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					 Calibrating Porosity to Core
					Data The proof of a log analysis is the degree to which the porosity
                matches core analysis porosity. The easiest way to check this
                is to plot the core analysis porosity on top of the log analysis
                on the same depth plot. If the overlay is quite good, no more needs to be done except show off the comparison
                and brag a bit. If the core is off depth to the log porosity,
                shift the core depths appropriately and re-display the results.
 
 
				 Comparison of Core Porosity with Log Analysis Porosity -
				black dots are
 core, smooth lines are log analysis.
 
			
			 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.
 If
                the comparison is poor, there are three choices. First make sure
                the core data is on depth with the logs and that each log curve
                is on depth with each other.
 
  CHOICE 1 
				(preferred): Adjust shale, matrix, and fluid parameters
                in the log analysis model until a better match is achieved. This
                may take several attempts and may require choosing a different
                mathematical model or mineral assemblage. 
 
  CHOICE 2: Crossplot core porosity vs log analysis porosity, and
                find a regression line that corrects the log result to the core,
                of the form: 1: PHIcorr = K1 * PHIe + K2
 
 Where:
 PHIcorr = corrected porosity (fractional)
 PHIe = effective porosity (fractional)
 K1 = slope of regression line
 K2 = intercept of regression line
 
 The regression should be the reduced major axis (RMA) method (see
                and not a simple least squares regression. RMA
                assumes errors occur in both axes and not just in the Y axis data.
                An eyeball line may be best as stray outliers can be discarded
                quickly. The before and after crossplots can be used to document
                the change. Do not use the regression unless the error is reasonably
                low (R-squared > 0.8 or so).
 
 CAUTION: Core data must be depth
                matched to logs before you do this. And some core data is faulty
				or not spread across a wide enough range of values. Porosity or
				shale laminations thinner than the tool resolution cause a fair
				scatter on crossplots and depth plots. There is no direct
				solution to obtain a better match except to match average
				porosity from log analysis with average porosity from the core.
 
 
  CHOICE 3: Perform the regression on a single input log curve instead
                of on PHIe, or separately on several curves. Pick the regression
                with the least standard deviation or highest R-squared. This creates
                a new log analysis model that may be used locally instead of the
                universal methods described in this Chapter. 
 You might need a multi-variant regression to account for all the
                minerals and fluids, or even a Principal Components analysis to
                obtain a statistical solution.
 
 It
                is also common to calibrate simple log analysis porosity methods to crossplot
                methods, which in turn might be calibrated to core, by overlay plots or regression. The calibration
                can then be carried to wells that do not have sufficient data
                for crossplot analysis.
 
 
			
			 Calibrating Porosity to PETROGRAPHIC
			Data There are many occasions when core analysis porosity is not available
                for calibration of log results. The next best data set is petrographic
                thin section visual porosity analysis. This usually excludes micro-porosity
                so a regression of thin section porosity vs log analysis porosity
                will give useful porosity (PHIuse) instead of PHIe. Most people
                like this result. Thin sections can often be made from sample
                chips when no core exists. Thin section samples are tiny and it
                is sometimes difficult to scale-up these results to the whole
                reservoir. A large number of samples in varying facies can give
                statistically meaningful results. A few samples are probably useless.
 
                
                  |  |  |  
                  | 
					15X
                      Magnification | 
					100X
                      Magnification |  
                  | Thin Section Images |  
                  |  |  
                
