08 - Electrical properties Flashcards
Ohm’s law:
Resistivity
Res = U’/I
how strongly a material opposes the flow of electric current
measurement resistivity
slide 2
cylindrical rock sample
2 electrodes for electric current I measurement
voltage U measurement
R_t = A/L * U/I
Dielectric permittivity or absolute permittivity epsilon
measure of polarizibility
conductive and dielectric properties are coupled complex and are frequency-dependent
only effective conductor among pore fluids
water
resistivity of water is controlled by .. (5)
chemical composition
concentration
Temperature of brine/electrolyte
Volume fraction (porosity,saturation) electrolyte distribution in rock
correlation of resisticity to salinity
decrease with higher salinity
resistivity in rocks
order from low to hight
sandstone, limestone, shale&clay, gneiss etc.
shale,clay
sandstone
limestone
gneiss etc.
Resistivity log SP
electrical resisticity
in ohm m
Spontaneus Potential log
natural or spontaneous potential difference between
the borehole and the surface
in mV
detect permeable beds and to estimate clay content and formation water salinity
cationic membranes
permeable to positively charged ions (cations) and impermeable to negative ions (anions)
mud-filtrate salinity is greater than the formation water salinity
positive SP deflections
salinities of the mud filtrate and formation water are similar
no SP is generated
Shale-baseline shifts
can occur when formation waters of different salinities are separated by a shale bed that is not a perfect cationic membrane
resisitivity depends on lithology:
Evaporates
Carbonates
Shales
Sandstones
Evaporates: high
Carbonates: high
Shales: medium
Sandstones: low
effect of geological processes on resistivity
All processes that enhance the amount of water in the rock likely decrease the bulk resistivity of the rock
clay alteration, faulting, salt, shearing, etc