Francesco
Chiabrera‡
ab,
Federico
Baiutti‡
*ac,
David
Diercks
d,
Andrea
Cavallaro
e,
Ainara
Aguadero
eg,
Alex
Morata
a and
Albert
Tarancón§
*af
aCatalonia Institute for Energy Research (IREC), Jardins de Les Dones de Negre 1, 08930 Sant Adrià del Besòs, Barcelona, Spain. E-mail: fbaiutti@irec.cat; atarancon@irec.cat
bDepartment of Energy Conversion and Storage, Functional Oxides Group, Technical University of Denmark, Fysikvej, 310, 233 2800 Kgs. Lyngby, Denmark
cDepartment of Materials Chemistry, National Institute of Chemistry, Hajdrihova 19, Ljubljana SI-1000, Slovenia
dDepartment of Metallurgical and Materials Engineering, Colorado School of Mines, Golden, CO 80401, USA
eDepartment of Materials, Imperial College London, Prince Consort Road, London SW7 2BP, UK
fICREA, 23 Passeig Lluís Companys, Barcelona 08010, Spain
gInstituto de Ciencia de Materiales de Madrid (ICMM-CSIC), Sor Juana Inés De la Cruz, 3, 28049, Madrid, Spain
First published on 17th January 2022
The call for material systems with enhanced mass transport properties is central in the development of next-generation fuel cells, batteries and solid state energy devices in general. While two-dimensional doping by artificial heterostructuring or nanoscaling has shown great potential for overcoming kinetic limitations of ion diffusion, the length scale of interface effects requires the development of advanced tools for capturing and quantifying local phenomena in greater detail. In the present paper, an in-depth study of grain boundary oxygen conduction in Sr-doped lanthanum manganite films is presented by means of novel isotope-exchange atom probe tomography. Local pathways for fast mass transport are directly mapped by two-dimensional reconstructions and line profiles of the oxygen isotope concentration. Accurate finite element modelling is employed to retrieve the local kinetic parameters, highlighting an enhancement of two orders of magnitude for both the diffusivity and surface exchange rate with respect to the bulk ( cm2 s−1 and cm s−1, respectively, for grain boundaries at 550 °C). Co-acquired reconstruction of the cationic distribution reveals strong inhomogeneities (dopant de-mixing) across the grain boundaries and in the sub-surface region, leading to local Sr accumulation. The findings provide unequivocal quantitative assessment of fast grain boundary oxygen diffusion in lanthanum strontium manganite, giving further insights into local stoichiometry deviations and promoting isotope exchange-atom probe tomography as a powerful tool for the study of local interface effects with high resolution. Different models for the explanation of the phenomena are critically discussed on the basis of the experimental findings.
While these results point out the potential of interface engineering for tuning oxygen kinetics and transport, the study of local mass transport presents a critical issue due to the impossibility of capturing such nanoscale effects with sufficient spatial resolution. Information obtained from diffusion profiles acquired by SoA techniques based on isotope exchange depth profiling (IEDP) is averaged over large areas (typically hundreds of μm2)21 and no information on the local chemical composition is usually accessible. These limitations prevent a complete understanding of diffusion phenomena and cause a considerable uncertainty for the retrieval of the kinetic parameters.22 Very recently, we have demonstrated how atom probe tomography (APT) is able to overcome such shortcomings by providing a 3D-resolved reconstruction of atomic positions with nm-resolution and isotopic sensitivity.20 In our previous studies, isotope exchange of thin films under controlled conditions allowed a direct observation – and reliable quantification – of fast oxygen diffusion pathways at LSCr grain boundaries and LSM–ceria interfaces.12,20 Independent work by Kaspar et al. recently presented a similar approach for the study of buried Fe2O3 interfaces, confirming the broad relevance of the isotope exchange APT (IE-APT) approach.23
In the present study, IE-APT was used for the first-time visualization – and direct quantification – of previously reported enhancement of local oxygen transport in interface-dominated LSM. Fully dense nanocrystalline thin films have been fabricated by pulsed laser deposition (PLD) for a subsequent ex situ exchange in an 18O-enriched atmosphere at controlled temperature. Sample conical tips of the exchanged films have been analyzed by APT providing a precise 3D chemical mapping and a direct visualization of nm-wide fast diffusion oxygen pathways. The experimental oxygen isotope fraction profiles have been simulated by finite element modelling (FEM) for a precise and independent quantification of the oxygen kinetic parameters for bulk, GBs (self-diffusion coefficient, D*, and effective surface exchange coefficient, k*) and for the analysis of mass transport in sub-surface regions. Local cationic distribution, as retrieved by IE-APT, is correlated to the observed functionalities.
