Jose M.
Porras-Vazquez
*a,
Enrique R.
Losilla
b,
Philip J.
Keenan
a,
Cathryn A.
Hancock
a,
Thomas F.
Kemp
c,
John V.
Hanna
*c and
Peter R.
Slater
*a
aSchool of Chemistry, University of Birmingham, Birmingham, B15 2TT, UK. E-mail: j.m.porras@bham.ac.uk; p.r.slater@bham.ac.uk; Fax: +44 (0)1214144403; ;; Tel: +44 (0)1214148672
bDepto de Química Inorgánica, Cristalografía y Mineralogía, Universidad de Málaga, Málaga, 29071, Spain
cDepartment of Physics, University of Warwick, Coventry, CV4 7AL, UK. E-mail: j.v.hanna@warwick.ac.uk
First published on 8th February 2013
In this paper we report the successful incorporation of silicon into Sr1−yCayMnO3−δ perovskite materials for potential applications in cathodes for solid oxide fuel cells. The Si substitution onto the B site of a 29Si enriched Sr1−yCayMn1−xSixO3−δ perovskite system is confirmed by 29Si MAS NMR measurements at low B0 field. The very large paramagnetic shift (∼3000–3500 ppm) and anisotropy (span ∼4000 ppm) suggests that the Si4+ species experiences both Fermi contact and electron-nuclear dipolar contributions to the paramagnetic interaction with the Mn3+/4+ centres. An improvement in the conductivity is observed for low level Si doping, which can be attributed to two factors. The first of these is attributed to the tetrahedral coordination preference of Si leading to the introduction of oxide ion vacancies, and hence a partial reduction of Mn4+ to give mixed valence Mn. Secondly, for samples with high Sr levels, the undoped systems adopt a hexagonal perovskite structure containing face sharing of MnO6 octahedra, while Si doping is shown to help to stabilise the more highly conducting cubic perovskite containing corner linked octahedra. The level of Si, x, required to stabilise the cubic Sr1−yCayMn1−xSixO3−δ perovskite in these cases is shown to decrease with increasing Ca content; thus cubic symmetry is achieved at x = 0.05 for the Sr0.5Ca0.5Mn1−xSixO3−δ series; x = 0.075 for Sr0.7Ca0.3Mn1−xSixO3−δ; x = 0.10 for Sr0.8Ca0.2Mn1−xSixO3−δ; and x = 0.15 for SrMn1−xSixO3−δ. Composites with 50% Ce0.9Gd0.1O1.95 were examined on dense Ce0.9Gd0.1O1.95 pellets. For all series an improvement in the area specific resistances (ASR) values is observed for the Si-doped samples. Thus these preliminary results show that silicon can be incorporated into perovskite cathode materials and can have a beneficial effect on the performance.
Our preliminary studies on Si incorporation were performed in cobalt-based perovskite electrode materials, showing the successful incorporation of Si into La0.6Sr0.4Co0.8Fe0.2O3−δ and Sr1−xYxCoO3−δ-based materials, with significant results in term of improvements in the conductivity and an enhancement in the stability towards CO2.32 Similarly, Si doping was shown to be successful in the manganese/cobalt-based perovskite electrode materials, SrMO3−δ (MCo, Mn).33 The silicon doping was shown to be successful results in terms of stabilization of the 3C-perovskite containing corner linked octahedra (the undoped composition is a 2H perovskite, containing face sharing of octahedra), and a consequent enhancement in the conductivity. However, for SrMnO3−δ, quite high levels (15%) of Si were required to stabilise the 3C-perovskite, and while the Si doping is beneficial in this respect, it might also be expected to show some detrimental effect in terms of partially disrupting the electronic conducting pathways. Therefore, in this work we have examined mixed calcium–strontium, SryCa1−yMnO3−δ systems, with a view to lowering the Si level needed to achieve this stabilisation. In this paper we therefore report studies into the effect of Si doping into SryCa1−yMnO3 and its effect on the electrical properties to examine the potential for SOFC applications. As a comparison to Si doping, another isovalent dopant, Ti, was also examined for selected systems.
