Peng Zhang,
Xiaobai Wang,
Wei Wang,
Xiang Lei and
Hua Yang*
College of Chemistry, Jilin University, Changchun, 130012, China. E-mail: huayang86@sina.com
First published on 13th February 2015
Single-phase Fe4N and Fe3C have been controllably synthesized from a coordination precursor by adjusting the molar ratio of hexamethylenetetramine to ferric chloride hexahydrate, both presenting good paramagnetic behavior, with maximum magnetizations that can reach 150.51 and 53.03 emu g−1 up to 17.5 kOe, respectively. The magnetic properties of Fe3C can be adjusted by the molar ratio of hexamethylenetetramine. Moreover, the structure, components and the possible mechanism were investigated carefully.
Herein, we demonstrated a flexible route for the controllable preparation of Fe3C and Fe4N by adjusting the molar ratio of HMTA to ferric chloride hexahydrate. The morphology, structure, the possible mechanisms and magnetic properties were also investigated carefully.
A further increase gradually brings in enough carbon to fabricate Fe3C, inducing the single-phase Fe3C at a proper ratio. However after the formation of the Fe3C structure, the excessive HMTA takes no effort to change the product species, only supplying a mass amorphous carbon matrix around the Fe3C.
Based on the XRD patterns, we proposed a possible mechanism of Fe4N and Fe3C. It is well-known that most methods to produce nitrides are based on thermal decomposition under nitrogen or an ammonolysis step with or without ammonia,14 which is also applicable to our study to some degree. As discussed in another study,10 gelatin releases ammonia to realize the nitridation process. This implies that the nitrogen gas not only provides protection from oxidation, but also suppresses the decomposition of ammonia at a high temperature range. Thus, nitrogen gas is necessary to realize the whole reaction. Previous studies show that the FeCl3·NH3 adduct is the ideal precursor of iron nitride. We believe that the HMTA will form a similar coordinate adduct with FeCl3·H2O, where a lone pair electrons from the nitrogen atom in HMTA can interact and coordinate with the Fe3+ cations. To support our proposed mechanism, UV-vis absorption spectra were ascertained to confirm the presence of a solid coordination precursor. Compared to the UV-vis absorption spectrum of ferric chloride hexahydrate, the precursors prepared from the increasing concentration of HMTA with constant FeCl3 show different UV-vis absorptions to support the presence of a new product, based on the ligand field theory. Interestingly, the decrease, and even disappearance of the absorption intensity and a gradual negative shift at around 412 nm and 480 nm, with an increasing concentration of HMTA with constant FeCl3, demonstrated the point that the Fe3+ cations are coordinated with nitrogen atoms in HMTA by UV-vis spectra, verifying our mechanism above and the different compositions of precursors (Fig. 2).
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Fig. 2 UV-vis absorption spectra of the precursors prepared with an increasing concentration of HMTA and constant FeCl3. |
If the HMTA is limited, the nitridation keeps the dominant role in the preparation of cubic Fe4N, due to the stronger interaction between the iron and nitrogen atoms. Noticeably, trace crystal water still exists, because the unsaturated Fe3+ orbits are occupied to keep stable, forming ferrite after calcination, when the amount of HMTA is rather small. Based on the results that the anhydrous ferric chloride will form Fe3N via a similar route, we believe the presence of crystal water is important for the crystallization of Fe4N, although the further mechanism is still unknown. The extra HMTA then enhances the reduction properties, resulting in the appearance of Fe. Besides, the metastability of Fe4N promotes the process mentioned above. We believe this reaction may be instant, due to the good dispersion and instability of nano-Fe4N. The further increasing HMTA will introduce the carbonization from nano-Fe to Fe3C, finally realizing the fabrication of Fe3C. As with Fe synthesis, the carbonization process will be at a high rate when the ratio of ferric chloride to HMTA is greater than 1:
1.5. Due to the excellent chemical stability, the excessive carbon cannot reduce the Fe3C or prepare other kinds of iron carbides by deep carbonization. Of note is that both Fe4N and α-Fe are the intermediates and precursors to Fe3C, analyzed from the reaction process. Thus, only by controlling the precious molar ratio of ferric chloride to HMTA, can Fe4N and α-Fe survive in the products.
The morphology of Fe4N and Fe3C was investigated by HRTEM (see Fig. 3). Both Fe4N and Fe3C are encapsulated by a mass amorphous carbon matrix, showing irregular particles with a large range of sizes. The lattice fringe spacing of 0.22 nm can be well index to the d (lattice plane distance) value of the (111) crystal plane of Fe4N in Fig. 3(D). It can be observed that the morphology shows more or less visible sharp edges, which can be ascribed to the particle coalescence. This sharp morphology depends on the distance between particles, ramping and the local temperature, according to a previous study.15 Noticeably, the carbon matrix surrounding Fe3C shows a graphite shell with an average thickness of 7 nm, as shown in Fig. 3(G), which is in agreement that the Fe3C can promote the formation of graphite. Besides, the d values of 0.34 and 0.21 nm can be indexed to the graphite and Fe3C in Fig. 3(H), respectively, supporting the presence of graphite and Fe3C. It is noted that the carbon grows with an increase of HMTA (Fig. 4).