FEM simulations have been employed in order to calculate the values of the oxygen transport parameters of LSM bulk and GB (k* and D*) by fitting the APT reconstruction profiles – Fig. 2. 2D model geometries were selected for accurately reproducing the out-of-plane IE-APT reconstructions (cf.Fig. 1a and ESI Fig. 2†), which present grain interior areas (characterized by and ) separated by 1 nm-thick GBs (with kinetic parameters and – fast GB core).18,20 An additional parameter was introduced in the model for qualitatively describing the (slower) diffusion of the grain interior in the subsurface region, which accounts for the observed initial steep decrease of the tracer fraction for Z < 5 nm (Fig. 2b). This assumption is justified on the basis of strong cationic deviations measured by APT – cf. later in the text – and of previous reports e.g. on Fe-doped SrTiO3, reporting slow subsurface oxygen diffusivity as a consequence of space-charge effects.25 Please refer to ESI Notes 1 and 2† for details on the FEM modelling, including sensitivity analysis. Fig. 2b shows the 2D contour of the FEM model after fitting of the experimental data (Fig. 2a) by systematic parameterization. The optimized FEM model is able to accurately describe the IE-APT results (apart from very local inhomogeneities) yielding: (i) fast oxygen incorporation and diffusivity at the GB ( cm2 s−1, cm s−1 at 550 °C); (ii) slower diffusivity and surface exchange rate for the bulk ( cm2 s−1, cm s−1); (iii) reduced sub-surface diffusivity ( cm2 s−1 – note that the sub-surface region width is assumed as 5 nm – cf. later in the text).
Unlike conventional tracing methods based on secondary ion mass spectrometry (SIMS) – which offer only averaged data over hundreds of μm2 – IE-APT allows extracting direct information on the local tracer fraction with nm-resolution in all directions (X–Y–Z). A segmented analysis of the data is therefore accessible for a separate study of the different sample areas as shown in Fig. 2c, in which light and dark green dotted lines correspond to 1D out-of-plane experimental profiles along bulk and a selected GB, respectively. In-plane 1D profiles of f(18O) are represented in Fig. 2d (profiles extracted along the dotted lines in Fig. 2a). Using these data, f(18O) for the two phases can be independently fit for a very precise quantification. The results highlight that isotopes incorporation in the bulk grain originates from lateral diffusion from the GBs ( cm2 s−1) giving rise to a concentration gradient in the X-direction (Fig. 2d). Conversely, vertical mass transport through the bulk is strongly suppressed. Finally, a local accumulation of oxygen isotope is confirmed in the sub-surface (cf. grain f(18O) profile in Fig. 2c, Z < 5 nm). This effect can be modelled by the introduction of the previously mentioned sub-surface diffusivity, , which strongly improves the fitting of the bulk tracer profile (while the quality of the GBs modelling remain largely unaffected – please refer to ESI Fig. 3,† which includes two FEM fittings obtained for the same set of parameters, with and without ).
Effects stemming from trajectory aberration are known to limit the APT resolution to ≈2 nm at phase contacts, preventing a local study of the oxygen content in the grain boundary core.26 In ESI Note 3,† we discuss an alternative FEM model based on the space-charge accumulation of oxygen vacancies (and strong reduction of oxygen diffusivity in the core). This behavior may originate from the segregation of the acceptor dopant () or cationic vacancies ( or ) in the core, giving rise to a negatively charged interface and promoting the accumulation of positively charged oxygen vacancies in the GB surroundings. We note that, in bulk LSM under oxidizing conditions, the concertation of cationic vacancies and acceptor dopant Sr is high,27 while oxygen vacancies, which are typically expected to segregate at the GB core in ionic conductors,28 are a minority defect. This interesting scenario was recently proposed by Börgers et al. to explain fast diffusion along dislocation in LSM.16 The result of the simulations (ESI Fig. 8†) show that also this model is able to adequately describe the f(18O) profiles.15,16 Importantly, the resulting kinetic parameters are very close to the ones obtained by considering fast core diffusivity (Fig. 2).
The resulting k* and D* are compared to literature data (stoichiometric13 and B-site deficient LSM14) in Fig. 3: the values (measured here for T = 550 °C) are well in line with previous literature reports, confirming the quality of our approach based on IE-APT. The observed enhancement of both and is about two orders of magnitude with respect to the bulk. is reduced by about one order of magnitude in comparison to , yet within typical values for bulk LSM.
