The microfabric of horizons in the surface and buried soils, XPL.
4.6 (355) · $ 9.00 · In stock
Download scientific diagram | The microfabric of horizons in the surface and buried soils, XPL. Left-surface soil; right-buried soil. (a) Ah2 horizon; (b)-Ahkb horizon; (c, d)-Bt1 and Btkb horizons. Note clay coatings in the micromass; (e, f)-2Ahkb1 (e) and 2Ahkb2 (f) horizons. Glauconite grains are distinguished by greenish color. (For interpretation of the references to color in this figure legend, the reader is referred to the Web version of this article.) from publication: Paleoenvironmental reconstruction based on soils buried under Scythian fortification in the southern forest-steppe area of the East European Plain | Landscape response to Late Holocene climatic cycles is based on detailed hierarchical morphological, analytical and micro-biomorphic research of a soil chronosequence which included a soil buried under a fortification earth wall of the Early Iron Age (Luvic Chernozem) and a | Fortification, Paleoenvironmental Reconstruction and Iron Age | ResearchGate, the professional network for scientists.
The buried soil Luvic Chernozem (Loamic). (a) general view of the
Clearance and Cultivation (Chapter 9) - Applied Soils and Micromorphology in Archaeology
Geoarchaeological Analysis of Soils and Structures of the Shumny Kurgan, Krasnodar Region
A. Microphotographs of soil thin sections showing alternating clay
Oxyaquic Vertic Hapludalf (fine, smectitic, hyperthermic)
Gypsiferous Gazha Soils of the Subboreal Zone of Eurasia
Geosciences, Free Full-Text
PDF) Micromorphology and development of loess-derived surface and buried soils along a precipitation gradient in Northern Iran
Changes in Soil Properties on Fallows in Kursk Oblast and Trends of Postagrogenic Soil Development in Forest-Steppe and Steppe Zones
Alexander MAKEEV, Senior Researcher, Dr. of Science, Faculty of Soil Science
PDF) Paleoenvironmental reconstruction based on soils buried under Scythian fortification in the southern forest-steppe area of the East European Plain
Dynamic interactions at the mineral–organic matter interface
