| Literature DB >> 35160360 |
Xingya Zhao1,2,3, Yipeng Qi1, Jianquan Li1, Qingyu Ma1.
Abstract
Herein, we present two novel ferrocene-containing porous organic polymers, FPOP-1 and FPOP-2, by the Heck reactions of 1,1'-divinylferrocene with two tetrahedral silicon-centered units, i.e., tetrakis(4-bromophenyl)silane and tetrakis(4'-bromo-[1,1'-biphenyl]-4-yl)silane. The resulting materials possess high thermal stability and moderate porosity with the Brunauer-Emmer-Teller (BET) surface areas of 499 m2 g-1 (FPOP-1) and 354 m2 g-1 (FPOP-2) and total pore volumes of 0.43 cm3 g-1 (FPOP-1) and 0.49 cm3 g-1 (FPOP-2). The porosity is comparable to previously reported ferrocene-containing porous polymers. These materials possess comparable CO2 capacities of 1.16 mmol g-1 (5.10 wt%) at 273 K and 1.0 bar, and 0.54 mmol g-1 (2.38 wt%) at 298 K and 1.0 bar (FPOP-1). The found capacities are comparable to, or higher than many porous polymers having similar or higher surface areas. They have high isosteric heats of up to 32.9 kJ mol-1, proving that the affinity between the polymer network and CO2 is high, which can be explained by the presence of ferrocene units in the porous networks. These results indicate that these materials can be promisingly utilized as candidates for the storage or capture of CO2. More ferrocene-containing porous polymers can be designed and synthesized by combining ferrocene units with various aromatic monomers under this strategy and their applications could be explored.Entities:
Keywords: carbon dioxide sorption; ferrocene; gas storage; porous organic polymers; silicon-centered monomers
Year: 2022 PMID: 35160360 PMCID: PMC8838439 DOI: 10.3390/polym14030370
Source DB: PubMed Journal: Polymers (Basel) ISSN: 2073-4360 Impact factor: 4.329
Scheme 1Synthesis routes of FPOP-1 and FPOP-2. Reaction condition: Pd(PPh3)4, DMF, and K2CO3, at 120 °C for 72 h. The fragments of FPOPs are shown as examples.
Figure 1FT-IR of FPOP-1 and FPOP-2.
Figure 2Solid-state 13C CP/MAS NMR spectra of FPOP-1 (a) and FPOP-2 (b). The peak indicated by asterisk may be assigned to the carbon atom from residual methanol resulting from the Soxhlet extraction.
Figure 3Solid-state 29Si NMR spectra of FPOP-1 (a) and FPOP-2 (b).
Figure 4FE-SEM images of FPOP-1 (a) and FPOP-2 (b).
Figure 5TGA curves of FPOP-1 and FPOP-2 in nitrogen atmosphere.
Figure 6Nitrogen adsorption (close symbols) and desorption (open symbols) isotherms of FPOP-1 and FPOP-2 measured at 77 K (a); pore size distribution curves of FPOP-1 and FPOP-2 calculated by NL-DFT (b).
Porosity data of FPOP-1 and FPOP-2.
| SBET (a)/m2 g–1 | Smicro (b)/m2 g–1 | Vtotal (c)/cm3 g–1 | Vmicro (d)/cm3 g–1 | Vmicro/Vtotal | CO2 Uptake (wt%) (e) | |
|---|---|---|---|---|---|---|
| FPOP-1 | 499 | 308 | 0.43 | 0.23 | 0.53 | 5.10 |
| FPOP-2 | 354 | 175 | 0.49 | 0.13 | 0.27 | 4.66 |
(a) Surface areas calculated from N2 adsorption isotherm using the BET method; (b) microporous surface areas calculated from N2 adsorption isotherm using the t-plot method; (c) total pore volumes calculated at P/P0 = 0.90; (d) microspore volumes derived using the t-plot method based on the Halsey thickness equation; (e) carbon dioxide uptakes at 1.0 bar and 273 K.
Figure 7CO2 adsorption isotherms of FPOP-1 and FPOP-2 at 273 and 298K (a); isosteric heat of CO2 adsorption of FPOP-1 and FPOP-2 (b).