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					 Water Saturation in the
					Dual Porosity Model The average
					water saturation of the composite system is calculated using
					a statistical parameter, P, originally introduced to the oil
					industry by Porter, Pickett, and Whitman. Empirically, it
					has been found that P has a normal distribution for
					intervals which are 100 per cent saturated with water.
					Intervals with some hydrocarbon saturation deviate from the
					normal distribution.
 
 
				
					| Calculating
					P
 For sonic logs:15a: P = (RESD * (DELT - DELTMA) ^ Md) ^ (1/2)
 For density logs:15b: P = (RESD * (DENS - DENSMA) ^ Md) ^ (1/2)
 If effective porosity has been computed from density
					neutron crossplot:15c: P = (RESD * (PHIe ^ Md) ^ (1/2)
 |  WHERE:DELT = sonic log reading (usec/ft
			or usec/m)
 DELTMA = sonic matrix
			transit time (usec/ft or usec/m)
 DENS = density log reading
			(g/cc or kg/m3)
 DENSMA = matrix density
			(g/cc or kg/m3)
 Md = cementation exponent
			for double porosity model, found from a Pickett plot
 P = statistical parameter
			(unitless)
 PHIe = effective porosity
			of double porosity system (fractional)
 RESD = deep resistivity
			log reading (ohm-m)
 
				 Pickett plot, partition factor, and probability
                graphs for Aguilera’s dual porosity model
 This
			illustration, bottom left, shows a schematic of P vs cumulative frequency
                on probability paper for a water and hydrocarbon system. The 100
                per cent water saturated zones form a straight line, and the hydrocarbon
                intervals deviate from this line and are thus easily recognized. Bottom right shows the same type of plot for only the
                water bearing intervals. The mean value of P for water zone, Pmean,
                is determined from this graph at a cumulative frequency of 50
                per cent. An arithmetic average of the P values from the water
                leg is usually satisfactory, so the probability plot is not necessary. Having
				the mean value of P from the water zone allows us to calculate
				the water saturation of the dual porosity system from the
				following. 
				
					| Partitioning water saturation
 16: Swd = (Pwtr / Phyd) ^ (1/N)
 17: Swf = (VISW * WOR) / (Bo * VISO + VISW * WOR)
 18: Swe = (Swd - V * Swf) / (1 - V)
 
 
 |  Where:Bo = oil formation volume
			factor (vol/vol)
 N = water saturation
			exponent (unitless)
 Phyd = parameter P for
			each hydrocarbon zone (unitless)
 Pwtr = mean value of P for
			water bearing intervals (unitless)
 Swd = water saturation for
			the double porosity system (fractional)
 Swe = water saturation for
			the matrix rock (fractional)
 Swf = water saturation for
			the fracture (fractional)
 VISW = water viscosity
			(cp)
 VISO = oil viscosity (cp)
 WOR = water/oil ratio, (vol/vol)
 This
			long evaluation process requires the reading, plotting, and
			crossplotting of large volumes of data, and requires a large number
			of calculations. This makes it an ideal computer application and
			hand calculation is not recommended. A solution for a gas reservoir
			was never published. In many cases Swf is assumed to be 0.0 (because
			WOR = 0) so this assumption can be used for gas wells also. NOTE:
			This is essentially an "Rwa type" saturation method and relies on
			the presence of a water zone. In the absence of a water zone, an
			rchie water saturation solution (Swa) will have to suffice, giving
			the equivalent of Swe. Swf is not derived from log data. If
			parameters are unknown, start with VISW =1.0, VISO = 2.0, WOR = 0.0,
			and Bo = 0.8. This makes Swf = 0.0 during production, which is close
			to the truth. 
				
					| 
					Standard
					Archie solution
 19: Swa
					= (A * RW@FT / (PHIe ^ Md) / RESD) ^ (1/N)
 |  Where:A = tortuosity exponent (unitless)
 Md = cementation exponent
			for matrix rock with fractures (unitless)
 N = saturation exponent (unitless)
 PHIe = effective porosity
			(fractional)
 RESD = deep resistivity
			log reading (ohm-m)
 RW@FT = water resistivity
			at formation temperature (ohm-m)
 Swa = effective water
			saturation (fractional)
 RECOMMENDED
                PARAMETERS:If zone is not heavily fractured:
 For sandstones:
 A = 0.62
 Mb = 2.15
 N = 2.00
  For
                carbonates:A = 1.00
 Mb = 2.00
 N = 2.00
 If
                zone is fractured:Mb = 1.4 to 2.0
 A = 1.00
 N = 2.00
 NOTE:
                The symbol M is used elsewhere in this book as the cementation
                exponent for the Archie equation. Mb is used here to indicate
                the use of Archie for the fractured reservoir case. 
				 Dual porosity model results in a Williston Basin
                well
 The
			log  shows the computed log results for a Williston Basin Mississippian
                fractured zone. The contribution of fracture related porosity is about
                1% porosity, but water saturation is 5 to 10% lower than the analysis
                without the fractures. The partitioning coefficient varies and
                was solved by iteration.
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