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- W2004148631 abstract "SummaryThe chemical composition of the soils and of the colloidal separates of twelve red earths from three widely differing locations in Italy has been determined. The red earths of southern Italy are characterized by low organic matter, little if any CaCO3, and appreciable quantities of soluble salts. Those of northern Italy have opposite characteristics. The SiO2/R2O3 ratios of the colloids range from 1.60 to 2.09 and bear no relationship to location or climatic factors.It is concluded that similar pedogenetic processes have occurred throughout the Italian peninsula and are independent of geographical position or climatic conditions. In particular the SiO2/R2O3 ratio of the colloids of the southern soils is not unusually low as has been suggested by other workers." @default.
- W2004148631 created "2016-06-24" @default.
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- W2004148631 date "1960-03-01" @default.
- W2004148631 modified "2023-09-26" @default.
- W2004148631 title "THE RED EARTHS AND THE COLLOIDS OF THE RED EARTHS" @default.
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- W2004148631 doi "https://doi.org/10.1111/j.1365-2389.1960.tb02204.x" @default.
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