Grant: Collaborative Research and Development Grants
University of Western Ontario
$11,700.00
Mudstone microstructure in a macro-stratigraphic context: Relationship to reservoir storage and flow capacity
FY 2016-17
Summary
Growing global demand for petroleum and natural gas has necessitated finding new supplies to replace declining conventional production. Traditionally, shales have been viewed as 'non-reservoir' rocks and hence of little economic importance. However, in the last decade, shales have undergone a dramatic re-appraisal in terms of their hydrocarbon resource potential. One aspect of this is driven by the development of horizontal drilling technology combined with multistage hydraulic fracture treatments to facilitate economic flow rates from very low permeability shale formations. In addition, there has been an explosion of interest in, and a steadily expanding understanding of, the various geological processes that govern mud sedimentation. Included are the physical, chemical and biological processes that cause mud particles to aggregate together, the physical processes that transport mud into and across sedimentary basins, the biochemical processes that control the cementation of mud and organic particles at burial depths of centimetres to a few metres, and the physical and chemical processes that control compaction and maturation of organic matter to burial depths of several km. This sequence of processes determines the microfabric governing the rock's capacity to store and transmit fluids, and may play an important role in the conversion of disseminated organic matter to petroleum. The proposed project will provide improved understanding of the depositional and burial processes that have affected specific shale formations in Alberta and British Columbia. The resulting knowledge may help to guide exploration efforts in these 'unconventional reservoirs', potentially leading to delineation of greater oil and gas reserves, with consequent implications for employment, royalties, and benefit to the overall Canadian economy.
Program
Collaborative Research and Development Grants
Recipient
Location
Ontario, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data
As published
Application id
461626-2013
Name nom
Plint, Guy
Department département
Earth Sciences
Organization id
36
Institution établissement
University of Western Ontario
Province en
Ontario
Province fr
Ontario
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2016
Competition year année de concours
2013
Award amount
11700
Program id
CRDPJ
Program name en
Collaborative Research and Development Grants
Program name fr
Subventions de recherche et développement coopérative
Group en
Research partnerships programs
Group fr
Programmes de partenariat
Committee code
96
Committee name en
RPP Internal Decision Cttee
Committee name fr
Cté de décision interne - PPR
Area of application code
300
Area of application group en
Energy resources
Area of application group fr
Ressources d'énergie
Area of application en
Energy resources (including production, exploration, processing, distribution and use)
Area of application fr
Ressources d'énergie (production, exploration, traitement, distribution et utilisation de l'énergie)
Research subject code
4007
Research subject group en
Earth science
Research subject group fr
Sciences de la terre
Research subject en
Sedimentology
Research subject fr
Sédimentologie
Partie
3
Nb partie
5
Application title
Mudstone microstructure in a macro-stratigraphic context: Relationship to reservoir storage and flow capacity
Keyword
NSERC
Application summary
Growing global demand for petroleum and natural gas has necessitated finding new supplies to replace declining conventional production. Traditionally, shales have been viewed as 'non-reservoir' rocks and hence of little economic importance. However, in the last decade, shales have undergone a dramatic re-appraisal in terms of their hydrocarbon resource potential. One aspect of this is driven by the development of horizontal drilling technology combined with multistage hydraulic fracture treatments to facilitate economic flow rates from very low permeability shale formations. In addition, there has been an explosion of interest in, and a steadily expanding understanding of, the various geological processes that govern mud sedimentation. Included are the physical, chemical and biological processes that cause mud particles to aggregate together, the physical processes that transport mud into and across sedimentary basins, the biochemical processes that control the cementation of mud and organic particles at burial depths of centimetres to a few metres, and the physical and chemical processes that control compaction and maturation of organic matter to burial depths of several km. This sequence of processes determines the microfabric governing the rock's capacity to store and transmit fluids, and may play an important role in the conversion of disseminated organic matter to petroleum. The proposed project will provide improved understanding of the depositional and burial processes that have affected specific shale formations in Alberta and British Columbia. The resulting knowledge may help to guide exploration efforts in these 'unconventional reservoirs', potentially leading to delineation of greater oil and gas reserves, with consequent implications for employment, royalties, and benefit to the overall Canadian economy.