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- B4fedfdd8fb5cec46ce6ada9749ccbcab hasDbXref Red_soil @default.
- B4fedfdd8fb5cec46ce6ada9749ccbcab type Axiom @default.
- B4fedfdd8fb5cec46ce6ada9749ccbcab annotatedProperty comment @default.
- B4fedfdd8fb5cec46ce6ada9749ccbcab annotatedSource ENVO_00005790 @default.
- B4fedfdd8fb5cec46ce6ada9749ccbcab annotatedTarget "Red soil typically derives from crystalline rock in warm, temperate, moist climates under deciduous or mixed forest. It has thin organic and organic-mineral layers, a black brown leached layer resting on an illuvium red layer. The majority of red soils have a loamy texture. Their chemical composition varies across regions, but often includes non-soluble material 90.47%, iron 3.61%, aluminium 2.92%, organic matter 1.01%, magnesium 0.70%, lime 0.56%, carbon dioxide 0.30%, potash 0.24%, soda 0.12%, phosphorus 0.09% and nitrogen 0.08%. On the uplands, they are thin, poor and gravelly, sandy, or stony and porous, light-colored soils on which food crops like bajra can be grown. In contrast, on the lower plains and valleys they are rich, deep, dark colored fertile loam on which, under irrigation, can produce excellent crops like cotton, wheat, pulses, tobacco, jowar, linseed, millet, potatoes and fruits." @default.