Abstract
ABSTRACT Origin of the humic substances formed in biological wastewater treatment system (abbreviated as bio-HS) still remains inconclusive. In this study, the bio-HS that contained humic acid (HA) and fulvic acid (FA) from effluent and activated sludge were isolated and purified with XAD-8 resin and ion exchange resin, and then the molecular weight, functional groups, contents and forms of phosphorus (P) using gel permeation chromatography (GPC), fourier transform infrared (FTIR), element analysis and P nuclear magnetic resonance (31P-NMR) were investigated. The results showed that HS was formed in biological wastewater treatment systems, and had a lower degree of humification than soil, peat, or marine HS, and mainly comprised diester and monoester P fragments. Specific signal peaks of intracellular materials and cell membranes (nucleic acid, phospholipids, and sugar phosphate) showed that microbial cell debris was the precursor of bio-HS. HA comprised diester P fragments and monoester P fragments that formed when diester P fragments degraded, while FA contained only diester P fragments. The monoester P fragments in HA may result from microbial degradation of diester P fragments, and FA may simultaneously condense into HA. These results show that microbial cell debris was first transformed into FA and then into HA.
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