Meng
Ge
a,
Taimin
Yang
a,
Yanzhi
Wang
b,
Francesco
Carraro
c,
Weibin
Liang
d,
Christian
Doonan
d,
Paolo
Falcaro
c,
Haoquan
Zheng
b,
Xiaodong
Zou
a and
Zhehao
Huang
*a
aDepartment of Materials and Environmental Chemistry, Stockholm University, Stockholm SE-106 91, Sweden. E-mail: zhehao.huang@mmk.su.se
bKey Laboratory of Applied Surface and Colloid Chemistry, Ministry of Education, School of Chemistry and Chemical Engineering, Shaanxi Normal University, Xi’an 710119, China
cInstitute of Physical and Theoretical Chemistry, Graz University of Technology, Stremayrgasse 9, 8010 Graz, Austria
dDepartment of Chemistry and the Centre for Advanced Nanomaterials, The University of Adelaide, Adelaide, 5005 South Australia, Australia
First published on 4th May 2021
Three-dimensional electron diffraction (3DED) has been proven as an effective and accurate method for structure determination of nano-sized crystals. In the past decade, the crystal structures of various new complex metal–organic frameworks (MOFs) have been revealed by 3DED, which has been the key to understand their properties. However, due to the design of transmission electron microscopes (TEMs), one drawback of 3DED experiments is the limited tilt range of goniometers, which often leads to incomplete 3DED data, particularly when the crystal symmetry is low. This drawback can be overcome by high throughput data collection using continuous rotation electron diffraction (cRED), where data from a large number of crystals can be collected and merged. Here, we investigate the effects of improving completeness on structural analysis of MOFs. We use ZIF-EC1, a zeolitic imidazolate framework (ZIF), as an example. ZIF-EC1 crystallizes in a monoclinic system with a plate-like morphology. cRED data of ZIF-EC1 with different completeness and resolution were analyzed. The data completeness increased to 92.0% by merging ten datasets. Although the structures could be solved from individual datasets with a completeness as low as 44.5% and refined to a high precision (better than 0.04 Å), we demonstrate that a high data completeness could improve the structural model, especially on the electrostatic potential map. We further discuss the strategy adopted during data merging. We also show that ZIF-EC1 doped with cobalt can act as an efficient electrocatalyst for oxygen reduction reactions.
Metal–organic frameworks (MOFs) or porous coordination polymers (PCPs) are a class of hybrid materials linking inorganic metal building units and organic ligands.26,27 The almost unlimited combination of inorganic and organic components has led to an ever-expanding family of MOFs with versatile structures and properties.28 However, due to the reversible coordination bonds, MOFs are sensitive to radiation damage by electron beam, which hampers their structural analysis using 3DED. This challenge has been tackled by the development of continuous rotation data collection, using one means a 3DED dataset can be acquired in less than a few minutes, with a dose rate lower than 0.1 e s−1 Å−2. The fast data collection minimizes loss of crystallinity due to beam damage, and consequently the quality of 3DED data, such as resolution, has been improved significantly.
Benefitting from continuous rotation electron diffraction, a growing number of MOF structures have been determined, with their unique properties revealed.29–38 However, the geometric constraints in a TEM impose a physical limitation on the tilt range on the goniometer. Even using a specialized tomography sample holder, 3DED data can be acquired only from −70° to +70°. The angular coverage of a maximum 140° represents ca. 78% sampling volume of reciprocal space, where the remaining 22% of reciprocal space is not accessible. In practice, the tilt range is lower than the maximum value due to the movement of the target crystal, and also overlaps the target crystal with other crystals or the TEM grid. The limited sampling therefore leads to incomplete 3DED data, known as the missing cone problem. The incomplete data could hinder an accurate structure determination, which is more severe for MOF crystals with low symmetry.
To solve this problem, Gruene et al. developed a specialized 3D TEM grid for 3DED data collection.39 As the data processing and structure determination using 3DED data are similar to those using SCXRD data, we present a strategy to improve data quality, particularly data completeness, by merging data from different individual crystals. We use ZIF-EC1 as an example to study the missing data problem. ZIF-EC1 was first discovered as a minor phase in a MOF mixture by continuous rotation electron diffraction (cRED). It crystallizes in a monoclinic space group P21/c with a = 13.462(2) Å, b = 14.659(3) Å, c = 14.449(2) Å, β = 118.12(1)°. The structure of ZIF-EC1 was first solved and refined using a single cRED data point obtained from a phase mixture, and then using merged data from nine crystals of its pure phase.40 Here we present a systematic study of the influence of data completeness on the structural analysis of ZIF-EC1. We show that data completeness can be improved after data merging. As each crystal has a different orientation and particle size, we further discuss the use of correlations of cRED intensity among different datasets, to choose the best combination to improve data quality. Moreover, merging of 3DED data is performed using different algorithms adapted from X-ray crystallography. We show that the structures could be solved and refined with high precision from individual datasets with a completeness as low as 44.5%. With increased data completeness, the structural model of ZIF-EC1 could be further improved, and peaks corresponding to atoms in the electrostatic potential map have well-defined isotropic shapes. By knowing the atomic structure and the underlying property, ZIF-EC1 was doped with cobalt and utilized as an electrocatalyst for the oxygen reduction reaction (ORR).
