化学可循环回收的封闭循环共价适应性网络,来源于基本硫
Chen-Yu Shi1, Xiao-Ping Zhang1, Qi Zhang1
1Key Laboratory for Advanced Materials and Joint International Research Laboratory of Precision Chemistry and Molecular Engineering, Feringa Nobel Prize Scientist Joint Research Center, Frontiers Science Center for Materiobiology and Dynamic Chemistry, Institute of Fine Chemicals, School of Chemistry and Molecular Engineering, East China University of Science and Technology 130 Meilong Road Shanghai 200237 P. R. China dahui_qu@ecust.edu.cn.
Chemical science
|October 7, 2024
概括
这项研究引入了由工业废物制成的富含硫的聚合物. 这些新的聚合物是可回收和透明的,提供先进的应用和上循环的机会.
科学领域:
- 聚合物化学 聚合物化学
- 材料科学 材料科学 材料科学
- 可持续化学 可持续化学
背景情况:
- 富含硫的聚合物提供了创新的工业废物回收利用.
- 目前的聚硫化物网络使用二烯交叉连接器,创建稳定的C-S键,防止降解.
- 有限的再加工和回收能力阻碍了硫基聚合物的广泛应用.
研究的目的:
- 探索S8和循环二硫化物的离子环开放共聚变.
- 开发强大的,高分子量,富含硫的共聚合物.
- 提高硫聚合物的再加工能力,机械适应性和光学透明度.
主要方法:
- 元素硫 (S8) 和循环二硫化物的离子环开放共聚化.
- 将聚硫化物段纳入聚合物网络.
- 使用动态二硫化物交联来实现可逆的S-S裂变.
主要成果:
- 合成了强大的富含硫的高分子量共聚合物.
- 由于激活的交联网络,实现了出色的再处理性和机械适应性.
- 在近红外区域获得高光学透明度.
- 通过可逆的二硫化物键裂变证明化学闭环可循环回收.
结论:
- 开发了一种使用动态二硫化物交叉连接器的创新反向火山化策略.
- 这种方法使高性能富硫聚合物的先进应用和再循环成为可能.
- 该研究为硫聚合物开发和废物利用提供了一个可持续的途径.
相关概念视频
Sulfur Assimilation
1
Sulfur is an essential element in biological systems, contributing to synthesizing key biomolecules, including amino acids such as cysteine and methionine, and cofactors such as coenzyme A and biotin. Microorganisms primarily assimilate sulfur as sulfate (SO₄²⁻) from the environment, which must undergo a series of biochemical transformations before it can be incorporated into cellular components. As sulfate is highly oxidized, it must undergo assimilatory sulfate reduction to...
1
Preparation and Reactions of Sulfides
4.7K
Sulfides are the sulfur analog of ethers, just as thiols are the sulfur analog of alcohol. Like ethers, sulfides also consist of two hydrocarbon groups bonded to the central sulfur atom. Depending upon the type of groups present, sulfides can be symmetrical or asymmetrical. Symmetrical sulfides can be prepared via an SN2 reaction between 2 equivalents of an alkyl halide and one equivalent of sodium sulfide.
4.7K
Network Covalent Solids
13.4K
Network covalent solids contain a three-dimensional network of covalently bonded atoms as found in the crystal structures of nonmetals like diamond, graphite, silicon, and some covalent compounds, such as silicon dioxide (sand) and silicon carbide (carborundum, the abrasive on sandpaper). Many minerals have networks of covalent bonds.
To break or to melt a covalent network solid, covalent bonds must be broken. Because covalent bonds are relatively strong, covalent network solids are typically...
To break or to melt a covalent network solid, covalent bonds must be broken. Because covalent bonds are relatively strong, covalent network solids are typically...
13.4K
Structure and Nomenclature of Thiols and Sulfides
4.6K
Thiols and sulfides are sulfur analogs of alcohols and ethers, respectively, where the sulfur atom takes the place of the oxygen atom. Thus, thiols are generally represented as RSH, where R is an alkyl substituent and —SH is the functional group. On the other hand, in sulfides, the central sulfur atom is bonded to two hydrocarbon groups on either side. Depending upon the type of group, sulfides can be either symmetrical or asymmetrical. Both thiols and sulfides display a bent geometry,...
4.6K
Carbon-dioxide Fixation
2
Carbon dioxide fixation in prokaryotes enables the assimilation of inorganic carbon into organic molecules, supporting biosynthetic pathways, sustaining ecosystems, and contributing to the global carbon cycle. It also has industrial applications in carbon capture and bioproduct synthesis. Autotrophic organisms rely on this process to utilize CO₂ as a carbon source in diverse environments.The Calvin CycleThe Calvin cycle is the most widespread carbon fixation mechanism, primarily used by...
2
The Sulfur Cycle
43.9K
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
43.9K


