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The Hawaii Scientific Observation Hole (SOH) Program: Summary of Activities

Olson, Harry J.; Deymonaz, John E.

Key words
Drilling; Exploration; Hawaii; Diamond Core Drilling; Rotary Drilling; Slim Holes; Assessment Drilling; Noise Mitigation; Noise Monitoring; Temperature Surveys; Drilling Costs; Kilauea East Rift Zone
Location
Puna, Hawaii
Conference
Geothermal Resources Council Transactions
Year
1992
Session
Operations management; Environmental aspects; Noise pollutio
Language
English

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Abstract

The Hawaii Scientific Observation Hole (SOH) program was planned, funded and initiated in 1988 by the Hawaii Natural Energy Institute, an institute within the School of Ocean and Earth Science and Technology at the University of Hawaii at Manoa. Initial funding for the SOH program was $3.25 million supplied by the State of Hawaii to drill six, 4,000 foot scientific observation holes on Maui and the Big Island of Hawaii to confirm and stimulate geothermal resource development in Hawaii. After a lengthy permitting process, three SOHs, totaling 18,890 feet of mostly core drilling were finally drilled along the Kilauea East Rift Zone (KERZ) in the Puna district on the Big Island. The SOH program was highly successful in meeting the highly restrictive permitting conditions imposed on the program, and in developing slim hole drilling techniques,establishing subsurface geological conditions and initiating an assessment and characterization of the geothermal resources potential of Hawaii - even though permitting specifically prohibited pumping or flowing the holes obtain data of subsurface fluid conditions. The first hole, SOH-4, reached a depth of 2,000 meters, recorded a bottom hole temperature of 306.1°C and established subsurface thermal continuity along the KERZ between the HGP-A and the True/Mid Pacific Geothermal Venture wells. Although evidence of fossil reservoir conditions were encountered, no zones with obvious reservoir potential were found. The second hole, SOH-1, was drilled to a depth of 1,684 meters, recorded a bottom hole temperature of 206.1°C effectively doubled the size of Hawaii Geothermal Project - Abbott/Puna Geothermal Venture (HGP-A/PGV) proven/probable reservoir, and defined the northern limit of the HGP-A/PGV reservoir. The final hole, SOH-2 was drilled to a depth of 2,073 meters, recorded a bottom hole temperature of 350.5°C, and has sufficient indicated permeability to be designated as a potential "discovery".

Copyright 1992, Geothermal Resources Council. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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