Micromorphological evidence for mineral weathering pathways in a coastal acid sulfate soil sequence with Mediterranean-type climate, South Australia

Abstract

Abstract. Soil micromorphology, using light microscopy and scanning electron microscopy (SEM), was used to describe detailed soil morphological and compositional changes and determine mineral weathering pathways in acid sulfate soils (ASS) from the following 2 contrasting coastal environments in Barker Inlet, South Australia: (i) a tidal mangrove forest with sulfidic material at St Kilda, and (ii) a former supratidal samphire area at Gillman that was drained in 1954 causing sulfuric material to form from sulfidic material. Pyrite framboids and cubes were identified in sulfidic material from both sites and are associated with sapric and hemic materials. Gypsum crystals, interpreted as a product of sulfide oxidation, were observed to have formed in lenticular voids within organic matter in the tidal mangrove soils at St Kilda. Sulfide oxidation was extensive in the drained soil at Gillman, evidenced by the formation of iron oxyhydroxide pseudomorphs (goethite crystallites and framboids) after pyrite and jarosite, and of gypsum crystals. Gypsum crystals occur where a local source of calcium such as shells or calcareous sand is present. Sporadic oxidation episodes are indicated by the formation of iron oxide and jarosite coatings around coarse biogenic voids. These observations indicate that mineral transformation pathways are strongly influenced by soil physico-chemical characteristics (i.e. oxidation rate, Eh, pH, soil solution chemistry, mineralogy, and spatial distribution of sulfides). This information has been used to illustrate the interrelationships of pyrite, carbonate, gypsum, jarosite, and organic matter and help predict soil evolution under changing hydro-geochemical, redoximorphic, and thermal conditions in soils from coastal environments.

Leaching of potential hazardous elements of coal cleaning rejects

“…As jarosite growth advances, a remnant of pyrite is eventually kept within its pseudomorphic form, as previously reported by Furbish (1963). In some cases, the boxwork has a rectilinear pattern, but mostly, it is quite irregular (Poch et al 2009). …”

Euhedral sparitic calcite in buried surface horizons in lake basins, southwestern Kalahari, Namibia

“…Granostriated b-fabrics can in principle have developed during intrasediment growth, as assumed for gypsum and other salt minerals (e.g. Poch et al, 2009;Tursina et al, 1980). However, as these fabrics also characterize detrital sand grains in the same interval they must be considered to have formed by swell-shrink behaviour of the smectite-bearing groundmass at a later stage.…”

Technogenic soils developed on mine spoils containing iron sulphides: Mineral transformations as an indicator of pedogenesis

“…The presence of cubic jarosite crystals may also suggest that they are pseudomorphs after pyrite, which was discussed in the literature (e.g. Dixon et al, 1982;Doner and Lynn, 1989, and the literature cited therein; Poch et al, 2009). …”