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Notional Field Development Final Report - EBN

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<strong>EBN</strong> <strong>Notional</strong> <strong>Field</strong> <strong>Development</strong> Plan<br />

but the clay bound water porosity sections were very similar to the uphole organic shales we are<br />

interested in. These lower sections will be mostly mechanically analogous because clay bound water<br />

drives the majority of the mechanical properties in these types of shales. The synthetic curves<br />

demonstrated good fidelity to the measured velocities over all ranges of porosity and lithology. we do<br />

have a measured DTC across the organic shales of interest in the KWK-01 well that will also allow us to<br />

quality check our synthetically derived DTC & DTS in that well.<br />

Figure 3-3, WWS-02 Stimlog Analysis - Best Fit Synthetic DTC-DTS<br />

3.1.3.2 Synthetic Neutron Calibration<br />

The OTL-1 well had both a neutron & DTC available across the target zones, so that well was used to<br />

baseline the calibration function. This may sound unorthodox, but the neutron and DTC both primarily<br />

respond to all the water in any formation. The only place they might significantly diverge is in a partially<br />

geopressured gas interval where the gas would make the DTC read higher and the neutron lower. In the<br />

crossplot data below, it is easy to see that the central range of data is going to only support a synthetic<br />

neutron with an accuracy of +/- .03 which is roughly a 10% swing in either direction. This will manifest<br />

itself in a total porosity that is too high by the same amount before we correct for clay and calculate<br />

kerogen volume.<br />

© 2011 Halliburton All Rights Reserved<br />

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