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Micromorphology and genesis of terra rossa of the U.S.S.R. and East Europe



Micromorphology and genesis of terra rossa of the U.S.S.R. and East Europe



Zeszyty Problemowe Postepow Nauk Rolniczych 123: 421-427



The genesis, particle size distribution, mineralogical composition and micromorphology of terra rossas were investigated. The soils were non-uniform in composition. Large particles were predominantly limestone and silt-sized particles were predominantly quartz. Mixed layer minerals (hydromica-montmorillonite) predominated in the clay fraction with varying amounts of a kaolinite-halloysite mineral. The contents of free Fe and Al were negligible.

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Accession: 000137769

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