1977•Communications in Soil Science and Plant AnalysisRequires access

Ammonium and nitrate nitrogen; Their behaviour in Nova Scotia's acid podzol soils

L. R. Townsend

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Abstract

The application of NH4NO3 to a light sandy loam and a heavy silty clay loam revealed that irrespective of whether soil was limed or unlimed, NH4‐N was neither nitrified nor lost during winter but NO3‐N was completely removed from the light soil and substantially reduced in the heavy. Under simulated summer weather much of the NH4‐N was nitrified when either the sandy loam or the silty clay loam was limed and it was in the NO3‐N form that most of the losses occurred, probably by denitrification.

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What this paper is about

The application of NH4NO3 to a light sandy loam and a heavy silty clay loam revealed that irrespective of whether soil was limed or unlimed, NH4‐N was neither nitrified nor lost during winter but NO3‐N was completely removed from the light soil and substantially reduced in the heavy. Under simulated summer weather much of the NH4‐N was nitrified when either the sandy loam or the silty clay loam was limed and it was in the NO3‐N form that most of the losses occurred, probably by denitrification.

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Available abstract

The application of NH4NO3 to a light sandy loam and a heavy silty clay loam revealed that irrespective of whether soil was limed or unlimed, NH4‐N was neither nitrified nor lost during winter but NO3‐N was completely removed from the light soil and substantially reduced in the heavy. Under simulated summer weather much of the NH4‐N was nitrified when either the sandy loam or the silty clay loam was limed and it was in the NO3‐N form that most of the losses occurred, probably by denitrification.

Key concepts: Loam, Podzol, Soil water, Ammonium, Nitrate, Ammonium nitrate, Chemistry, Nitrogen

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