Alkalization-induced disintegration increased redox activity of solid humic acids and its soil biogeochemical implications

Abstract

Solid humic acids (HAsolid) plays a significant role in maintaining soil ecosystem services, especially in alkaline soil. The unique chemical structures and electrochemical properties are the cores that HAsolid works. In this study, the alkalization-induced variations of particle morphology, functional groups and redox activity of HAsolid were investigated and its soil biogeochemical implications were discussed. Atomic force microscopy (AFM) deflection images and zeta potential results showed that alkalization induced disintegration of HAsolid, with particle size reducing to 200 nm when pH value reached 10.0. This result suggested that HAsolid could exist in alkaline soil. AFM-IR along with fluorescence intensity of HAsolid at different pH further proved that the supramolecular aggregation of HAsolid became loose and dispersive with more redox-active functional groups exposure after alkalization, which could lead to HAsolid susceptible to degradation in alkaline soil. Conductivity of HAsolid decreased 42.86 % when pH increased from 5.0 to 10.0, while electron exchange capacity (EEC) of HAsolid increased 45.30 %, indicating the increase of redox activity of HAsolid. Increase of redox activity of HAsolid by alkalization-induced disintegration not only can accelerate organic pollutant degradation via enhancing microbial co-metabolism, but also speed up the organic carbon loss. This study contributes to a better understanding of the role of HAsolid in organic carbon stocks and fluxes of alkaline soils and has great implications for soil biogeochemical process.