GAS CORRECTIONS IN HEAVY MINERALS
in many carbonate reservoirs, and some sandstones with lots of heavy minerals, the heavy mineral effect  (separation) is offset by the gas effect (crossover) on the density neutron log. The net result is that the gas goes unnoticed because there is no crossover, and the lithology is misinterpreted because the density neutron separation is reduced. Observation of the PE curve will point out the inconsistency. In the absence of the PE, sample descriptions and core data will point out the problem.

IF gas is known to be present but NO crossover occurs after shale corrections, this usually means gas in dolomite or in a sandstone with lots of heavy minerals. First, assume or calculate the matrix density(DENSMAgc) based on the PE curve (PE is the only curve unaffected by gas):
      1: V1 = (PE - Vsh * PESH - PE2) / (PE1 - PE2)
      2: V2 = 1 - V1
      3: DENSMAgc = V1 * DENS1 + V2 * DENS2

Where:
  DENSMAgc =  matrix density for gas correction (kg/m3 or gm/cc)
  DENS1 = matrix density of mineral 1 (kg/m3 or gm/cc)
  DENS2 = matrix density of mineral 2 (kg/m3 or gm/cc)
  PE = measured PE log value of rock mixture
  PE1 = PE of first mineral (fractional)
  PE2 = PE of second mineral (fractional)
  V1 = volume of first mineral (fractional)
  V2 = volume of second mineral (fractional)
  Vsh = volume of shale (fractional)

DENSMAgc can be computed as a continuous curve or used as a zone parameter to replace DENSMA in equation 8.

Apply gas correction:

4: PHIx = – PHIdc / (PHInc / 0.8 – 1) / (1 + PHIdc / (0.8 – PHInc))

5: PHIxdn = PHIx + KD3 * (0.30 – PHIx) * (DENSMAgc / KD1 – KD2)

Where:  KD1 = 1.00 for English units

 KD1 = 1000 for Metric units

 KD2 = 2.65 for Sandstone scale log

 KD2 = 2.71 for Limestone scale log

 KD3 = 1.80 for Sandstone scale log

 KD3 = 2.00 for Limestone scale log

 Density Neutron Complex Lithology Crossplot - Gas zones with NO crossover. Enter shale corrected data and then slide data point to the right until it reaches the line representing the matrix density of the reservoir - travel parallel to the nearest heavy black line. Do not use Dolomite scale log for this special case.

An illustration of how the points move under different conditions is given below.

Graph for Gas Correction on Density Neutron Crossplot Porosity, showing how the raw data points
 move under various assumptions. (Porosity scales are in Limestone Units)

Point A goes to A1, if CNL and DENSMA = 2710 (crossover)
               goes to A2, if SNP regardless of DENSMA
               goes to A3, if CNL and DENSMA = 2870.

Point B goes to B1, if CNL and DENSMA = 2870 and gas correction is IMPOSED
               goes to B2, if CNL and DENSMA = 27l0 and gas correction is IMPOSED
               goes to B3, if CNL and DENSMA = 2650 and gas correction is IMPOSED
               stops at B if gas correction is not imposed or if SNP

Point C goes to C1, if CNL and DENSMA = 2870 and gas correction is IMPOSED
               goes to C2, if CNL and DENSMA = 2710 and gas correction is IMPOSED
               stops at C if gas correction not imposed or if SNP

The author is indebted to Jim Hamilton of Dome Petroleum for first suggesting this approach to one pass gas corrections. The approach has proved extremely successful and has matched core on hundreds of projects in many reservoir conditions.

Before the introduction of the photo-electric effect (PE) log curve, it was easy for a log analyst to miss a gas filled dolomite reservoir. The standard density neutron crossplot would show a low porosity limestone, when in fact the zone is a medium porosity dolomite. Since the density neutron looks like limestone (curve separation is small) and the PE looks like dolomite (PE near 3.0), this discrepancy is a red flag that a special case exists. Many computer programs will not trigger gas corrections unless density neutron crossover is present, and most programs do not contain explicit algorithms to handle this special case.

The illustration below  shows the effect of using this gas correction. Notice that computed porosity does not match core porosity unless the correct DENSMA is chosen. DENSMA should reflect the matrix density of the expected lithology. The correction is usually needed in dolomite or dolomitic sands or high porosity shaly sands with low to moderate invasion.

Effect of DENSMA on density neutron crossplot porosity with gas in heavy minerals. Core porosity (square black lines) and log analysis porosity (smooth black curves) show a good match when DENSMA was set at
2710 - 2740 kg/m3. Log analysis shows near zero porosity if DENSMA set at 2650 for this heavy sandstone.

Gas in dolomite example with no correction applied (left) and after correction (rig