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1963
DOI: 10.4141/cjss63-041
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The Effect of Nitrate Nitrogen in the Soil Profile on the Response of Barley to Fertilizer Nitrogen

Abstract: Barley was shown to have a variable response to fertilizer nitrogen in nine field trials on non-fallow land. A large part of this variability could be accounted for by differences in the nitrate nitrogen content of the soil profile at seeding time.It was demonstrated that nitrate nitrogen can accumulate in non-fallow soil profiles in large amounts and that this nitrogen influences the uptake of nitrogen by barley to the same extent as does nitrogen added as fertilizer.Various tests for "available" nitrogen wer… Show more

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Cited by 68 publications
(34 citation statements)
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“…Soil test labs generally consider nitrate to a depth of 60 cm (Selles et al 1992), but residual nitrate to 120 cm is also accessible (Soper and Huang 1963). For the purposes of production, it is differences in plant-available N supply which are of interest.…”
Section: Residual Nitratementioning
confidence: 99%
“…Soil test labs generally consider nitrate to a depth of 60 cm (Selles et al 1992), but residual nitrate to 120 cm is also accessible (Soper and Huang 1963). For the purposes of production, it is differences in plant-available N supply which are of interest.…”
Section: Residual Nitratementioning
confidence: 99%
“…Soil NO 3 -N tests have been developed to predict the amount of inorganic fertilizer N required to obtain optimum yield for many crops under a wide variety of climatic conditions (Hergert 1986). Soil NO 3 -N tests are used in western Canada and USA prior to planting to predict N requirements of wheat (Triticum aestivum L.) and corn (Zea mays L.) (Soper and Huang 1963;Dahnke and Johnson 1990). A midseason test is also used to determine the need for additional N fertilizer for corn (Sims et al 1995;Zebarth and Paul 1997).…”
Section: Mots Clésmentioning
confidence: 99%
“…To reduce N losses to the environment, new techniques for predicting fertilizer N requirements of crops are required. A test of soil NO 3 -N is a good direct measure of available N under hot and dry environments such as those in western Canada and the Great Plains of the United States of America (Soper and Huang 1963;Dahnke and Johnson 1990). Under the cold-humid environment of Atlantic Canada, a test of soil NO 3 -N might not work as well because mineralization of organic N supplies represents a significant portion of the total crop N requirements.…”
mentioning
confidence: 99%