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Micronutrient Distribution in Different Physiographic Units of the Siwalik Hills of the Semiarid Tract of Punjab, India
23
Citations
12
References
1999
Year
NutritionDiethylenetriamine Pentaacetic AcidEngineeringAgricultural EconomicsEarth ScienceSoil PropertyEnvironmental ChemistryProfile DistributionPlant NutritionPublic HealthSiwalik HillsBiogeochemistrySoil ScienceGeographyMicronutrientsSemiarid TractMicronutrient DistributionNutritional RequirementOrganic MatterSoil ChemistryGeochemistry
We investigated the profile distribution of total and diethylenetriamine pentaacetic acid ( DTPA )- extractable micronutrients ( Zn , Mn , Cu , Fe ) in soils developed on six physiographic units of the semiarid Siwalik hills of Punjab in northwest India . The soils showed a gradual fining of texture from shoulder slopes to toe slopes . All soils were alkaline and calcareous . In general , total and DTPA-extractable micro nutrients were higher in surface horizons and decreased in subsurface horizons . However , none of the micronutrients exhibited any consistent pattern of distribution with depth on different geomorphic surfaces . Physiography had a strong influence on the spatial distribution of total and available micronutrients . Contents of all micronutrients and their forms were higher in fine-textured and uneroded soils than in coarse-textured eroded soils . Soil pH , calcium carbonate , organic matter , and size fractions had strong influence on the distribution of total and extractable micronutrients . Based on linear coefficients of correlation , total content of micro nutrients increased with increase in clay content , whereas DTPA - extractable micronutrient content increased with increase in organic carbon and decreased with increase in pH and CaCO3 content . Except for Cu , no other micronutrient showed influence of total reserves on availability of the respective micronutrient . Among the various micronutrients , deficiency of Zn was found to be widespread , followed by Fe and Cu in the cultivated soils on foot slopes , toe slopes , and floodplains .
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