Rock core water-containing analysis method
An analysis method and core technology, which is applied in the analysis of drilling and exploration cores, and in the field of core water analysis, can solve the problems of not being able to meet the needs of rapid on-site analysis, many supporting equipment, and long test periods, so as to improve the interpretation rate, use less, and The effect of easy operation
- Summary
- Abstract
- Description
- Claims
- Application Information
AI Technical Summary
Problems solved by technology
Method used
Examples
Embodiment 1
[0028] Embodiment one: the rock core water content analysis method of the present invention adopts the following process steps:
[0029] Take a core sample from Well XX at a depth of 2100.5 meters 2cm 3 , after the core sample is crushed, a volume of 10cm is added to the test cylinder 3 Deionized water floods the core sample for efficient leaching of various ions. Fractured core samples are routine techniques. The test cylinder is a sealable container, which can be a general-purpose graduated cylinder or any other type of container.
[0030] 2. Seal the test cylinder and soak the core sample at room temperature for 24 hours; the test cylinder should be airtight to prevent inaccurate data caused by deionized water and various ion losses. The soaking time should not be too short, otherwise various ions will not be completely leached out, and the measured data will be unreliable. The longer the soaking time, the more complete the diffusion of various ions, but it is not neces...
Embodiment 2
[0046] Take a 2cm core sample from Well X at a depth of 2106.5 meters 3 , put in a 10cm 3 Soak in the test cylinder of deionized water for 48 hours. After measuring the conductivity, the relationship between conductivity and salinity is converted, and the calculated salinity is 50mg / L. It is known that the porosity of this sample is 15%, and the salinity of formation water is 6000mg / L.
[0047] Calculate the water saturation of the core according to the following formula:
[0048] S w =V 水 K 测 / (V 岩 K 地 φ)
[0049] =10×50 / (2×6000×15%)
[0050]= 27.78%.
[0051] That is, the water saturation of this sample is 27.78%, which is a low aquifer.
Embodiment 3
[0053] Take a 5cm core sample from Well Y at a depth of 1800.5 meters 3 , put in a 10cm 3 Soak in the test cylinder of deionized water for 24 hours. After measuring the conductivity, the relationship between conductivity and salinity is converted, and the calculated salinity is 100mg / L. It is known that the porosity of this sample is 10%, and the salinity of formation water is 10000mg / L.
[0054] Calculate the water saturation of the core according to the following formula:
[0055] S w =V 水 K 测 / (V 岩 K 地 φ)
[0056] =10×100 / (5×10000×10%)
[0057] = 20%.
[0058] That is, the water saturation of this sample is 20%, which is a low aquifer.
PUM
Property | Measurement | Unit |
---|---|---|
porosity | aaaaa | aaaaa |
porosity | aaaaa | aaaaa |
porosity | aaaaa | aaaaa |
Abstract
Description
Claims
Application Information
- R&D Engineer
- R&D Manager
- IP Professional
- Industry Leading Data Capabilities
- Powerful AI technology
- Patent DNA Extraction
Browse by: Latest US Patents, China's latest patents, Technical Efficacy Thesaurus, Application Domain, Technology Topic, Popular Technical Reports.
© 2024 PatSnap. All rights reserved.Legal|Privacy policy|Modern Slavery Act Transparency Statement|Sitemap|About US| Contact US: help@patsnap.com