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a Dep. of Forest Resources, Univ. of Idaho, P.O. Box 441133, Moscow, ID 83844-1133
b current address: Dep. of Life and Physical Sciences, Lincoln Univ., 816 Chestnut St., Jefferson City, MO 65101
* Corresponding author (stephank{at}lincolnu.edu).
Knowing the isotopic signature of inorganic N in soil is an important component in understanding N cycling processes. We tested the suitability of the diffusion method, a relatively simple and inexpensive method commonly applied to samples containing 15N at tracer level, for KCl extracts containing low amounts of NH4+ and NO3– at natural 15N abundance. We developed methods to quantify and correct errors affecting target
15N values resulting from N contamination in reagents and incomplete N recovery from KCl solution. After correcting for these sources of error, we assessed precision and accuracy. We found contamination in reagents to be negligible (0.8–2% of total sample N; sample N = target N + contaminant N) for NH4+ diffusions but considerable (7–13.4% of total sample N) in NO3– diffusions containing 50 µg target N. Failure to correct for the isotopic values of contaminants, which we found to be depleted by 10
relative to target
15N, in NO3– diffusions would have resulted in underestimating target
15N by 0.8 to 1.6
, depending on the amounts of reagents used. We found that sample
15N will be underestimated by approximately 0.2
(NH4+ diffusions) and 0.26
(NO3– diffusions) for every 1% short of complete recovery of sample N. After correcting for reagent N contamination and incomplete recovery, we found the precision and accuracy (1 SD) of the diffusion procedure to range from 0.2 and 1.3%. We conclude that the diffusion method can be applied to KCl extracts containing 15N at natural abundance if a precision or accuracy of <1.3
is not required.
Abbreviations: CI, confidence interval DA, Devarda's alloy DI, deionized IRMS, isotope ratio mass spectrometer ISIL, Idaho Stable Isotope Laboratory
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