z-logo
Premium
Diffusion technique for 15 N and inorganic N analysis of low‐N aqueous solutions and Kjeldahl digests
Author(s) -
Chen Rui Rui,
Dittert Klaus
Publication year - 2008
Publication title -
rapid communications in mass spectrometry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.528
H-Index - 136
eISSN - 1097-0231
pISSN - 0951-4198
DOI - 10.1002/rcm.3525
Subject(s) - chemistry , kjeldahl method , aqueous solution , diffusion , analytical chemistry (journal) , chromatography , nuclear chemistry , inorganic chemistry , nitrogen , organic chemistry , physics , thermodynamics
Diffusion of ammonia is a common sample preparation method for the stable isotope analysis of inorganic nitrogen in aqueous solution. Classical diffusion methods usually require 6–12 days of diffusion and often focus on 15 N/ 14 N analysis only. More recent studies have discussed whether complete N recovery was necessary for the precise analysis of stable N isotope ratios. In this paper we present a newly revised diffusion technique that allows correct and simultaneous determination of total N and 15 N at% from aqueous solutions and Kjeldahl digests, with N concentrations down to sub‐0.5‐mg N L −1 levels, and it is tested under different conditions of 15 N isotope labelling. With the modification described, the diffusion time was reduced to 72 h, while the ratios of measured and expected 15 N at% were greater than 99% and the simultaneous recovery of total N was >95%. Analysis of soil microbial biomass N and its 15 N/ 14 N ratio is one of the most important applications of this diffusion technique. An experiment with soil extracts spiked with 15 N‐labelled yeast showed that predigestion was necessary to prevent serious N loss during Kjeldahl digestion of aqueous samples (i.e. soil extracts). The whole method of soil microbial biomass N preparation for 15 N/ 14 N analysis included chloroform fumigation, predigestion, Kjeldahl digestion and diffusion. An experiment with soil spiked with 15 N‐labelled yeast was carried out to evaluate the method. Results showed a highly significant correlation of recovered and added N, with the same recovery rate (0.21) of both total N and 15 N. A k N value of 0.25 was obtained based on the data. In conclusion, the diffusion method works for soil extracts and microbial biomass N determination and hence could be useful in many types of soil/water studies. Copyright © 2008 John Wiley & Sons, Ltd.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom