“…2,3,7,[11][12][13] While sedimentary DOM from peat layers, 9,[14][15][16] as well as surfacederived organic carbon, [17][18][19] have been suggested, the source of labile DOM is still a matter of much debate. 20,21 Beyond labile DOM, recent studies also highlight the potential influence of humic and fulvic acids (refractory organic polymers) in As mobilization through electron shuttling, [22][23][24][25] or competition for sorption, 26 and complexation processes. 27,28 Since the chemical composition of DOM defines its reactivity in the environment, 29,30 the ability to track the different chemical fractions of DOM is essential to better understand its role on arsenic mobilization in groundwater.…”