“…17,24 It is interesting to note that NOM in natural waters and DOM in soil solutions largely contains hydrophilic fractions including short chain aliphatic carboxylic acids, hydrocarbons and amino acids but few highmolecular-weight, aromatic compounds, and phenolic components. 58 This is highly consistent with the DOM fractions in the supernatant after molecular fractionation by iron oxyhydroxides that we observed in the present study and in aluminum oxides reported by Galindo et al 17,24 Therefore, it is to be expected that the adsorptive fractionation of DOM at hydroxylated mineral surfaces to a great extent determines the chemical components of DOM in labile phases such as surface water and pore water, and a large scale field investigation is needed using ultrahigh resolution mass spectrometry to reveal the molecular composition of labile organic matter in the aquatic and terrestrial environments. In addition, from an environmental perspective, such fractionation led to changes in chemical components of DOM as well as the surface characteristics of the minerals, which will further impact the behaviors of contaminants in the environment such as sorption, transportation and transformation processes.…”