Phosphorus Competition in Bioinduced Vivianite Recovery from Wastewater

• Published in: Environmental science & technology Vol. 52; no. 23; pp. 13863 - 13870
• Main Authors: Wang, Shu, An, Jingkun, Wan, Yuxuan, Du, Qing, Wang, Xin, Cheng, Xiang, Li, Nan
• Format: Journal Article
• Language: English
• Published: United States American Chemical Society 04.12.2018
• Subjects: Biomass; Competition; Crystals; Eutrophication; Geobacter; Iron; Mineralization; Minerals; Nodules; Optimization; Phosphorus; Recovery; Reduction; Reduction (metal working); S curves; Sewage; Soil water; Vivianite; Wastewater; Water treatment
• ISSN: 0013-936X; 1520-5851
• DOI: 10.1021/acs.est.8b03022

Phosphorus undergoes a one-way flow from minerals to soil to water, which creates a phosphorus crisis as well as aquatic eutrophication. Dissimilatory metal reduction bacterial (DMRB)-induced vivianite recovery from wastewater is a promising route to solve these problems synthetically. In this study, phosphorus competition between biomass growth and bioinduced vivianite mineralization was investigated at the batch scale. Biomass growth leads to phosphorus utilization over vivianite mineralization. Geobacter was selected as the main functional microorganism and presented higher vivianite recovery rates (20–48%) than sewage biomass (7–33%). An optimal Fe/P stoichiometric ratio of 1:1 was observed for both sewage biomass and Geobacter-inoculated batches. The highest vivianite yield of 4.3 mM was obtained in Geobacter-inoculated batches at a Fe:P of 1:1, with values 59% higher than those at a Fe:P of 1:0.67 (equal to the Fe/P molar ratio in vivianite). Sufficient PO4 3– stimulated cell growth and yielded a higher Fe3+ reduction rate and vivianite yield. Nevertheless, excessive PO4 3– facilitated the precipitation of KFe3 (PO4)2(OH)·8H2O and Fe7 (PO4)6, which inhibited vivianite synthesis. In the optimal Geobacter batch, the μ–S curve indicated a mixed order reaction (0 < x < 1) for both vivianite formation and biomass growth. The vivianite growth series proceeded as follows: tiny blue particles, plain pieces, dark blue nodules, and large spherical crystals.