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					 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 are 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. Log 
					normalization involves a
			"stretch" or "squeeze" of the data values between two scale end
			points or between two arbitrary log values. The math is shown in a 
					later Section on this webpage.
 
 Log re-scaling
					is a simplified form of normalization. It can involve an equal linear shift of the two scale end-points, or 
					applying a multiplication factor to all data points.in the 
					log curve. This is often needed to change older log curve 
					scales to match modern logs or to convert Metric scales to 
					English units and vice-versa.
 
 For example,convert gama ray in units of ug-ra-equiv/ton to 
					API units:
 1:  GRapi = GRug-ra * 10
 
 Convert neutron porosity from limestone to sandstone units:
 2: PHIN_SS = PHIN_LS + 0.03
 
 Convert somic log from English to Metric units:
 3: DTCmetric = DTCenglish * 3.281
 
 Re-scaling a resistivity log is a little trickier since the 
					tools actually measures comductivity, so we need to create a 
					COND curve from RESD:
 4: COND = 1000 / RESD
 Adlust the somde error by adding or subtracting a few 
					milliSermens from COND. This will stretch or squeeze the 
					high resistivity and do almost nothing to the low 
					resistivity.
 
					      5: CONDnew = COND + X    
					where X = sonde error correctionConvert COND back to RESD:
 6: RESDnew = 1000 / CONDnew
 
					
			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. 
 
  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..
 
			 Numerical 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
 
			
			 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.
 
 
  Nunerucak 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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