Case History: New Gas Flow Computer Design Facilitates Offshore Measurement In Gulf Coast Project

1998 ◽  
Author(s):  
Mike Chunn ◽  
Wayne Bonin ◽  
Danny E. McFarland ◽  
Ken Jenkins ◽  
Kevin D. Fink
1999 ◽  
Author(s):  
Wayne Bonin ◽  
Mike Chunn ◽  
Danny E. McFarland ◽  
Ken Jenkins ◽  
Kevin Fink

1994 ◽  
Vol 13 (8) ◽  
pp. 858-860 ◽  
Author(s):  
Scott MacKay ◽  
Bill Dragoset
Keyword(s):  

2018 ◽  
Vol 2018 (8) ◽  
pp. 4-13
Author(s):  
Лидия Нартова ◽  
Lidiya Nartova ◽  
Валерий Бодрышев ◽  
Valeriy Bodryshev

In the work there is offered a generalized method for complex surface geometrical modeling with regard to a wide class of problems with an engineering direction. This method is based on the investigation of the applicability of frame, surface or solid-state models. The investigations were based on the analysis of the practical application of frame, surface and solidstate models and their images on the basis of presentday software tools. By the example of deciphering a problem of a cylindrical object flow with a gas supersonic flow according to an intensity parameter of a frame image the 3D image of the “image intensity” function with the use of MatLab and SolidWorks programs is formed. The results of a geometrical solution are compared and an optimum surface image is chosen. The investigation for a specific version provides a visualization of a supersonic gas flow motion and finally offers recommendations for an optimum design of a product. The method described may be used in the course of designing objects having a gas or liquid flow, complex surfaces in the products of aircraft industry. It is approbated at lecturing subjects “Engineering and Computer Graphics”, “Descriptive Geometry”, and also in scientific and diploma works of students with specialties “Aircraft and Helicopter Manufacturing”, “Aircraft Engines”, “Computer design in Aircraft Manufacturing”.


Geophysics ◽  
1989 ◽  
Vol 54 (4) ◽  
pp. 426-439 ◽  
Author(s):  
James L. Allen ◽  
J. M. Bruso

False structures can appear on seismic data in the shadow of normal growth faults, with the upthrown time structure appearing to roll into the fault where no such roll exists in depth. This phenomenon was encountered in a prospect in the Frio formation of the Texas Gulf Coast, where a large growth fault expanded a thick, low‐velocity shale above the Frio. Two check‐shot velocity surveys, one at either end of the seismic control, demonstrated a severe average velocity gradient across the prospect at the level of the objective geologic formation. Assuming first one and then the other velocity survey was valid over the entire area for conversion of well data to time produced a drastic difference in the structural interpretation of the seismic data. The more obvious interpretation required a down‐to‐the‐northwest fault with a downthrown rollover anticline at the objective formation. This interpretation had been previously tested with a dry hole on the crest of the time structure. This interpretation also contradicted a dipmeter in this “crestal” well. Using a model derived from interval velocities from the nearby check‐shot surveys, we were able to demonstrate that over 200 ms of apparent seismic dip in the shadow of the growth fault was false. When we used stacking velocities to perform a depth conversion of the seismic time section, both the apparent dip direction of the formation and interpreted throw direction of the fault were reversed. Based on these results, a well was drilled which demonstrated the qualitative success of our model. We also discovered that minor buried faulting mapped behind the major fault was a false effect caused by velocity contrasts across the growth fault. This case history proves that the recognition and proper use of velocity gradients can be extremely important in the Gulf Coast.


