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*Corresponding author Email id: bhargavnarasimha444@gmail.com
Nine typical pedons representing uplands, midlands and lowlands in the Ganjigatti sub-watershed, Karnataka, were selected and studied for their morphological, physical and chemical properties in relation to variation in physiography during 2021-23. The profile development was lowest in the uplands and highest in the lowlands. The upland soils (pedons 1, 2, 3 and 4) had a medium, moderate and subangular to angular blocky structure, shallow deep, yellowish-red to strong brown colour (5 YR to 7.5 YR), sandy clay loam texture, strongly acidic to neutral pH, 5.20 to 38.48 cmol(p+)kg-1 CEC and medium base saturation. Moving to midland soils (pedons 5, 6 and 7), they exhibited a fine to medium, moderate structure characterized by granular to sub-angular blocky formations. These soils were moderately shallow to moderately deep, with a dark brown to very dark brown hue (7.5 YR to 10 YR), sandy clay to clay texture, neutral pH, 18.52 to 41.54 cmol (p+) kg-1 CEC and high base saturation. Descending to the lowland regions, the soils (pedons 8 and 9) were fine, strong, granular to angular blocky, very deep, with a brown to very dark brown colour (10 YR), clay texture, neutral to alkaline pH, 16.26 to 51.50 cmol(p+)kg-1 CEC and high base saturation. Based on soil profile development and diagnostic characteristics, we classify the soils at the sub-group level as Lithic Ustorthents (pedons 1 and 4), Typic Ustorthents (pedons 3 and 7), Lithic Haplustalfs (pedon 2), Typic Haplustalfs (pedon 6), Typic Haplustepts (pedon 5), Vertic Haplustepts (pedon 8) and Typic Haplusterts (pedon 9).
Hilly zone, Characterization, Classification, Entisols, Inceptisols, Alfisols, Vertisols