Fig. 3 Diffusivity (a) and surface exchange coefficient (b) for nanocrystalline LSM measured by APT and compared to literature values (for stoichiometric and B-site deficient (LSM0.85) materials).13,14,29 Values from Saranya et al. 2015 (ref. 14) have been updated using the FEM model introduced by the authors in Saranya et al. 2018 (ref. 18). The error bars are calculated from the sensitivity analysis described in ESI Note 2.† |
Fig. 4 shows independent 2D contour plots of the different ionic species (La, Mn, Sr and O in Fig. 4a–d, respectively) and linescans along horizontal (Z = 20 nm in Fig. 4f) and vertical directions (X = 0 in Fig. 4g). As a first general observation, important deviations from the nominal stoichiometry are present for A-site cations with Sr-content x ranging from ∼0.10 to ∼0.5 in La1−xSrxMnO3, within a length scale ≈10 nm. (Please note that some uncertainty in the absolute atomic concentration may be introduced by the APT technique).12,30Fig. 4a (La contour) also highlights a strong modulation of La concentration (especially in the proximity of the fast oxygen diffusion pathways), which is complementary to Sr (cf. also Fig. 4c and f). Although such a relation is predictable (Sr being an A-site substitutional dopant), such a very broad non-stoichiometry at the nanoscale level is unexpected. It is noteworthy that this uneven distribution of A-site cations does not involve variations in the Mn distribution map within the resolution of the technique (Fig. 4b), confirming a homogeneous presence of the ABO3 perovskite phase (cf. also Fig. 1). Intriguingly, the variation of the A-site distribution is different for each GB (labelled as GB1 and GB2) and clear compositional differences can be observed between the two GBs. This is particularly clear in the 1D profiles shown in Fig. 4e (crossing GB1 and GB2). Namely, GB1 is characterized by a strong Sr accumulation (up to x ∼ 0.5) that is not observed for GB2 (which is closer to stoichiometry). In both cases, Sr depletion occurs especially on one side of the boundary. As far as the total oxygen content is concerned (18O + 16O), a clear depletion is found in correspondence to the high Sr concentration areas (Fig. 4d), in agreement with a classical electroneutral situation .31 Oxygen diffusivity, however, seems not to be directly related to such strong compositional variations, as similar kinetic parameters characterize GB1 and GB2 (cf.Fig. 1). We ascribe such an apparent discrepancy to the different lengths scales under consideration (≈10 nm for the observed stoichiometry changes vs. <3 nm for fast-conducting GB width),16,17 alongside possible mobility effects. Note that the observed strong dopant segregation is expected to have a stronger impact on the electronic conductivity and magnetic properties of LSM.32–34 Overall, such findings (and similar observations previously reported by our group for nanocrystalline lanthanum chromite)20 call attention to the need of accurate models which capture the different driving forces for a proper description of local chemistry and relevant cation non-stoichiometry in non-dilute systems. A Poisson–Cahn approach, accounting for the electrostatic, but also structural and elastic contributions in non-diluted system, could in principle provide the rationale for the observed ion accumulation at the grain boundaries.16,35,36 Improved models will be of utmost importance to understand and qualify the recently reported tendency of dopant de-mixing in MIEC materials.37
Lastly, the out-of-plane ionic profiles are analyzed in Fig. 4f (grain interior). A progressive decrease of the Mn content towards the free surface of the film (Z = 0) is highlighted, alongside a very strong accumulation of Sr and La in the sub-surface region (Z < 10 nm).38,39 Notably, the thickness of such a region, characterized by different stoichiometry, corresponds to the oxygen isotope accumulation area highlighted in Fig. 1 and can therefore be tentatively accounted for the local low described previously. Note also that APT is able to retrieve local information on single grains and is therefore in principle unaffected by intergranular porosity/roughness for the assessment of the surface region.
APT (Cameca LEAP 4000X Si) was performed at 45.5 K using a 30 pJ laser energy and 500 kHz pulse rate. The flight path length was 90 mm and the ion detection rate was set to 5 ions per 1000 pulses, resulting in a bias range of 5000–7400 V during the data collection. Reconstructions were generated in Cameca's IVAS 3.6.18 software using the TEM images of the specimens before and after APT analysis (ESI Fig. 9†) for setting the reconstruction parameters.42 A systematic energy deficit correction was employed to improve the mass spectral resolution.43
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/d1ta10538h |
‡ Equal contribution. |
§ Albert Tarancón writes: the paper is dedicated to John Kilner who possesses an innate talent for ionics and people. John is always opening doors for everyone. Indeed, meeting him opened the front door to this community for me. I will be always grateful for this. The current work is probably an ultimate answer to years of discussion with him on the outstanding ionic conductivity of LSM thin films. I am sure he will enjoy it. |
This journal is © The Royal Society of Chemistry 2022 |