Bayou Choctaw Salt Dome, SPR

Bayou Choctaw Salt Dome, SPR PDF Author:
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ISBN:
Category :
Languages : en
Pages : 532

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Bayou Choctaw Salt Dome, SPR

Bayou Choctaw Salt Dome, SPR PDF Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 532

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Book Description


Features of Bayou Choctaw SPR Caverns and Internal Structure of the Salt Dome

Features of Bayou Choctaw SPR Caverns and Internal Structure of the Salt Dome PDF Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 64

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Book Description
The intent of this study is to examine the internal structure of the Bayou Choctaw salt dome utilizing the information obtained from graphical representations of sonar survey data of the internal cavern surfaces. Many of the Bayou Choctaw caverns have been abandoned. Some existing caverns were purchased by the Strategic Petroleum Reserve (SPR) program and have rather convoluted histories and complex cavern geometries. In fact, these caverns are typically poorly documented and are not particularly constructive to this study. Only two Bayou Choctaw caverns, 101 and 102, which were constructed using well-controlled solutioning methods, are well documented. One of these was constructed by the SPR for their use while the other was constructed and traded for another existing cavern. Consequently, compared to the SPR caverns of the West Hackberry and Big Hill domes, it is more difficult to obtain a general impression of the stratigraphy of the dome. Indeed, caverns of Bayou Choctaw show features significantly different than those encountered in the other two SPR facilities. In the number of abandoned caverns, and some of those existing caverns purchased by the SPR, extremely irregular solutioning has occurred. The two SPR constructed caverns suggest that some sections of the caverns may have undergone very regular solutioning to form uniform cylindrical shapes. Although it is not usually productive to speculate, some suggestions that point to the behavior of the Bayou Choctaw dome are examined. Also the primary differences in the Bayou Choctaw dome and the other SPR domes are noted.

Strategic Petroleum Reserve (SPR) Geological Site Characterization Report, Bayou Choctaw Salt Dome. Sections I and II.

Strategic Petroleum Reserve (SPR) Geological Site Characterization Report, Bayou Choctaw Salt Dome. Sections I and II. PDF Author:
Publisher:
ISBN:
Category :
Languages : en
Pages :

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This report comprises two sections: Bayou Choctaw cavern stability issues, and geological site characterization of Bayou Choctaw. (DLC).

Strategic Petroleum Reserve

Strategic Petroleum Reserve PDF Author: United States. Strategic Petroleum Reserve Office
Publisher:
ISBN:
Category : Environmental impact analysis
Languages : en
Pages : 806

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Final Environmental Impact Statement for Bayou Choctaw Salt Dome

Final Environmental Impact Statement for Bayou Choctaw Salt Dome PDF Author: United States. Strategic Petroleum Reserve Office
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 200

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Draft Environmental Impact Statement for Bayou Choctaw Salt Dome

Draft Environmental Impact Statement for Bayou Choctaw Salt Dome PDF Author: United States. Strategic Petroleum Reserve Office
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 618

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Strategic Petroleum Reserve

Strategic Petroleum Reserve PDF Author: United States. Strategic Petroleum Reserve Office
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 192

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Supplement to Final Environmental Impact Statement for Bayou Choctaw Salt Dome

Supplement to Final Environmental Impact Statement for Bayou Choctaw Salt Dome PDF Author: United States. Strategic Petroleum Reserve Office
Publisher:
ISBN:
Category : Petroleum
Languages : en
Pages : 202

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Strategic Petroleum Reserve (SPR) Additional Geologic Site Characterization Studies, Bayou Choctaw Salt Dome, Louisiana

Strategic Petroleum Reserve (SPR) Additional Geologic Site Characterization Studies, Bayou Choctaw Salt Dome, Louisiana PDF Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 91

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Book Description
This report revises and updates the geologic site characterization report that was published in 1980. Revised structure maps and sections show interpretative differences in the dome shape and caprock structural contours, especially a major east-west trending shear zone, not mapped in the 1980 report. Excessive gas influx in Caverns 18 and 20 may be associated with this shear zone. Subsidence values at Bayou Choctaw are among the lowest in the SPR system, averaging only about 10 mm/yr but measurement and interpretation issues persist, as observed values often approximate measurement accuracy. Periodic, temporary flooding is a continuing concern because of the low site elevation (less than 10 ft), and this may intensify as future subsidence lowers the surface even further. Cavern 4 was re-sonared in 1992 and the profiles suggest that significant change has not occurred since 1980, thereby reducing the uncertainty of possible overburden collapse -- as occurred at Cavern 7 in 1954. Other potential integrity issues persist, such as the proximity of Cavern 20 to the dome edge, and the narrow web separating Caverns 15 and 17. Injection wells have been used for the disposal of brine but have been only marginally effective thus far; recompletions into more permeable lower Pleistocene gravels may be a practical way of increasing injection capacity and brinefield efficiency. Cavern storage space is limited on this already crowded dome, but 15 MMBBL could be gained by enlarging Cavern 19 and by constructing a new cavern beneath and slightly north of abandoned Cavern 13. Environmental issues center on the low site elevation: the backswamp environment combined with the potential for periodic flooding create conditions that will require continuing surveillance.

Threat of a Sinkhole

Threat of a Sinkhole PDF Author:
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ISBN:
Category :
Languages : en
Pages : 15

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Cavern Lake at Bayou Choctaw salt dome resulted from the failure of Cavern 7 in 1954. Uncontrolled solutioning of this cavern through the thin caprock had set the stage for overburden to collapse into the cavern below. A similar situation developed with nearby Cavern 4, but with less dissolutioning of the caprock. Because pressure loss was already a problem and because another 800 ft diameter lake would have endangered surface operations, solutioning of Cavern 4 was stopped and the cavern abandoned in 1957 in order to protect the already-small site. In 1978 the Strategic Petroleum Reserve (SPR) acquired a number of caverns at Bayou Choctaw, including Cavern 4, and the possible repeat of the Cavern 7 failure and formation of another lake thus became an issue. The cavern dimensions were re-sonared in 1980 for comparison with 1963 and 1977 surveys. Annual surface leveling between 1982--1992 showed less subsidence occurring than the site average, and a cavern monitoring system, installed in 1984, has revealed no anomalous motion. Repeat sonar surveys in 1992 showed very little, if any, change occurred since 1980 although a small amount of uncertainty exists as a result of changing sonar techniques. We conclude that significant additional solutioning or erosion of the caprock has not occurred and that there is no increased threat to SPR operations.