| Literature DB >> 32733844 |
Yong-Tao Zhang1, Fu-Lin Chen1, Shi-Jie Yu2, Fei Wang1.
Abstract
Gas hydrates have promising application prospects in the fields of future energy sources, natural gas storage and transportation, CO2 capture and sequestration, gas separation, and cold energy. However, the application of hydrate technologies is being restricted due to the slow formation rate of gas hydrates. Kinetic promoters have been receiving increased attention, given that they can improve the hydrate formation rate with very small doses and do not affect gas storage capacity. However, most kinetic promoters are non-renewable, petrochemical-derived, non-degradable materials, inevitably leading to resource waste and environmental pollution. Biopromoters, derived from biomass, are renewable, biodegradable, environmentally friendly, non-toxic (or low toxic), and economically feasible. This mini review summarizes the current status of already discovered biopromoters, including lignosulfonate, amino acid, biosurfactant, and biological porous structures, which have the potential to replace petrochemical-derived promoters in hydrate technologies. Finally, future research directions are given for the development of biopromoters.Entities:
Keywords: biomass; biopromoter; gas hydrate; kinetic promoter; mechanism
Year: 2020 PMID: 32733844 PMCID: PMC7360788 DOI: 10.3389/fchem.2020.00514
Source DB: PubMed Journal: Front Chem ISSN: 2296-2646 Impact factor: 5.221
Figure 1(A) Spherical microgel model of an LS macromolecule. Reproduced from Rezanowich and Goring (1960) with permission from Elsevier. (B) CH4 formation kinetics in a Ca-LS aqueous solution at 273.2 K and 9.5 MPa. Reproduced from Wang et al. (2012) with permission from the Royal Society of Chemistry. (C) Schematic diagram of the promoting mechanism of LSs. (D) CH4 formation kinetics in a L-leucine aqueous solution at 273 K and 9.5 MPa. Reproduced from Liu et al. (2015) with permission from John Wiley and Sons. (E) CO2 formation kinetics in L-methionine aqueous solution at 273.2 K and 3.3 MPa. Reproduced from Cai et al. (2017) with the permission from the John Wiley and Sons. (F) Schematic diagram of the promoting mechanism of biosurfactant in seabed sands/clay; (G) CH4 and CO2 formation kinetics for tomato, eggplant, and mushroom samples. Reproduced from Wang et al. (2013) with permission from the Royal Society of Chemistry. (H) SEM image of a mushroom sample showing a fine porous structure. Reproduced from Wang et al. (2013) with permission from the Royal Society of Chemistry.