Abstract
Within the frame of an EFP-95 project NMR methods for porosity determination in 2D, and for fluid saturation determination in 1D and 2D have been developed. The three methods have been developed and tested on cleaned core samples of chalk from the Danish North Sea.
The main restriction for the use of the methods is the inherently short T2 relaxation constants of rock samples. Referring to measurements conducted at 200 MHz, the 2D porosity determination method is applicable to sample material with T2 relaxation constants down to 5 ms. The 1D fluid saturation determination method is applicable to sample material with T2 relaxation constants down to 3 ms, while the 2D fluid saturation determination method is applicable to material with T2 relaxation constants down to 8 ms. In the case of the 2D methods these constraints as a minimum enables work on the majority of chalk samples of Maastrichtian age. The ID fluid saturation determination method in addition is applicable to at least some chalk samples of Danian and pre-Maastrichtian age.
The spatial resolution of the 2D porosity determination method, the 1D fluid saturation methods, and the 2D fluid saturation method is respectively 0.8 mm, 0.8 mm and 2 mm. Reproducibility of pixel values is for all three methods 2 %- points.
The main restriction for the use of the methods is the inherently short T2 relaxation constants of rock samples. Referring to measurements conducted at 200 MHz, the 2D porosity determination method is applicable to sample material with T2 relaxation constants down to 5 ms. The 1D fluid saturation determination method is applicable to sample material with T2 relaxation constants down to 3 ms, while the 2D fluid saturation determination method is applicable to material with T2 relaxation constants down to 8 ms. In the case of the 2D methods these constraints as a minimum enables work on the majority of chalk samples of Maastrichtian age. The ID fluid saturation determination method in addition is applicable to at least some chalk samples of Danian and pre-Maastrichtian age.
The spatial resolution of the 2D porosity determination method, the 1D fluid saturation methods, and the 2D fluid saturation method is respectively 0.8 mm, 0.8 mm and 2 mm. Reproducibility of pixel values is for all three methods 2 %- points.
| Original language | English |
|---|---|
| Place of Publication | Copenhagen |
| Publisher | GEUS |
| Number of pages | 33 |
| DOIs | |
| Publication status | Published - 18 Apr 1997 |
Publication series
| Series | Danmarks og Grønlands Geologiske Undersøgelse Rapport |
|---|---|
| Number | 35 |
| Volume | 1997 |
Keywords
- Denmark
Programme Area
- Programme Area 3: Energy Resources
Fingerprint
Dive into the research topics of 'Quantitative NMR measurements on core samples. Technical report for the EFP-95 project : "Core investigations by use of different physical measurements" ENS Journal no. 1313/95-0007'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver