The Influence of Fabric Arrangement on Oil Sand Samples from the Estuarine Depositional Environment of the Upper McMurray Member

The Upper McMurray Formation of Canada, more specifically samples from the estuarine depositional settings taken in Athabasca, displayed high porosity based on an initial study. This work involved thin section imaging and micro CT-scanning in determining reservoir characteristics. The results from the thin section analysis for the porosity estimation showed that the estimated porosity lay between 30% and 50%, which is analogous to tests performed in well laboratories. Data and results obtained from the two experiments were then used to compute the pore size distribution, connectivity of pores and estimates of the porosity and permeability of the reservoir. The analysis of the spatial arrangement and distribution of the oil sand constituents showed that bitumen was distributed within the quartz grains and also between the quartz grains. Another distinctive feature was the distribution of bitumen in the nonconnecting large pores (vugs). The micromass was observed as forming bridges between the quartz grains and may be associated to larger clay bands. Importantly, soil structure was observed in thin section to be associated with Spodic horizons and the fabric of the grains ranged from Enaulic to Gefuric c/f related distribution patterns. This indicates that the oil and meteoric water migrated into a sandy material with inherited soil structure. An analysis of this type has the potential to differentiate between parts of the formation where connectivity will have a bearing on the relative ease and cost of production of steam-assisted gravity drainage (SAGD) projects. It should then be possible to identify “sweet” spots along the reservoir interval where completion design factors (such as sand/clay control or temperature/pressure profile control between injector and producer) can be employed more effectively to target specific intervals for optimum production. Copyright © AAPG. Serial rights given by author. For all other rights contact author directly. Introduction As there have been few large discoveries of conventional oil in recent times, research into unconventional oil, such as heavy oil and oil sand, is becoming increasingly inevitable. Oil sand is a naturally occurring mixture of sand, clay, water and extremely dense viscous oil (bitumen). With the demand for more oil, heavy oil is seen as a viable option. During previous low prices of oil, unconventional oil was not economic due to the cost involved in production and lack of appropriate technology for recovery. With the recent advancement in technology and high price of oil, interest in heavy oil has substantially increased. Alberta’s heavy oil deposit contains 1.7 trillion barrels of heavy oil and an estimated 179 billion barrels is recoverable based on current technology (Canada National Energy Board, 2004). With new technology and improved oil prices and economics, interest in Alberta’s oil reserves is bound to intensify. Regional Geology of Athabasca The McMurray Formation is part of the Lower Cretaceous Mannville Group (Cant and Abrahamson, 1996). The formation lies at the base of the group on an angular unconformity from the Devonian comprised of limestone and calcareous shale in the east and carbonate rocks in the west. Sediments in the McMurray Formation were deposited in a ridge and valley system trending north-south that were formed by fluvial processes but later changed to a marginal-marine depositional environment during an Early Cretaceous sea-level rise. Overall, the McMurray Formation has very complex sedimentary relationships that vary considerably, both laterally and vertically over short distances, indicating complex depositional environments with common transgression and regression cycles (Hein et al., 2001). The McMurray Formation is divided into three members, a Lower, Middle and Upper (Carrigy, 1959). Textural variations occur between the three members and ranges from: the lower member being a conglomerate, poorly sorted and argillaceous sand, silt and clay; the middle member comprised of moderately well-sorted, fine-grained sand and argillaceous silt; and the upper member consists of very fine grained sands and argillaceous silt. Distinct facies, based largely on sedimentary features, characterise the three members. Bitumen is located throughout the formation. Fabric of Athabasca Oil Sands Much research and studies have been carried out on the nature of the fluid in oil sands of Athabasca in the form of PVT and viscosity analysis to establish the volumetrics, porosity and permeability. However, few studies have been carried out on the fabric of the Athabasca oil sands. Some of the early microscopic work was done by Takamura (1982). Takamura observed that connate water forms an up to 10 μm thick film of water as coatings around quartz grains and entirely surround the grain. Bitumen fills voids between grains. The presence of this aqueous film has long been recognised as a characteristic feature of the Athabasca oil sands. The aqueous film or hydrophilic nature of the sand is important for the hot water (steam) extraction process of bitumen. Previous descriptions of the arrangement of oil sands constituents were mostly carried out on disturbed samples. Other key fabric studies include Dusseault (1980) who performed analysis on in-situ oil sands samples with similar findings to Takamura (1982). He did note that fine-grained clay and feldspars minerals were dispersed through the water film surrounding the sand grains. Czarnecki et al. (2005) countered that even though the existence of aqueous film in the Athabasca oil sands remains a reasonable yet unproven postulate. They argued that the aqueous film separating clean, hydrophilic quartz and bitumen is stable under most conditions but unstable for acidic oil sand ores. Material and Methods The site selected for this study was the Hangingstone River area near Fort McMurray, Canada and from a well documented estuarinetidal depositional environment from the Upper McMurray Formation (Hein et al., 2001). Notable sedimentary features in the Upper McMurray Formation include those interpreted from a tidally influenced point bar and an estuarine depositional environment, more specifically, brackish water trace fossil assemblages that indicate an estuary environment (Pemberton et al., 1982). These estuarinetidal channels and point bars are significant facies as they are common bitumen-sand reservoirs. There are variations in oil content among the various sedimentary environments, although the estuarine environment is considered to have the highest oil saturation (Czarnecki et al., 2005). Thin sections were prepared according to the usual process of production of soil thin sections according to Jongerius and Heintzberger (1975) and Fitzpatrick (1983) although procedures were modified in order to maintain sample integrity and minimize alteration of the oil contained in the samples. Thin sections were analysed and described according to Stoop (2003). Additionally, micro CT scans were carried out on the same material. The ultimate desktop X-ray Microtomograph SKYSCAN 1172 was used in this study. The cone microfocus beam source is based on a tungsten X-ray tube having focal spot of 7 μm at 10A isowatts. Voltage can be set from 20 to 100 kV with current which meets 250 mA. An undisturbed subsample having a diameter of 3.2 cm was scanned at 1.3 and 8 μm resolution. Results and Discussion The concept of soil fabric was introduced by Kubiena (1938) as “the arrangement of constituents of the soil in relation to each other”. This concept was further developed by Brewer and Sleeman (1960) in reference to the relative distribution of “skeleton grains” and “plasma”. According to Stoops (2003) important elements of fabric are spatial distribution, orientation, size, sorting and shape. Fabric can be determined according to size of component and spatial distribution. Coarse components of the groundmass are commonly single mineral grains, compound mineral grains or rock fragments, inorganic residues of biological origin and anthropogenic elements (Stoops, 2003). The fine mineral component of the groundmass forms a partial fabric known as the micromass and generally cannot be determined by its optical characteristics (Karale et al., 1974). The concepts of spatial units are based on coarse and fine (c/f) components with c/f related distribution patterns “expresses the distribution of individual fabric units in relation to smaller fabric units and associated pores” (Stoops and Jongerius, 1975). As observed in thin section, the Athabasca oil sands from the estuarine depositional environment of the Upper McMurray Formation consisted predominately of coarse component of rounded to angular quartz grains imbedded in a micromass of silt and clay. Some of the quartz grains displayed different degrees of weathering. Bitumen was observed both within the micromass and as exotic feature. The analysis of the spatial arrangement and distribution of the oil sand constituents showed that bitumen was distributed within the quartz grains and also between the quartz grains. Another distinctive feature was the distribution of bitumen in the non-connecting large pores (vugs). The results from thin section analysis for porosity showed that the estimated porosity lay between 30% and 50%, which is analogous to tests performed in well laboratories. During thin section preparation various resins and hardeners were used, including both epoxies and polyester resins. When samples were prepared with epoxy resin and epoxy diluents added in order to lower viscosity for a better penetration in the pores of the samples, little disturbance occurred. The overall c/f related distribution pattern was Porphyritic (Figure 1). During sample preparation using polyester resins, the exothermic reaction of the epoxy resin polymerization could have induced the dissolution of oil between the grains. This dissolution of the oil between grains allowed for observat