The characterisation of these Si doped systems has been undertaken using XRD, TGA, SEM, impedance measurements and 29Si solid state MAS NMR spectroscopy. The 29Si MAS NMR measurements reported within provide the first unambiguous demonstration of the Si incorporation occurring directly into the perovskite structure of such manganite systems.
Powder X-ray diffraction (XRD) (Bruker D8 diffractometer with Cu Kα1 radiation) was used to demonstrate phase purity, as well as for cell parameters determination. For the latter, the GSAS suite of programs was used.34
Oxygen contents were estimated from thermogravimetric analysis (Netzsch STA 449 F1 Jupiter Thermal Analyser), a method commonly used in the determination of the oxygen content in cathode materials.35–37 Samples were heated at 10 °C min−1 to 1200 °C in N2 and held for 30 minutes to reduce the Mn oxidation state to 3+. This is consistent with prior reports on the reduction of undoped SrMnO3 to Sr2Mn2O5.38 The original oxygen content and average Mn oxidation state then was determined from the mass loss observed.
Pellets for conductivity measurements were prepared as follows: the powders were first ball-milled (350 rpm for 1 hour), before pressing (200 MPa) as pellets and sintering at 1350 °C for 12 h. Conductivities were then measured using the four probe dc method. Four Pt electrodes were attached with Pt paste, and then the sample was fired to 800 °C in air for 1 hour to ensure bonding to the sample. The samples were then furnace cooled to 350 °C in air and held at this temperature for 12 hours to ensure full oxygenation.
The morphology of the sintered pellets was studied using a JEOL SM-6490LV scanning electron microscope. The ceramic surfaces were polished with diamond spray from 6 to 1 mm of diameter and then thermally etched at 50 °C below the sintering temperature for 15 min at a heating/cooling rate of 5 °C min−1. Finally, the samples were sputtered with graphite for better image definition.
To elucidate the potential of these materials as SOFC cathodes, symmetrical electrodes were coated on both sides of dense Ce0.9Gd0.1O1.95 (CGO10, Aldrich) pellets (sintered at 1500 °C for 12 h) using a suspension prepared with a mixture of electrolyte and electrodes (1:
1 wt%) and Decoflux™ (WB41, Zschimmer and Schwarz) as binder material. The symmetrical cells were fired at 900 °C for 1 h in air. Afterwards, a Pt-based ink was applied onto the electrodes to obtain a current collector layer and finally fired at 800 °C for 1 hour. Area-specific resistance (ASR) values were then obtained under symmetrical air atmosphere in a two electrode configuration. Impedance spectra of the electrochemical cells were collected using a HP4912A frequency analyser, at open circuit voltage (OCV), in the 5 Hz–13 MHz frequency range with ac signal amplitude of 100 mV. The spectra were fitted to equivalent circuits using the ZView software,39 which allows an estimation of the resistance and capacitance associated with the different cell contributions.
All 29Si MAS NMR measurements were performed on a low field Chemagnetics CMX-100 spectrometer (B0 = 2.35 T) operating at a 29Si Lamor frequency of 29.88 MHz. MAS NMR experiments were undertaken using a Doty 4 mm MAS probe in which MAS frequencies (νr) of 15 kHz were achieved. Pulse time calibration was performed on a sample of solid kaolinite where a B1 field of 83 kHz delivered a π/2 pulse width of 4 μs. The 29Si MAS NMR data were acquired using both single pulse and rotor-synchronised spin echo (θ − τ − 2θ − τ) experiments. Single pulse measurements used a π/4 flip angle which equated to an excitation pulse width of 2 μs, while the rotor-synchronised spin echo experiments utilised θ/2θ flip angles of π/4/ π/2 (2/4 μs, respectively) and a τ delay of 50 μs. The reported 29Si chemical shifts are referenced to the primary IUPAC standard of TMS (δ 0 ppm) via a secondary solid standard of kaolinite (δ −92 ppm) which was also used for the pulse time calibration. Single pulse measurements which focussed on diamagnetic components within each sample used recycle delays of 60 s, while the spin echo experiments were used to study the paramagnetic component of these samples which permitted much shorter recycle delays of 0.25 s to be implemented.
