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					 CALIBRATING Water
					Saturation During coring, moveable
					hydrocarbons are flushed from the core and replaced by mud
					filtrate, leaving residual oil and irreducible water. Some
					of the irreducible water may be replaced by mud filtrate as
					well. During recovery and transport of the core, the
					majority of the water will drain out, leaving residual oil
					and irreducible water. The sum of residual oil saturation
					plus irreducible water saturation is usually less than 1.0,
					the balance being the moveable oil saturation. In older
					reservoirs with many years of production, there may also be
					some moveable water. This will also be flushed by the mud
					filtrate. To appreciate the meaning of the core saturations, 
					it is important to know the history of a reservoir relative
					to the when the core was cut.
 
 In petrophysical analysis, we utilize the core water
					saturation as a guide to the irreducible water saturation in
					a reservoir above the transition zone. In a core, the
					difference between residual oil and water saturation is
					usually assumed to be the moveable oil fraction of the
					reservoir fluids, when the reservoir is at initial
					conditions. The core water saturation is usully assumed to
					be close to the irreducible water saturation.
 
 In older reservoirs, no longer at initial conditions,, there
					may be some moveable water as well as the moveable oil. This
					can often be seen on the log analysis results depth plots
					where log analysis saturation is higher than core water
					saturation. The excess water saturaton is a measure of
					potential water production.
 If corroboration of water
			saturation is required, air-brine capillary pressures should be
			taken, along with electrical properties, from at least a dozen core
			plugs with some variations in porosity or pore geometry. This will
			resolve the initial irreducible water saturation question. A
			reservoir simulation history match would be
			needed to resolve the question of moveable water saturation. 
 Cores
			taken in oil based mud give a better view of irreducible water, as
			these muds do not displace the water.
 
			The main use for core analysis oil saturation is to estimate
			minimum possible residual oil saturation, and to assist in locating
			gas-oil and oil-water contacts. Gas and water zones have low
			residual oil, unless they were once oil zones (recently or in
			earlier geologic time). Oil saturation from core analysis is quite
			useful in tar sand and sometimes in heavy oil evaluations, where
			flushing is minimal.  
					
			
			 CALIBRATING LOG ANALYSIS TO CORE SATURATION EXAMPLES These examples demonstrate the close match between log analysis
			water saturation and core analysis water saturation. It works most
			of the time, especially with cores cut after the mid 1980's,
			provided they have been handled according to best practices. If it
			doesn't work, or doesn't seem to make sense, forget it and move on.
 
			
			 Bakken “Tight Oil” example showing core porosity (black dots), core
			oil saturation (red dots). core water saturation (blue dots), and
			permeability (red dots). Note excellent agreement between log
			analysis and core data. Separation between red dots and blue water
			saturation curve indicates significant moveable oil, even though
			water saturation is relatively high. Log analysis porosity is from
			the complex lithology model and lithology is from a 3-mineral PE-D-N
			model using quartz, dolomite and pyrite.
 
 
    Sandstone example (left) and carbonate example (right) showing close
			match of log analysis and core analysis water saturation. Black dots
			are core porosity and permeability. Light blue dots are core
			analysis water saturation, which fall close to log analysis
			saturation curve (blue). Red dots on sandstone example are residual
			oil saturation, showing lots of moveable oil between the water
			curve, even though the water saturations are quite high (due to poor
			pore geometry).
 
			
					
			 Moveable Hydrocarbon EXAMPLE This example shows a comparison of residual oil from core in a
			depleted zone (M1 interval) and in a bypassed zone (M3 interval).
			The Sor from core equals (1 - SW) from log analysis, so there is no
			moveable oil in the M1. The close match suggests that most of the
			saturation parameters (A, M,
			N, RW@FT) and porosity are reasonably well calibrated. Since the
			world abounds with depleted zones (most are well known to the well
			operators) this test should always be made to confirm SW parameters
			where ever core data is available.
 
			
			 Computed results for carbonate example. Note higher water saturation
			on M1 compared to M3. M3 is bypassed pay. M1 is depleted oil. Dots
			are core data. Note that residual oil on core in M1 matches
			calculated
 Sor = (1 - SW). In M3, Sor on core is less than (1 - SW) from log
			analysis, so there is moveable oil in
 M3 interval but not in M1. Calibration to core permeability needs more work to get a
			decent match.
 
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