                  | 
					Depth,
                      ft. | 
					9403.70 | 
					9407.00 | 
					9413.50 | 
					9419.20 |  
                  | 
					Porosity
                      @ NOB (%) | 
					12.4 | 
					8.2 | 
					10.9 | 
					5.0 |  
                  | 
					Air
                      Perm. @ NOB (md) | 
					0.296 | 
					0.034 | 
					0.338 | 
					0.0054 |  
                  | 
					Grain
                      Density (g/cc) | 
					2.81 | 
					2.83 | 
					2.82 | 
					2.79 |  
                  | 
					PRIMARY
                      MINERAL |  |  |  |  |  
                  | 
					Dolomite | 
					60.0 | 
					81.2 | 
					80.0 | 
					79.6 |  
                  | 
					Calcite | 
					Tr | 
					0.0 | 
					0.0 | 
					0. |  
                  | 
					Anhydrite | 
					1.2 | 
					0.4 | 
					0.8 | 
					0.0 |  
                  | 
					Pyrite | 
					2.0 | 
					1.6 | 
					1.6 | 
					1.6 |  
                  | 
					Quartz | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Feldspar | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Authigenic
                      Clay | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Bitumen | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Other | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Total | 
					63.2 | 
					83.2 | 
					82.4 | 
					81.2 |  
                  | 
					SILCLASTICS |  |  |  |  |  
                  | 
					Mono
                      Quartz | 
					8.8 | 
					2.0 | 
					4.4 | 
					7.2 |  
                  | 
					Poly
                      Quartz | 
					0.0 | 
					0.0 | 
					Tr | 
					0.0 |  
                  | 
					Plagioclase | 
					2.0 | 
					0.8 | 
					0.8 | 
					1.6 |  
                  | 
					Potassium
                      Feldspar | 
					3.6 | 
					1.2 | 
					0.8 | 
					3.2 |  
                  | 
					Chert | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Rock
                      Fragments | 
					0.0 | 
					0.4 | 
					0.0 | 
					0.0 |  
                  | 
					Shale
                      Fragments | 
					0.0
                       | 
					Tr | 
					0.0 | 
					0.0 |  
                  | 
					Muscovite | 
					Tr | 
					0.4 | 
					0.0 | 
					Tr |  
                  | 
					Biotite | 
					2.0 | 
					0.8 | 
					0.0 | 
					0.0 |  
                  | 
					Heavy
                      Minerals | 
					0.0 | 
					Tr | 
					0.0 | 
					0.4 |  
                  | 
					Carbonaceous
                      Fragments | 
					1.2 | 
					0.4 | 
					Tr | 
					Tr |  
                  | 
					Glauconite | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Detrital
                      Clay Matrix | 
					3.2 | 
					1.6 | 
					1.6 | 
					1.2 |  
                  | 
					Other | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Total | 
					20.8 | 
					7.6 | 
					7.6 | 
					13.6 |  
                  | 
					POROSITY |  |  |  |  |  
                  | 
					Primary
                      Interparticle | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Primary
                      Intraparticle | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Secondary
                      Intraparticle (Carbonate Grains)
 | 
					0.0 | 
					0.0 | 
					1.2 | 
					0.0 |  
                  | 
					Tertiary
                      Intraparticle(Carbonate Grains)
 | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Secondary
                      Intraparticle(Siliciclastic)
 | 
					Tr | 
					0.0 | 
					Tr | 
					0.0 |  
                  | 
					Vugular | 
					0.0 | 
					0.0 | 
					Tr | 
					0.0 |  
                  | 
					Intercrystalline | 
					16.0 | 
					9.2 | 
					8.4 | 
					3.6 |  
                  | 
					Micropores | 
					0.0 | 
					0.0 | 
					0.0 | 
					0.0 |  
                  | 
					Fracture | 
					0.0 | 
					0.0 | 
					0.4 | 
					0.8 |  
                  | 
					Secondary
                      Intracrystalline | 
					Tr | 
					Tr | 
					0.0 | 
					0.4 |  
                  | 
					Total | 
					16.0 | 
					9.2 | 
					10.0 | 
					5.2 |  
                  |  |  |  |  |  |  
                  |  | 
					100.0 | 
					100.0 | 
					100.0 | 
					100.0 |  Typical Thin Section Point Count Analysis with
                primary, secondary, and non-useful porosity breakdown 
			Not all thin section reports are as detailed as this one. Scanning
                electron micrograph data (SEM) is also widely used, in the same
                way as thin section data.
 
 
  Calibrating Porosity to SAMPLE
			DESCRIPTIONS Porosity ranges as seen by microscopic examination of samples
                are also used as a guide. This may be useful in the absence of
                more quantitative data or where rough hole conditions make log
                analysis ambiguous. The black bar graph in the illustration
			below shows visual
                porosity spanning three ranges. Log analysis should at least see
                porosity in the same zones and somewhat in proportion to the variations
                in visual porosity values.
 
				 Sample Description Log with Microscopic Visual Porosity
                (black bar graph in center of plot)
 
 
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