TY - JOUR
T1 - A technique to facilitate diffusions for nitrogen-isotope analysis by direct combustion
AU - Moran, K. K.
AU - Mulvaney, R. L.
AU - Khan, S. A.
N1 - Copyright:
Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2002
Y1 - 2002
N2 - A technique was developed that permits the use of boric acid-indicator solution in carrying out diffusions for inorganic 15N analysis of soil extracts by direct combustion, so as to eliminate the need for a separate quantitative determination. In this technique, the titrated sample is acidified with 2.5 M KHSO4 and subsequently treated with methanol to remove H3BO3. The NH4+-N is dissolved in 1 mL of deionized water, concentrated after transfer to a microcentrifuge tube, and freeze-dried in a tin capsule. Isotope-ratio analyses were accurate to within 5% when diffusions were performed on 100 to 1000 μg of NH4+-N (0.2-10 atom % 15N), whereas errors of 8 to 17% occurred with 25 to 50 μg of labeled N, even after correction for isotopic dilution by atmospheric NH3. The technique described permits 15N analysis of any form of N that can be recovered by H3BO3 diffusion of soil, soil extracts, soil hydrolysates, Kjeldahl digests, water, or wastewater.
AB - A technique was developed that permits the use of boric acid-indicator solution in carrying out diffusions for inorganic 15N analysis of soil extracts by direct combustion, so as to eliminate the need for a separate quantitative determination. In this technique, the titrated sample is acidified with 2.5 M KHSO4 and subsequently treated with methanol to remove H3BO3. The NH4+-N is dissolved in 1 mL of deionized water, concentrated after transfer to a microcentrifuge tube, and freeze-dried in a tin capsule. Isotope-ratio analyses were accurate to within 5% when diffusions were performed on 100 to 1000 μg of NH4+-N (0.2-10 atom % 15N), whereas errors of 8 to 17% occurred with 25 to 50 μg of labeled N, even after correction for isotopic dilution by atmospheric NH3. The technique described permits 15N analysis of any form of N that can be recovered by H3BO3 diffusion of soil, soil extracts, soil hydrolysates, Kjeldahl digests, water, or wastewater.
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U2 - 10.2136/sssaj2002.1008
DO - 10.2136/sssaj2002.1008
M3 - Article
AN - SCOPUS:0036240245
SN - 0361-5995
VL - 66
SP - 1008
EP - 1011
JO - Soil Science Society of America Journal
JF - Soil Science Society of America Journal
IS - 3
ER -