--> ABSTRACT: A Case Study of Non-Uniform Layering Approach to Optimize Simulation Grid Design, by Al Shemsi, Abdullah H.; Khemissa, Hocine; Fathalla, Magdy; Walia, Samir; #90141 (2012)
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A Case Previous HitStudyNext Hit of Non-Uniform Layering Approach to Optimize Previous HitSimulationNext Hit Grid Design

Al Shemsi, Abdullah H.1; Khemissa, Hocine *1; Fathalla, Magdy 1; Walia, Samir 2
(1) ADMA-OPCO, Abu Dhabi, United Arab Emirates. (2) Roxar, Abu Dhabi, United Arab Emirates.

Upscaling is required to build Previous HitreservoirNext Hit Previous HitsimulationNext Hit grids model guided by the criteria’s, the design has to retain the structure and the heterogeneity of the detailed geological model, it has to be able to meet Previous HitreservoirNext Hit management needs in defining new drilling well locations, sidetracks and workovers, the Previous HitsimulationNext Hit layers have to be detailed enough to define any vertical barriers, high permeability streaks and to handle any changes in flow or storage capacity.

The Previous HitreservoirNext Hit corresponds to an alternate of high heterogeneous porous and dense layers, with lithology limestone and dolomite, vugs and high permeability streaks.

To maintain our Previous HitreservoirNext Hit heterogeneity during Upscaling, a difficulty was faced which is Previous HitsimulationNext Hit “CPU” capability. Therefore, a new method called ‘optimal Previous HitsimulationNext Hit grid design’ provided by IRAP/RMS (SPE 95759 King , et al.) has been applied to upscale a large geological model with objectives to capture maximum heterogeneity in Previous HitsimulationNext Hit grid keeping in mind “CPU” limitation (computing speed and time and create the irregular 3D grid in all I, J and K direction.

In the present case Previous HitstudyNext Hit, challenge was to upscale the 20 million cell size fine geological grid up to 2.5 million cell size Previous HitsimulationNext Hit grid. The “optimal Previous HitsimulationNext Hit grid design” is a recursive algorithm works by merging two adjacent layers with the minimum variation change, until a single layer model is generated. This algorithm is using the model properties such as bulk volume, porosity, permeability and rock type as input to quantify the heterogeneity.

The lateral and vertical heterogeneities were calculated for each zone. The heterogeneity versus model layers was plotted and the number of irregular Column, Row and Layer versus the heterogeneity was optimized. Later on the facies and properties were up scaled to the Previous HitsimulationNext Hit grid. Various methods such as histograms, scatter plots and streamline Previous HitsimulationNext Hit have been used to compare properties between geological and Previous HitsimulationNext Hit grid. The high quality of Previous HitsimulationNext Hit grid and Geological heterogeneity are also confirmed by Previous HitreservoirTop engineer.

 

AAPG Search and Discovery Article #90141©2012, GEO-2012, 10th Middle East Geosciences Conference and Exhibition, 4-7 March 2012, Manama, Bahrain