A technique to recover tracer as carboxyl-carbon and alpha-nitrogen from amino acids in soil hydrolysates

J AOAC Int. 2003 Nov-Dec;86(6):1106-11.

Abstract

Isotope analysis of biochemical compounds provides an unequivocal means for detecting assimilation of tracer C and N into microbial biomass. A diffusion method recently developed to determine amino acid-N by ninhydrin oxidation of soil hydrolysates was modified to permit simultaneous collection of the CO2 liberated during this oxidation. In the technique described herein, this is accomplished after removal of (NH4+ + amino sugar)-N, by performing ninhydrin oxidation at 90 degrees C for 7 h in a 1.9 L Mason jar sealed with a lid equipped to support a petri dish containing 5 mL 0.2N NaOH. Recoveries of carboxyl-C and alpha-N ranged from 98 to 101% in evaluations with standard solutions of amino acids, whereas these recoveries exceeded 90% for 14C and 94% for 15N when soil hydrolysates amended with labeled amino acids were analyzed.

MeSH terms

  • Alanine / analysis
  • Amino Acids / analysis*
  • Carbon / analysis*
  • Diffusion
  • Hydrolysis
  • Indicators and Reagents
  • Ninhydrin
  • Nitrogen / analysis*
  • Reproducibility of Results
  • Soil / analysis*

Substances

  • Amino Acids
  • Indicators and Reagents
  • Soil
  • Carbon
  • Ninhydrin
  • Nitrogen
  • Alanine