For the Ca endmember samples, CaMn1−xSixO3−δ, X-ray diffraction data showed the successful incorporation of silicon up to x = 0.05 with no change in cell symmetry on doping. Higher dopant amounts led to the segregation of secondary phases, such as Ca4Mn3O10 (PDF 089-5427). For these doped compositions, although they were still orthorhombic, the difference between the a and c parameters became lower, suggesting that the silicon doping increases the “tetragonality” of this series (see Table 1). If we examine the ratio a/c for this series we can see that this number decreases from 1.0030 for CaMnO3−δ to values around 1.0008 for the doped compositions. Confirmation of the introduction of silicate was shown by the fact that equivalent Mn deficient samples CaMn1−xO3−δ (x = 0.05) with no added silicate gave the segregation of secondary phases, such as Ca4Mn3O10.
SryCa1−yMn1−xSixO3−δ | ||||||
---|---|---|---|---|---|---|
Sr (y) | 0 | 0.5 | ||||
Si (x) | 0 | 0.05 | 0.10 | 0 | 0.10 | 0.15 |
a (Å) | 5.2673(1) | 5.2800(2) | 5.2929(5) | 5.3308(11) | 3.7916(1) | 3.7988(2) |
b (Å) | 5.2828(1) | 5.2855(3) | 5.2967(4) | 5.3303(12) | 3.7916(1) | 3.7988(2) |
c (Å) | 7.4575(1) | 7.4682(3) | 7.4770(6) | 7.5448(3) | 3.7916(1) | 3.7988(2) |
V/Z (Å3) | 51.89(1) | 52.10(1) | 52.40(4) | 53.60(2) | 54.51(1) | 54.82(1) |
For the SryCa1−yMn1−xSixO3−δ series (y = 0.5, 0.7 and 0.8), single phase samples could be achieved up to higher levels of silicon, x ≤ 0.125. As for Si doping in CaMnO3−δ, exceeding this Si content led to the segregation of secondary phases. Without Si doping, the samples were shown to be either hexagonal perovskites (at high Sr levels, y = 0.8) as for the Sr endmember, SrMnO3−δ, a mixture of hexagonal and cubic perovskites (y = 0.7), or a mixture of tetragonal and orthorhombic (y = 0.5). As the silicon content was increased, the level of cubic perovskite was increased, with the amount of silicon needed to produce a single phase cubic perovskite sample increasing as the strontium content increases (Fig. 1). The single phase cubic samples were achieved at x = 0.05 for the Sr0.5Ca0.5Mn1−xSixO3−δ series, x = 0.075 for Sr0.7Ca0.3Mn1−xSixO3−δ, and x = 0.10 for Sr0.8Ca0.2Mn1−xSixO3−δ, which compares to x = 0.15 for SrMn1−xSixO3−δ in our previous study.33 The Rietveld refinement for Sr0.7Ca0.3Mn0.925Si0.075O3 is shown in Fig. S1.† The figure shows a very good fit with very low R factors (Rwp = 2.40% and RF = 1.43%). In addition the Bragg reflections for this composition are marked and it can be seen that there are no secondary phases. Moreover, if we refine the occupancy factors for the Ca and Sr and the Mn and Si pairs, the values are very close to the theoretical values. Similar results and R factors are obtained for the rest of the samples.
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Fig. 1 X-ray diffraction patterns for (a) Sr0.7Ca0.3MnO3−δ; (b) Sr0.7Ca0.3Mn0.925Si0.075O3−δ; (c) Sr0.7Ca0.3Mn0.9Si0.1O3−δ; (d) Sr0.8Ca0.2MnO3−δ; (e) Sr0.8Ca0.2Mn0.925Si0.075O3−δ; and (f) Sr0.8Ca0.2Mn0.9Si0.1O3−δ. Hexagonal perovskite peaks marked with asterisks. |
In Fig. 2, SEM micrographs are shown for (a) Sr0.5Ca0.5MnO3−δ; (b) Sr0.5Ca0.5Mn0.95Si0.05O3−δ; (c) Sr0.7Ca0.3MnO3−δ and (d) Sr0.7Ca0.3Mn0.925Si0.075O3−δ. Comparing Sr0.5Ca0.5MnO3−δ and Sr0.5Ca0.5Mn0.95Si0.05O3−δ, there is no significant difference in the morphology on Si doping. In the case of Sr0.7Ca0.3MnO3−δ, the SEM micrographs show evidence for striations on the grains, consistent with strain effects. These strain effects can be explained by the fact that hexagonal perovskites typically transform to cubic perovskites at elevated temperatures (e.g. those used in the sintering), reverting slowly back to hexagonal perovskites on cooling. In contrast, the grains for the Si doped sample, Sr0.7Ca0.3Mn0.925Si0.075O3−δ, showed no such evidence of strain effects, which can be explained by both the low temperature and high temperature structure being cubic, and thus there being no phase changes on heating and cooling.
