Ohmin
Kwon
a,
Masaaki
Hirayama
a,
Kota
Suzuki
a,
Yuki
Kato
b,
Toshiya
Saito
b,
Masao
Yonemura
c,
Takashi
Kamiyama
c and
Ryoji
Kanno
*a
aDepartment of Electronic Chemistry, Interdisciplinary Graduate School of Science and Engineering, Tokyo Institute of Technology, 4259 Nagatsuta, Midori, Yokohama, Kanagawa 226-8502, Japan. E-mail: kanno@echem.titech.ac.jp; Fax: +81 45-924-5401; Tel: +81-45-924-5401
bBattery Research Division, Higashifuji Technical Center, Toyota Motor Corporation, 1200 Mishuku, Susono, Shizuoka 410-1193, Japan
cNeutron Science Laboratory, Institute of Materials Structure Science, High Energy Accelerator Research Organization (KEK), 1-1 Oho, Tsukuba, Ibaraki 305-0801, Japan
First published on 19th November 2014
A solid solution of the lithium superionic conductor Li10+δGe1+δP2−δS12 (0 ≤ δ ≤ 0.35) was synthesized and its structure and ionic conductivity were examined. The highest ionic conductivity value of 1.42 × 10−2 S cm−1 was obtained at 300 K with a sintered pellet of the sample having the highest solid solution lithium content of δ = 0.35. The Arrhenius conductivity curves obtained for this material exhibited a gradual change in slope over the temperature range of 193–373 K and the activation energy for ionic conduction decreased from 26 kJ mol−1 below 373 K to 7 kJ mol−1 above 573 K, which is typical of highly ionic conducting solids. The crystal structures of the solid solutions were determined using neutron diffraction, and conduction pathways were visualized through analysis by applying the maximum entropy method. The lithium distribution was found to disperse significantly throughout a one-dimensional conduction pathway as the temperature was increased from 4.8 K to 750 K. In addition, two-dimensional distribution of lithium along the ab plane became apparent at high temperatures, suggesting that the conduction mechanism changes from one-dimensional to three-dimensional with increasing temperature.
Although inorganic solid electrolytes offering extremely high lithium ionic conductivities have been developed, further studies clarifying the conduction mechanism and increasing the range of electrolyte materials are still necessary to allow the practical applications of these electrolytes. LGPS is known to have a three-dimensional framework structure composed of one-dimensional chains formed by Ge(P)S4 tetrahedra and LiS6 octahedra with edge sharing along the c direction of the tetragonal structure. These one-dimensional chains are connected with each other through PS4 octahedra by corner sharing. Within this framework structure, lithium occupies the tetrahedral sites along the c direction, and the results of neutron diffraction studies have suggested that this contributes to the ionic conduction process. Theoretical analyses based on first-principles calculations have indicated the presence of a two-dimensional conduction pathway through lithium in the octahedral coordination environment.7,8
Following the development of this LGPS-type parent structure having extremely high ionic conductivity,9–12 it was recognized that similar solid solution systems with different lithium contents might exhibit even higher levels of ionic conduction. In addition, cation and anion substitutions of the LGPS framework structure are also important means of achieving higher ionic conductivity values. In the present study, a solid solution with an LGPS-type structure was produced based on a powder synthesis process that offers a practical means of fabricating solid electrolytes. The composition and ionic conductivity of this new solid solution system, Li10+δGe1+δP2−δS12, were subsequently examined and the conduction mechanism within this material was studied using neutron diffraction analysis.
X-ray diffraction patterns of the powdered samples were obtained using an X-ray diffractometer (Rigaku, RAD, Ultima or Smart Lab) with CuKα radiation. The diffraction data were collected by applying a 0.02° step width over the 2θ range from 10° to 80°. Synchrotron X-ray diffraction measurements were performed at the BL02B2 beamline at Spring-8 in Japan, employing a Debye–Scherrer diffraction camera. Specimens were sealed in a quartz capillary (about 0.3 mm diameter) under vacuum. Diffraction data were collected in 0.01° steps over the 2θ range of 0° to 70.0°. The incident beam wavelength was calibrated using a NIST SRM Ceria 640b CeO2 and fixed at 0.59960 Å. Neutron diffraction data were obtained using time-of-flight (TOF) diffractometers: Super HRPD (BL08)13 and iMATERIA (BL20)13,14 at the Material and Life science Facility (MLF) of the Japan Proton Accelerator Research Complex (J-PARC). A 6 mm diameter vanadium cell was used and samples were sealed with an indium ring under Ar or He atmospheres. The diffraction data were collected for 12 h at several temperatures: Li10.5Ge1.5P1.5S12: 300 K, Li10.35Ge1.35P1.65S12: 4.8, 135, and 300 K, Li10.2Ge1.2P1.8S12: 300 K and Li10.05Ge1.05P1.95S12: 10, 135, 300, 450, and 750 K. Structural parameters were refined using the Rietveld refinement programs Z-Rietveld15 and RIETAN-FP16,17 for neutron and for high-flux synchrotron X-ray diffraction data, respectively. During neutron data analysis, the d region from 1.0 to 3.5 Å was used for the Rietveld analysis. The Z-MEM program was employed during calculations based on the maximum entropy method (MEM).18 Z-3D19 was used to visualize the nuclear density map of the structure.
