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					 Porosity from the Density Log The density log is widely used to estimate porosity. The method 
					works well when shale volume and matrix rock density are 
					accurately known. Errors as large as 12% porosity can occur, 
					and 3 to 6% are common if incorrect assumptions are made.
 
 If both density and neutron logs are available, a superior 
					model that does not require matrix rock properties is the
					Shale Corrected Density Neutron 
					Complex Lithology Crossplot Method. The Meta/Kwik 
					spreadsheet for this model is available at 
					
					Downloads and Spreadsheets.
 
 
  Density Log RESPONSE EQUATION The response equation for the density log in porosity units follows
                the classical form:
 1:
                PHID = PHIe * Sxo * PHIDw                                          (water term)
 + PHIe * (1 - Sxo) * PHIDh                                    (hydrocarbon term)
 + Vsh * PHIDsh                                                     (shale term)
 + (1 - Vsh - PHIe) * Sum (Vi * PHIDi)                      (matrix term)
 
 Where:
 PHIDh = log reading in 100% hydrocarbon
 PHIDi = log reading in 100% of the ith component of matrix rock
 PHID = log reading
 PHIDsh = log reading in 100% shale PHIDw = log reading in 100%
                water
 PHIe = effective porosity (fractional)
 Sxo = water saturation in invaded zone (fractional)
 Vi = volume of ith component of matrix rock
 Vsh = volume of shale (fractional)
 
 To solve for porosity from the density log, we assume PHIDh, PHIDi,
                PHIDsh, PHIDw, and Vsh are known. We also assume PHIDw = PHIDh and
                Sxo = 1.0 when no gas is present. If gas is indicated, we make
                assumptions about PHIDh and Sxo, usually in the form of a correction
                factor to the gas free case, as described later.
 
 This response equation is rigorous. Mineral and fluid parameters
			are shown HERE. Shale properties are selected from
			the log in an obvious shale zone.
 
 
  References: 
 
			
					 1.  Logging Empty HolesC.G. Rodermund, R.P. Alger, J. Tittman, 
			
					Oil and Gas Journal, 1961
 
 2. Formation Density Log Application in Liquid-Filled Holes
 R.P. Alger, L.L. Raymer, W.R. Hoyle , M.P. 
					Tixier, JPT, 1964
 
 3.  Litho-Density Log Interpretation
 J.S. Gardner, J.L. Dumanoir, SPWLA, 
					1980
 
                	
					
					
					 POROSITY FROM Density Log Calculate density porosity from density data.
 2: PHID = (DENS - DENSMA) / (DENSW - DENSMA)
 
 Apply density shale correction:
 3: PHIDSH = (DENSH - DENSMA) / (DENSW - DENSMA)
 4: PHIdc = PHID - Vsh * PHIDSH
 
 Apply density gas correction.
 5: IF DENSITYGASSWITCH$ = "ON"
 6: THEN PHIdc = KD * PHIdc
 
 Where:
 DENS = density log reading in zone of interest (gm/cc or kg/m3)
 DENSMA = density log reading in 100% matrix rock (gm/cc or kg/m3)
 DENSSH = density log reading in 100% shale (gm/cc or kg/m3)
 DENSW = density log reading in 100% water (gm/cc or kg/m3)
 KD = density log gas correction (fractional)
 PHID = porosity from uncorrected density log (fractional)
 PHIdc = porosity from density log corrected for shale (fractional)
 PHIDSH = apparent density log porosity of 100% shale (fractional)
 Vsh = shale volume (fractional)
 
 
  COMMENTS: A graphical solution, with shale correction, is shown below.
 
				 Chart for Estimating Shale Corrected Density Porosity
 The
                density log corrected for shale is a very good approximation to
                porosity, but the log was not common before 1965, so sonic or
                neutron methods may be necessary for wells drilled before that
                time.
 KD is in the range of 0.5 - 1.0 depending on invasion, gas density
                and local experience. A correction is almost always needed if
                gas is present.
 
 Use gas correction only if PHIdc is too high compared to other
                sources and if gas is known to be present. This correction may
                be necessary even in shaly sands, since the depth of investigation
                of the density log is deep enough to see beyond the flushed zone.
 
 WHEN DENSITY LOG IS IN POROSITY UNITS, POROSITY MAY BE WRONG
				BECAUSE THE POROSITY SCALE DOES NOT MATCH THE ROCK MINERALOGY.
				SEE NEXT SECTION FOR CORRECTIONS.
 If density porosity data is in percent, rather than fractional,
                divide the data values by 100 before Step 2 and 3 are applied.
 No compaction correction is made to density log data.
 
