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- W2313439905 abstract "It has been shown that accumulative form of gypsum is influenced by evolution and from micromorphological point of view, gypsic horizons have different trend of evolution and various geomorphologic surface. The purpose of this research work is to study gypsum formation on two landforms of pediment and flood plain in south of Ahar. Undisturbed samples from soils of both landforms were Processed at thin section preparations for gypsum pedofeature identification with a polarize microscope. The results showed more evidence of soil development on pediment as compared with flood plain. Continuous gypsum infillings, consisting of large gypsum crystals, high degree of weathering of primary minerals and plant residues, and evidences for polygenesis were among important indication for long soil pedological processes. Gypsum in both land forms is pedogenic, with large euhedral crystals in pediment and fine euhedral and subhedral crystals in flood plain." @default.
- W2313439905 created "2016-06-24" @default.
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- W2313439905 date "2012-01-01" @default.
- W2313439905 modified "2023-09-24" @default.
- W2313439905 title "Evolution of Gypsum and its Pedofeatures in Soils on Pediment and Flood-Plain, South of Ahar Region, East Azerbaijan, Iran" @default.
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