Researchers collected samples that included approximately a dozen dead oil samples, 5 gallons of dead oil, 5 gallons of oily sand, and several well logs.
The project team has made over 15 presentations at technical meetings (e.g., SEG, ACS, etc.). Five students completed graduate degrees and theses (two Ph.D. and three M.S.); two additional students are finishing thesis work. Two peer reviewed papers were published, several are under review, and several more will be completed in the last weeks of the project.
Saturate-Aromatic-Resin-Asphaltene (SARA) fractions have been measured on site and by an outside laboratory. The SARA technique has large experimental variation when used to measure heavy oils. Asphaltene content varied from 3 to 9% in the same sample measured by CSM and an outside laboratory. More powerful chemical characterization techniques are being pursued.
The oils (including more than 18 oil, oil/sand, oil/water, and oil/sand/water mixtures) exhibited non-Newtonian characteristics, including shear thinning and a non-zero shear modulus. The complex viscosity of the dead oils has been found to be as high as 7,000 Pa-s and a shear modulus at -10 oC above 10,000 Pa (and frequency dependent). A complete set of “live” oil rheology experiments were completed. A large range of temperatures (-10 to 60°C) and pressures (15 to 2000 psi) were controlled and viscosity measured in novel high-pressure rheology setup.
A number of field trips to North Slope Alaska (January 2009, August 2010, November 2010, March 2012) were undertaken to coordinate sample/core retrieval, discuss objectives, and complete a sample testing plan with BP. Two presentations were given at the BP Heavy Oil Symposium in November 2010 with 150 people (from industry, academia, and government) attending in Anchorage, AK.
Development of the rock physics model continued with the addition of the Cold Heavy Oil Production Sands (CHOPS) hypothesis and an estimation of the properties of the wormholes for the Ugnu Formation. The model showed significant evidence of absorption due to the presence of the wormholes, suggesting the possibility of detecting small changes in the reservoir. The capacity of imaging such changes both in the amplitude spectrum and the image space has been quantified.
The Measured velocity-temperature trend on heavy oil sands suggests that the thermal damage to the sand frame is caused by thermal pressure of heavy oil. Thermal damage mainly occurs at low temperature and is reduced with increasing temperature. The thermal damage is limited by rock texture and degree of compaction. Analysis of measured data suggests that Gassmann’s model works well for heavy oil sands at temperature higher than the liquid point. The thermal damage effect on sand frame will need to be accounted for when modeling the velocity-temperature trend of heavy oil sands.