Variation with depth and season in metal sulfides in salt marsh soils

Seasonal monitoring of metal sulfides was carried out in four soils ofthe Ría de Ortigueira salt marshes. Soils from the high salt marsh (withsuboxic redox conditions at the surface), had low concentrations of ironsulfides (AVS and pyrite fraction) and thus a low degree of trace metalpyritization (DTMP) in surface layers (0–10 cm), butconcentrations of metals associated with the pyrite fraction increasedconsiderably at depth (27.5 cm). In the low salt marsh soils (withanoxic conditions at the surface) maximum concentrations of metal sulfides werefound in the surface layers of soils colonized by Spartinamaritima. These results are explained by the double effectexerted by roots in strongly reduced soils. On the one hand, they stimulate theactivity of sulfate-reducing bacteria and on the other, they favour the partialoxidation of the soil, thus generating polysulfides with which Fe²⁺immediately precipitates as pyrite, whereas in the deepest, permanently anoxiclayers, pyrite must be formed in a reaction in which FeS is an intermediate, asfollows: FeS + H₂S FeS₂ + H₂.Concentrations of metal sulfides also varied greatly with the season, with twopatterns being distinguished. In soils colonized by S.maritima in both high and low salt marshes, the lowestconcentrations were found in summer. At this time of the year there is a netloss of metal sulfides throughout the profile, presumably due to physiologicalactivity of plants (evapotranspiration and release of oxygen from roots). Incontrast, maximum concentrations of AVS and pyritic metals were found in thesummer in the low salt marsh soils not colonized by vascular plants (creekbottom). In this case, the higher temperatures increased the activity ofsulfur-reducing bacteria leading to synthesis and accumulation of metalsulfidesin the soil.