Dataset no. | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 |
---|---|---|---|---|---|---|---|---|---|---|
Group | A | A | A | A | B | B | C | C | D | D |
Rotation range (°) | 122.71 | 103.77 | 97.20 | 87.15 | 81.89 | 108.92 | 102.05 | 94.07 | 44.31 | 42.34 |
Tilting rate (° s−1) | 1.13 | 1.13 | 1.13 | 1.13 | 0.45 | 0.45 | 0.45 | 0.45 | 0.45 | 0.45 |
Collection time (s) | 108.3 | 91.7 | 86.1 | 77.7 | 181.0 | 239.5 | 223.7 | 208.5 | 97.7 | 93.6 |
Resolution (Å) | 0.70 | 0.78 | 0.75 | 0.74 | 0.76 | 0.78 | 0.93 | 0.92 | 1.21 | 1.00 |
Completeness (%) | 44.5 | 47.1 | 55.0 | 58.3 | 52.9 | 71.6 | 62.9 | 32.5 | 40.8 | 24.1 |
Dataset no. | 1 | M_A1 | M_A2 | M_A3 | 5 | M_B | 7 | M_C | M_BC | M_ABC | M_ABCD |
---|---|---|---|---|---|---|---|---|---|---|---|
Datasets used for merging | N/A | 1 & 2 | 1–3 | 1–4 | N/A | 5 & 6 | N/A | 7 & 8 | 5–8 | 1–8 | 1–10 |
a The structural model refined against dataset M_ABC was used as the reference to calculate the ADRA values. | |||||||||||
Completeness (%) | 44.5 | 71.5 | 75.5 | 81.4 | 53.5 | 85.0 | 62.9 | 63.3 | 87.0 | 89.1 | 92.0 |
Resolution (Å) | 0.78 | 0.78 | 0.78 | 0.78 | 0.78 | 0.78 | 0.93 | 0.93 | 0.78 | 0.78 | 0.78 |
No. of reflections (total) | 3935 | 9224 | 14352 | 19372 | 6502 | 16354 | 4958 | 7456 | 23817 | 43219 | 46079 |
No. of reflections (all unique) | 2189 | 3615 | 3848 | 4654 | 3132 | 4859 | 2088 | 2138 | 4976 | 5093 | 5262 |
No. of reflections (I > 2 sigma(I)) | 1495 | 2420 | 2845 | 3306 | 1874 | 3263 | 1221 | 1409 | 3345 | 3933 | 3669 |
R 1 (I > 2 sigma(I)) | 0.174 | 0.179 | 0.178 | 0.181 | 0.178 | 0.182 | 0.153 | 0.150 | 0.170 | 0.173 | 0.181 |
R 1 (all reflections) | 0.204 | 0.213 | 0.204 | 0.211 | 0.219 | 0.211 | 0.193 | 0.181 | 0.201 | 0.193 | 0.250 |
GooF | 1.564 | 1.486 | 1.542 | 1.544 | 1.870 | 1.442 | 1.321 | 1.409 | 1.450 | 1.676 | 1.530 |
ADRA (Å)a | 0.035 | 0.027 | 0.018 | 0.015 | 0.038 | 0.015 | 0.036 | 0.034 | 0.010 | 0 | 0.012 |
Fig. 1 (a) SEM image of ZIF-EC1 crystals. (b) The structural model of ZIF-EC1. Cyan tetrahedra: Zn atoms; red spheres: O atoms; blue spheres: N atoms; grey spheres: C atoms. |
To improve the overall data quality, XSCALE was applied for data merging. We performed systematic studies by merging a different number of datasets to study the influence of data completeness on the structural analysis of ZIF-EC1. We divided the ten datasets into four groups, collected under different tilting rates and/or with different resolutions. Group A includes four datasets 1–4 collected using a high tilting rate (1.13° s−1), all with high resolution (0.70–0.78 Å). The remaining datasets 5–10 were collected using a low tilting rate (0.45° s−1). The groups were in accordance with the data resolution: datasets 5–6 with 0.76–0.78 Å resolution belong to group B, datasets 7–8 with 0.92–0.93 Å resolution to group C, and datasets 9–10 with 1.00–1.21 Å resolution to group D. We first merged datasets in group A, which has completeness ranging from 44.5% to 58.3%. The data completeness was improved steadily from 44.5% of the single dataset 1 to 71.5, 75.5, and 81.4% for combining two (M_A1, merged dataset A1), three (M_A2), and four datasets (M_A3), respectively (Table 2). To investigate the relationship between data completeness and the structural model, we refined the structural model of ZIF-EC1 against the data merged from different numbers of cRED datasets. While the number of unique