科研之友
微信
新浪微博
Facebook
分享链接
摘要
Iron has profound influence on anaerobic organic matter oxidation and Fe-S-C biogeochemical cycling in tidal marshes. To examine the abundance and speciation of iron, six iron species (poor crystalline Fe(III), crystalline Fe(III), non-sulfidic Fe(II), porewater Fe2+, FeS, and FeS2) were investigated in a cross transect (span = 250 m, depth = similar to 1.2 m) in a tidal marsh of the Min River Estuary in the East China Sea. The results suggested that sediment characteristics, pH, redox condition, conductivity, chloride, sulfate, and organic matter create a highly heterogeneous geochemical framework in the cross transect. Correspondingly, the zonation of iron species differed significantly across the tidal marsh. Poor crystalline Fe(III) (48 +/- 24 mu mol g 1) and crystalline Fe(III) (75 +/- 32 mu mol g 1) accumulated on the surface of the high-tide zone and decreased with elevation. The non-sulfidic Fe(II) minerals (140 +/- 61 mu mol g 1) accounted for the largest proportion of the six iron species. The porewater Fe2+ was enriched within the deep layer of the upland region (pH = 6.2-6.5) and exhibited a maximum of 11.49 mM. The aqueous sulfide concentration was below detection. FeS (39 +/- 6 mu mol g 1) and FeS2 (57 +/- 25 mu mol g 1) accumulated closer to the lower extremity. Tidal water brought O-2 and removed certain amounts of dissolved organic carbon, dissolved inorganic carbon, and Fe(III)-bearing particles in an element budget during tidal inundation. Variations of topography, tidal hydrology, seawater intrusion, and organic matter altered the dominant organic matter oxidation pathway and further affected iron mineralization.