2022 ◽  
Author(s):  
Mark Norris ◽  
Marc Langford ◽  
Charlotte Giraud ◽  
Reginald Stanley ◽  
Steve Ball

Abstract Hydraulic fracturing has been well established in the Southern North Sea (SNS) since the mid-1980s; however, it has typically been conducted as the final phase of development in new gas fields. One of these fields is Chiswick located in the Greater Markham area 90 miles offshore UK in 130 ft of water. Following an unsuccessful well repair of the multi-fractured horizontal well C4, it was decided to cost-effectively and expediently exploit the remaining pressure-depleted reserves near the toe via a single large fracture initiated from a deviated sidetrack wellbore designated C6. A deviated wellbore was chosen versus the original near-horizontal well to reduce well risk and costs and ultimately deliver an economic well. Several key challenges were identified, and mitigating measures were put in place. Modular formation dynamics tester data from the sidetrack open hole indicated the reservoir pressure gradient had depleted to 0.23 to 0.25 psi/ft, raising concerns about the ability of the well to unload the fluid volumes associated with a large fracture treatment. Wellbore deviation and azimuth with the associated potential for near-wellbore tortuosity would drive a typically short perforation interval (i.e., 3 ft). However, a compromise to mitigate convergent pressure loss in depletion was required, and the perforation interval was therefore set at 14 ft with provision made for robust step-down tests (SDT) and multi-mesh sand slugs. To further offset any near-well convergence pressure drop during cleanup, an aggressive tip screenout (TSO) proppant schedule, including a high concentration tail-in (12 PPA) with an aggressive breaker schedule, was executed to fully develop propped hydraulic width. Following formation breakdown and SDT to 40 bbl/min, the well went on near-instantaneous vacuum. Clearly, an extremely conductive feature had been created or contacted. However, upon use of a robust crosslinked gel formulation and 100-mesh sand, the bottomhole and positive surface pressure data allowed a suitable fracture design to be refined and placed with a large width, as evidenced by the extreme 2,309-psi net pressure development over that of the pad stage while placing 500,500 lbm of 16/30 resin-coated (RC) intermediate strength proppant (ISP) to 12 PPA. Although a lengthy nitrogen lift by coiled tubing (CT) was planned, the well cleanup response in fact allowed unaided hydrocarbon gas flow to surface within a short period. The well was then further beaned-up under well test conditions to a flow rate of approximately 26 MMscf/D under critical flowing conditions with a higher bottomhole flowing pressure than that of the original C4 well. Given the last producing rate of the original multiple fractured horizontal wellbore was 27 MMscf/D at a drawdown of 1,050 psi through two separate hydraulic fractures, then the outcome of this well was judged to be highly successful and at the limit of predrill expectations. This case history explains and details the rationale, methods, and techniques employed in well C6 to address the challenge of successful hydraulic fracture stimulation in a depleted formation. Challenges were addressed by combining a number of techniques, coupled with field experience, resulting in a highly productive well despite the relatively low reservoir pressure coupled with a limited time frame to plan and execute. These techniques are transferrable to other offshore gas fields in the region where reservoir depletion makes economic recovery difficult or indeed prohibitive.


Author(s):  
N. David Theodore ◽  
Mamoru Tomozane ◽  
Ming Liaw

There is extensive interest in SiGe for use in heterojunction bipolar transistors. SiGe/Si superlattices are also of interest because of their potential for use in infrared detectors and field-effect transistors. The processing required for these materials is quite compatible with existing silicon technology. However, before SiGe can be used extensively for devices, there is a need to understand and then control the origin and behavior of defects in the materials. The present study was aimed at investigating the structural quality of, and the behavior of defects in, graded SiGe layers grown by chemical vapor deposition (CVD).The structures investigated in this study consisted of Si1-xGex[x=0.16]/Si1-xGex[x= 0.14, 0.13, 0.12, 0.10, 0.09, 0.07, 0.05, 0.04, 0.005, 0]/epi-Si/substrate heterolayers grown by CVD. The Si1-xGex layers were isochronally grown [t = 0.4 minutes per layer], with gas-flow rates being adjusted to control composition. Cross-section TEM specimens were prepared in the 110 geometry. These were then analyzed using two-beam bright-field, dark-field and weak-beam images. A JEOL JEM 200CX transmission electron microscope was used, operating at 200 kV.


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