reflections increased significantly, from 2189 for a single dataset 1 to 4154 by merging four datasets, the R1 values are very similar, varying between 0.204 and 0.213. This indicates that all datasets have similar degrees in consistence with the structural models. The improvement can be easily visualized in the corresponding electrostatic potential maps (Fig. 3a–d and k–n). For those with high data completeness (75.5% for M_A2 and 81.4% for MA_3), the peaks appear more spherical with similar peak heights for the same atom types (Fig. 3d and n). In contrast, data with low completeness (44.5% for 1 and 62.6% for M_A1) resulted in either missing peaks with large variations in peak heights (Fig. 3a and k) or severe peak elongation (Fig. 3a, b, k and l). Because the electrostatic potential map is the basis of a structural model, distortion of the map leads to reduced reliability and accuracy of the atom coordinates and atomic displacement parameters. Therefore, even though a structural model can be obtained from a single dataset, it is vital to improve data completeness.
Furthermore, we applied data merging on datasets collected using a low tilting rate (groups B and C). The completeness increased significantly from 53.5% for single dataset 5 to 85.0% upon merging datasets 5 and 6 (M_B). However, there is little increase in data completeness for group C, when datasets 7 and 8 are merged (from 62.9% for 7 to 63.3% for M_B). The electrostatic potential maps present a significant improvement from single dataset 5 to M_B as the completeness is increased from 53.5 to 85.0% (Fig. 3f, g, p, and q). On the contrary, there is very limited improvement in the electrostatic potential maps from single dataset 7 to M_C, because the completeness was only increased by 0.4% (Fig. 3h, i, r, and s). Notably, merging the four datasets 5–8 in groups B and C (M_BC) led to improved completeness (87.0%), and the electrostatic potential map (Fig. 3j and t). Further merging all the aforementioned datasets 1–8 (M_ABC) resulted in the highest completeness (89.1%), and thus the best electrostatic potential map with most spherical peaks (Fig. 3e and o). The structural model refined against the dataset M_ABC is therefore used as a reference model, to which the atomic coordinates from the structural models obtained from datasets M_A3, M_B, M_C and M_BC were compared. It shows that with a low completeness, e.g. 63.3% for M_C, the corresponding structural model resulted in higher deviations on atomic positions, compared to those from other datasets with high completeness (Table 3). We further calculated the average deviation from reference atoms (ADRA)45 values to compare the different models (Table 2). The ADRA values decreased successively from 0.035 Å to 0.015 Å by merging more and more datasets in group A (M_A3). Improving completeness from 53.5 to 85.0% in group B (M_B) also led to decreasing ADRA values from 0.038 Å to 0.015 Å. On the other hand, the ADRA values showed little improvement by merging datasets 7 and 8 in group C (M_C), varying from 0.036 to 0.034 Å, with a completeness of 62.9 and 63.3%, respectively. Moreover, merging the four datasets 5–8 in groups B and C (87.0%, M_BC) led to a reduced ADRA value (0.010 Å). Fig. 4 shows a clear trend that the ADRA values are reduced with the increase of the data completeness as well as the increase in the number of unique reflections.
