Introduction
1. Geological and development characteristics of shale oil in China and North America
Table 1. Comparison of shale oil geological and development characteristics between China and America |
| Shale oil field/ reservoir | Sedimentary environment | Organic geochemical characteristics | Reservoir characteristics | Fluid characteristics | Initial daily oil production/t | |||
|---|---|---|---|---|---|---|---|---|
| Ro/% | TOC/% | Porosity/ % | Pressure coefficient | Crude oil density/ (g·cm-3) | GOR/ (m3·m-3) | |||
| Bakken oilfield in America | Marine deep-water anoxia | 0.70-1.30 | 10.0-20.0 | 5.0-12.0 | 1.3-1.6 | 0.78-0.83 | 50-375 | 10-300 |
| Eagelford oil field in America | Marine deep-water anoxia | 0.50-2.00 | 4.0-7.0 | 6.0-12.0 | 1.3-1.8 | 0.77-0.79 | 90-850 | 10-300 |
| Jimsar sag, Junggar Basin | Shore shallow lake-semi deep lake | 0.60-1.10 | 3.0-6.0 | 5.0-18.0 | 1.1-1.8 | 0.88-0.92 | 17 | 15 (average) |
| Mahu sag, Junggar Basin | Semi deep-deep alkali Lake | 0.85-1.40 | 0.2-4.1 | 3.0-8.0 | >1.5 | 0.84-0.88 | 44 (Maye 1 well) | |
| Gulong sag, Songliao Basin | Freshwater lake basin | 0.70-1.13 | 1.4-4.5 | 1.4-8.7 | 1.2-1.6 | 0.78-0.87 | 30-800 | 31 (Guye Youping 1 well) |
| Cangdong sag, Bohai Bay Basin | Inland saline lake basin | 0.50-1.10 | 1.5-3.5 | 3.0-7.0 | 0.9-1.2 | 0.86-0.89 | 82-103 | 5-20 |
| Jiyang Depression, Bohai Bay Basin | Semi deep-deep saline lake basin | 0.50-1.00 | 0.6-16.7 | 1.7-12.0 | 1.2-1.8 | 0.77-0.93 | 0-100 | 6-44 |
| Chang 7 member of Ordos Basin | Semi deep lake- deep lake | 0.70-1.10 | 6.0-38.0 | 2.0-3.0 | 0.6-0.8 | 0.84-0.86 | 60-120 | 8-18 |
2. Evaluation methods and techniques of continental shale oil development
2.1. Lithofacies evaluation technology
2.1.1. Classification of shale lithofacies
Fig. 1. Microscopic characteristics of common shale lithofacies types in Jiyang Depression. (a) Organic rich sparitie laminar calcareous shale; (b) Organic rich cryptocrystalline laminar calcareous shale; (c) Organic rich cryptocrystalline laminar calcareous- argillaceous shale; (d) Organic rich cryptocrystalline layered calcareous-argillaceous shale; (e) Organic cryptocrystalline layered calcareous-argillaceous shale; (f) Organic cryptocrystalline massive calcareous-argillaceous shale. |
2.1.2. Lithofacies identification technology
2.2. Reservoir characterization technology
Table 2. Comparison of quantitative characterization techniques of reservoir space |
| Method | Advantage | Disadvantage |
|---|---|---|
| High- pressure mercury injection | Fast test, relatively simple principle and operation. It can obtain many important pore physical parameters such as porosity, pore size distribution, skeleton density, apparent density and specific surface area. It has certain advantages in studying the distribution of large pores and determining the effective porosity of shale. | The surface heterogeneity and liquid-solid interaction of rock samples will affect the measurement of surface tension and diffusion coefficient, and cause the measurement error of pore distribution. The actual mercury saturation is low and the data is incomplete. High pressure will open cracks in shale, resulting in measurement errors. Mercury injection method is used to measure the maximum pore opening size, so the pore throat makes the measurement result of pore size distribution deviate from the real value. |
| Nitrogen adsorption | No damage test method. The specific surface area, fractal dimension and pore size distribution can be obtained. It has certain advantages in studying micropore and mesopore of shale. | The test results are affected by the selected model and the accuracy varies greatly. Throat and pore cannot be distinguished in pore distribution measurement. The pore distribution and structural characteristics of macropores cannot be characterized. The porosity information of the sample cannot be obtained separately. Different working gases correspond to different test pore ranges. |
| NMR | No damage test method. It can accurately characterize the pore size distribution in the whole pore scale, such as porosity, permeability, fluid saturation. | Nanoscale pore relaxation time is short and difficult to be completely detected. Water and organic matter in shale pores are difficult to distinguish and their data interpretation are difficult. The transverse relaxation time curve can only reflect the distribution trend of pore size. They are not the absolute pore size, so the pore size should be calculated by mercury injection. |
2.3. Mobility evaluation technology
2.4. Fracability evaluation technology
2.5. Productivity evaluation
2.5.1. Productivity evaluation based on production data analysis
Fig. 2. Comparison of prediction results with different productivity evaluation methods. |