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ChemComm
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COMMUNICATION
ChemComm
3-6
DOI: 10.1039/C6CC04285F
confirmed that these probes are stable in various organic
solvents, yet sensitive to moisture content in organic solvents
and aqueous solutions. We monitored the time-dependent
fluorescence changes for the most efficient probes
4 and 6, and
found that they follow pseudo-first order kinetics as evidenced
from the single exponential decay. The kinetics study in buffer
solutions at various pH levels revealed that the hydrolysis of
and was remarkably enhanced in acidic solutions, in contrast
to basic solutions, not exhibiting catalytic effects. Thus, the
probe is expected to be an efficient potential fluorescent
moisture sensor at neutral or acidic pH. The experimentally
observed kinetics were rationalised by the analysis of the solid
state conformation in the crystal structure as well as pH
dependent theoretical calculations. The probe was further
determined to exhibit a limit of detection (LOD) and limit of
quantitation (LOQ) of 0.18% and 0.54% v/v water in DMSO.
Taken together these results indicate the strong potential of
Schiff base bearing fluorophores as highly sensitive water
sensors in organic solvents via a hydrolysis mechanism.
4
Fig. 6 (a) Fluorescence intensity at 536 nm and of
6 in DMSO with
6
increasing water content in the range of 0-10% (v/v) (b) linear fit of the
range (below 1.0% v/v). λex = 459 nm, data recorded after 800s of
equilibration.
6
In the first water addition step, the reactant complex (RC) of
4
shows two water molecules involved in an hydrogen bonding
network with the imine bonds. The RC of is similar to , but
6
4
shows an additional water molecule interacting with the
nitrogen atom of the pyridine ring through hydrogen bonding as
shown in the SI (Fig. S14, ESI†). The additional water
molecule in
6 plays a role as a blocking group, without which
the nitrogen atom of pyridine destroys the hydrogen bonding
network. Subsequently, the hemiaminal intermediate was
formed through a transition state (TS1) containing a 6-
membered ring as shown in Fig. S14, ESI†. Finally, the
intermediate dissociates into the final products, aldehyde and
amine, through the transition state (TS2) also containing a 6-
membered ring. The natural bond orbital (NBO) population
(charge) on the imine bond can be used as be a simple estimate
for the reactivity of the water addition. The atomic charges of C
and N of the imine bond were calculated to be 0.106e and -
This work was funded by CRI project (No. 2009-0081566,
J.S.K.)
and
the
Basic
Science
Research
Program
(2015R1A6A3A04058789, H.S.J.) from the National Research
Foundation of Korea (NRF) funded by the Ministry of Education as
well as a Korea University Grant (P.V.). The work at SKKU was
supported by Ministry of Science, ICT and Future Planning,
subjected project to the project EDISON (Education-research
Integration through Simulation On the Net, Grant No.
2012M3C1A6035359).
0.481e for
the water addition to the more positive carbon of
easier compared with . In acidic solutions, protonation at the
4
, and 0.123e and -0.519e for
6
, respectively. Thus,
6
would be
Notes and references
4
nitrogen atom of the imine bond can induce some charge
transfer from the carbon atom of the imine bond, making the
carbon more electron deficient, hence prone to water addition.
The atomic charges of C and N of the imine bond under these
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conditions were calculated to be 0.176e and -0.495e for
4, and
12191.
0.184e and -0.519e for , respectively. The protonation at N of
6
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the imine bond can also reduce the barrier by stabilizing the
accumulated negative charge at the nitrogen atom after water
addition. This charge redistribution is consistent with the
calculated activation barriers.
Finally, the performance of probe
6 in the determination of
the water content in DMSO solutions was assessed. Probe
6
was subjected to increased amounts of water in DMSO. Upon
excitation at 459 nm, the fluorescence at 536 nm was monitored
in the 0–10% v/v water in DMSO range (Fig. 6a). The probe
showed a good linear response in the 0–1% (v/v) range (Fig.
6b), allowing for the determination of the limit of detection
(LOD) and limit of quantitation (LOQ) as defined in equations
6 and 7, with
σ being the standard deviation of the blank and m
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the slope of the calibration curve (Fig. 6b):
2015, 6, 1127; (b) Z. Yang, M. She, J. Zhang, X. Chen, Y. Huang, H.
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LOD = 3.3휎
(6)
(7)
푚
LOQ = 10휎
푚
11. L. A. Carpino, J. Am. Chem. Soc., 1993, 115, 4397.
12. Gaussian 09 (Revision D.01). M. J. Frisch, et al. Gaussian, Inc.,
Wallingford CT, 2009.
Thus the LOD and the LOQ of
6 for water in DMSO were
determined to be 0.18% and 0.54% v/v demonstrating the
highly sensitive nature of this type of Schiff base bearing
fluorophores for the determination of moisture in organic
solvents.
4 | J. Name., 2012, 00, 1-3
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