Abstract
Nitrogen-isotope analysis by the Rittenberg technique requires N in the form of NH4. Conversion of organic N to NH4-N is normally accomplished by the Kjeldahl method, which involves digestion with concentrated H2SO4. A diffusion method recently developed for isotope-ratio analysis of inorganic N in soil extracts was modified for use with Kjeldahl digests. An aliquot of the digest (to 20 mL) containing 50 to 150 µg of N was neutralized by overturning a vial with 2 mL of 20 M NaOH in a 118-mL specimen container sealed with a screw-top lid, and the NH3 liberated was collected for 6 d at room temperature in a 7-mm-diam. glass-fiber disk acidified with 10 µL of 1 M H2SO4. For automated Rittenberg analysis of the diffused NH3-N by mass spectrometry, the glass disk was tranferred to a plastic sample tray (96 samples per tray), treated with 10 µL of 28.9 M (concentrated) HF, and dried in a desiccator over anhydrous CaSO4. Studies showed that diffusion was complete (>97%) and that, when correction was made for isotopic dilution by natural-abundance N in reagents, isotope-ratio analyses of diffused N (0.2–4.2 atom % 15N) were in close agreement with analyses using conventional steam-distillation and concentration techniques.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 1151-1154 |
| Number of pages | 4 |
| Journal | Soil Science Society of America Journal |
| Volume | 56 |
| Issue number | 4 |
| DOIs | |
| State | Published - Jul 1 1992 |
ASJC Scopus subject areas
- Soil Science
Fingerprint
Dive into the research topics of 'Diffusion of Kjeldahl Digests for Automated Nitrogen-15 Analysis by the Rittenberg Technique'. Together they form a unique fingerprint.Cite this
- APA
- Standard
- Harvard
- Vancouver
- Author
- BIBTEX
- RIS