Evaluating And Imaging Volumetric Void Space Location For Cement Evaluation
US-2017199298-A1 · Jul 13, 2017 · US
US10215876B2 · US · B2
| Field | Value |
|---|---|
| Publication number | US-10215876-B2 |
| Application number | US-201615286776-A |
| Country | US |
| Kind code | B2 |
| Filing date | Oct 6, 2016 |
| Priority date | Oct 6, 2016 |
| Publication date | Feb 26, 2019 |
| Grant date | Feb 26, 2019 |
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In-phase and quadrature components have different relationships with some important petrophyscial parameters, such as water saturation and mineral cation exchange capacity (CEC). In clay-containing subterranean rock formation such as shaly sand formations, these parameters can be estimated using different components of array induction tool data combined with other knowledge about the clay-containing formation. Some parameters, such as mobility and fraction of counterions are valid in cases where the pore water solution is an electrolyte of NaCl.
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What is claimed is: 1. A method of estimating parameters for a clay-containing subterranean rock formation comprising: positioning a tool in a borehole traversing the clay-containing formation, the tool comprising one or more transmitter coils and a plurality of receiver coils; inducing alternating current loops in the clay-containing formation using the one or more transmitter coils; measuring a signal resulting from the induced current loops using the receiver coils; combining measurements from the receiver coils and knowledge about the clay-containing formation to obtain an estimate of water saturation in the formation and an estimate of cation exchange capacity in the formation; and wherein the estimate of water saturation in the formation and the estimate of cation exchange capacity are obtained using a first relationship between real conductivity and a first plurality of formation parameters and a second relationship between complex conductivity and a second plurality of formation parameters. 2. The method of claim 1 wherein the first and second pluralities of formation parameters both comprise water saturation and the estimate of cation exchange capacity. 3. The method of claim 2 wherein the first plurality of formation parameters further comprises: water conductivity, grain density; mobility of counterions; and an electric formation factor. 4. The method of claim 3 wherein said water conductivity is calculated using water salinity and temperature. 5. The method of claim 4 wherein said water salinity is estimated using borehole water samples. 6. The method of claim 5 wherein said temperature and said grain density are obtained from temperature and laboratory density measurement data. 7. The method of claim 2 wherein the second plurality of formation parameters further comprises: grain density; a fraction of counterions in a Stern layer; and mobility of counterions within the Stern layer. 8. The method of claim 1 wherein said knowledge about the formation is obtained from laboratory measurements and/or measurement logs. 9. The method of claim 8 wherein said measurement logs include a laboratory density measurement and a temperature log from which temperature and grain density is obtained. 10. The method of claim 1 wherein the clay-containing subterranean rock formation is a shaly-sand formation. 11. The method of claim 1 wherein the tool is suspended from a wireline. 12. The method of claim 1 wherein said plurality of receiver coils comprises at least three receiver coils arranged in a receiver array.
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