LOG NORMALIZATION BASICS
Log normalization is based on the concept that Maximum and minimum log readings in a zone in an area should have the same log reading. The assumption includes the fact that there no major geological reasons for the values to vary across space.

Reasons for log normalization are numerous:  poor tool calibration, mis-labeled scales, unconventional units of measurement, mud weight, borehole size, temperature, rock alteration, and many more.


Log normalization is the process of re-scaling a log so that it matches its neighbours, based on some logical reasoning. Re-scaling can involve an equal linear shift of the two scale end-points, or a "stretch" or "squeeze" of the data values between the two scale end points or between two arbitrary log values.


Log normalization is most often applied to gamma ray logs. Here we re-scale the GR logs so that a particular clean sand in all wells have the same GR value. Likewise, the key shale zones in all wells have the same GR value. This makes correlation of zones easier and helps the analyst to better understand reservoir quality without additional calculations.

The technique is widely used for sonic, density, density porosity, and neutron logs. In these cases, the equation is the same but the MIN and MAX terms apply to low and high log readings chosen in particular geological horizons, for example in a low porosity and a shale interval.

Another approach is to run a statistical analysis over the same geological interval in many wells, select the wells with similar min, max, and median values as "key" wells, then shift the outlier logs so that the median matches the key wells.

CAUTION: Normalization can remove natural geological variations that may have significance in understanding the reservoir variations across space. For example, if calcite cement varies from place to place, normalization will remove porosity trends that vary with cementation. Similarly, on a GR log if feldspar content or clay type varies, this knowledge will be lost.

LOG_NORM1 -- NORMALIZATION WITH CONSTANT OFFSET
The equation is:
      1: XXXn = XXX + SHIFT

Where:
  XXXn =  normalized XXX log value
  XXX = input XXX log curve value
  SHIFT =  value that moves the median curve value in this zone in this well to the median value
                 of the key wells.

COMMENTS
This method is helpful when neutron log scale (Sandstone vs Limestone) is unknown or ambiguous. Can be applied to any porosity log or the logarithm of resistivity. Not recommended for GR or SP..

EXAMPLE
Median sonic log value over selected interval in Key wells is DTCavg = 225 usec/m.

Median sonic log value over selected interval in THIS well is DTCavg = 221 usec/m.
SHIFT = 225 - 221 = +4 usec/m.
DTCn = DTC + 4

LOG_NORM2 -- NORMALIZATION By STREtCH or SQUEEZE
The equation is:
      1: XXXn = XXXMIN + (XXXMAX - XXXMIN) * (XXX - XXXLOW) / (XXXHIGH - XXXLOW)

Where:
  XXXn =  normalized log value
  XXX = input log curve value
  XXXMIN = minimum XXX log value to normalize to
  XXXMAX = maximum XXX log value to normalize to
  XXXLOW = actual XXX log value in this zone in this well that corresponds to XXXMIN
  XXXHIGH = actual XXX log value in this zone in this well that corresponds to XXXMAX

COMMENTS
This is the method most used for GR and SP curves but can be used with care on any log curve.

EXAMPLE
Assume you want to re-scale all GR logs so that all clean lines are at 20 API units and all shale lines are at 120 API units. That makes GRMIN = 20 API units, GRMAX = 120 API units for all wells
Assume GRLOW = GR0 = 30 API units, GRHIGH = GR100 = 155 API units in THIS zone in this well.
Assume actual GR at a depth level = 55 API units

   1: GRn = 20 + (120 - 20) * (55 - 30) / (155 - 30) = 40 API units


Red curve in Track 1 is normalized GR (GRn), black curve is original gamma ray in a radioactive sand. Because uranium content is nearly constant, we can re-scale the total GR to a more useful shale indicator by normalizing. Parameters used were GRMIN = 25, GRMAX = 275, GRLO = GR0 = 100, GRHIGH = GR100 = 350
 (off scale but available from LAS file).
 

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