D.B. Jiang et al.
Journal of Physics and Chemistry of Solids 112 (2018) 209–215
absorption wavelength of 617 nm.
3. Results and discussion
3.1. Structure and morphology of double-shell Fe2O3
The typical X-ray diffraction (XRD) patterns of the diatomite@FeOOH
and double-shell hollow Fe2O3 are shown in Fig. 1. It can be seen from
Fig. 1a that the diffraction peaks at 2θ of 21.9ꢀ, 28.4ꢀ, 31.4ꢀ, and 36.0ꢀ
are in good agreement with the standard pattern of the SiO2 phase
(JCPDS card no. 39-1425), corresponding to (101), (111), (102), and
(200) planes. The other diffraction peaks at 26.7ꢀ, 33.1ꢀ and 53.9ꢀ are in
clear accordance with the standard pattern of the goethite phase (JCPDS
card no. 29-0713), corresponding to (120), (130) and (221) planes. In
Fig. 1b, diffraction peaks of (012), (104), (110), (113), (024), (116),
(214) and (300) are well indexed to the hematite phase (JCPDS card no.
33-0664), and the characteristic peaks of the SiO2 disappear completely.
This suggests that SiO2 was etched completely and the FeOOH was
transformed to Fe2O3.
Fig. 2a confirms the presence of FeOOH on the surface of the diato-
mite. The spectrum of diatomite@FeOOH exhibits a broad stretch at
Fig. 2. FT-IR spectra of (a) diatomite@FeOOH and (b) double-shell hollow Fe2O3.
3453 cmꢁ1 and 1644 cmꢁ1 that corresponds to O H stretching and
–
bending vibrations, respectively. The characteristic sharp peak at
hollow structure of the pure Fe2O3 was obtained by etching the hollow
shell of diatomite while replicating its morphology. Furthermore, the
collapse of the broken structure in Figs. 3c and 1S confirms that the
hollow structure has a double-shell. The detailed elemental composition
mapping of double-shell hollow Fe2O3, as shown in Fig. 3e and f, reveal
that the Fe and O signals have similar shapes, further confirming the
uniform distribution of the double-shell hollow Fe2O3 nanosheets. In
addition, it can be observed that the double-shell hollow Fe2O3 has the
same nanosheet morphology as the FeOOH, suggesting that double-shell
hollow Fe2O3 has high specific area and porosity, which is beneficial for
their application in wastewater treatments.
1094 cmꢁ1 is assigned to the asymmetric stretching vibration of
– – – –
O Si [21]. The bending vibration of O Si O group appears at
477 cmꢁ1 [22].
Si
As shown in Fig. 2b, after the etching process, the peaks of the
– – – –
bration disappear. Meanwhile, the new bands at 551 cmꢁ1 and 470 cmꢁ1
Si
O Si asymmetric stretching vibration and O Si O bending vi-
–
appear, which corresponds to the vibration of Fe O group in Fe2O3
[23,24]. This result suggests that the synthesized material is pure Fe2O3
after the etching process, which is also consistent with the XRD
characterization.
Fig. 3 illustrates the morphology and structure of the diatom-
ite@FeOOH and double-shell hollow Fe2O3 examined by FIB/SEM. As
shown in Fig. 3a, the detailed surface image of the FeOOH nanosheets,
template-engaged redox etched from the MnO2 nanosheets, shows good
replication of the structure of diatomite@ MnO2 [25], and it can be
observed from Fig. 3b that the abundant ultrathin FeOOH nanosheets are
well coated on the diatomite and interconnected to each other, forming a
highly uniform surface morphology. Fig. 3c and d shows the SEM images
of double-shell hollow Fe2O3, indicating that double-shell hollow Fe2O3
sustains the framework of the diatomite@FeOOH. The double-shell
The nitrogen adsorptionꢁdesorption isotherm and Bar-
rettꢁJoynerꢁHalenda (BJH) were employed to determine the pore-size
distribution of diatomite@FeOOH and double-shell hollow Fe2O3.
Fig. 4a shows that diatomite@FeOOH and double-shell hollow Fe2O3
both exhibit an isotherm of type IV. The isotherm of double-shell hollow
Fe2O3 has
a sharp inflection at a relative pressure around P/
P0 ¼ 0.50–1.0, which suggests the double-shell hollow Fe2O3 is a typical
mesoporous material [26]. The hysteresis loop (Type H3) in the isotherm
of double-shell hollow Fe2O3 was caused by the slit-shaped pores
resulting from aggregates of plate-like particles, suggesting the existence
of nanosheet-like morphology. After etching the diatomite, the observed
BET surface area and pore volume of double-shell hollow Fe2O3 increased
from 22.12 m2/g and 0.077 cm3/g to 47.64 m2/g and 0.215 cm3/g,
respectively. The corresponding pore size distribution curves, shown in
Fig. 4b, display the same broad pore size distribution of diatom-
ite@FeOOH and double-shell hollow Fe2O3, which proves that
double-shell hollow Fe2O3 replicated the FeOOH nanosheet structure
[27]. The hollow and mesoporous structures favour the promotion of the
catalytic degradation efficiency.
3.2. Photo-Fenton degradation of MG by double-shell hollow Fe2O3
Fig. 5 reports the degradation efficiency of MG by using the double-
shell hollow Fe2O3 catalyst. As shown in Fig. 5a, under visible light
irradiation, when only double-shell hollow Fe2O3 or only H2O2 was used
as a catalyst, the degradation efficiency of MG is less than 10% in 60 min.
When both the double-shell hollow Fe2O3 and H2O2, were used in the
dark, the degradation efficiency of MG increased approximately to
43.7%, indicating that the Fenton system has a certain degradation ca-
pacity for MG. However, under the double-shell hollow Fe2O3/H2O2/vis
system, the degradation rate of MG remarkably increased to 99.9% in
60 min, which demonstrates the remarkable synergetic effect of the
Fig. 1. XRD patterns of (a) diatomite@FeOOH and (b) double-shell hollow Fe2O3.
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