Studies on genesis, characterization and classification of soils in central and Eastern parts of Prakasam district in Andhra Pradesh

Ch. Chandra Sekhar, D. Balaguravaiah, M.V.S. Naidu

2014 · 14 citations · 12 references

Concepts

Abstract

Seven typical pedons representing major land forms in central and eastrern parts of Prakasam district viz., plains and uplands developed from granite-gneiss, sand- stone and alluvium parent material under varying land use were studied for their mor- phological characteristics, physical and physico-chemical properties, soil genesis and nutrient status. Soils were shallow to very deep, slightly acidic to slightly alkaline (pH 6.02 to 8.45) in reaction, non-saline and had iso-hyperthermic temperature and ustic soil moisture regimes. Texture, organic carbon, CEC and base saturation were ranged from sand to clay in surface and sub-surface, 0.12 to 0.68 per cent, 3.48 to 48.74 cmol (p + ) kg - 1 and 73.44 to 91.52 per cent, respectively. Soils were low in available nitrogen, medium in available phosphorus, low to high in available potassium and high in available sul- phur. However, the soils were deficient in DTPA-extractable Zn and sufficient in Fe (except in pedon 6, surface horizon of pedon 4 and sub-surface horizons of pedon 2), Cu and Mn. Pedons 2 and 6 were grouped under Entisols due to absence of sub-surface diagnostic horizon and were classified as Typic Ustipsamments and Typic Ustorthents, respectively whereas pedons 1, 4, 5 and 7 were placed under Inceptisols due to presence of cambic (Bw) sub-surface diagnostic horizon and classified as Typic Haplustepts (pedons 1, 4 and 5) and Lithic Haplustepts (pedon 7). Due to the presence of vertic features like slickensies, pressure faces, cracks and presence of more than 30 % clay in all the horizons, the pedon 3 was grouped under Vertisols and classified as Typic Haplusterts. The soils were also evaluated for commonly grown crops of the area.

References

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