2018
DOI: 10.1306/eg.04121817020
|View full text |Cite
|
Sign up to set email alerts
|

A multi-isotope approach to determine the origin of methane and higher alkanes in groundwater of the St. Lawrence Platform, Saint-Édouard area, eastern Canada

Abstract: Hooshang Pakdel and Jade Bergeron from the GSC-Quebec Delta-Lab, Yves Gélinas from Concordia University, the GSC field crews involved in acquiring the data, and Marianne Molgat for her support, interest and for the sharing of information and data from Talisman Energy. The project was supported by the Ministère du Développement durable, de l'Environnement et de la near major fault zones indicates that these may serve as preferential migration pathway over a certain depth, but most likely no more than 200 to 500… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

1
13
0

Year Published

2018
2018
2024
2024

Publication Types

Select...
5

Relationship

2
3

Authors

Journals

citations
Cited by 10 publications
(14 citation statements)
references
References 63 publications
(87 reference statements)
1
13
0
Order By: Relevance
“…Considering the CH4- 2 H values in our samples, and based on published isotopic fractionation factors for methane oxidation, this process does not appear to be significant in the Saint-Édouard area, except for Ca-HCO3 type samples with very low methane concentrations and relatively high CH4-δ 13 C values (pink diamonds on Figure 8-A). Moreover, comparison of CH4- H and H2O- 2 H values confirmed that methane isotopic values in most samples are consistent with regular (non-oxidized) microbial methane formed via the CO2 reduction pathway using the local groundwater (Bordeleau et al, 2018b).…”
Section: Resultssupporting
confidence: 63%
See 4 more Smart Citations
“…Considering the CH4- 2 H values in our samples, and based on published isotopic fractionation factors for methane oxidation, this process does not appear to be significant in the Saint-Édouard area, except for Ca-HCO3 type samples with very low methane concentrations and relatively high CH4-δ 13 C values (pink diamonds on Figure 8-A). Moreover, comparison of CH4- H and H2O- 2 H values confirmed that methane isotopic values in most samples are consistent with regular (non-oxidized) microbial methane formed via the CO2 reduction pathway using the local groundwater (Bordeleau et al, 2018b).…”
Section: Resultssupporting
confidence: 63%
“… 13 C values resembling thermogenic gas, and higher than expected DIC- 13 C values. An in-depth interpretation of these geochemical parameters (Bordeleau et al, 2018b) revealed that many samples contained late-stage microbial gas (Figure 8-C). Noteworthy, several of these samples also contain some thermogenic gas (Figure 8-B, C).…”
Section: Resultsmentioning
confidence: 99%
See 3 more Smart Citations