Insights into the role of dissolved organic matter derived from paddy soils with different parent materials in the environmental behavior of heavy metal adsorbed by ferrihydrite

Abstract

The interaction between dissolved organic matter (DOM) and ferrihydrite (Fh) is a crucial process to control the environmental behavior of heavy metals (HMs) in soil environments, with DOM playing a particularly strong role in HMs fate. Since chemical properties of DOM vary based on different soil parent materials, the underlying impact of DOM-Fh associations on HMs binding remains unclear. This study systematically investigated the interactions between DOM from three soil parent materials (fluvial alluvium: FDOM, sand-shale: SDOM and granite: GDOM) and Fh, and meanwhile understand their effects on the environmental behavior of Cd and Pb under various environmental conditions. An increased Cd and Pb binding during DOM-Fh interactions was observed and attributed to the introduction of additional binding sites by the organic functional groups with a variety of metal affinities. Specifically, more aromatic carboxyl groups in FDOM and more aliphatic groups in SDOM strongly promoted the adsorption of Pb and Cd, respectively. Meanwhile, Higher pH and increased C/Fe also promoted HMs adsorption, particularly in the presence of DOM. Further characterization indicated that electrostatic attraction, ion exchange and surface complexation were primary mechanisms of HMs adsorption. These finding highlight the significant impact of DOM-Fh interactions, dependent on different soil parent materials, on the mobility and fate of HMs in soils, providing valuable insights into the role of DOM composition in influencing HMs contamination, which offer theoretical guidance for environmental management, especially in agricultural and contaminated soils.