PNGE 450 EXAM 1 SP Log Flashcards
SP Log introduction
(Spontaneous Potential Log)
SP is a passive measurement and no energy is provided
by the logging tool.
SP log is a record of direct current (DC) voltage
differences between the naturally occurring potential of a
moveable electrode in the well bore, and the potential of
a fixed electrode located at the surface.
Electric potentials are created by chemically induced
electric current.
This electric potential is measured in millivolts.
Applications
Indicating permeable zones
Detecting permeable zone boundary
Indicating shaliness (shale volume) of a formation
Determining Rw and hence of formation water salinity
Indicating depositional environment changes
Correlation
- Liquid Junction Potential (Elj)
Diffusion of ions with higher mobility (Cl-) from concentrated solution to the dilute solution.
Happens from virgin zone to the invaded zone
- Membrane Potential (Em)
Selective diffusion of ions (Na+) from concentrated solution to the dilute solution.
Happens from virgin zone to the borehole.
Dominant source of SP
Liquid Junction Potential
If two sodium chloride solutions of different concentrations
are separated by a permeable membrane, then ions from
the most concentrated solution will tend to migrate into the
less concentrated solution.
Na+ and Cl- ions do not move with the same alacrity. Cl
ions (anions) move faster than Na+ ions (cations). The net
effect of more anions (negative ions) in the weak solution
and more cations (positive ions) in the more concentrated
solution creates a potential difference. This is known as a
liquid junction effect.
In terms of the solutions present in a formation, mud filtrate can be substituted for the weak solution and formation water for the more concentrated solution. The potential is referred
to as the liquid-junction potential (Elj)
Membrane Potential
Shales are permeable to Na+ ions, but not so
permeable to Cl- ions. A shale, therefore, acts as
an ionic sieve. This phenomenon occurs because
of the crystalline structure of clay minerals, which
have exterior surfaces with exchange sites to
which cations can temporarily cling.
Because Na+ ions effectively manage to
penetrate the shale bed from the saline formation
water to the less saline mud column, a so-called
membrane potential (Em) is created.
ET= Elj +Em =SP
Study Reference
slide 7 and 8 SP LOG slides
Reverse SP
A. Rw»_space; Rmf Large positive (right) deflection
B. Rw > Rmf Positive (right deflection)
C. Rw = Rmf No deflection
Normal SP
D. Rw < Rmf Negative (left) deflection
E. Rw «_space;Rmf Large negative (left) deflection
Static SP (SSP)
In the terminology used here, SP refers to observed SP deflection on the log and SSP
(static SP) to the value it would have had if all disturbing influences were removed. These
disturbing influences result in a smaller recorded SP deflection than SSP deflection.
Conditions where SP measurement is equal to SSP:
Thick formations
Water-bearing zones
Clean (no shale) zones
High permeable formation
Factors Affecting SP
No SP in oil-based muds: absence of electrical path in the
mud column
Shaly formation will reduce the measured SP.
Hydrocarbon saturation reduces SP deflection.
Thin beds avoid SP to fully develop.
SP amplitude deflection is also affected by following
parameters:
* The formation true resistivity, Rt .
* The invaded zone diameter, Di
.
* The invaded zone resistivity, RXO.
* The surrounding formations resistivity, Rs
* The mud resistivity, Rm.
* The diameter of the borehole, dh.
Summary 1
- SP log deflection is the result of electric potential exists between the wellbore and formation due to
the different salinity/resistivity between mud filtrate and formation water:
Negative deflection (normal SP) when Rmf > Rw
Positive deflection (Reverse SP) when Rmf < Rw
No deflection when Rmf = Rw
Summary 2
SP log can be used to:
Detect permeable formations
Detect boundary of permeable formation
Calculate Shale volume, Vsh
Calculate formation water resistivity, Rw