![]() | ||
Fig. 2 (a) Impedance plots obtained for Li10+δGe1+δP2−δS12 (δ = 0.35) over a range of temperatures. (b) Arrhenius plots of the ionic conductivity values of Li10+δGe1+δP2−δS12 (δ = 0.05 and 0.35). |
When assessing the practical applicability of highly ionic conducting materials as solid electrolytes in all solid-state batteries, the conductivity of pressed pellets of the powdered samples is one of the most important parameters in terms of estimating the resistivity of composite electrodes and electrolytes. The ionic conductivity values of pressed powder samples were therefore measured at room temperature. The samples were each pressed under a pressure of 165 MPa and their conductivity values were determined using the AC impedance method. The impedance plots were each composed of a semi-circular region and a spike, corresponding respectively to the bulk/grain boundary and electrode contributions. In this respect, the plots were similar to those produced by sintered pellets and the conductivity values of the bulk/grain boundary are plotted as a function of the composition in Fig. 3. The conductivity values are seen to change with variations in the composition, and the highest ionic conductivity of 6.09 × 10−3 S cm−1 was obtained at a δ value of 0.35, corresponding to the sintered pellet composition that exhibited the highest conductivity. On the other hand, the ionic conductivity of δ = 0.50, which is expected to be the highest value, showed a lower value than that expected in the solid solution. This might originate from a small amount of impurities such as β-Li3PS4, although it is hardly detected by XRD.
![]() | ||
Fig. 3 (a) Dependence of room temperature ionic conductivities of pressed powder samples on composition. (b) Room temperature impedance plots obtained for powder samples. |
Model with a Li4 site | Model without a Li4 site | |
---|---|---|
R wp | 3.06% | 3.43% |
R p | 2.52% | 2.77% |
R e | 2.32% | 2.41% |
R b | 8.58% | 11.0% |
R F | 5.83% | 8.25% |
S 2 | 1.75 | 2.03 |
Atom | Site | g | x | y | z | U/Å2 |
---|---|---|---|---|---|---|
a Space group P42/nmc, a = 8.713023 (5) Å, c = 12.639695 (11) Å, Rwp = 3.06%, Rp = 2.52%. Note: the form of the anisotropic temperature factor is exp[−2p2(h2a*2U11 + k2b*2U22 + l2c*2U33 + 2hka*b*U11 + 2hla*c*U13 + 2klb*c*U23)]. | ||||||
Ge(1) | 4d | 0.675 (12) | 0 | 1/2 | 0.6885 (10) | 0.046 |
P(1) | 4d | 0.325 (12) | = x(Ge1) | = y(Ge1) | = z(Ge1) | = B(Ge1) |
Ge(2) | 2b | 0.00 (2) | 0 | 0 | 1/2 | 0.046 |
P(2) | 2b | 1.00 (2) | = x(Ge2) | = y(Ge2) | = z(Ge2) | = B(Ge2) |
S(1) | 8g | 1 | 0 | 0.1920 (2) | 0.4090 (2) | 0.046 |
S(2) | 8g | 1 | 0 | 0.2958 (2) | 0.0989 (2) | 0.048 |
S(3) | 8g | 1 | 0 | 0.7005 (3) | 0.7885 (2) | 0.035 |
Li(1) | 16h | 0.473 (11) | 0.2477 (9) | 0.2616 (13) | 0.2018 (11) | 0.108 |
Li(2) | 4d | 1 | 0 | 1/2 | 0.9524 (4) | 0.060 |
Li(3) | 8f | 0.75 (2) | = y(Li3) | 0.2463 (4) | 0 | 0.118 |
Li(4) | 4c | 0.77 (2) | 0 | 0 | 0.2585 (7) | 0.077 |
Atom | U 11/Å2 | U 22/Å2 | U 33/Å2 | U 12/Å2 | U 13/Å2 | U 23/Å2 |
---|---|---|---|---|---|---|
Ge(1) | 0.052 (10) | 0.044 (14) | 0.043 (13) | 0 | 0 | 0 |
P(1) | = U11(Ge1) | = U22(Ge1) | = U33(Ge1) | = U12(Ge1) | = U13(Ge1) | = U23(Ge1) |
Ge(2) | = U22(Ge2) | 0.038 (11) | 0.062 (3) | 0 | 0 | 0 |
P(2) | = U11(Ge2) | = U22(Ge2) | = U33(Ge2) | = U12(Ge2) | = U13(Ge2) | = U23(Ge2) |
S(1) | 0.078 (2) | 0.023 (2) | 0.038 (3) | 0 | 0 | 0.014 (10) |
S(2) | 0.055 (2) | 0.036 (2) | 0.052 (3) | 0 | 0 | −0.010 (10) |
S(3) | 0.044 (2) | 0.009 (2) | 0.052 (2) | 0 | 0 | 0.002 (2) |
Li(1) | 0.074 (8) | 0.050 (8) | 0.20 (2) | 0.019 | −0.097 (11) | −0.059 (11) |
