26
L. Chen et al. / Inorganica Chimica Acta 446 (2016) 24–31
d (ppm): 11.4, 14.7, 22.0, 41.3, 52.6, 114.8, 120.1, 121.4, 122.2, 123.7,
124.8, 127.7, 128.5, 130.1, 133.6, 142.5, 150.1, 151.7, 152.9, 158.5.
MS m/z: [m+1]+ calc. for C29H33N5O5Si, 559.2; found, 560.4.
Ru(bpy)2Cl2 was obtained using a literature procedure [11,12].
Below chemicals were added into a flask and heated at 110 °C for
a whole day under N2 atmosphere, including RuCl3ꢀnH2O (5 mmol),
bpy (11 mmol) and redistilled DMF (35 mL). Solvent was then
extracted by rotary evaporation. Solid residue was dispersed in
acetone (70 mL). The remaining solid sample was mixed with etha-
nol (100 mL) and water (100 mL) and heated at 85 °C for 5 h under
N2 atmosphere. Later, anhydrous LiCl (100 g) was added under stir-
ring. Ethanol was extracted by rotary evaporation. The remaining
solution was cooled in refrigerator for 10 h. Crude product was
recrystallized in mixed solvent ethanol:water (V:V = 1:1) and dried
in vacuum at 120 °C for 2 days. MS m/z: [m]+ calc. for C20H16N4-
RuCl2, 484.0; found, 484.4.
to ꢃ260 nm. Its surface is obviously smoothed, but aggregation
between SiO2@Fe3O4 particles is still obvious, which means that
this thin SiO2 layer is effective on modifying particle surface but
limited in decreasing magnetic attraction. After MCM-41 construc-
tion and probe loading procedures, diameter of Ru-Phen@MCM-
41@Fe3O4 is finally increased to 370 nm, with smooth surface
and nearly monodispersal. Its TEM image shown in Fig. 1 indicates
a clear core–shell structure in it. It is thus confirmed that MCM-41
layer has successfully blocked magnetic aggregation between these
particles, showing a good dispersal. MCM-41 layer thickness is
determined as ꢃ55 nm which is slightly smaller than literature
values [17,18]. We assume that these short MCM-41 tunnels may
favor oxygen sensing by decreasing the number of ‘‘dead-sites”
which are inaccessible to O2 diffusion, giving improved sensitivity
and fast response.
3.2. Superamagnetic feature of Ru-Phen@MCM-41@Fe3O4
2.3. Construction of SiO2@Fe3O4
In our target structure, magnetic core is designed for site-speci-
fic aggregation. Magnetic response of Ru-Phen@MCM-41@Fe3O4 is
thus analyzed to evaluate its potential for site-specific aggregation.
That of Fe3O4 core is shown in Fig. 2 for comparison. It is observed
that our as-synthesized Fe3O4 core follows superamagnetic behav-
ior, showing no hysteresis. Such superamagnetic nature enables it
either to be aggregated to a specific-site in the presence of a mag-
net or to be highly dispersed in the absence of external magnetic
field. Saturate magnetization value of our Fe3O4 core is measured
as 67.1 emu gꢁ1. This value is slightly lower than literature values
which can be explained by the small size of our Fe3O4 particles
[17,18]. Literatures have suggested that Fe3O4 particles larger than
30 nm are supposed to follow magnetic behavior instead of supera-
magnetic one [19]. In this work, however, superamagnetic behav-
ior is still observed from our as-synthesized Fe3O4 particles even
though their diameter is as wide as 250 nm. Considering the bulges
and graves on their surface, we assume that each visible Fe3O4 par-
ticle is actually composed of sub-particles smaller than 30 nm. As
for Ru-Phen@MCM-41@Fe3O4, silica encapsulation and MCM-41
growth decrease its saturate magnetization value to 51.3 emu gꢁ1
with its superamagnetic behavior well preserved. This decreased
superamagnetic behavior is still strong enough for site-specific
aggregation [17,18].
Precursor for magnetic supporting matrix SiO2@Fe3O4 was con-
structed following below procedure [17,18]. Glycol (15 mL), SDS
(0.2 g), NaAc (1.5 g) and FeCl3ꢀ6H2O (0.5 g) were mixed together
and stirred at room temperature for 30 min. This mixture was
sealed into a Teflon reaction kettle and heated at 200 °C for 12 h.
