Response of salinity gradient power generation to inflow mode and temperature difference by reverse electrodialysis

J Environ Manage. 2022 Feb 1:303:114124. doi: 10.1016/j.jenvman.2021.114124. Epub 2021 Nov 25.

Abstract

Sustainable utilization has been becoming the core idea of concentrated seawater disposal, which makes the harvest of salinity gradient power based on reverse electrodialysis (RED) become one of the important ways. As the important factors affecting RED performance, different flow orientations along the membrane and solution temperature have been studied in the previous researches. However, there are still some details that need to be clarified. In this study, the inflow mode was further detailed investigated. The results showed that after eliminating the interference of bubbles in the counter-current, the co-current was still better than the counter-current; when the solution of HCC (high concentration compartment) and LCC (low concentration compartment) was circulated for 3 h, the concentration of concentrated seawater discharge liquid was reduced by 6.93%, which was conducive to reducing the negative impact on the marine ecological environment. Meanwhile, the response of salinity gradient power generation to temperature difference was that high temperature had a positive effect on power density, and the order was both the HCC and LCC (0.44 W m-2) > LCC (0.42 W m-2) > HCC (0.39 W m-2). Although the RED performance was more sensitive to the temperature rise of LCC, the positive temperature difference between HCC and LCC is a more practical advantage because the temperature of concentrated seawater in HCC is usually high. These new observations could provide supports for the industrial development of RED in generating electricity economically and reducing the negative environmental impact of concentrated seawater.

Keywords: Concentrated seawater; Inflow mode; Reverse electrodialysis; Salinity gradient power; Temperature difference.

MeSH terms

  • Ecosystem
  • Electricity
  • Renewable Energy*
  • Salinity*
  • Seawater*
  • Temperature