface. As heating continues, precipitation of La2O3 or MnO begins. This is consistent with experimental observations by Kuo et al., 1989. A similar degradation process without Sr doping would require stronger overheating or very strongly reducing conditions. Detailed LCAO hybrid functional calculations of oxygen atom adsorption are necessary (see preliminary results in Piskunov et al, 2011), in order to check PW91-GGA prediction (discussed in previous subsection) that the MnO2-terminated surface is stabilized by adsorbed oxygen atoms.

Figure 5.

LCAO calculated cross-sections of surface stability diagram for LSM (001) surface structures along (a) SrO and (b) LaMnO3 precipitation lines for O2 partial pressure p=0.2p0. Meaning of colors (terminations) and numbers (correspond to precipitation lines) are the same as in Figure 4.

4.4. Oxygen adsorption and vacancy formation in LMO

As shown above, the MnO2-terminated (001) surface of LaMnO3 appears to be the most stable one. Therefore, we optimized the atomic structure of surface oxygen vacancies, as well as O atoms and O2 molecules adsorbed at different sites on this surface. For a comparison we also optimized the structure of oxygen vacancies in the LaMnO3 bulk and at the LaO-terminated [001] surface. These simulations were performed using plane wave BS and PW91 functional. Details of the atomic position optimization are described by Mastrikov et al., 2010. In this Chapter, we limit our discussion only to the energies of different adsorbed species and vacancies and thermodynamic consideration of the relevant processes. Note that some adsorbed species have tilted geometry. For example, the lowest energy for the adsorbed O2 molecule on MnO2-terminated surface is atop of Mn ion with the angle between O-O bond and Mn-O direction being ~50o.

The adsorption energies for O atoms (ΔEadssurf(LaMnO3:Oads)and O2 molecules (ΔEadssurf(LaMnO3:O2,ads)), as well as the surface and bulk formation energies (ΔEfsurf(LaMnO3:VO)andΔEfbulk(LaMnO3:VO)) for oxygen vacancies are collected in Table 5. For a classification of different molecular oxygen species we considered atomic charges and the O-O bond length. The data in Table 5 suggest that atomic adsorption of O atoms is energetically more preferable than adsorption of O2 molecule. In both cases the best adsorption site for both O atom and O2 molecule on MnO2-terminated surface is on top of surface Mn ion. Oxygen vacancies have smaller formation energy on MnO2-terminated surface than in the bulk suggesting vacancy segregation towards this surface. In contrary, much more energy is required to create an oxygen vacancy on LaO-terminated surface.

Label of configuration-Ef or Eads ,
eV
Charge, e0O-O distance, Å"chemical assignment"
0.1.30gaseous O2
I-1.1a)-0.421.36tilted superoxide atop one Mnsurf
II-0.9a)-0.651.42horizontal peroxide atop one Mnsurf
III-0.9a)-0.691.41horiz. peroxide atop Osurf
VII-0.5 a)-0.841.62TS of dissociation without Vö, atop Osurf and bridging two Mnsurf
IV-2.8a)-1.191.50tilted peroxide in Vö
V-2.4a)-1.251.50"vertical peroxide" in Vö
V+0.9b)-1.251.50TS of O- diffusion along surface
VI-1.1b)-0.62O- adsorbed atop Mn
VI’-1.8 b)O- adsorbed next to a surface vacancy
VIII-3.3b)-1.19O ion in MnO2[001] surface layer
IX-4.3b)-1.25bulk O ion
X-5.1b)-1.32O ion in LaO[001] surface layer

Table 5.

Bond lengths, Bader charges and "chemical assignment" of the different oxygen species. Experimental O-O bond lengths (NIST, 2010) for comparison: gaseous O2 1.21 Å, hydrogen superoxide radical HO2 1.33 Å, hydrogen peroxide H2O2 1.48 Å. TS = transition state. Energies (compare Figure 4.6; for adsorbate coverage of 12.5 %): a) relative to gaseous O2 in triplet state over defect-free surface, b) relative to half a gaseous O2 over defect-free surface.

Figure 6.

