Salt dissolution and collapse at the Wink Sink in West Texas

Technical Report · Sun Jun 01 04:00:00 EDT 1986

OSTI ID:5658932

Johnson, K S

The Wink Sink, in Winkler County, Texas, is a collapse feature that formed in June 1980 when an underground dissolution cavity migrated upward by successive roof failures until it breached the land surface. The original cavity developed in the Permian Salado Formation salt beds more than 1300 feet below ground level. Natural dissolution of salt occurred in the vicinity of the Wink Sink in several episodes that began as early as Salado time and recurred in later Permian, Triassic, and Cenozoic time. Although natural dissolution cavity and resultant collapse were influenced by petroleum production activity in the immediate area. Drilling, completion, and plugging procedures used on an abandoned oil well at the site of the sink appear to have created a conduit that enabled water to circulate down the borehole and dissolve the salt. When the dissolution cavity became large enough, the roof failed and the overlying rocks collapsed into the cavity. Similar collapse features exist where underground salt beds have been intentionally dissolved during solution mining or accidentally dissolved as a result of petroleum production activities.

• Research Organization: Battelle Memorial Inst., Columbus, OH (USA). Office of Nuclear Waste Isolation
• DOE Contract Number: AC02-83CH10140
• OSTI ID: 5658932
• Report Number(s): BMI/ONWI-598; ON: DE86012245
• Country of Publication: United States
• Language: English

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