Soil, Regolith, and Weathered Rock Theoretical Concepts and Evolution
Geoderma 368 (2020) 114261 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Soil, regolith, and weathered rock: Theoretical concepts and evolution in T old-growth temperate forests, Central Europe ⁎ Pavel Šamonila,b, , Jonathan Phillipsa,c, Pavel Daněka,d, Vojtěch Beneše, Lukasz Pawlika,f a Department of Forest Ecology, The Silva Tarouca Research Institute for Landscape and Ornamental Gardening, Lidická 25/27, 602 00 Brno, Czech Republic b Department of Forest Botany, Dendrology and Geobiocoenology, Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemědělská 1, 613 00 Brno, Czech Republic c Earth Surface Systems Program, Department of Geography, University of Kentucky, Lexington, KY 40506, USA d Department of Botany and Zoology, Faculty of Science, Masaryk University, Kotlářská 267/2, 611 37 Brno, Czech Republic e G IMPULS Praha Ltd., Czech Republic f University of Silesia, Faculty of Earth Sciences, ul. Będzińska 60, 41-200 Sosnowiec, Poland ARTICLE INFO ABSTRACT Handling Editor: Alberto Agnelli Evolution of weathering profiles (WP) is critical for landscape evolution, soil formation, biogeochemical cycles, Keywords: and critical zone hydrology and ecology. Weathering profiles often include soil or solum (O, A, E, and Bhor- Soil evolution izons), non-soil regolith (including soil C horizons, saprolite), and weathered rock. Development of these is a Saprolite function of weathering at the bedrock weathering front to produce weathered rock; weathering at the boundary Weathering front between regolith and weathered rock to produce saprolite, and pedogenesis to convert non-soil regolith to soil. Hillslope processes Relative thicknesses of soil (Ts), non-soil regolith (Tr) and weathered rock (Tw) can provide insight into the Geophysical research relative rates of these processes at some sites with negligible surface removals or deposition.
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