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green emission at 550 nm originates from the deep level (DL) material may also be applied for the degradation of other
defect emission associated with oxygen vacancies in ZnO hazardous dyes found in industrial waste and dye contaminated
lattices.18 The blue emission may be from zinc ion vacancies and water. Further modications, like doping noble metals, which
interstitial zinc defects.19 The green-yellow emission is stronger may improve its photocatalytic activity, require further research.
in comparison with the blue emission. FTIR spectra of the as-
We would like to thank the Department of Science and
synthesized ZnO owers have broad bands around 3429 cmꢂ1 Technology, New Delhi for the nancial support (GPP-0267). We
and 1589 cmꢂ1, which are due to the surface adsorbed O–H are also grateful to Dr R. C. Boruah, Acting Director, Dr D. K.
stretching and bending mode of the vibration respectively Dutta, Chief Scientist, Dr Pinaki Sengupta, Head and Chief
(Fig. S2, ESI†). The sharp band at 419 cmꢂ1 is a characteristic Scientist, Materials Science Division and Mr Ananta Kr Sarma,
vibration mode of Zn–O bonding. The UV-Visible spectra of the Biotechnology Division, CSIR-North East Institute of Science
ZnO owers have a UV absorption peak at 388 nm and a very and Technology, Jorhat for their support.
broad visible absorption peak (Fig. S3, ESI†). The Brunauer–
Emmett–Teller (BET) specic surface area of the material
measured by a N2 adsorption–desorption technique is 26.94 m2
Notes and references
gꢂ1, with a hysteresis loop of type IV isotherm (Fig. S4, ESI†)
revealing the existence of mesopores in the architecture. The
corresponding pore diameter distribution curves (inset in
Fig. S4†) show that the size of the mesopores is not uniform but
hierarchically distributed, and we mainly attribute the larger size
of the mesopores to the explosive release of CO2 in the conned
space of the smaller mesopores during the thermal process. It is
reasonable that the release of CO2 and the collapse of the
interconnected mesopores enlarge and change the smaller
mesopores into the irregularly shaped larger mesopores.20
The synthesized ZnO owers were efficiently tested as an
excellent photocatalyst for the self sensitized photodegradation
of a cationic triphenylmethane dye, Malachite Green (MG),
under solar light. The amount of degradation of MG was almost
94% of the initial dye concentration of 0.2 g Lꢂ1 and the initial
catalyst amount was 0.02 g in 100 mL solution as shown in
Fig. 3.
The possible reason for its excellent photocatalytic activity
may be the high surface oxygen vacancies in the ZnO ower
conrmed from its room temperature photoluminescence
spectra. These high surface oxygen vacancies may allow it to
adsorb more O2 from the water resulting in the formation of a
greater number of reactive radicals like O2c, OHc which
contribute to its excellent photocatalytic activity.
Photodegradation of the dye leads to complete mineraliza-
tion under solar light which was conrmed by qualitatively
measuring the CO2 production using Warburg apparatus. The
Warburg manometric method is generally used for biological
samples to measure gas absorption as well as gas production.21
We took 4 mL of 0.2 g Lꢂ1 MG dye and 0.002 g catalyst initially
for the experiment. The evolved gas was conrmed to be CO2 as
a BaCO3 precipitate was formed by adding BaCl2 solution to the
KOH solution, removed from the centre wells of the Warburg
vessels, using CO2 free water.
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In summary, ower shaped homocentric pencil like ZnO
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8258 | RSC Adv., 2014, 4, 8256–8259
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