Construction of a Fluorescence/Phase-Change Dual-Mode Sensor Based on Carbon Dots/Poly(acrylic acid) for Highly Selective and Sensitive Detection of Ferric Ions
Yao Zhou, Huidong Li, Junqi Gu, Ying Fu, Jingchun Liu, Zhaoyang Li, Xinlong Li, Xunyong Liu, Zhuhui Qiao, Yi Liu
Abstract
Fe 3+ is one of the crucial metal ions in biological systems, and its excess or deficiency in the body can trigger various diseases, posing a serious threat to human health. Moreover, improper handling or disposal of Fe 3+ can lead to water pollution, thereby harming the environment. Therefore, the development of highly selective and sensitive Fe 3+ detection probes is particularly urgent. In this paper, a dual-mode sensor based on sol–gel and fluorescence signal responses was developed for the visual detection of Fe 3+ . The visual sensing method based on the simultaneous response of Fe 3+ -triggered dual signals can minimize the interference from false-positive signals and enhance detection accuracy. The dual-mode sensor, denoted as PAA@CDs, was constructed by incorporating high-brightness (high fluorescence emission intensity) green-yellow carbon dots (CDs) into poly(acrylic acid) (PAA), which possesses a large number of carboxyl functional groups. Based on the interaction of Fe 3+ with the surface functional groups of CDs, nonfluorescent complexes are formed, leading to nonradiative electron transfer, which induces fluorescence quenching and produces a fluorescence signal visible to the naked eye. Additionally, the interaction of Fe 3+ with the carboxyl groups of PAA triggers the cross-linking of PAA, causing a sol–gel phase change signal. Consequently, the PAA@CDs exhibit a dual-response signal in Fe 3+ detection. Based on the fluorescence method, the linear detection range of PAA@CDs for Fe 3+ is 0.05–2.60 mM with a limit of detection (LOD) of 5.14 μM. Meanwhile, using the sol–gel method, the linear detection range is 0.02–2.20 mM, and the LOD is 42.5 μM. Furthermore, the PAA@CDs probes can be successfully applied to the detection of Fe 3+ in real water samples, demonstrating their potential value in the analysis of real samples containing multiple ions.