Onepot You wrote "I want to understand how the field size / boundary is established. I want to understand how the water molecules at this boundary behave / move."
My understanding is as follows: # Any voids in granite are full of superheated water naturally (Remember it used to be called hot dry rocks. Well its wet) # Applied pressure of 9000 psi has fractured an area some 2km (X direction arbitrary) by 3 km (Y direction) by 100metres deep (Z direction.) # In terms of boundaries there is the original boundary which to my understanding the granite has a very limited (neglible) porosity though by virtue of the fact that it saturated I assume it has some porosity.) # The 2nd boundary to consider is the boundary established by the fracturing. Relative to the naturally occuring fractures these are large. # I understand that there is expected to be nil or neglible loss of water once the system is primed and operational # The tracers which are to be added to the water during the closed circulation testing I expect will answer a lot of questions as to the primary water movements, effective surface area of the system and if any water is lost from the system.
RNE Price at posting:
0.0¢ Sentiment: LT Buy Disclosure: Held
A personalised tool to help users track selected stocks. Delivering real-time notifications on price updates, announcements, and performance stats on each to help make informed investment decisions.
(20min delay)