Chinese

Fluorescence spectroscopic characterization of dissolved organic matter fractions in soils in soil aquifer treatment

Date: 2024-03-05    Source: 


                                                                                    Shuang Xue, Youtao Song, Mei Tie

                                                                      School of Environmental Science, Liaoning University

                                                                                      Qingliang Zhao, Liangliang Wei

                                              School of Municipal and Environmental Engineering, Harbin Institute of Technology


Abstract

This work investigated the effect of soil aquifer treatment (SAT) operation on the fluorescence characteristics of dissolved organic matter (DOM) fractions in soils through laboratory-scale soil columns with a 2-year operation. The resin adsorption technique (with XAD- 8 and XAD-4 resins) was employed to characterize the dissolved organic matter in soils into five fractions, i.e., hydrophobic acid (HPO-A), hydrophobic neutral (HPON), transphilic acid (TPI-A), transphilic neutral (TPI-N), and hydrophilic fraction (HPI). The synchronous fluorescence spectra revealed the presence of soluble microbial byproduct- and humic acid-like components and polycyclic aromatic compounds in DOM in soils, and SAT operation resulted in the enrichment of these fluorescent materials in all DOM fractions in the surface soil (0– 12.5 cm). More importantly, the quantitative method of fluorescence regional integration was used in the analysis of excitation–emission matrix (EEM) spectra of DOM fractions in soils. The cumulative EEM volume (ΦT, n) results showed that SAT operation led to the enrichment of more fluorescent components in HPO-A and TPI-A, as well as the dominance of less fluorescent components in HPO-N, TPI-N, and HPI in the bottom soil (75–150 cm). Total ΦT, n values, which were calculated as ΦT,n×DOC, suggested an accumulation of fluorescent organic matter in the upper 75 cm of soil as a consequence of SAT operation. The distribution of volumetric fluorescence among five regions (i.e., Pi, n) results revealed that SAT caused the increased content of humic-like fluorophores

as well as the decreased content of protein-like fluorophores in both HPO-A and TPI-A in soils.


Read the full article here:   65-Fluorescence spectroscopic characterization of dissolved organic matter fractions in soils in soil aquifer treatment.pdf