scholarly journals Isotope applications to soil science at the University of Alberta — an historical perspective

2020 ◽  
Vol 100 (4) ◽  
pp. 344-355
Author(s):  
Brett C. Feland ◽  
Sylvie A. Quideau

For the past 70 yr, researchers in the Soil Science/Renewable Resources Department at the University of Alberta have used isotopes to study topics of ecological importance. This review highlights the soil isotope research conducted within our department over this time, including an historical overview of studies of interest. Analytical techniques and advances in instrumentation are discussed, focusing on the measurement of light stable isotope ratios (i.e., for C, H, N, S, and O) using isotope ratio mass spectrometry (IRMS). Early soil isotope work (1950–2000s) focused on agricultural soils and soil fertility issues. These studies included the use of radioactive isotopes such as 14C and 35S, and (or) artificially enriched stable isotopes including 15N-labelled fertilizers. More recently (2000–present), the scope of research widened to include natural-abundance stable isotope ratio studies as higher-sensitivity IRMS systems became more prevalent. Current isotope research topics include N biogeochemistry in natural and managed ecosystems, land management effects on greenhouse gas emissions, carbon cycling in northern landscapes, paleo-reconstruction in peatlands, carbon sequestration in boreal forests, and biodegradation of petroleum hydrocarbons. Further technological progress also enabled new techniques such as compound-specific IRMS analysis, including δ13C and δ2H measurements of soil n-alkanes and phospholipid fatty acids. In conclusion, current IRMS instrumentation presents unparalleled opportunities for multidisciplinary research to track carbon, plant nutrients, and pollutants as they move through soils.

2014 ◽  
Vol 86 (17) ◽  
pp. 8514-8520 ◽  
Author(s):  
Wiebke Mohr ◽  
Tiantian Tang ◽  
Sarah R. Sattin ◽  
Roderick J. Bovee ◽  
Ann Pearson

1992 ◽  
Vol 75 (6) ◽  
pp. 1107-1111 ◽  
Author(s):  
Landis W Doner, ◽  
Allan R Brause ◽  
Donald R Petrus

Abstract Stable isotope ratio mass spectrometry has shown that pure frozen concentrated orange juices (FCOJ) of 63-67° brix possess a mean δ18 value of +14.28%o, with a standard deviation of 1.80. Beet invert syrups, which are produced using ground water, possess negative values. As a result, δ18 values decrease on addition of such syrups to FCOJ. Samples with values less than +8.9%o (3 standard deviations from the mean for pure FCOJs) can confidently be considered as adulterated. A collaborative study was conducted in which a pure FCOJ and 4 samples adulterated to various levels with medium beet invert syrup were sent to each of 6 collaborators. In all but 2 instances, juices containing more than 10% beet syrup would have been classified as adulterated by the collaborators; none would have classified pure juice as adulterated. The plot of mean δ18 values for all collaborators at each adulteration level has a correlation coefficient >0.999. The method has been adopted first action by AOAC International.


2016 ◽  
Vol 217 ◽  
pp. 119-125 ◽  
Author(s):  
D.A.F. da Silva ◽  
N.P. Biscola ◽  
L.D. dos Santos ◽  
M.M.P. Sartori ◽  
J.C. Denadai ◽  
...  

2012 ◽  
Vol 60 (45) ◽  
pp. 11268-11273 ◽  
Author(s):  
Matteo Scampicchio ◽  
Tanja Mimmo ◽  
Calogero Capici ◽  
Christian Huck ◽  
Nadia Innocente ◽  
...  

2010 ◽  
Vol 24 (5) ◽  
pp. 495-500 ◽  
Author(s):  
Jennifer A. J. Dungait ◽  
Roland Bol ◽  
Elisa Lopez-Capel ◽  
Ian D. Bull ◽  
David Chadwick ◽  
...  

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