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Five sites were chosen in Kalar city based on their respective topographic position. The results of particle size distribution of the studied pedons revealed that the majority of pedons were produced with Ochric epitopes and Cambic and Argillic endopedons, as well as pedons, indicating that there are substantial differences between sand and clay in surface horizons, particularly in pedons, despite poor elevation in comparison to other pedons. These soils are in an aridic moisture regime, including the Ochric diagnostic surface horizons with Argillic and Cambic diagnostic subsurface horizons, and they belong to Aridisols order with suborders Argids and Cambidsas these soils are in the aridic moisture regime.
Source link: https://doi.org/10.24017/science.2016.1.2.1
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