Spectrum of possible “one-particle“ states, where “particles“ are O atoms (right panel) and O2 molecules (left panel). Each level in these panels corresponds to relative energies (∆Er) of different molecular and atomic species occurring during oxygen incorporation reaction on the MnO2[001]-terminated surface of LaMnO3, cf. Table 5. The axes on the left and right give the energy ∆Er relative to resting O2 molecule away from the surface (on the left) or an atom in such O2 molecule (on the right). In the ground state of the crystal all lattice sites in crystal bulk (states X) and I surface (states VIII) are occupied (red levels) and the rest of the “one-particle” states vacant. The numbers at levels correspond to the numbers assigned to respective states in Table 5. The highest level on the right panel corresponds to a free (not in a molecule) O atom away from the crystal. The central panel shows the experimental T- and pO2-dependence of the Gibbs energy of gaseous O2 (Table 1 and Eq.(50)), its energy scale refers to an O2 molecule on the left and to an O atom in an O2 molecule on the right. The labels m on the lines represent the pressure: pO2=10m atm. The arrows indicate various Gibbs reaction energies due to moving of a “particle” between crystal and gas: red = formation of adsorbed superoxide O2− on defect-free surface; green = formation of adsorbed O- atop Mn on defect-free surface; black = incorporation of oxygen into a surface oxygen vacancy.

The collected energies allow us to draw the diagram shown in Figure 6. This diagram is based on a standard model of “non-interacting particles”, where “particles” are O atoms and O2 molecules in different positions. The energy levels drawn at the side panels represent single- particle energies corresponding to bringing a particle to a given position at the surface or in the bulk. The left hand panel refers to bringing a free gas-phase O2 molecule to the crystal surface. Similarly, the right hand panel refers to taking an O atom from a free O2 molecule and placing it on the crystal surface. These processes include also placing of an atom or a molecule into surface vacancies: this is a process inverse to the formation of a vacancy. Therefore, to place the corresponding energy level (at right hand panel), one has to use the vacancy formation energy with the opposite sign. A similar logic was applied in placing the energy level for bringing an oxygen atom into vacancy in the bulk. Such an O atom in a vacancy becomes actually a regular O atom in the crystal lattice (wherever, in the bulk or in the surface). Therefore, the energies of such states can be considered as those for an O atom in the bulk or on the surface. In the ground state of the crystal all lattice sites (states VIII, IX and X) are occupied and all other states vacant.

The variation of the oxygen chemical potential is drawn in the central panel as a function of temperature for several gas partial pressures. These curves are drawn in the same way as similar lines on the right hand side in Figure 1, including the offset defined by Eq. (54). Because the energy scale at the left panel is twice as large as at the right panel, the same curves represent variations either in the chemical potentials for an O2 molecule, if they are referred to the left panel, or for O atom, if they are referred to the right one. In such an arrangement, the diagram in Figure 6 can be used to represent the Gibbs energies for reactions of exchange with O atoms or O2 molecules between oxygen gas and both crystal bulk and surfaces. For example, red arrow represents an adsorption of an O2 molecule atop surface Mn ion in the tilted position (configuration I) from oxygen gas under partial pressure pO2=1 atm. and T=1000 K. The Gibbs free energy of corresponding reaction can be obtained by subtracting the energy of the initial state from that of the final state. For the reaction described by the red arrow this energy indeed corresponds to the adsorption energy for O2 molecule. Similarly, the green arrow describes the adsorption of O atom atop Mn ion in MnO2 –terminated surface. Lastly, the black arrow describes incorporation of an O atom into a surface oxygen vacancy. In the latter case, an arrow with opposite direction corresponds to the formation of a surface oxygen vacancy, as it can be confirmed by a comparison with Eqs. (60, 61).

The diagram in Figure 6 is very suitable way of a graphical representation of the exchange between a gas and a crystal with various species and the analysis of corresponding processes. For a given temperature and oxygen partial pressure this diagram allows one to read the Gibbs reaction energy of a process and thus to obtain its mass action constant. As an example, let us discuss some processes under typical fuel cell conditions of T = 1000 K and pO2 = 1 atm. The formation of molecular adsorbates (superoxide I = red arrow, and peroxide II) is endergonic by ∆rG +2 eV per O2 since the entropy loss overcompensates the electronic energy gain. Even the formation of adsorbed atomic O- (species VI, green arrow) is still slightly endergonic, by ∆rG +0.5 eV per O, what leads the low adsorbate coverage under SOFC conditions. Only the oxygen incorporation into a surface vacancy (black arrow) is strongly exergonic, by ∆rG -1.7 eV per O (i.e. the inverse process, surface oxygen vacancy formation, is endergonic by +1.7 eV). Also, changes in temperature and/or partial pressure can change the sign of the reaction energy. To give an example: while oxygen atom adsorption is exothermic here, it changes from exergonic at low temperatures and/or high partial pressures to endergonic at higher temperatures and/or lower pressures.

