The very high proportion of soil N occurring in amino sugar N in non responsive soils used by Mulvaney and Khan prompted a re-examination of the basis of amino sugar N determinations by a) alkali estimation of amino sugar N in situ using the diffusion method (Illinois soil N test) and b) alkali estimation of amino sugar N in neutralized soil acid hydrolysates using the steam distillation method.
Results show that both methods share common deficiencies that may lead to underestimation of amino sugar N e.g. inadequate temperature control.
Additionally not more than 1% of the N contained in polymeric amino sugars such as chitin, free or present in microbial cell walls and soil organic matter could be released as ammonia after 5 hours exposure to 2M NaOH at 50°C whereas 90% of the N present in glucosamine and galactosamine could be accounted for as ammonia under these conditions.
Acid hydrolysis completely solubilized chitin and steam distillation of neutralized hydrolysates with buffer accounted for >90% and 50% of glucosamine and galactosamine-N respectively as ammonia. Use of NaOH increased recovery of galactosamine-N to 80% during steam distillation.
It is suggested that the usefulness of the Illinois soil N test may be limited to local rather than universal use and that the search for chemical tests of soil fertility need to include a fuller understanding of the below ground system and its linkages above ground.
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