Online induction heating for determination of isotope composition of woody stem water with laser spectrometry: a methods assessment

2016 ◽  
Vol 52 (3) ◽  
pp. 309-325 ◽  
Author(s):  
Brynne E. Lazarus ◽  
Matthew J. Germino ◽  
Jessica L. Vander Veen
2019 ◽  
Vol 15 ◽  
pp. 02033
Author(s):  
B. Gabel

Global wine and alcohol trade faces a serious economic problem linked to counterfeiting of these commodities. Recently applied authentication methods and techniques pose more difficulties for counterfeiters but they are apparently not effective once we consider economical losses identified by EU legal authorities. The presented solution links isotopic characteristics of the soil, plant, technological intermediate product and the final food product (wine, grapes) on the basis of 87Sr/86Sr isotopes ratios. For the isotopic signature of wines, the average isotope composition of the substrate cannot be a reliable indicator. Only the isotopic composition of pore water can, as it leaches various mineral phases at different stages and passes into vine root system. Instead of complicated sampling of pore water, an original method of preparing and processing soil samples and consequently must & wine samples was developed. Based on both, soil and biological material analysis, we can unquestionably determine not only geographical but also regional and local authenticity of the wine. Determination of red wines isotopic signature is more straightforward process in comparison to white wines, because of technologically different processing of grapes. That is the reason why, in case of white vines, the 87Sr/86Sr ratio of bentonites (natural purifier and absorbent useful in the process of winemaking) must also be taken into consideration. Results of analyses of Slovak wines from geographically diverse regions as well as from sites in close-by distances have clearly established reliability of presented concept, in which the soil is linked to the plant and to the final food product (wine or table grapes).


1995 ◽  
Vol 31 (3) ◽  
pp. 2158-2161 ◽  
Author(s):  
Ghun-Deok Suh ◽  
Hong-Bae Lee ◽  
Song-Yop Hahn ◽  
Tae-Kyung Chung ◽  
Il-Han Park

2017 ◽  
Vol 36 (3) ◽  
pp. 421-425 ◽  
Author(s):  
Guangliang Wu ◽  
Jian-Ming Zhu ◽  
Decan Tan ◽  
Guilin Han ◽  
Lixing Zhang ◽  
...  

2011 ◽  
Vol 149 (1) ◽  
pp. 141-145 ◽  
Author(s):  
HUAIYU HE ◽  
JIMIN SUN ◽  
QIULI LI ◽  
RIXIANG ZHU

AbstractKnowing when the Tibetan Plateau reached its present elevation is important for understanding the uplift history of Tibet. Recently, Rowley & Currie (2006) suggested that central Tibet exceeded 4000 m from 35 Ma to the Pliocene using the oxygen-isotope composition of calcareous minerals in Lunpola basin sediments. However, they adopted a poor age assignment for the Dingqing Formation in the Lunpola basin based on previous microfossil studies. In this study, we present SIMS U–Pb zircon dates from a bentonite layer intercalated within the middle to lower Dingqing Formation. Twenty-six measurements yield a highly reliable U–Pb age of 23.5 ± 0.2 Ma (2σ, MSWD = 1.1), suggesting that the deposition age of the Dingqing Formation is late Oligocene to early Miocene, much older than the Miocene–Pliocene age used by Rowley & Currie (2006). This age robustly constrains the age of Cenozoic sedimentary strata in central Tibet, and hence provides an important basis for estimating the palaeoelevation in the high Tibet during the geological past.


1999 ◽  
Vol 71 (23) ◽  
pp. 5297-5303 ◽  
Author(s):  
E. R. Th. Kerstel ◽  
R. van Trigt ◽  
J. Reuss ◽  
H. A. J. Meijer

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