Summary
The downward movement of the nitrate ion in the top 5 ft of Tippera clay loam was followed by applying sodium nitrate at the rate of 2000 pounds per acre to bare fallow soil after different rain intervals during the 1957/58 wet season. At the end of the season soil samples were collected at 6-inch intervals and compared with samples from adjacent plots that received an equivalent anion quantity of sodium chloride after the same rain intervals. After 23.7 inches of rain the distribution of nitrate and chloride anions the soil profile was nearly identical and it was concluded that the anions are equally mobile in this soil.
The mean movement of the anion was 1.075 inches for each inch of rainfall. A high positive correlation of 0.946 was obtained between mean movement and rainfall. The downward movement of both anions out of the topsoil appeared to be enhanced by channels left by partly decomposed roots.
Application of sodium chloride on sandier soils revealed a much higher mean movement of anions on Blain sand than on Tippera clay loam after equal amounts of rain, but on Florina sand with a high silt content in the topsoil the mean anion movement approached that of the clay soil. The difference is explained in terms of low infiltration rate into the Florina soil.
The practical implications of leaching of nitrate in Tippera soil are briefly discussed.
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Wetselaar, R. Nitrate distribution in tropical soils. Plant Soil 16, 19–31 (1962). https://doi.org/10.1007/BF01378155
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DOI: https://doi.org/10.1007/BF01378155