5. Conclusions and perspectives

In this Chapter, combining ab initio calculations of the atomic and electronic structure with chemical thermodynamics, we have described how to predict surface stabilities with different orientations and terminations for ABO3 perovskite materials and solid solutions. We considered also adsorption and formation of vacancies in the bulk and at the surfaces. The input data for such thermodynamic analyses are available from standard DFT calculations. We neglected vibrational contributions to the Gibbs free energies in present simulations, since there are good arguments that these contributions are quite small. However, the latest versions of the computer codes used here (VASP and CRYSTAL) are capable to perform the calculations of phonon spectra, which can be used to include vibration contributions into thermodynamic potentials. Despite currently such surface phonon calculations are computationally very expensive, with development of new algorithms and faster computers such analysis in near future could become a routine practice.

We have applied the described techniques to experimentally well studied SOFC cathode materials (LMO and LSM). The energies calculated by DFT techniques allow us to draw the surface stability diagrams showing that under the SOFC operational conditions MnO2-terminated surface of defect/dopant-free LMO is the most stable. The MnO2-terminated surface with adsorbed O atoms becomes more stable in a cubic phase of LMO. (The analysis based on results of calculations with hybrid functional gives higher precision of the obtained diagrams). Introduction of Sr dopant into LMO leads to a significant decrease of stability of MnO2-terminated surface with respect to stability of Sr-containing La1xsSrxsO-terminated surface. At elevated temperatures only the latter one can be found within an entire region of LSM stability which definitely should affect the LSM cathode performance due to our prediction that oxygen vacancies easily segregate from LMO bulk towards MnO2-terminated surface but not to the LaO-terminated one (Mastrikov et al, 2010).

Thermodynamic consideration of oxygen adsorption and formation of surface vacancies allowed us to move beyond the usual analysis of purely DFT electronic energy differences in these processes at zero K and to describe changes in the Gibbs free energies under realistic environmental conditions (high temperature and partial pressure of oxygen gas). In particular, we have shown that an oxygen adsorption from the gas phase is exergonic at low temperatures, but becomes endergonic at SOFC operational temperatures. Consideration of the energy differences between O atoms and O2 molecules in the gas phase and at surfaces makes it possible to determine theoretically preferred adsorption sites, adsorption energies and formation energies for vacancies (e.g. Kotomin et al., 2008, Mastrikov et al., 2010, and Piskunov et al, 2011). Thus the obtained data can be used for analysis of the kinetics of chemical reactions and investigation of their mechanisms. For example, we performed such an analysis (Mastrikov et al., 2010) in the study of oxygen reduction and incorporation into the LMO surfaces.

Note also that under realistic experimental conditions in a multinary crystal typically only one component is reversibly exchangeable so that only one chemical potential can be varied in-situ. Typically the others are varied under preparation conditions, and then so-established sublattice stoichiometry is frozen under experimental conditions. This complex interplay of in-situ and ex-situ parameters has been discussed by Maier, 2003.

Various questions, where thermodynamic approach is necessary, are still open. One example is Sr segregation towards LSM surfaces which was experimentally observed e.g. by Fister et al., 2008 and Herger et al., 2008. In the study by Herger et al., 2008, the Sr segregation energy was estimated to be ~0.16 eV while preliminary theoretical estimate gave the segregation energy ~0.54 eV (Piskunov et al., 2008). Another question is, how vacancy formation and oxygen adsorption energies depend on surface Sr concentration. Lastly, our present simplified simulations assume that LMO and LSM have large flat surfaces. However, one can expect in reality much more rough surface structure containing many facets and steps. This is important also because SOFC cathode materials are polycrystalline. Therefore, there is a necessity to check, which kinds of steps and facets are the most stable ones and likely to exist at LMO and LSM surfaces and how their presence affects adsorption of oxygen atoms and molecules, vacancy formation and reactions occurring at the surfaces.

Acknowledgments

EH is indebted to the Max Planck Institute for financial support through the honorary contract. EK, YM thank the EC FP7 NASA-OTM project (grant agreement N 228701) for partial financial support. S.P. is thankful for the financial support through the ESF project Nr. 2009/0216/1DP/1.1.1.2.0/09/APIA/VIAA/044. This study was supported by a grant of computer time at the EMS Laboratory at PNNL (Project No 42498). Authors are greatly indebted to R. Merkle, J. Fleig, R.A. Evarestov, D. Gryaznov, C. Noguera, and M. W. Finnis for many stimulating discussions.

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Eugene Heifets, Eugene A. Kotomin, Yuri A. Mastrikov, Sergej Piskunov and Joachim Maier (November 2nd 2011). Thermodynamics of ABO3-Type Perovskite Surfaces, Thermodynamics - Interaction Studies - Solids, Liquids and Gases, Juan Carlos Moreno-Pirajan, IntechOpen, DOI: 10.5772/20114. Available from:

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