Summary
An inorganic (Bainsville) and an organic (Farnham) soil were hydrolyzed by continuous and stepwise hydrolysis with hot 3N HCl for 1, 2, 3, 4, 11, 15, 18 and 24 h and continuously with hot 6N HCl for 24 h. The following nitrogen forms were determined: total N, hydrolyzable-N, amino acid-N, amino sugar-N and ammonia-N. Proportions of ‘unknown’ N were computed from these data.
Continuous hydrolysis with 3N HCl yielded more amino acid-N and less ‘unknown’ N than did stepwise hydrolysis with the same acid strength. But continuous hydrolysis for 24 h with 6N HCl produced more amino acid-N and less ‘unknown’ N than did hydrolysis with 3N HCl by either method. It was estimated that 33 and 54% of the total N in the inorganic and organic soil, respectively, was protein-N. The ‘unknown’ N in the inorganic and organic soil constituted 51 and 37% of the total N, respectively. From our work it appears that the ‘unknown’ N is not proteinaceous. It can be readily degraded chemically and microbiologically to NH3 and N-gases. More attention needs to be given to identifying the ‘unknown’ N which constitutes a large portion of the total soil-N. A more adequate knowledge of the chemical constitution of the ‘unknown’ soil N may lead to the development of technologies that will make more efficient use of the N in soils.
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Schnitzer, M., Hindle, D.A. Effects of different methods of acid hydrolysis on the nitrogen distribution in two soils. Plant Soil 60, 237–243 (1981). https://doi.org/10.1007/BF02374108
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DOI: https://doi.org/10.1007/BF02374108