The resulting solid sample was washed with deionized water, re-
dispersed in ethanol (40 mL) and exposed to ultrasonic bath for
30 min. During this time, deionized water (40 mL), TEOS (0.5 g)
and NH3ꢀH2O (2 mL) were slowly added. This mixture was allowed
to react at room temperature for 6 h, giving SiO2@Fe3O4.
2.4. Construction of Ru-Phen@MCM-41@Fe3O4 and a reference sample
Our site-specific oxygen sensing composite (Ru-Phen@MCM-
41@Fe3O4) was constructed following below procedure. First,
MCM-41 was grew onto SiO2@Fe3O4 surface with TEOS and
Phen-Si as silica source. SiO2@Fe3O4 (0.5 g), TEOS (1.5 g), Phen-Si
(0.12 g), CTAB (0.5 g), deionized water (150 mL) and NH3ꢀH2O
(3 mL) were mixed together and allowed to react at room temper-
ature for 6 h. The resulting solid product was collected and stirred
in ethanol (200 mL) and concentrated HCl (10 mL) for 2 days to
remove template reagent CTAB. Then this product was mixed with
Ru(bpy)2Cl2 (0.5 g, excess) and ethanol (50 mL), and allowed to
react at 80 °C for 8 h. The final solid product was collected, washed
with ethanol and dried in vacuum to give Ru-Phen@MCM-
41@Fe3O4 as pale dark powder. Yield (0.4 g). Elemental analysis
for Ru-Phen@MCM-41@Fe3O4, found: C, 6.28, H, 1.22, N, 1.07%.
A similar procedure was carried out except that no Phen-Si was
used in this run, giving a reference sample, so that performance
comparison between this reference sample and Ru-Phen@MCM-
41@Fe3O4 could be performed.
3.3. XRD pattern of Ru-Phen@MCM-41@Fe3O4
The Fe3O4 core in Ru-Phen@MCM-41@Fe3O4 is further analyzed
and confirmed by its wide angle XRD (WAXRD) pattern, as shown
in Fig. 3A. That of our as-synthesized Fe3O4 particles is shown for
comparison. Six well-resolved diffraction peaks are observed for
our as-synthesized Fe3O4 particles, which are indexed as (220),
(311), (400), (422), (551), (440), respectively. After consulting
literature reports, we come to a conclusion that Fe3O4 core has
been successfully constructed [17,18]. Diameter of these Fe3O4 par-
ticles is calculated as 14.78 nm using Scherrer equation, which
confirms our hypothesis that each visible Fe3O4 particle is actually
composed of sub-particles smaller than 30 nm [17,18]. As for
Ru-Phen@MCM-41@Fe3O4, these six diffraction peaks are still
observed, which means that the Fe3O4 core has been well pre-
served after a sires procedures of silica encapsulation, MCM-41
growth and probe loading. On the other hand, their diffraction
intensity is slightly decreased, which should be explained by the
fact that above modification procedures actually decrease regular-
ity of Fe3O4 core.
3. Results and discussion
3.1. Morphology of Ru-Phen@MCM-41@Fe3O4
Scanning electron microscope (SEM) and transmission electron
microscope (TEM) images of Ru-Phen@MCM-41@Fe3O4 are shown
in Fig. 1 to get a visual understanding on its morphology. SEM
images of Fe3O4 core and SiO2@Fe3O4 are shown in Fig. 1 as well
for comparison. Owing to its magnetic nature, Fe3O4 particles are
intensively aggregated with bad dispersal. These particles are gen-
erally spherical ones with mean diameter of ꢃ250 nm which is
slightly smaller than literature values [17,18]. Their surface, how-
ever, is rather rough with multiple bulges and graves. As for
SiO2@Fe3O4, silica encapsulation procedure increases its diameter
For a tentative investigation on the mesoporous tunnels on
Ru-Phen@MCM-41@Fe3O4 surface, its small angle XRD (SAXRD)
pattern is measured and shown as Fig. 3B. That of a reference sam-
ple is shown for comparison. The reference sample exhibits a sharp