Grant: Discovery Grants Program - Individual
Memorial University of Newfoundland
$16,480.00
Modelling and inversion of geophysical electromagnetic data
FY 2010-11
Summary
The goal of geophysics is to understand, and perhaps predict, the dynamic processes that move and shape the Earth beneath our feet, and to ""look"" into the Earth to see these processes in action, or their consequences. One technique for remotely sensing what the structure of the subsurface is, even to depths of tens of kilometres, uses electromagnetic fields. In this technique, electric currents are induced to flow in the rocks. The strength and disposition of the currents depend on rock type. Metallic ores, for example, are relatively good at conducting electricity. The induced currents in the ground give rise, in turn, to electromagnetic fields which can be measured. The strengths and variations of these measurements depend on the induced currents, and so on the rocks themselves. It is therefore possible to turn the measurements on their heads, that is, invert them, and extract information about what the rock types are in the subsurface. The proposed research determines to (i) improve the mathematics used by computer programs to predict what the induced currents would be if the rock types in the subsurface were known, and (ii) improve the programs that invert measurements of the electromagnetic fields to generate models of the structure of the Earth. Recent advances have produced what is effectively the first generation of these programs for fully three-dimensional models of the Earth. However, the mathematical representations these programs use for the arrangements of rock types in the subsurface are basic, being neither flexible enough to cope with the complicated structures that occur in nature, nor precise enough to handle the dramatic changes between adjacent rock types that can exist for certain important features such as ore deposits. This research programme will investigate the use of more sophisticated and refined representations of the subsurface to overcome these problems. The result will be computer programs that can provide more detailed and more reliable models, or ""images"", of the subsurface. These programs will be of use to the mining industry, enabling new ore deposits to be found. They will also be of use in remotely sensing groundwater resources, geotechnical applications, and in determining the deep structure of the Earth's crust.
Program
Discovery Grants Program - Individual
Recipient
Location
Newfoundland and Labrador, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data
As published
Application id
326988-2007
Name nom
Farquharson, Colin
Department département
Earth Sciences
Organization id
89
Institution établissement
Memorial University of Newfoundland
Province en
Newfoundland and Labrador
Province fr
Terre-Neuve-et-Labrador
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2010
Competition year année de concours
2007
Award amount
16480
Program id
RGPIN
Program name en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
8
Committee name en
Solid Earth Sciences
Committee name fr
Sciences de la Terre solide
Area of application code
202
Area of application group en
Natural resources (economic aspects)
Area of application group fr
Ressources naturelles (aspects économiques)
Area of application en
Mineral resources ( prospecting, exploration, mining, extraction, processing)
Area of application fr
Ressources minérales (prospection, exploration, mines, extraction et préparation)
Research subject code
4300
Research subject group en
Geophysics
Research subject group fr
Géophysique
Research subject en
Geophysics
Research subject fr
Géophysique
Partie
4
Nb partie
5
Application title
Modelling and inversion of geophysical electromagnetic data
Keyword
NSERC
Application summary
The goal of geophysics is to understand, and perhaps predict, the dynamic processes that move and shape the Earth beneath our feet, and to ""look"" into the Earth to see these processes in action, or their consequences. One technique for remotely sensing what the structure of the subsurface is, even to depths of tens of kilometres, uses electromagnetic fields. In this technique, electric currents are induced to flow in the rocks. The strength and disposition of the currents depend on rock type. Metallic ores, for example, are relatively good at conducting electricity. The induced currents in the ground give rise, in turn, to electromagnetic fields which can be measured. The strengths and variations of these measurements depend on the induced currents, and so on the rocks themselves. It is therefore possible to turn the measurements on their heads, that is, invert them, and extract information about what the rock types are in the subsurface. The proposed research determines to (i) improve the mathematics used by computer programs to predict what the induced currents would be if the rock types in the subsurface were known, and (ii) improve the programs that invert measurements of the electromagnetic fields to generate models of the structure of the Earth. Recent advances have produced what is effectively the first generation of these programs for fully three-dimensional models of the Earth. However, the mathematical representations these programs use for the arrangements of rock types in the subsurface are basic, being neither flexible enough to cope with the complicated structures that occur in nature, nor precise enough to handle the dramatic changes between adjacent rock types that can exist for certain important features such as ore deposits. This research programme will investigate the use of more sophisticated and refined representations of the subsurface to overcome these problems. The result will be computer programs that can provide more detailed and more reliable models, or ""images"", of the subsurface. These programs will be of use to the mining industry, enabling new ore deposits to be found. They will also be of use in remotely sensing groundwater resources, geotechnical applications, and in determining the deep structure of the Earth's crust.