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Mr. Erik Milito - The House Committee on Natural Resources ...

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54 API STANDARD 65-2<br />

Cooke’s study [24,25] discovered fundamental mechanisms and explanati<strong>on</strong>s supporting some theories <strong>on</strong> loss of<br />

hydrostatic pressure and invalidating others. <str<strong>on</strong>g>The</str<strong>on</strong>g>se discoveries were verified by others such as a similar separate<br />

downhole sensor study (SPE 19552) by Morgan [40] while running and cementing casing in the North Sea. Morgan<br />

also reported how these downhole measurements indicated the failure to set an ECP.<br />

An analysis of downhole annular pressure measurements can explain other difficult to find or complex root causes for<br />

other cause effects such as high ECD pressures when cementing liners. Brehme et al [41] et al found that downhole<br />

pressure sensor measurements are a reliable method to help diagnose and evaluate liner running and liner<br />

cementing operati<strong>on</strong>s. Cementing simulati<strong>on</strong> computer model results were favorably compared to the actual<br />

downhole pressures. Brehme et al [41] proposed this process to help predict and evaluate results in future cementing<br />

operati<strong>on</strong>s by downhole gauge diagnosis of c<strong>on</strong>diti<strong>on</strong>s not included in software models such as annular restricti<strong>on</strong>s<br />

by cuttings, hole cleaning performance, and liner hanger equipment functi<strong>on</strong>s. For example, this data can help<br />

operators find answers for some annular flows linked to lost circulati<strong>on</strong> events such as those caused by complete or<br />

partial flow restricti<strong>on</strong>s in liner overlaps or liner hanger bypass or cross-secti<strong>on</strong>al areas plugged by cuttings not<br />

removed during hole cleaning operati<strong>on</strong>s.<br />

A.14 Some Key Results from Cooke's Study [24,25]<br />

Some of the key results from Cooke’s study [24,25] are as follows.<br />

1) Downhole sensor measurements proved that the loss of hydrostatic pressure in columns of unset cement may<br />

be reduced to values below those found in cement mixwater (fresh, sea or saltwater) density gradients [see A.3,<br />

no.4.a)]. See Figure A.2 (Figure 9 in SPE 11206) showing that the cement hydrostatic head from the sensor at<br />

1900 ft. in well G decreased from 13.4 lb/gal to 2.5 lb/gal equivalent density in ca. 420 minutes. This<br />

measurement is 6.0 lb/gal equivalent density below the average seawater gradient of 8.5 ppge. Cooke<br />

c<strong>on</strong>cluded that SGS development caused the cement hydrostatic head to regress to 2.5 ppge based <strong>on</strong> hole<br />

c<strong>on</strong>diti<strong>on</strong>s such as formati<strong>on</strong>s with little or no permeability across and above the sensor at 1900 ft. This<br />

invalidates the idea claimed in SPE 8255 [42] that the loss of hydrostatic head in the cement column never falls<br />

below the cement’s mixwater density gradient. It also invalidates the associated practice [38] of adding salt in<br />

cement slurries to increase the gradient and reduce the loss of hydrostatic head.<br />

2) Surface pressure applied to the annulus may not reach the desired depth depending <strong>on</strong> drilling fluid and cement<br />

properties such as gel strength development (A.3, no.4.b. and 5.7.8). See Figure A.3 (Figure 4 in SPE 11206)<br />

that illustrates the lack of pressure resp<strong>on</strong>se in 3 sensors at 4430 ft, 5454 ft, and 7412 ft in well B when surface<br />

pressure is applied. Also notice the large amount of pressure applied after 2100 minutes was high enough to<br />

break the cement SGS and allow hydrostatic pressure to be measured at 2 of the 3 sensors. Figure A.3 (Figure 2<br />

in SPE 11206) also shows no pressure resp<strong>on</strong>se from all sensors in well A by the applicati<strong>on</strong>s of surface<br />

pressure designed to test the validity of said practice described in SPE 8255 [42] . <str<strong>on</strong>g>The</str<strong>on</strong>g> surface pressure was<br />

applied 24 minutes after the cement job ended. This uncertainty in transmitting hydrostatic pressure through<br />

unset cement slurry at various times during a cement’s curing phase makes it unreliable to carry out the practice<br />

of applying and maintaining an annular surface pressure to compensate for hydrostatic head pressure losses as<br />

claimed in SPE 8255[42]. <str<strong>on</strong>g>The</str<strong>on</strong>g>refore, applying surface pressure by pumping into the top of the annulus should be<br />

c<strong>on</strong>sidered <strong>on</strong>ly for well c<strong>on</strong>trol purposes such as c<strong>on</strong>trolling a kick in the annulus. However, in some recent<br />

cases applying small amounts of surface pressure in the form of c<strong>on</strong>trolled pressure pulses has worked in some<br />

wells to help prevent annular flows when the entire process, including the cement system, is properly engineered,<br />

understood by all involved, and validated by relevant means such as the lab testing described in 5.7.8.<br />

3) Prior to Cooke’s study [24,25] our industry did not have relevant field data to fully understand and c<strong>on</strong>firm the<br />

theoretical mechanisms accounting for the rapid losses of designed overbalances after cementing jobs. Cooke’s<br />

measurement of this rapid decrease in cement column hydrostatic pressures to underbalanced c<strong>on</strong>diti<strong>on</strong>s<br />

across potential flow z<strong>on</strong>es helped explain the cause of many LWC incidents. It also helped explain how other<br />

annular flows such as cross-flows and underground blowouts were initiated. <str<strong>on</strong>g>The</str<strong>on</strong>g> understanding of how SCP<br />

may initiate via different types of annular pathways was also improved. Figure A.4 (Figure 2 in SPE11206)<br />

presents annular pressure and temperature measurements in well A that illustrate how the hydrostatic head

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