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Fig. 3 (A)–(D) are HRTEM images of Fe4N at different scales; (E)–(H) are HRTEM images of Fe3C prepared at a ratio of 1![]() ![]() |
To investigate the component of the products, thermal gravimetric (TG) analysis was introduced to evaluate the carbon content in Fe4N and Fe3C, in which the consequently iron element transfers into Fe2O3. The calculated carbon contents of different ratios are 16.96%, 67.83%, 84.32% and 89.36%, corresponding to the weight loss of 111.72%, 42.89%, 20.90% and 14.19%, as shown in Fig. 4. It is noticed that the carbon contains graphitic carbon, which has a large impact on the magnetic stability and property by reducing the random flipping of the magnetic moments, which result from thermal fluctuations16 and can be measured by Raman spectra, as shown in Fig. 5. The peaks at around 1350 and 1590 cm−1, can be indexed to the D- and G- bands of carbon, respectively.17–19 The proportions of ID/IG are 1.17, 1.22, 1.35 and 1.39, indicating the HMTA ratio has an important impact on the graphite degree of the carbon matrix.20 The intensity of ID/IG for the Fe3C samples enhances with an increase in the molar ratio of HMTA, implying the decreasing degree of graphite. It can be easily understood that the catalytic activity of Fe3C may promote the surrounding amorphous carbon to form the graphite structure, which is confirmed in the HRTEM images. When excessive HMTA is added into the reaction system, more carbon is formed after the calcination process. However, only the carbon surrounding the surface of as-synthesized Fe3C forms graphitic carbon, leading to the increasing ID/IG value. Interestingly, the value of ID/IG for Fe4N is much smaller than Fe3C, which has been confirmed the catalytic property to graphite and carbon nanotube, implying a better graphite degree. However, the distinguished graphite structure is not observed in the HRTEM images. We suppose that the high graphitic degree is assigned to the synergic effect of low carbon content caused by the limited ratio of HMTA and crystallization of Fe4N. As distinguishable graphite has not been observed in the HRTEM images, the catalytic activity of Fe4N to graphite cannot be confirmed.
The magnetic hysteresis loops of Fe4N and Fe3C were measured on the vibrating sample magnetometer (VSM). It is obvious that Fe4N shows good soft magnetic and paramagnetic behaviors with a maximum magnetization of 150.51 emu g−1 up to 17.5 kOe (Fig. 6 and Table 1). The rather low squareness of 2.53% (maximum magnetization/retentivity) broaden the physical application of Fe4N as a soft magnetic material. The superior maximum magnetization and trace retentivity and coercivity can be assigned to the positive crystallization degree of Fe4N and a little carbon matrix left in the product. While, the Fe3C also shows paramagnetism, with maximum magnetizations that can reach 53.03, 29.47 and 12.22 emu g−1 up to 17.5 kOe as the HMTA ratio increases. The other magnetic parameters are listed in Table 1. It should be noted that, the as-synthesized Fe3C presents some coercivity and retentivity, which is very different from that of Fe4N. The unexpected coercivity and retentivity can be due to the interference of the carbon matrix, leading to magnetic exchange coupling behavior from the insulation of amorphous carbon, which is commonly reported in magnetic material synthesis. Due to the increasing content and impact of the carbon matrix from an increased amount of HMTA, both squareness and coercivity increase sharply, as shown in Table 1. The carbon matrix contributes to the decreasing value of maximum magnetization of Fe3C (much lower than the theoretical value of 120 emu g−1), due to the mass remainder from increasing HMTA carbonization. As a result, the magnetic properties of Fe3C particles can be controlled by adjusting the amount of HMTA added. Furthermore, the carbon matrix prevents Fe4N and Fe3C from oxidation and corrosion.
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Fig. 6 The magnetic hysteresis loops of Fe4N and Fe3C prepared from different ratios of FeCl3 to HMTA. The inset is the local magnification with the applied field between −0.4 and 0.4 kOe. |
Ratio | Saturation magnetism (emu g−1) | Retentivity (MR, emu g−1) | Coercivity (HC, Oe) |
---|---|---|---|
1![]() ![]() |
150.51 | 3.81 | 43.36 |
1![]() ![]() |
53.03 | 5.91 | 274.30 |
1![]() ![]() |
29.47 | 4.56 | 318.39 |
1![]() ![]() |
16.24 | 3.12 | 324.68 |
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/c5ra00336a |
This journal is © The Royal Society of Chemistry 2015 |