Unaffected soils |
Podzol |
hornblende, hyperstene, magnetite, garnet |
Susceptibility of different minerals to weathering |
Matelski and Turk (1947) |
Acid forest soil profiles (pH 4–5), galciofluvial substrate |
apatite, titanite, hornblende, garnet, epidote, zircon |
Documenting weathering trends |
Lång (2000) |
Pre-tsunami soils |
pyroxene and amphibole group, opaque minerals |
Soil erosion, provenance of detrital material |
Jagodziński et al. (2012) |
Entisols and Aridisols |
non-opaque heavy minerals (zircon, tourmaline, rutile, garnet, sillimanite, and andalusite) |
Provenance of detrital material |
Sulieman et al. (2015) |
Podzol |
apatite, amphibole, epidote, hematite, hornblende, garnet, monazite, olivine, pyrite, pyroxene, titanite, zircon, rutile, and ilmenite |
Determine if there is a significant contribution from these minerals to the surface geochemical signature, particularly radiogenic Pb of the soils |
Carlson (2016) |
Unspecified |
zircon, magnetite, ilmenite, rutile and monazite |
Mineral contribution to elevated contents of some elements in soils in ship-breaking yards |
Khan et al. (2019) |
Initial soils |
transparent heavy-minerals |
Documenting weathering patterns and pedogenetic processes and the addition of allochthonous material |
Tangari et al. (2021) |
Terra rosa represented by red palaeosol, red polygenetic soil, and two pedosedimentary complexes |
epidote and amphibole groups |
The provenance of initial soil material (origin of the parent material) |
Razum et al. (2023) |
Soils affected by mining and smelting |
The rhizosphere of industrial soils near Zn–Pb mines and metallurgical plants (Poland) |
Pb, Cd, Zn carbonates, As-Pb sulphosalts, polymineralic spherules |
Identification of processes in the rhizosphere leading to alteration and formation of secondary metal-rich phases, the importance of plant-root exudation solutions is stressed |
Cabała, Teper (2007) |
Industrial soils near mining and smelting areas |
Slag particles >1 mm in diameter |
Establishing slag-derived dust as a main carrier of trace elements in studied soils |
Chopin and Alloway (2007) |
Soils close to major smelter centers at Coppercliff, Coniston, and Falconbridge in the Sudbury area, Canada |
Spherical particles composed of magnetite, hematite, Fe-silicates, sulfides, spinels, delafossite, and cuprite or tenorite |
Origin and potential alteration (e.g. dissolution rates and particle-soil interaction) of spherical particles |
Lanteigne et al. (2012) |
Soil adjacent to mining areas |
Particulate matter such as Fe silicates, spinels, sulfides, NiO, and their weathering products |
Distribution of metals and metalloids in particulate matter, their formation, weathering, and mobility in soils |
Lanteigne et al. (2014) |
Soils within the protection zone of copper smelter (Poland) |
Diverse particles associated with mining and smelting |
Detecting weathering reactions in the heavy particles, implications for metal mobility |
Tyszka et al. (2016) |
Four different forest and grassland soils (site for the long-term experiment) |
Flue dust composed predominately of arsenolite As2O3 |
Transformation of As-rich (>50 wt% As) copper smelter dust in the soil to understand As mobility and pollution risks |
Jarošíková et al. (2018) |
Soils developed on the slag heap after Zn–Pb smelting (Poland) |
Diverse particles associated with Zn–Pb smelting |
Estimating modal proportions of primary to secondary phases using automated electron microscopy |
Pietranik et al. (2018) |
Topsoils from hot semi-dry area (Namibia) |
Diverse particles associated with mining and smelting |
Automated SEM used to understand the fate/binding of metal (loids) in soils |
Tuhý et al. (2020) |
Biomass-rich savanna soils, semi-arid (Namibia) |
Ferric oxides, arsenolite, metal arsenates, As apatite, enargite |
Understanding temperatures of mineralogical transformations and potentially toxic elements remobilization under wildfire conditions (laboratory combustion experiment) |
Tuhý et al. (2021) |
Soils affected by Zn mining (Lanping Pb–Zn mine, China) |
Cadmium-bearing sphalerite and smithsonite |
Mobility and behavior of Cd and Zn derived from smithsonite and sphalerite and their transport mechanisms in soils |
Li et al. (2022) |