Organic geochemical research analytics of the petroleum industry: enhanced data density and method flexibility using gas chromatograph multiple detector coupling

2018 ◽  
Vol 484 (1) ◽  
pp. 97-106 ◽  
Author(s):  
M. Doerner ◽  
U. Berner ◽  
M. Erdmann ◽  
T. Barth

AbstractIn traditional organic geochemical investigations analyses are usually segmented in rather time-consuming single working steps that also require off-line preparation for each analytical instrument which can add to analytical bias. Since industry laboratories need to be precise, as well as cost- and time-efficient, we present a flexible and modular analytical concept which enables the user to perform advanced organic geochemical methods on a single gas chromatograph coupled to multiple detectors. The coupled analytical system can perform analyses of natural gas composition up to n-butane, stable carbon isotopes of natural gas compounds up to n-butane, identification and quantification of major compounds in oils and extracts, and compound-specific isotopes of oil and extracts. The analytical methodologies are appropriate for enhancement to broaden the application spectrum of coupled detectors.

2020 ◽  
Author(s):  
Jeffrey Osterhout ◽  
◽  
J. William Schopf ◽  
Anatoliy B. Kudryavtsev ◽  
K.D. McKeegan

2020 ◽  
Vol 58 (9) ◽  
pp. 981-993
Author(s):  
Yu. A. Morozov ◽  
V. S. Sevastianov ◽  
A. Yu. Yurchenko ◽  
O. V. Kuznetsova

2012 ◽  
Vol 42 (3) ◽  
pp. 517-531 ◽  
Author(s):  
Robert Au ◽  
Jacques C. Tardif

Stable carbon isotopes (δ13C) fixed in tree rings are dependent upon environmental conditions. Old northern white-cedar ( Thuja occidentalis L.) trees were sampled at their northwestern limit of distribution in central Canada. The objectives of the study were (i) to investigate the association between tree-ring δ13C values and radial growth in addition to the response of these variables to climate, (ii) to assess site differences between two sites varying in moisture regime, and (iii) to compare tree-ring δ13C of T. occidentalis with that of other boreal tree species growing at the northern limit of their distribution in central Canada. Over 2500 tree rings comprised of 15 T. occidentalis trees were analyzed for δ13C. Annually resolved δ13C (1650–2006) and ring-width (1542–2006) chronologies were developed. During the year of ring formation, ring width was associated with spring and early-summer conditions, whereas δ13C was more indicative of overall summer conditions. However, compared with δ13C values, ring width was more often associated with climate conditions in the year prior to ring formation. Conditions conducive to moisture stress were important for both parameters. Although ring width and δ13C corresponded to the drought intervals of the 1790s, 1840s, 1890s, 1930s, and 1960–1970, ring width may be more responsive to prolonged drought than δ13C. Tree-ring δ13C could, however, provide important information regarding physiological adaptations to drought.


2011 ◽  
Vol 18 (3) ◽  
pp. 253-264 ◽  
Author(s):  
Roland Kays ◽  
Robert S. Feranec

Author(s):  
Silviu-Laurentiu Badea ◽  
Diana-Ionela Stegarus ◽  
Violeta-Carolina Niculescu ◽  
Stanica Enache ◽  
Amalia Soare ◽  
...  

2008 ◽  
Vol 41 (3) ◽  
pp. 265-275 ◽  
Author(s):  
E. G. Morgun ◽  
I. V. Kovda ◽  
Ya. G. Ryskov ◽  
S. A. Oleinik

2003 ◽  
Vol 22 (2) ◽  
pp. 179-184 ◽  
Author(s):  
Liu Qiming ◽  
Wang Shijie ◽  
Piao Hechun ◽  
Ouyang Ziyuan

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