The challenge of understanding how localized deformation modifies fluid flow in porous rock is addressed. New approaches are presented, based on neutron radiography and digital image analyses, to track fluid flow in rock specimens and to calculate flow velocity fields providing local flow measurements. The results show that neutron radiography, backed up by appropriate image analysis, is a very powerful tool in this context, being far more sensitive to the fluids in the rock than X-ray radiography. Analysis of neutron radiography images of water imbibition into a laboratory-deformed sandstone specimen has provided new measurements of local fluid flow velocities within a shear band, indicating that flow is faster and water storage is higher ...
Neutron imaging is used for direct observation of evolving water–air and deuterated water–normal wat...
Understanding fluid flow in rocks is crucial to quantify many natural processes such as ground water...
Understanding fluid flow in rocks is crucial to quantify many natural processes such as ground water...
Understanding fluid flow through rocks is of key interest in hydrocarbon production and CO(2) seques...
Understanding fluid flow through rocks is of key interest in hydrocarbon product...
Understanding the mechanical behaviour of porous rocks and how this influences the fluid flow is key...
Understanding the mechanical behaviour of porous rocks and how this influences the fluid flow is key...
The behaviour of subsurface-reservoir porous rocks is a central topic in the resource engineering in...
The behaviour of subsurface-reservoir porous rocks is a central topic in the resource engineering in...
Neutron transmission imaging is a technique ideally suited for imaging various flow phenomena in con...
High speed neutron tomographies 1 min acquisition have been acquired during water invasion into a...
AbstractEnhanced geothermal systems seek to expand the potential for geothermal energy by engineerin...
The textural and geometrical properties of the pore networks (i.e., such as pore size distribution, ...
The behaviour of subsurface reservoir porous rocks is a central topic in the resource engineering in...
A new approach to characterise the evolution and coupling of deformation and fluid flow in geomateri...
Neutron imaging is used for direct observation of evolving water–air and deuterated water–normal wat...
Understanding fluid flow in rocks is crucial to quantify many natural processes such as ground water...
Understanding fluid flow in rocks is crucial to quantify many natural processes such as ground water...
Understanding fluid flow through rocks is of key interest in hydrocarbon production and CO(2) seques...
Understanding fluid flow through rocks is of key interest in hydrocarbon product...
Understanding the mechanical behaviour of porous rocks and how this influences the fluid flow is key...
Understanding the mechanical behaviour of porous rocks and how this influences the fluid flow is key...
The behaviour of subsurface-reservoir porous rocks is a central topic in the resource engineering in...
The behaviour of subsurface-reservoir porous rocks is a central topic in the resource engineering in...
Neutron transmission imaging is a technique ideally suited for imaging various flow phenomena in con...
High speed neutron tomographies 1 min acquisition have been acquired during water invasion into a...
AbstractEnhanced geothermal systems seek to expand the potential for geothermal energy by engineerin...
The textural and geometrical properties of the pore networks (i.e., such as pore size distribution, ...
The behaviour of subsurface reservoir porous rocks is a central topic in the resource engineering in...
A new approach to characterise the evolution and coupling of deformation and fluid flow in geomateri...
Neutron imaging is used for direct observation of evolving water–air and deuterated water–normal wat...
Understanding fluid flow in rocks is crucial to quantify many natural processes such as ground water...
Understanding fluid flow in rocks is crucial to quantify many natural processes such as ground water...