Li(2) | 0.104 (4) | 0.051(6) | 0.024 (5) | 0 | 0 | 0 |
Li(3) | = U22(Li3) | 0.048 (5) | 0.259 (11) | −0.0335 (3) | = −U23(Li3) | −0.0929 (4) |
Li(4) | 0.026 (9) | 0.096 (11) | 0.108 (10) | 0 | 0 | 0 |
Fig. 5 provides the structure of Li10.35Ge1.35P1.65S12 (δ = 0.35) as determined in the present study. At δ = 0.35, the 4d site is occupied by Ge and P with a Ge/P ratio of 0.675/0.325. The framework of Li10GeP2S12 is composed of (Ge/P)S4 tetrahedra and Li2S6 octahedra in 4d sites, connected to one another by edge sharing. The one-dimensional connections between the Li1S4 and Li3S4 tetrahedra are located at the 16h and 8f sites, forming a one-dimensional tunnel along the c-axis. The Li4 site introduced in this study is located at the 4c site with a fractional coordinate (z ∼ 0.2585) and the Li4 is connected to six sulfide ions with distances of 2.5(Li4–S1), 2.7(Li4–S2), and 3.3 (Li4–S3) Å and is situated near the center of eight Li1 sites (see Fig. 5) with distances between the Li1 and Li4 sites being 3.2 (× 4) and 3.1 (× 4) Å. The Li4S6 octahedra are also connected to PS4 tetrahedra by edge sharing along the c direction and to four Li2S6 octahedra and two Ge1S4 tetrahedra by corner sharing.
![]() | ||
Fig. 6 The occupation parameter, g, at each Li site in Li10+δGe1+δP2−δS12 as a function of δ. The values at δ = 0.0 are taken from ref. 4. |
The temperature dependencies of the lattice parameters were assessed for the compositions in which δ = 0.05 and 0.35, based on synchrotron X-ray diffraction and neutron diffraction analyses. Fig. 7 shows the lattice parameter changes with temperature for both samples. The lattice parameters and the volume are seen to have increased with increasing temperature up to 750 K, although no significant phase changes were observed. Fig. 8 shows the temperature dependence of the occupation parameter, g, at each Li site in Li10.35Ge1.35P1.65S12 and Li10.05Ge1.05P1.95S12, as measured over the temperature ranges of 4.8–300 K and 10–750 K, respectively. For both compositions, the g value at the Li2 site was constant at 1.0 throughout the entire temperature range, indicating that the Li2 sites form a framework structure with the GeS4 and PS4 tetrahedra. In contrast, the g values of the Li1 and Li4 sites increased while that of the Li3 site decreased with increasing temperature. These slight changes in the occupation parameters with temperature may suggest that these sites contribute to the lithium ionic conduction. The g value of the Li3 site decreased and that of the Li1 site increased with increasing temperature, which corresponds to more highly disordered lithium distributions at higher temperatures. The temperature dependence of the total quantity of lithium ions in the unit cell was calculated by the MD simulation method23 and the occupation parameters and thermal evolution of these parameters were found to be quite consistent with those determined for the composition Li10.35Ge1.35P1.65S12 based on neutron diffraction data.
Fig. 9 shows the temperature dependence of the isotropic displacement parameter of each Li site in Li10.35Ge1.35P1.65S12 (δ = 0.35) and Li10.05Ge1.05P1.95S12 (δ = 0.05), as assessed over the temperature ranges of 4.8–300 K and 10–750 K, respectively. These isotropic displacement parameters were calculated from the final anisotropic displacement parameters. For both compositions, the B values at the Li2 site were lower than those of the other Li sites, indicating that the Li2 sites form the framework structure along with the GeS4 and PS4 tetrahedra.
