scholarly journals Assessing potential impacts of shale gas development on shallow aquifers through upward fluid migration: A multi-disciplinary approach applied to the Utica Shale in eastern Canada

2019 ◽  
Vol 100 ◽  
pp. 466-483 ◽  
Author(s):  
C. Rivard ◽  
G. Bordeleau ◽  
D. Lavoie ◽  
R. Lefebvre ◽  
P. Ladevèze ◽  
...  
2018 ◽  
Vol 108 ◽  
pp. 157-170 ◽  
Author(s):  
P. Ladevèze ◽  
S. Séjourné ◽  
C. Rivard ◽  
D. Lavoie ◽  
R. Lefebvre ◽  
...  

2020 ◽  
Vol 35 (6) ◽  
pp. 1353-1370
Author(s):  
Laura S. Farwell ◽  
Petra B. Wood ◽  
Randy Dettmers ◽  
Margaret C. Brittingham

Ground Water ◽  
2017 ◽  
Vol 55 (4) ◽  
pp. 443-454 ◽  
Author(s):  
Jean-Philippe Nicot ◽  
Toti Larson ◽  
Roxana Darvari ◽  
Patrick Mickler ◽  
Michael Slotten ◽  
...  

2015 ◽  
Vol 49 (7) ◽  
pp. 4765-4771 ◽  
Author(s):  
Anja Moritz ◽  
Jean-Francois Hélie ◽  
Daniele L. Pinti ◽  
Marie Larocque ◽  
Diogo Barnetche ◽  
...  

Author(s):  
Ann M. Eisenberg

The debate surrounding the use of hydraulic fracturing (also known as “fracking” or “HF”) to extract natural gas from the Marcellus and Utica shale deposits is often characterized as a tension between economic development and environmental risks.  But frequently missing from this dichotomy is the fact that the concerns of many who oppose HF use extend beyond the purely “environmental,” and also include concerns about issues such as “the natural resource curse” and losing autonomy.  These concerns ring of “environmental justice” rather than “environmentalism.”  Environmental justice espouses the belief that no group should bear disproportionate environmental consequences resulting from industrial activity, and that people affected by industrial activity should be meaningfully involved in implementation.  Although some federal and state policies acknowledge principles of environmental justice, it has yet to be meaningfully incorporated into any legal framework in the United States.This Article argues that a nuanced characterization of the HF controversy should include a more robust discussion of both environmental justice and discourse in order to account for the inordinate burden residents of Appalachia have historically borne in fossil fuel production.  Part I examines relevant regional economic and social dynamics, including the natural resource curse, Appalachia’s unique vulnerabilities, efforts to portray opponents of shale gas development as “anti-science,” and the environmental justice movement’s relationship to extractive industries.  Part II reviews the use of modern HF technology and applicable legal frameworks in West Virginia, Pennsylvania, Ohio, and New York.  Part III argues that across Ohio, Pennsylvania, and West Virginia, environmental justice issues have arisen from shale gas development, including problems stemming from information asymmetries, power asymmetries, and limited access to justice.  In Part IV, the Article argues that the “anti-science” portrayal of shale gas opponents is unjustified, and that such “discourse-framing” obfuscates the actual costs and limitations on benefits of HF use, and thus, becomes an environmental justice issue itself.  Part IV also argues that environmental justice concerns shaped public sentiment in New York, and that the resulting “moral outrage” added to New York’s policy decision to ban HF altogether.  In Part V, the Article suggests that ideas which transcend the study of “moral outrage”/risk assessment and environmental justice advocacy may offer a way forward.


1999 ◽  
Vol 3 (3) ◽  
pp. 421-427 ◽  
Author(s):  
H. S. Salem

Abstract. Fluid transmissivity (layer thickness times permeability) and electric transverse resistance (layer thickness time resistivity) are important parameter in groundwater and hydrocarbon exploration. Determination of these parameters provides a good knowledge of the potential of porous media, because they relate fluid flow to electric-current conduction, in terms of layer thickness, permeability and resistivity. In this study, both parameters were determined for shallow aquifers (Schleswig-Holstein, northern Germany) and deep reservoirs (Jeanne d'Arc Basin, offshore of eastern Canada), utilizing surface and well-log electric measurements. Direct relationships between both parameters, with coefficients of correlation of 0.99 (for the aquifers) and 0.94 (for the reservoirs), were obtained. The relationships suggest that an increase in both parameters indicate presence of zones of high fluid potential within the aquifers and the reservoirs.


Ground Water ◽  
2015 ◽  
Vol 54 (3) ◽  
pp. 345-353 ◽  
Author(s):  
Liwei Zhang ◽  
Daniel J. Soeder

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