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Fig. 2 SEM micrographs for (a) Sr0.5Ca0.3MnO3−δ; (b) Sr0.5Ca0.5Mn0.95Si0.05O3−δ−; (c) Sr0.7Ca0.3MnO3−δ and (d) Sr0.7Ca0.3Mn0.925Si0.075O3−δ−. |
Cell parameters for these systems were determined from the X-ray diffraction data using the Rietveld method (see Tables 1 and 2). The change in cell parameters for these oxyanion doped perovskite materials is a balance between the effect of the smaller size of Si4+, which would be expected to lead to a reduction in cell volume, and the associated reduction in the average Mn oxidation state, which would be expected to lead to an increase in cell volume. In line with prior works on manganite systems, mixed valence Mn3+/4+ is assumed, although there is a possibility that Si incorporation may locally stabilize some Mn2+. The partial reduction of Mn4+ through Si doping is predicted by the following defect equation, assuming tetrahedral coordination for Si and reduction to Mn3+, which illustrates that for each Mn replaced by Si a reduction of 2Mn4+ to Mn3+ would be predicted.
SiO2 + 3MnMn + OO → SiMn + 2MnMn′ + V··O + 1/2O2 + MnO2 | (1) |
SryCa1−yMn1−xSixO3−δ | |||||||||
---|---|---|---|---|---|---|---|---|---|
Sr (y) | 0.7 | 0.8 | 1 | ||||||
Si (x) | 0 | 0.075 | 0.1 | 0 | 0.10 | 0.125 | 0 | 0.15 | 0.175 |
a (Å) | 5.3963(1) | 3.7988(1) | 3.8019(1) | 5.4072(1) | 3.8127(2) | 3.8157(2) | 5.4481(1) | 3.8380(3) | 3.8456(3) |
b (Å) | 9.3424(1) | 3.7988(1) | 3.8019(1) | 9.3755(1) | 3.8127(2) | 3.8157(2) | 5.4481(1) | 3.8380(3) | 3.8456(3) |
c (Å) | 9.1208(1) | 3.7988(1) | 3.8019(1) | 9.0990(1) | 3.8127(2) | 3.8157(2) | 9.0796(2) | 3.8380(3) | 3.8456(3) |
V/Z (Å3) | 57.47(2) | 54.82(2) | 54.95(1) | 57.66(2) | 55.42(1) | 55.55(1) | 58.35(1) | 56.53(1) | 56.87(3) |
As can be seen from the above equation, a key driving force for the reduction of Mn is the introduction of oxide ion vacancies due to the lower coordination (tetrahedral rather than octahedral) preference of the Si dopant (i.e. for x = 0, the B cation site is completely occupied by 6 coordinate Mn, while for x > 0 some Si is on this site, with the tetrahedral coordination preference leading to a reduction in the total oxygen content). Thus, while we are nominally performing an isovalent (Si4+ in place of Mn4+) substitution, the generation of oxide ion vacancies results in partial reduction, i.e. electron doping. The stabilization of the cubic perovskite polymorph on silicon doping can then be related to the lower average Mn oxidation state, and hence average B cation size, reducing the tolerance factor. The difference in Si content required to achieve this stabilisation across the SryCa1−yMnO3−δ series can be explained by the fact that for samples with the highest levels of Sr, the average size of the A site is higher, and hence the starting tolerance factor for the parent phase is higher. Consequently, it is necessary to reduce a larger amount of Mn4+ to Mn3+ and hence introduce a larger Si content.