Atoms | M_A3 | M_B | M_C | M_BC |
---|---|---|---|---|
Zn1 | 0.004(3) | 0.005(4) | 0.028(7) | 0.005(3) |
Zn2 | 0.002(4) | 0.005(5) | 0.031(8) | 0.003(4) |
Zn3 | 0.004(5) | 0.006(4) | 0.015(7) | 0.006(4) |
N1 | 0.008(15) | 0.014(12) | 0.030(21) | 0.014(10) |
N2 | 0.019(17) | 0.014(10) | 0.014(14) | 0.013(13) |
N3 | 0.019(17) | 0.027(11) | 0.014(17) | 0.021(12) |
N4 | 0.001(17) | 0.014(14) | 0.051(19) | 0.006(13) |
N5 | 0.007(12) | 0.013(14) | 0.045(20) | 0.003(11) |
N6 | 0.012(13) | 0.017(11) | 0.048(21) | 0.008(11) |
N7 | 0.012(10) | 0.010(14) | 0.069(17) | 0.015(12) |
N8 | 0.011(15) | 0.015(15) | 0.037(16) | 0.005(16) |
N9 | 0.008(13) | 0.008(15) | 0.040(18) | 0.005(11) |
N10 | 0.019(16) | 0.015(10) | 0.033(16) | 0.006(11) |
O1 | 0.025(13) | 0.015(17) | 0.048(22) | 0.010(18) |
C1 | 0.012(11) | 0.024(14) | 0.040(18) | 0.004(11) |
C2 | 0.013(17) | 0.006(12) | 0.024(17) | 0.004(12) |
C3 | 0.020(13) | 0.020(9) | 0.033(21) | 0.020(10) |
C4 | 0.007(13) | 0.003(14) | 0.037(23) | 0.010(15) |
C5 | 0.009(17) | 0.019(13) | 0.017(28) | 0.015(13) |
C6 | 0.030(19) | 0.033(17) | 0.041(20) | 0.018(16) |
C7 | 0.032(19) | 0.031(14) | 0.053(17) | 0.027(18) |
C8 | 0.034(15) | 0.004(14) | 0.073(29) | 0.019(13) |
C9 | 0.025(16) | 0.003(18) | 0.030(18) | 0.007(17) |
C10 | 0.015(15) | 0.015(14) | 0.041(21) | 0.010(12) |
C11 | 0.007(20) | 0.016(15) | 0.025(21) | 0.013(14) |
C12 | 0.010(16) | 0.017(18) | 0.022(19) | 0.008(16) |
C13 | 0.022(17) | 0.012(15) | 0.017(16) | 0.014(14) |
C14 | 0.029(16) | 0.009(14) | 0.034(26) | 0.008(14) |
C15 | 0.019(20) | 0.045(14) | 0.030(23) | 0.015(13) |
C16 | 0.007(14) | 0.006(18) | 0.016(28) | 0.005(19) |
C17 | 0.008(21) | 0.006(14) | 0.030(20) | 0.005(13) |
C18 | 0.019(17) | 0.027(21) | 0.028(7) | 0.008(20) |
C19 | 0.025(21) | 0.015(20) | 0.031(8) | 0.012(19) |
C20 | 0.022(16) | 0.027(16) | 0.015(7) | 0.006(14) |
During data merging, correlation coefficients of the common reflection intensities (CCI) between two datasets are calculated by XSCALE, which indicate the degree of intensity similarity between the datasets (Table 4). The correlation among the datasets 1–8 are very high, as indicated by the CCI values (>0.95). In contrast, datasets 9 and 10 are rather poorly correlated with the other datasets with the CCI values are mostly below 0.80. Combining the additional datasets 9 and 10 to the merged dataset M_ABC increased the data completeness from 89.1% to 92.0%. However, this led to a significant increase of the R1 values for all reflections, from 0.193 to 0.250. On the other hand, very little change is observed in the electrostatic potential maps (Fig. 5), and the ADRA remains at a low value. This indicates that the structural models are very similar, and the increased R1 value mainly results from merging poorly correlated datasets. Therefore, there would be little benefit to add more datasets with low intensity correlations, after reasonable data completeness has already been reached.
