Estimating formation properties using saturation profiles

1. A method of estimating a T 2 cutoff of a porous media, the method comprising:

saturating a sample of the porous media with a fluid;

measuring a spatial T 2 distribution of the sample while saturated;

preparing the sample for unsaturated measurement by:

spinning the sample in a centrifuge with a first end of the sample closer to an axis of rotation of the centrifuge than a second end of the sample;

obtaining a saturation profile of the sample; and

identifying a first low-saturation portion of the sample;

measuring a spatial T 2 distribution of the porous media on the first low-saturation portion of the sample;

obtaining a first estimate of the T 2 cutoff of the porous media by comparing the spatial T 2 distribution measured on the first low-saturation portion of the sample with the spatial T 2 distribution measured under saturated conditions;

saturating the sample of the porous media with the fluid;

measuring a spatial T 2 distribution of the sample while saturated;

preparing the sample for unsaturated measurement by:

spinning the sample in a centrifuge with the second end of the sample closer to the axis of rotation of the centrifuge than the first end of the sample;

obtaining a saturation profile of the sample; and

identifying a second low-saturation portion of the sample;

measuring a spatial T 2 distribution of the porous media on the second low-saturation portion of the sample;

obtaining a second estimate of the T 2 cutoff of the porous media by comparing the spatial T 2 distribution measured on the second low-saturation portion of the sample with the spatial T 2 distribution measured under saturated conditions; and

averaging the first estimate of the T 2 cutoff and the second estimate of the T 2 cutoff.

2. The method of claim 1 , wherein obtaining the saturation profile of the sample comprises performing NMR measurements on the sample.

3. The method of claim 1 , comprising determining that the sample is heterogeneous.

4. The method of claim 3 , wherein determining that the sample is heterogeneous comprises comparing a maximum porosity and a minimum porosity of the sample.

5. The method of claim 1 , wherein identifying the first low-saturation portion of the sample comprises identifying a portion of the sample in which saturation of the sample is within 10% of a minimum saturation of that portion of the sample.

6. The method of claim 1 , wherein comparing the spatial T 2 distribution measured on the first low-saturation portion of the sample with the spatial T 2 distribution measured under saturated conditions comprises comparing the spatial T 2 distribution measured on the first low-saturation portion of the sample with a portion of the spatial T 2 distribution measured under saturated conditions that corresponds with the first low-saturation portion of the sample.

7. A method of estimating a T 2 cutoff of a porous media, the method comprising:

saturating a sample of the porous media with a fluid;

measuring a spatial T 2 distribution of the sample while saturated;

preparing the sample for unsaturated measurement by:

spinning the sample in a centrifuge with a first end of the sample closer to an axis of rotation of the centrifuge than a second end of the sample;

obtaining a saturation profile of the sample; and

identifying a first low-saturation portion of the sample;

measuring a spatial T 2 distribution of the porous media on the first low-saturation portion of the sample; and

obtaining a first estimate of the T 2 cutoff of the porous media by comparing the spatial T 2 distribution measured on the first low-saturation portion of the sample with the spatial T 2 distribution measured under saturated conditions.

8. The method of claim 7 , comprising determining that the sample is heterogeneous.

9. The method of claim 8 , comprising:

saturating the sample of the porous media with the fluid;

measuring a spatial T 2 distribution of the sample while saturated;

preparing the sample for unsaturated measurement by:

spinning the sample in a centrifuge with the second end of the sample closer to the axis of rotation of the centrifuge than the first end of the sample;

obtaining a saturation profile of the sample;

identifying a second low-saturation portion of the sample;

measuring a spatial T 2 distribution of the porous media on the second low-saturation portion of the sample;

obtaining a second estimate of the T 2 cutoff of the porous media by comparing the spatial T 2 distribution measured on the second low-saturation portion of the sample with the spatial T 2 distribution measured under saturated conditions; and

averaging the first estimate of the T 2 cutoff and the second estimate of the T 2 cutoff.

10. The method of claim 9 , wherein obtaining the saturation profile of the sample comprises performing NMR measurements on the sample.

11. The method of claim 9 , wherein identifying the first low-saturation portion of the sample comprises identifying a portion of the sample in which saturation of the sample is within 10% of a minimum saturation of that portion of the sample.

12. The method of claim 9 , wherein comparing the spatial T 2 distribution measured on the first low-saturation portion of the sample with the spatial T 2 distribution measured under saturated conditions comprises comparing the spatial T 2 distribution measured on the first low-saturation portion of the sample with a portion of the spatial T 2 distribution measured under saturated conditions that corresponds with the first low-saturation portion of the sample.

13. A method of estimating a property of a porous media, the method comprising:

saturating a sample of the porous media with a fluid;

spinning the sample in a centrifuge with a first end of the sample closer to an axis of rotation of the centrifuge than a second end of the sample;

measuring a first property of the porous media to obtain a first estimate of the first property;

saturating the sample of the porous media with the fluid after obtaining the first estimate of the first property;

spinning the sample in a centrifuge with the second end of the sample closer to the axis of rotation of the centrifuge than the first end of the sample;

measuring the first property of the porous media to obtain a second estimate of the first property; and

determining the second property of the porous media based at least in part on the first estimate of the first property and the second estimate of the first property.

14. The method of claim 13 , comprising determining that the sample is heterogeneous.

15. The method of claim 13 , comprising measuring the first property of the porous media after saturating the sample and before spinning the sample to obtain the first estimate of the first property.

16. The method of claim 13 , wherein the first property and the second property are different properties.

17. The method of claim 16 , wherein the first property is a spatial T 2 distribution.

18. The method of claim 17 , wherein the second property is a T 2 cutoff of the porous media.

19. The method of claim 13 , wherein determining the second property of the porous media comprises calculating a first estimate of the second property based on the first estimate of the first property, calculating a second estimate of the second property based on the second estimate of the first property, and averaging the first estimate of the second property and the second estimate of the second property.

20. The method of claim 13 , wherein measuring a first property of the porous media to obtain a first estimate of the first property comprises identifying a low-saturation portion of the sample and measuring a first spatial T 2 distribution of the porous media on the identified portion of the sample.

21. The method of claim 20 , wherein measuring a first property of the porous media to obtain a second estimate of the first property comprises identifying a low-saturation portion of the sample and measuring a second spatial T 2 distribution of the porous media on the identified portion of the sample.

22. The method of claim 21 , comprising calculating a first estimate of a T 2 cutoff of the porous media based the first spatial T 2 distribution, calculating a second estimate of the T 2 cutoff of the porous media based the first spatial T 2 distribution of the porous media, and averaging the first estimate of the T 2 cutoff and the second estimate of the T 2 cutoff.

23. The method of claim 20 , wherein identifying the low-saturation portion of the sample comprises performing NMR measurements on the sample.