Direct evidence for Si4+ incorporation into the perovskite structure is provided by the low field 29Si MAS NMR results shown in Fig. 3. This figure compares the data obtained from a physical (highly ground) mixture of 29Si enriched SiO2 with undoped Sr0.8Ca0.2MnO3−δ (see Fig. 3a), and that acquired from a 29Si doped Sr0.8Ca0.2Mn0.9Si0.1O3−δ sample (see Fig. 3b and c). As observed from Fig. 3a and the expansion of this data shown in Fig. 4a, the 29SiO2/Sr0.8Ca0.2MnO3−δ mixture yields a single 29Si resonance with a chemical shift δ −113 ppm which is characteristic of the 29SiO2 component only. However, similar measurements on the 29Si doped Sr0.8Ca0.2Mn0.9Si0.1O3−δ system produces two very different signals; one narrow resonance that occurs downfield from the 29SiO2 resonance at δ −70 ppm (see Fig. 3b and 4b), and one very broad resonance with a large downfield shift of ∼3000–3500 ppm (see Fig. 3c). From the narrow linewidth and long T1 (>180 s) characterising the δ −70 ppm resonance it is concluded that it represents a diamagnetic impurity phase formed under the Si incorporation conditions, and the chemical shift suggests that it's likely to be a strontium/calcium silicate phase. In this respect, this sample did indeed show very weak impurities, such as Sr2SiO4. It has been previously reported that the chemical shift for Si is −69.42 ppm,40 very close to the experimental value determined, −70 ppm. The significantly broadened resonance centred at ∼3000–3500 ppm shown in Fig. 3c was acquired with a rotor synchronised spin echo experiment using a short recycle delay of 0.25 s. These characteristics establish that this is a paramagnetically influenced Si species in the Sr0.8Ca0.2Mn0.9Si0.1O3−δ structure which is probably experiencing both Fermi contact and electron-nuclear dipolar contributions within the overall paramagnetic interaction with the Mn centres, as evidenced by the large paramagnetic shift and broad anisotropic lineshape spanning ∼4000 ppm, respectively. These data, therefore, provide the first direct evidence of Si incorporation into the perovskite framework in such manganite perovskites. The tetrahedral environment of silicon is not possible to state due to the fact that its resonance is paramagnetically influenced and very displaced. The only previous reports of Si in perovskites relates to their high interest for earth scientists, where perovskites such as CaSiO3, and MgSiO3 are believed to be the main components of the earth's lower mantle. These studies have shown that to achieve octahedral Si, extremely high pressures are required, and at lower pressures Si will be tetrahedral. It is therefore quite reasonable to propose tetrahedral coordination for Si and indeed this tetrahedral coordination helps to explain the observed reduction in the Mn oxidation state and enhancement in conductivity/change to a cubic cell.
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Fig. 3 Low field (B0 = 2.35 T) solid state 29Si MAS NMR data for (a) the physical mixture of 29SiO2 and Sr0.8Ca0.2MnO3 (δ −113 ppm), and (b, c) the 29Si doped Sr0.8Ca0.2Mn0.9Si0.1O3−δ (δ −70 ppm and ∼3000–3500 ppm). The data from the 29SiO2/Sr0.8Ca0.2MnO3 physical mixture in (a) and the narrow component from the doped Sr0.8Ca0.2Mn0.929Si0.1O3−δ system in (b) were acquired at ambient temperature with a single pulse experiment and an MAS frequency of νr = 15 kHz. The broad data from the doped Sr0.8Ca0.2Mn0.929Si0.1O3−δ system in (c) was acquired with a rotor synchronised spin echo experiment with νr = 15 kHz and a frequency offset of +35 kHz. |
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Fig. 4 Expansion of the solid state 29Si MAS NMR data for (a) the physical mixture of 29SiO2 and Sr0.8Ca0.2MnO3 (δ −113 ppm), and (b) 29Si doped Sr0.8Ca0.2Mn0.9Si0.1O3−δ (δ −70 ppm), acquired at low B0 field (2.35 T) and at ambient temperature. These data were acquired using a single pulse experiment and νr = 15 kHz. |
The average oxidation states of Mn in these systems are reported in Table 3, and as can be seen, the average oxidation states are closer to 3 as the silicon content increases. Overall the oxygen contents determined from TGA, suggest that once the cubic perovskite forms, further loss of oxygen occurs, since the oxygen contents determined are lower than the value assuming eqn (1) is the only origin of oxide ion vacancies (e.g. for 5% Si doping, a stoichiometry of CaMn0.95Si0.05O2.95 might be predicted from eqn (1), while TGA studies indicated a lower oxygen content, CaMn0.95Si0.05O2.8).