 
 NUMERICAL EXAMPLE:1. Assume a zone with:
 DENS = 2.15 gm/cc
 DENSW = 1.00 gm/cc
 DENSMA = 2.65 gm/cc
 Vsh = 0.33
 DENSSH = 2.60 gm/cc
 
 PHID = (2.15 - 2.65) / (1.00 - 2.65) = 0.30
 PHIDSH = (2.60 - 2.65) / (1.00 - 2.65) = 0.03
 PHIdc = 0.30 - 0.33 * 0.03 = 0.29
 No gas correction is required.
 
                
  Porosity From Density Log With Matrix Offset One step that is often required is to convert apparent porosity
                on the density log into density units, then reconstitute porosity
                from this value corrected for a desired matrix and fluid value.
                This is done by rearranging the response equation of the previous
                section.
 
				Calculate density from density porosity.7: DENS = (PHID * KD1 + (1 - PHID) *
			KD2
 Where:English Units  
			Metric Units    Log Scale
 KD1       1.00                
			1000              
			All
 KD2       2.65                
			2650          
			Sandstone
 KD2      
			2.71                
			2710          
			Limestone
 KD2      
			2.87                
			2870          
			Dolomite
 
                Calculate shale density.
 8: DENSSH = (PHIDSH * KD1 + (1 - PHIDSH)
			* KD2
 
 Calculate porosity with new matrix and fluid.
 9: PHIDm = (DENS - DENSMA) / (DENSW - DENSMA)
 10: PHIDSHm = (DENSSH - DENSMA) / (DENSW - DENSMA)
 11: PHIdc = PHIDm - Vsh * PHIDSHm
 
 Apply density gas correction.
 12: IF DENSITYGASSWITCH$ = "ON"
 13: THEN PHIdc = KD * PHIdc
 
 Where:
 DENSSH = density log reading in 100% shale reconstituted from
                density porosity data (gm/cc or kg/m3)
 DENS = density value reconstituted from density porosity data
                (gm/cc or kg/m3)
 DENSMA = matrix density (gm/cc or kg/m3)
 DENSW = fluid density (gm/cc or kg/m3)
 PHID = porosity from uncorrected density log (fractional)
 PHIdc = porosity from density log corrected for shale (fractional)
 PHIDm = density porosity log reading corrected for matrix offset
                (fractional)
 PHIDSH = density porosity log reading in 100% shale (fractional)
 PHIDSHm = density porosity log reading in 100% shale corrected
                for matrix offset (fractional)
 Vsh = volume of shale (fractional)
 
 COMMENTS:
 See previous Section above.
 
				
				
				 ANCIENT DENSITY LOGS Ancient density logs,
				and many modern slimhole density logs,
			are recorded in gamma ray counts per second. You get to work out
			the transform to density using a semi-logarithmic High - Low
			porosity technique as described for the neutron log. Here, high
			count rate = low density = high porosity. Semi-log crossplots of
			count rate versus core density or core porosity will calibrate the
			method. These tools have a single detector and are not compensated
			for borehole effects. Slim hole versions were widely used in strat
			holes and in mineral exploration projects. Charts for some specific
			tools can be found in the literature, such as the one shown below.
 
			 Counts per second to density transform for a Schlumberger PGT-A
			density tool. Each tool iteration and each service company requires
			a specific chart. Density varies with hole size  mud weight, 
			and  , An equation for the 8 inch borehole case is DENScps = 
			-0.88 * LOG(CPS) + 4.71
 
			These tools are severely affected by hole size, mud weight, mud cake
			thickness, source type and strength, source detector spacing, and
			detector efficiency. The High-Low calibration method compensates for
			all these problems, but available charts do not. In the earliest
			versions of these tools, the source strength decayed  rapidly, so
			count rates definitely need to be normalized on a well by well
			basis.  
			 Most density transforms never made it into
			published chart books. This one did -
			Schlumberger PGT-C or D density count rates to porosity. Additional
			charts are available to correct for mud cake thickness and mud
			weight, and for air-filled holes. The count rate charts appeared in
			1966 chart books, well after they were no longer needed, and
			disappeared after 1968. Most density count rate charts are
			very hard to find unless you have a good supply of ancient chart
			books from 1958 through 1968 - a 10 CD set of ancient chart books was published by Denver
			Well Log Society and sold through 
			SPWLA.
 
				
				 DENSITY LOG PARAMETERS 
  
  
 
			
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