| Literature DB >> 30228278 |
Laura Ascherl1, Emrys W Evans2, Matthias Hennemann3, Daniele Di Nuzzo2, Alexander G Hufnagel1, Michael Beetz1, Richard H Friend2, Timothy Clark3, Thomas Bein4, Florian Auras5.
Abstract
Covalent organic frameworks (COFs) are an emerging class of highly tuneable crystalline, porous materials. Here we report the first COFs that change their electronic structure reversibly depending on the surrounding atmosphere. These COFs can act as solid-state supramolecular solvatochromic sensors that show a strong colour change when exposed to humidity or solvent vapours, dependent on vapour concentration and solvent polarity. The excellent accessibility of the pores in vertically oriented films results in ultrafast response times below 200 ms, outperforming commercially available humidity sensors by more than an order of magnitude. Employing a solvatochromic COF film as a vapour-sensitive light filter, we demonstrate a fast humidity sensor with full reversibility and stability over at least 4000 cycles. Considering their immense chemical diversity and modular design, COFs with fine-tuned solvatochromic properties could broaden the range of possible applications for these materials in sensing and optoelectronics.Entities:
Year: 2018 PMID: 30228278 PMCID: PMC6143592 DOI: 10.1038/s41467-018-06161-w
Source DB: PubMed Journal: Nat Commun ISSN: 2041-1723 Impact factor: 17.694
Fig. 1Synthesis of the imine-linked COFs. Combining the tetraphenylpyrene tetraamine Py(NH2)4 with the tetradentate pyrene aldehyde Py(CHO)4 in a 1:1 molar ratio yields the microporous Py–Py COF (left), whereas the combination of Py(NH2)4 with linear dialdehydes in a 1:2 molar ratio produces the mesoporous Py–TT and Py–1P COFs, respectively (right)
Fig. 2Structure analysis and solvatochromism of the Py–TT COF bulk powder. a Experimental PXRD pattern (black dots) of the Py–TT COF powder. Rietveld refinement (red line) using the structure model displayed in b provides a very good fit to the experimental data with only minimal differences between the experimental and the refined patterns (green line). Rwp = 4.9%, Rp = 10.5%. Bragg positions are indicated by blue ticks. Inset, magnified view of the 2θ > 9° region. b Top view (left) and side view (right) of the corresponding unit cell reveal the pseudo-quadratic, offset-stacked structure that is typical for pyrene-based COFs. Crystallographic data are available as Supplementary Data 1. The structure has a Connolly surface of 2139 m2 g−1, an accessible surface area of 1808 m2 g−1 and a pore volume of 1.01 cm3 g−1. c Nitrogen sorption isotherm of the Py–TT COF recorded at 77 K. Inset, QSDFT calculation using an equilibrium model yields a very narrow pore size distribution with a maximum at 2.1 nm. d High-resolution TEM image showing the large crystal domains of the Py–TT COF. Scale bar: 40 nm. Inset, magnified view onto a COF crystallite visualizing the pseudo-quadratic arrangement of the COF pores with a periodicity of 2.6 ± 0.1 nm. Scale bar: 20 nm. e Diffuse reflectance spectra of the dry (orange) and water vapour-saturated (brown) Py–TT COF powder showing a strong solvatochromic red-shift
Fig. 3Solvatochromism of Py–TT COF oriented thin films. a GIWAXS pattern of a 360 nm thick Py–TT COF film grown on a sapphire substrate. The intensity of hk0 reflections is concentrated directly above the sample horizon, whereas the 001 and other low-index hk1 reflections appear close to the substrate normal. b UV–Vis absorption spectra of the Py–TT COF film recorded at different relative pressures of H2O in N2. Increasing water content causes a strong absorption increase in the 520–640 nm region, accompanied by a reduced absorption in the 440–500 nm and 280–380 nm regions. Insets, photographs of the COF film in the dry and water-saturated states. c Corresponding plot of the humidity-induced absorbance changes, Ahumid−Adry, at different H2O relative pressures. The grey line indicates the wavelength used for the response time measurements (see below). d UV–Vis spectra of the same COF film in saturated atmospheres of various solvents. The solvatochromic shift increases monotonically with increasing ETN polarity of the solvents. e Solvatochromic response of the Py–TT COF film towards step changes between dry and H2O-saturated N2 streams. Ten individual data sets (black dots) recorded at λ = 560 nm have been averaged (red line). The response times τrise and τfall are determined between the 10% and 90% thresholds. f TD-DFT calculated electron density difference upon the one-electron excitation from the ground state (S0) to the first singlet excited state (S1). This transition involves a reduction of the electron density on the pyrene moieties and an electron density gain of the thienothiophene bridges, and hence possesses a pronounced charge-transfer character. Electron density isosurfaces are displayed at an isovalue of 5e−5