For environmental reasons, there are times when the use of radioactive chem
ical sources for density and neutron logging is not possible. The inability
to use these logging tools seriously affects porosity determination in gas
-bearing reservoirs. Several tools, such as the nuclear magnetic resonance
(NMR) tool, the sonic tool, or a minitron-based tool, determine porosity wi
thout using a radioactive source. These tools, however, are influenced by m
any effects and, when used alone, cannot deliver an accurate gas-independen
t porosity.
A new methodology that combines sonic and NMR logs for improved porosity ev
aluation in gas-bearing reservoirs is proposed. The first variant of the me
thod uses the sonic compressional transit time and the total NMR porosity (
Phi (t.NMR)) to determine the total porosity, corrected for the gas effect,
and the flushed-zone gas saturation. In this approach, a linear time-avera
ged equation corrected for compaction is applied to the sonic compressional
log. The simplicity of the solution, much like the previously published DM
R1 Density-Magnetic Resonance interpretation Method, allows fast, easy comp
utation and a complete error analysis to assess the quality of the results.
In the second variant of the method, we show that the rigorous Gassman equa
tion has a very similar response to the Raymer-Hunt-Gardner (RHG) equation
for a water/gas mixture. This allows substitution of the complex Gassman eq
uation by the much simpler RHG equation in the combined sonic-NMR (SMR) tec
hnique to estimate total porosity and flushed-zone gas saturation in gas-be
aring formations.
Both techniques are successfully applied to an offshore gas well in Austral
ia. In this well, the porosity in the well-compacted sands is in the 20 to
25 p.u. range and the compaction factor is approximately 0.77. The sonic-ma
gnetic resonance results compared favorably to the established density-magn
etic resonance results and also to core data. In another offshore gas well
from the North Sea, the porosity in the highly uncompacted sands is in the
35 to 40 p.u. range, and the compaction factor is around 1.85. Both SMR tec
hniques were able to produce a very good porosity estimate comparable to th
at estimated from the: density-neutron logs.