Dataset no. | Dataset no. | No. of common reflections | CCI | Dataset no. | Dataset no. | No. of common reflections | CCI | |
---|---|---|---|---|---|---|---|---|
1 | 2 | 2077 | 0.973 | 3 | 8 | 1181 | 0.979 | |
1 | 3 | 1572 | 0.967 | 4 | 8 | 944 | 0.983 | |
2 | 3 | 1323 | 0.964 | 5 | 8 | 870 | 0.985 | |
1 | 4 | 2904 | 0.986 | 6 | 8 | 1305 | 0.982 | |
2 | 4 | 1783 | 0.975 | 7 | 8 | 867 | 0.982 | |
3 | 4 | 1274 | 0.981 | 1 | 9 | 536 | 0.695 | |
1 | 5 | 2096 | 0.972 | 2 | 9 | 398 | 0.660 | |
2 | 5 | 1018 | 0.961 | 3 | 9 | 359 | 0.783 | |
3 | 5 | 1220 | 0.991 | 4 | 9 | 432 | 0.617 | |
4 | 5 | 1620 | 0.988 | 5 | 9 | 221 | 0.684 | |
1 | 6 | 2463 | 0.953 | 6 | 9 | 346 | 0.456 | |
2 | 6 | 1663 | 0.978 | 7 | 9 | 193 | 0.927 | |
3 | 6 | 1606 | 0.952 | 8 | 9 | 218 | 0.772 | |
4 | 6 | 1999 | 0.981 | 1 | 10 | 580 | 0.826 | |
5 | 6 | 1962 | 0.962 | 2 | 10 | 508 | 0.775 | |
1 | 7 | 684 | 0.961 | 3 | 10 | 592 | 0.856 | |
2 | 7 | 898 | 0.977 | 4 | 10 | 477 | 0.556 | |
3 | 7 | 934 | 0.995 | 5 | 10 | 410 | 0.722 | |
4 | 7 | 504 | 0.954 | 6 | 10 | 475 | 0.748 | |
5 | 7 | 484 | 0.990 | 7 | 10 | 312 | 0.369 | |
6 | 7 | 747 | 0.975 | 8 | 10 | 406 | 0.449 | |
1 | 8 | 1317 | 0.967 | 9 | 10 | 141 | 0.948 | |
2 | 8 | 1642 | 0.974 |
Due to the development of a continuous rotation setup for collecting cRED data, software for X-ray crystallography can be easily used to process 3DED data. Thus, we investigate different algorithms of X-ray crystallography for data merging and evaluate the data quality. XSCALE, XPREP46 and AIMLESS47 are among the other programs that are commonly applied for merging datasets. We chose datasets 1–8 for merging because they have high correlation between each other. Using different algorithms for scaling and merging data, XSCALE, XPREP, and AIMLESS resulted in slightly different completeness of 89.1, 85.2, and 90.4%, respectively (Table 5). The R1 values are also similar (0.192–0.213), and the electrostatic potential maps exhibit well defined and spherical peaks (Fig. 6). Although using kinematical assumption, this indicates that different merging algorithms in X-ray crystallography programs can be used to process cRED data for high data completeness.
Software used for merging | XSCALE | XPREP | AIMLESS |
---|---|---|---|
No. of reflections (all unique) | 5093 | 5046 | 5116 |
Completeness (%) | 89.1 | 85.2 | 90.4 |
Resolution (Å) | 0.78 | 0.78 | 0.78 |
No. of reflections (I > 2 sigma(I)) | 3933 | 3964 | 3879 |
R 1 (I > 2 sigma(I)) | 0.172 | 0.193 | 0.187 |
R 1 (all reflections) | 0.192 | 0.210 | 0.213 |
GooF | 1.676 | 1.956 | 1.536 |
As 3DED revealed the accurate structure of ZIF-EC1, ZIF-EC1 has been utilized as a precursor to generate carbon materials for catalyzing electrochemical reactions due to its high density of metal ions.40 Here, we added Co(II) ions in the synthesis to further take advantage of the highly dense structure of ZIF-EC1, and use its pristine form for electrocatalytic oxygen reduction reaction (ORR). The electroactivity of ZIF-EC1(Zn,Co) was tested in 0.1 M KOH solution using the rotating disk electrode (RDE). The cyclic voltammetry (CV) data of ZIF-EC1(Zn,Co) showed that a strong electrocatalytic oxygen reduction peak near 0.74 V was observed in O2-saturated solution, while there was no reduction peak in an Ar-saturated solution (Fig. 7). Linear sweep voltammetry (LSV) further confirmed the good catalytic performance of ZIF-EC1, showing an onset potential (Eonset) of 0.85 V and a half-wave potential (E1/2) of 0.78 V. In addition, the electrocatalytic ORR limiting current density can reach 4.7 mA cm−2. The efficiency of ZIF-EC1(Zn,Co) for ORR is among one of the best MOF electrocatalysts in comparison with the others.48–51
Fig. 7 (a) CVs of ZIF-EC1(Zn,Co) catalyst in 0.1 M KOH in an Ar/O2-saturated solution. (b) LSV curves of ZIF-EC1(Zn,Co) catalyst in 0.1 M KOH in an O2-saturated solution at 1600 rpm. |
Footnote |
† CCDC The crystallographic data for the datasets 1, M_A1, M_A2, M_A3, 5, M_B, 7, M_C, M_BC, M_ABC and M_ABCD have been deposited at the Cambridge Crystallographic Data Centre (CCDC) under deposition number CCDC 2063943–2063953. For crystallographic data in CIF or other electronic format see DOI: 10.1039/d1fd00020a |
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