Characterization of Thermogenic Gases from Polish Bituminous Coals by Hydrous Pyrolysis and Stable Isotopes :ABSTRACT

AAPG Bulletin ◽  
1997 ◽  
Vol 81 (1997) ◽  
Author(s):  
KOTARBA, MACIEJ J., and MICHAEL D.
2016 ◽  
Vol 46 (3) ◽  
pp. 271-284 ◽  
Author(s):  
Guillem Mateu-Vicens ◽  
Teresa Sebastián ◽  
Anna Khokhlova ◽  
Maria del Mar Leza ◽  
Salud Deudero

2003 ◽  
Vol 19 (2) ◽  
pp. 209-214 ◽  
Author(s):  
Jean-François Mauffrey ◽  
François Catzeflis

Stable isotopes are commonly used in ecological studies to infer food resources (Ambrose & DeNiro 1986, Bocherens et al. 1990,1991,1994;Yoshinaga et al. 1991) since isotopic composition is conserved during the feeding process. Moreover,for herbivorous (sensu lato) species, it is often possible to identify the main resource because different photosynthetic pathways generate different values of carbon isotope ratios (Park & Epstein 1961, Sternberg et al. 1984). This allows the characterization of broad biota such as savannas or forest and discrimination of grazers from sympatric folivorous species (DeNiro & Epstein 1978).


2009 ◽  
Vol 23 (9) ◽  
pp. 4553-4561 ◽  
Author(s):  
Josefa M. Griffith ◽  
Caroline E. Burgess Clifford ◽  
Leslie R. Rudnick ◽  
Harold H Schobert

Oecologia ◽  
1996 ◽  
Vol 107 (2) ◽  
pp. 232-238 ◽  
Author(s):  
J. Vaun McArthur ◽  
Kevin K. Moorhead

OENO One ◽  
1995 ◽  
Vol 29 (2) ◽  
pp. 75
Author(s):  
M. Day ◽  
Ben Li Zhang ◽  
Gérard J. Martin ◽  
Christian Asselin ◽  
René Morlat

<p style="text-align: justify;">Stable isotope and elemental analyses were applied to the study of wines produced from the Cabernet Franc vine variety cultivated during several years (1982 to 1990) on specific parts of the Saumur-Champigny vineyard dedicated to the « terroir » experiment of INRA. The purpose of this work was to describe the behaviour or <sup>2</sup>H, <sup>13</sup>C and <sup>18</sup>O isotopes in the water and ethanol of wines in terms of the meteorological conditions (temperature, precipitation and insolation) which govern vine growing. Since the « terroir » concept involves a synergy between the c1imate and the soil, the distribution of typical metallic elements was also determined by flame and electrothermal ionization atomic absorption. About twenty parcels, carefully described from the geological and pedological point of view were considered in this study which demonstrated the ability of Sr, Al and Rb to discriminate between wines from the same year but grown on adjacent parcels. The content in trace elements of the wines was also shown to be correlated with the geological nature of the soil. As far as stable isotopes are considered, it appears that the climate of the year of production of a given region has a drastic influence on the isotope ratios of water and ethanol of wines and good correlations way be computed between these parameters and temperature and precipitations. From a more basic aspect, it is also shown that the nature of the soil which governs, at least in a part, the water use efficiency of vine, induces typical variations in the isotopic composition of wines. The results of this study demonstrate also the ability of stable isotope and elemental analyses to determine the geographical origin of a wine, and when the region of production is known, to infer the year of production from meteorological data. This method might prove to be an alternative method to radio carbon analysis for the next vintages.</p>


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