共 50 条
Upcycling of exhausted reverse osmosis membranes into value-added pyrolysis products and carbon dots
被引:26
|作者:
Liang, Lili
[1
,2
,3
]
Veksha, Andrei
[3
]
Amrad, Muhammad Zahin Bin Mohamed
[1
]
Snyder, Shane Allen
[1
,3
]
Lisak, Grzegorz
[1
,3
]
机构:
[1] Nanyang Technol Univ, Sch Civil & Environm Engn, Singapore 639798, Singapore
[2] Nanyang Technol Univ, Interdisciplinary Grad Program, 1 Cleantech Loop,CleanTech One, Singapore 637141, Singapore
[3] Nanyang Technol Univ, Residues & Resource Reclamat Ctr, Nanyang Environm & Water Res Inst, 1 Cleantech Loop,CleanTech One, Singapore 637141, Singapore
关键词:
Reverse osmosis membrane;
Pyrolysis;
Hydrothermal method;
Carbon dots;
Fe3+ determination;
GRAPHENE QUANTUM DOTS;
ONE-STEP SYNTHESIS;
HYDROTHERMAL SYNTHESIS;
GREEN SYNTHESIS;
WASTE;
NITROGEN;
FLUORESCENCE;
POLYOLEFINS;
ENERGY;
CONVERSION;
D O I:
10.1016/j.jhazmat.2021.126472
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
Polymeric reverse osmosis (RO) membranes are widely used worldwide for production of fresh water from various sources, primarily ocean desalination. However, with limited service life, exhausted RO membrane modules often end up as plastic wastes disposed of predominantly by landfilling. It is imperative to find a feasible way to upcycle end-of-life RO membrane modules into valuable products. In this paper, the feasibility of RO membrane recycling via pyrolysis and subsequent conversion of resulting char into carbon dots (CDs) through H2O2-assisted hydrothermal method was investigated. RO membrane module pyrolysis at 600 degrees C produced oil (28 wt%), non-condensable gas (17 wt%), and char (22 wt%). While oil and gas can serve as fuel and chemical feedstock due to rich hydrocarbon content, char was found a suitable precursor for the synthesis of functional CDs. The resulting CDs doped with N (4.8%) and S (1.8%) exhibited excellent water dispersibility, narrow size distribution of 1.3-6.8 nm, high stability, and strong blue fluorescence with a quantum yield of 6.24%. CDs demonstrated high selectivity and sensitivity towards Fe3+ in the range of 0-100 mu M with the limit of detection of 2.97 mu M and were capable of determining Fe3+ in real water samples (tap water and pond water).
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