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Pedogenic information from fine sand: A study in Mediterranean soils
Author(s) -
MartínGarcía Juan M.,
MolineroGarcía Alberto,
Calero Julio,
SánchezMarañón Manuel,
FernándezGonzález María V.,
Delgado Rafael
Publication year - 2020
Publication title -
european journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 1351-0754
DOI - 10.1111/ejss.12935
Subject(s) - geology , illite , weathering , mineralogy , chlorite , kaolinite , pedogenesis , biotite , ilmenite , zircon , geochemistry , dolomite , clay minerals , vermiculite , soil water , quartz , soil science , paleontology
Abstract The fine sand fraction (50–250 μm) of Mediterranean soils from southern Spain provides valuable information on soil genesis and the origin of their parent materials. This study considers the whole fine sand and heavy fine sand (ρ > 2.82 g cm −3 ) of Luvisols, Calcisols and Fluvisols, which form a chronosequence (ages from 600 to 0.3 ka) of the River Guadalquivir terrace system. Advanced techniques (X‐ray diffraction, inductively coupled plasma mass spectrometry, inductively coupled plasma atomic emission spectroscopy, variable pressure scanning electron microscope with an energy dispersive X‐ray spectroscopy system and Raman analysis) were employed. Inheritance is the principal pedogenic process. The whole fine sand consisted of carbonates (calcite and dolomite), tectosilicates (quartz, K‐feldspar and plagioclases), phyllosilicates (illite/moscovite, biotite, Na‐mica, chlorite, kaolinite, interstratified vermiculite‐chlorite, vermiculite‐illite and smectite‐illite) and iron oxides (goethite and haematite). The minor minerals (rutile, anatase, ilmenite, zircon, staurolite, monazite, barite, apatite, andalusite, garnet and titanite) are concentrated, also through inheritance, in the heavy fine sand. However, there is also substantiated evidence for neoformation of rutile in these soils, never reported previously. In addition, we report that (a) the geochemical indices calculated in fine sand (SiO 2 /CaO, Chemical Index of Weathering (CIW), Weathering Index of Parker (WIP), Weathering Index (WI), Base Depletion Index (BDI), Weathering Ratio (WR) and Sr/Zr) are closely related to soil age, allowing chronofunctions to be established, and (b) geochemical indices provide information on the origin of soils and permit the establishment of a “critical point” corresponding to “time zero;” that is, the start of pedogenic alteration of the parent material. Highlights Mineralogy and geochemistry inform on the provenance of the fine sand Rutile is neoformed in the fine sand and co‐exists with the polymorph anatase The properties of the fine sand including geochemical indexes fit chronofunctions Geochemical indices determine a “critical point” related to the start of weathering