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Determination and Isotope‐Ratio Analysis of Different Forms of Nitrogen in Soils: 7. Urea
Author(s) -
Keeney D. R.,
Bremner J. M.
Publication year - 1967
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1967.03615995003100030011x
Subject(s) - chemistry , urease , urea , distillation , titration , soil water , ammonium , potassium , ammonium nitrate , extraction (chemistry) , potassium phosphate , chromatography , nitrogen , nitrate , soil test , potassium nitrate , steam distillation , environmental chemistry , inorganic chemistry , biochemistry , organic chemistry , environmental science , soil science
Two methods of determining urea in soils are described. In one (extraction‐distillation method), the soil sample is extracted with 2 M KCl (10 ml/g of soil) for 5 min, and an aliquot of the extract is treated with potassium phosphate buffer (pH 8.0) and urease for 2 hours at 30C to convert urea N to ammonium N. In the other (direct‐distillation method), the soil sample is treated directly with pH 8.0 potassium phosphate buffer and urease for 1 hour at 30C. In both, the ammonium released by the urease treatment is separated by steam distillation of the treated sample for 3.3 min and determined by titration of the distillate with standard acid. The extraction‐distillation method is useful when analyses for nitrate and nitrite as well as urea are required, but it does not give completely quantitative recovery of urea added to some soils. The methods are rapid, specific and precise, and they permit isotope‐ratio analysis of urea N in N 15 ‐tracer studies of urea transformations in soils.