This document discusses requirements for cavern storage in salt beds. It provides a history of cavern storage starting in 1961. Comparisons show that caverns have higher deliverability and capacity per well than other storage types. Requirements for cavern storage include suitable location of salt beds, adequate caprock above the salt, sources of raw water for leaching and brine disposal, and infrastructure. The leaching process and mechanics of cavern development are described. Operating a storage cavern involves injection and withdrawal facilities connected to pipelines. Variables like minimum pressure, insoluble content, and bed thickness impact cavern size.
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OUTLINE
History
Comparisons
Cavern Storage Requirements
Cavern Storage Operations
Effect of Variables
Questions
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HISTORY
1961 Southeastern Michigan Gas converts abandoned
brine caverns in bedded salt to gas storage.
1963 Saskatchewan Power Corporation commences
operations of first caverns designed specifically for gas
storage in bedded salt.
1964 First cavern storage in Armenia.
1966 First cavern storage in West Germany.
1968 First cavern storage in France.
1970 Transcontinental Gas Pipe Line Corporation commences
operations of first caverns designed specifically for gas
storage in a salt dome.
1974 First cavern storage in United Kingdom.
1981 First cavern storage in Denmark.
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COMPARISONS
RESERVOIR AQUIFER REEF MINE CAVERN
BASE GAS
59% 67% 40% 28% 29%
CAPACITY
PER
WELL 470 785 1,225 165 1,890
DELIVERABILITY
PER
WELL 3,320 3,395 20,930 10,940 72,715
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LOCATION
Acreage
Proximity to Pipelines
Proximity to Markets
Proximity to Raw Water Supply
Proximity to Brine Disposal
Proximity to Utilities
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SALT
Salt Purity
Existence and Nature of Caprock
Existence and Nature of Interbeds
Distribution of Interbeds
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ADVANTAGES OF SALT
Impervious to Hydrocarbons
Very High Compressive Strength
Ability to Yield and Divert Stresses
Ability to Flow and Heal Fractures
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CAPROCK
Not Present in Bedded Salts
Exact Origin Unknown
Believed to be Accumulation of Insolubles
Originally Transported in the Salt
Usually Comprised of Anhydrites, Gypsum,
and Dolomite
May be Highly Fractured with Numerous Lost
Circulation Zones
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RAW WATER
Fresh, Brackish, or Unsaturated Brine
Sources
Aquifers
Rivers
Canals
Lakes
Municipal Supplies
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BRINE DISPOSAL
Wells
Chemical Feedstock
Evaporation Plants
Solar Evaporation
Surface Waters
Displacement
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CAVERN SHAPING
Top of Insolubles
Raw Water Injection
Brine Return
Blanket Level
Production Casing
Brine Return
Raw Water Injection
SUMP DEVELOPMENT CAVERN DEVELOPMENT
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CAVERN MECHANICS
Sump Building Partially Cavern
BRINE
RETURN
INSOLUBLES
WATER INJECTION
BLANKET
LEVEL
BRINE
RETURN
WATER
INJECTION
BOTTOM
OF CAVERN
BRINE RETURN
BLANKET LEVEL
BOTTOM OF
CEMENTED CASING
BRINE
RETURN
DEPTH OF
ORIGINAL HOLE
BLANKET
LEVEL
INSOLUBLES
INSOLUBLES
Near Completion Developed Cavern Near Completion
WATER
INJECTI
ON