Estimating adsorbed gas volume from NMR and dielectric logs
US-9753176-B2 · Sep 5, 2017 · US
US9939506B2 · US · B2
| Field | Value |
|---|---|
| Publication number | US-9939506-B2 |
| Application number | US-201314406503-A |
| Country | US |
| Kind code | B2 |
| Filing date | May 24, 2013 |
| Priority date | Jun 8, 2012 |
| Publication date | Apr 10, 2018 |
| Grant date | Apr 10, 2018 |
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A methods are provided for investigating a sample containing hydrocarbons by subjecting the sample to a nuclear magnetic resonance (NMR) sequence using NMR equipment, using the NMR equipment to detect signals from the sample in response to the NMR sequence, analyzing the signals to extract a distribution of relaxation times (or diffusions), and computing a value for a parameter of the sample as a function of at least one of the relaxation times (or diffusions), wherein the computing utilizes a correction factor that modifies the value for the parameter as a function of relaxation time for at least short relaxation times (or as a function of diffusion for at least large diffusion coefficients).
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What is claimed is: 1. A method of investigating a geological formation traversed by a borehole, comprising: a) obtaining a nuclear magnetic resonance (NMR) tool; b) subjecting a sample of known porosity to a nuclear magnetic resonance (NMR) sequence with a pulse echo spacing using the NMR tool; c) determining a normalized bias B(T 2 ) of said NMR tool as a function of T 2 relaxation times; d) locating the NMR tool in the borehole and detecting signals in response to said NMR sequence at at least one depth in the borehole; e) analyzing a decay of the detected signals with a computer processor, in order to extract a distribution of the T 2 relaxation times; and f) computing and providing, with the computer processor, a value for porosity of the formation at said depth as a function of at least one of said T 2 relaxation times, wherein said computing utilizes a correction factor that modifies the value of the parameter as a function of the T 2 relaxation time for at least the T 2 relaxation times occurring on the order of said pulse echo spacing, wherein said correction factor is a function of said normalized bias. 2. A method according to claim 1 , wherein: said pulse echo spacing is approximately 0.2 ms, and said relaxation times on the order of said pulse echo spacing are 1 ms and less. 3. A method according to claim 1 , wherein: said correction factor is c f (T 2 )=1/(1+B(T 2 )). 4. A method according to claim 2 , wherein: B ( T 2 ) ≈ ϕ ^ ( T 2 ) - ϕ T ϕ T where ϕ T and {circumflex over (ϕ)}(T 2 ) are respectively a true and an estimated porosity of a calibration sample obtained from a porosity sensitivity curve for said NMR tool. 5. A method according to claim 1 , wherein: said correction factor is c f ( T 2 ) = 1 1 + B ( T 2 ) R ( T 2 ) β ( R ( T 2 ) ) + R ( T 2 ) where R ( T 2 ) = ϕ ^ ( T 2 ) σ ϕ ( T 2 ) and corresponds to a signal to noise ratio for a given T 2 , β is a scalar, < > is an average computed over T 2 , B ( T 2 ) ≈ ϕ ^ ( T 2 ) - ϕ T ϕ T is the relative bias obtained from an NMR sensitivity curve of said NMR tool where ϕ T is a true porosity of a calibration sample and ϕ(T 2 ) is an estimated porosity of the calibration sample, and σ ϕ is a standard deviation of the estimated porosity. 6. A method according to claim 5 , wherein: said correction factor tends to a value of 1 with respect to a particular T 2 relaxation time when said signal to noise ratio is small for that particular T 2 relaxation time. 7. A method acco
Relaxometry, i.e. quantification of relaxation times or spin density (G01R33/50 takes precedence) · CPC title
Processing data, e.g. for analysis, for interpretation, for correction · CPC title
Signal processing systems, e.g. using pulse sequences {; Generation or control of pulse sequences; Operator console} · CPC title
operating with electron or nuclear magnetic resonance · CPC title
Making measurements of geologic samples, e.g. measurements of moisture, pH, porosity, permeability, tortuosity or viscosity · CPC title
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