SryCa1−yMn1−xSixO3−δ | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|
Sr (y) | 0 | 0.5 | 0.7 | 0.8 | 1 | |||||
Si (x) | 0 | 0.05 | 0 | 0.10 | 0 | 0.075 | 0 | 0.10 | 0 | 0.15 |
Oxygen deficiency (δ) | 0.04 | 0.20 | 0.01 | 0.27 | ∼0 | 0.29 | ∼0 | 0.31 | ∼0 | 0.23 |
Oxidation state | 3.93 | 3.56 | 3.98 | 3.41 | ∼4 | 3.37 | ∼4 | 3.31 | ∼4 | 3.23 |
Conductivity at 700 °C (S cm−1) | 3.2 | 38.1 | 2.5 | 34.2 | 0.4 | 29.5 | 0.3 | 24.9 | 0.01 | 11.2 |
Conductivity at 800 °C (S cm−1) | 7.6 | 40.2 | 3.4 | 36.3 | 0.7 | 30.4 | 0.6 | 26.1 | 0.03 | 14.0 |
ASR at 700 °C (Ω cm2) | 12.3 | 3.49 | 11.07 | 1.21 | 0.70 | 0.44 | 1.60 | 0.49 | 1.23 | 0.67 |
ASR at 800 °C (Ω cm2) | 1.50 | 0.35 | 1.73 | 0.20 | 0.11 | 0.08 | 0.36 | 0.07 | 0.20 | 0.09 |
An illustration of the importance of the lower coordination preference of Si (4 versus 6 for Mn) in these systems is shown by a comparison with Ti-doped Sr1−xCaxMnO3−δ samples: SrMn0.85Ti0.15O3−δ and Sr0.8Ca0.2Mn0.9Ti0.1O3−δ. As in the case of Si-doping, for these latter Ti doped systems, we are also nominally performing an isovalent (Ti4+ in place of Mn4+) substitution. However, in this case we do not expect any reduction of Mn4+ or generation of oxide vacancies, due to the preference of the Ti for octahedral coordination, as for the Mn, rather than the tetrahedral coordination of Si. Therefore, Ti-doping is not expected to lead to any decrease in the average Mn oxidation state, and, thus, no change in the symmetry from the undoped compositions to the Ti-doped ones for low level Ti doping. If we examine the XRD patterns of SrMn0.85Ti0.15O3−δ and Sr0.8Ca0.2Mn0.9Ti0.1O3−δ, we can see that the predicted behaviour is confirmed, i.e. the cubic form is not stabilized (Fig. S2†). This illustrates that it is the oxygen vacancies incorporated as a result of the lower coordination of Si that are key to the beneficial effects on Si doping.
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Fig. 5 Plot of log σ vs. 1000/T for CaMnO3−δ (□), CaMn0.975Si0.025O3−δ (○), CaMn0.95Si0.05O3−δ (△) and CaMn0.90Si0.10O3−δ (∇). |
As for the CaMn1−xSixO3−δ systems, the mixed Sr/Ca systems, SryCa1−yMn1−xSixO3−δ showed very low conductivities between 600 and 800 °C for the samples without Si (x = 0): 0.16–0.57 S cm−1, for Sr0.8Ca0.2MnO3−δ; 0.17–0.70 S cm−1, for Sr0.7Ca0.3MnO3−δ; and 1.7–3.4 S cm−1 for Sr0.5Ca0.5MnO3−δ. The low conductivities can be attributed to the lack of significant mixed valency, as well as the presence of poorly conducting hexagonal perovskite. In all doped compositions there is an improvement in conductivity, even for the Si-doped samples where complete conversion to the cubic perovskite has not occurred. The highest conductivity values were, however, reached for the samples which XRD showed were single phase cubic perovskites; i.e. x = 0.10 for Sr0.8Ca0.2Mn1−xSixO3−δ (23.1–26.1 S cm−1, between 600–800 °C) and x = 0.05 for Sr0.5Ca0.5Mn1−xSixO3−δ (31.5–36.3 S cm−1); and x = 0.075 for Sr0.7Ca0.3Mn1−xSixO3−δ (28.0–30.4 S cm−1). Fig. 6 shows the temperature dependence of the conductivity for Sr0.8Ca0.2Mn1−xSixO3−δ series. All other series show a similar behaviour.
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Fig. 6 Plot of log σ vs. 1000/T for Sr0.8Ca0.2MnO3−δ (□), Sr0.8Ca0.2Mn0.925Si0.075O3−δ (○), Sr0.8Ca0.2Mn0.9Si0.1O3−δ (Δ) and Sr0.8Ca0.2Mn0.875Si0.125O3−δ (∇). |
As shown previously,33 for the strontium endmember samples, SrMn1−xSixO3−δ, the undoped (x = 0) composition showed very low conductivities, 0.008–0.03 S cm−1 between 600–800 °C, while the Si doped samples for which a cubic perovskite was observed (x ≥ 0.15) showed much higher conductivities. The highest conductivity values were achieved for x = 0.15 (24.0–29.4 S cm−1 between 600–800 °C).
Overall the results from this work show a significant enhancement in the conductivity on Si doping, with the maximum conductivity for all series matching the composition with the minimum Si content that achieves the full stabilization of the cubic form. Increasing the Si contents beyond this amount led to lower conductivities, likely due to a partial disruption of the electronic conduction pathways by silicon at these high doping levels. This conclusion is consistent with the fact that maximum conductivity observed for these Si doped samples decreases in moving across the series from CaMnO3−δ to SrMnO3−δ, since for the latter end higher Si contents are necessary to stabilise the cubic perovskite and hence achieve this maximum.
In Fig. 7, we show the impedance spectra for the symmetrical cells with SrMnO3/CGO10 and SrMn0.85Si0.15O3−δ/CGΟ10 cathodes. The spectra can be decomposed into two overlapped contributions, a high frequency arc (assigned to the transport of O2− ions and intermediate species through the cathode and at the cathode–electrolyte interface), and a low frequency arc (assigned to the competitive reactions at the TPB: adsorption, transfer of species and surface diffusion).41 As can be seen, the two phenomena are much smaller for the Si-doped sample, which can be explained by the increase in electronic conductivity and likely also oxide ion conductivity (due to the generation of oxide ion vacancies caused by the oxyanion doping).
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Fig. 7 Impedance spectra of the symmetrical cells for SrMnO3 (□) and SrMn0.85Si0.15O3−δ (■)/CGO10 composites at 700 °C. The serial resistance was subtracted for better comparison of the spectra. |
The dependences of ASR with temperature are shown in Fig. 8 and Table 3. For all series an improvement in the ASR values was observed for the Si-doped samples with respect to the undoped compositions. For instance, for CaMn0.95Si0.05O3, Sr0.7Ca0.3Mn0.925Si0.075O3 and SrMn0.85Si0.15O3, the values obtained at 800 °C, were 0.35, 0.08 and 0.09 Ω cm2 respectively, and these results entail a significant improvement with respect to the corresponding samples without Si doping: 1.50, 0.11 and 0.20 Ω cm2 for CaMnO3, Sr0.7Ca0.3MnO3 and SrMnO3, respectively. We can see that there is a non-linear behaviour of the ASR data, with a bigger drop in the values at the higher temperatures. This behaviour is likely due to the greater loss of oxygen at high temperature, causing a higher amount of oxide vacancies and a better oxide ion mobility and ASR values. Thus, in this work we show that in addition to enhancing the conductivities, silicon doping has a positive effect on the ASR of the perovskite-CGO cathode composites. Overall the lowest ASR values were observed for the Sr rich systems, which may be related to improved oxide ion conduction in such systems as a result of the increase in cell size.
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Fig. 8 Plot of log(area-specific resistance (ASR)) vs. 1000/T for SrMnO3−δ (■), SrMn0.85Si0.15O3−δ (□), Sr0.8Ca0.2MnO3−δ (●), Sr0.8Ca0.2Mn0.90Si0.10O3−δ (○), CaMnO3−δ (▲) and CaMn0.95Si0.05O3−δ (Δ). |
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/c3dt32561j |
This journal is © The Royal Society of Chemistry 2013 |