The B values of the Li1 and Li3 sites increase with temperature from 4.8–10 K to 300 K and become almost constant above 300 K. These behaviors are consistent with the previous indications that these two sites participate in lithium ionic conduction within the structure. Higher B values at these Li1 and Li3 sites also suggest that these sites make a contribution to Li ion conduction. In contrast, the B value of the Li4 site increases from 10 to 300 K and becomes quite a high value at 750 K, and so the Li4 site is expected to play a significant role in ionic conduction at high temperatures.
Fig. 10 presents the temperature dependencies of the atomic distances between Li1 and Li1, and Li1 and Li3 for the compositions of Li10.35Ge1.35P1.65S12 (δ = 0.35) and Li10.05Ge1.05P1.95S12 (δ = 0.05). In the case of both compositions, the Li1–Li1 distances decrease and the Li1–Li3 distances increase with increasing temperature. The Li1–Li1 distance approaches 1.3 Å at 300 and 750 K for the δ = 0.05 and 0.35 materials, a value that is close to twice the Li+ ionic radius in tetrahedral coordination (0.59 Å),20 suggesting that these two Li sites are situated close to one another. The increase in the occupation parameter at the Li1 site and the decrease in the Li1–Li1 distance with increasing temperature point to an elevated extent of lithium disordering along these Li1 sites. The decrease in the g parameters at the Li3 sites and the increase in the Li4 and Li1 sites with an expansion of the Li1–Li3 distance might correspond to a lithium site change from the Li3 to the Li1 and Li4 sites. This result indicates that the conduction mechanism changes from a one-dimensional –Li1–Li3–Li1–Li1– pathway to a two-dimensional –Li1–Li4–Li1–Li1– pathway. However, the thermal parameters associated with the Li1 and Li3 sites are larger than those of the Li4 sites below 300 K, which may indicate that the one-dimensional conduction pathway is still dominant below room temperature.
![]() | ||
Fig. 10 Temperature dependencies of the atomic distances between Li1 and Li1, and Li1 and Li3 for the compositions Li10.35Ge1.35P1.65S12 (δ = 0.35) and Li10.05Ge1.05P1.95S12 (δ = 0.05). |
Lithium ion distribution was visualized using the MEM analysis in conjunction with the neutron diffraction data obtained for Li10.05Ge1.05P1.95S12 (δ = 0.05) (x = 0.65 in Li4−xGe1−xPxS4) at 100 and 750 K. Fig. 11 shows the atomic distribution in the unit cell, in which the probability of an atom being present is represented only for the negative scattering powers, which corresponds to the lithium ion distribution in the unit cell. These probabilities were calculated using an iso-surface level of 0.08 for the structure at both temperatures. At 100 K, the Li1, Li1, and Li3 sites are connected along the c-axis, while the other lithium sites (the Li2 and Li4 sites) are isolated from each other. This indicates that the one-dimensional conduction pathway represents the primary means of lithium ion conduction at 100 K. The one-dimensional conduction pathway along the c-axis becomes more evident at 750 K. In addition to the one-dimensional connection between the Li1, Li1, and Li3 sites, continuous lithium distribution between the Li1 and Li4 sites is also now observed. These results demonstrate that the lithium ion conduction takes on a three-dimensional character, as opposed to one-dimensional, at higher temperatures. The existence of three-dimensional ionic conduction at high temperatures is consistent with the observed atomic distribution and thermal parameter changes at each lithium site. Thus the LGPS-type structure is evidently well-suited to three-dimensional conduction. Even though one-dimensional conduction is dominant at lower temperatures, the conduction pathway associated with Li1 and Li4 sites over the ab plane becomes evident at high temperatures. These conduction behaviors are also consistent with the previously reported results of MD simulation studies.23 Isotropic ionic diffusion in a solid electrolyte is favorable in terms of practical application of the material in an all solid-state battery, since anisotropic ionic diffusion may prevent high ionic diffusion between the electrolyte and the electrode particles and thus reduce the ability of the solid-state cell to generate current. The LGPS structure is therefore suitable for practical applications, such as in all solid-state batteries.
Footnote |
† Electronic supplementary information (ESI) available. CCDC 1027666. For ESI and crystallographic data in CIF or other electronic format see DOI: 10.1039/c4ta05231e |
This journal is © The Royal Society of Chemistry 2015 |