Hawaii Play Fairway: Preliminary Core Box Photos, Lanai Island, Hawaii

Lautze, Nicole; Thomas, Donald; Haskins, Eric

doi:10.15121/1888759

Title: Hawaii Play Fairway: Preliminary Core Box Photos, Lanai Island, Hawaii

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Abstract

Photos of core samples from Lanai Island. During the third phase of the Hawaii Play Fairway project, further exploration involved drilling a groundwater well in Lanai's Palawai Basin and performing more geophysical surveys. The project deepened an existing water well on Lanai. Drilling occurred 24/7 the entire month of June 2019 over which time Lanai Well 10 was deepened from 427 m to 1057 m, with continuous core collected. The roughly linear temperature gradient was an average of 42 degC/km, and a maximum bottom hole temperature, 66 degC. This gradient is more than twice the background for Hawaii and within a range of gradients measured in this depth range for some exploration wells within KERZ. The Hawaii Play Fairway project seeks to explore the geologic structures that exist in the caldera region of Hawaiian volcanoes; how those structures influence groundwater storage and flow; and how the magmatic heat from Hawaiian shield volcanoes cools over time. The Hawaii Groundwater and Geothermal Resources Center (Hawaii Institute of Geophysics and Planetology, University of Hawaii at Manoa) executed the Hawaii Play Fairway project. For more information, go to HGGRC's website that is linked in the resources.

Authors:: Lautze, Nicole; Thomas, Donald; Haskins, Eric

Publication Date:: Mon Jul 01 00:00:00 EDT 2019

Other Number(s):: 1411

DOE Contract Number:: EE0006729

Research Org.:: USDOE Geothermal Data Repository (United States); Univ. of Hawaii, Honolulu, HI (United States)

Sponsoring Org.:: USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Program (EE-4G)

Collaborations:: University of Hawaii

Subject:: 15 Geothermal Energy

Keywords:: geothermal; energy; Hawaii; Lanai; PFA; Play Fairway Analysis; core photos; core; well data; Palawai Basin; exploration; characterization; hydrothermal; KERZ

Geolocation:: 20.97895794151,-156.77844892578|20.708216372159,-156.77844892578|20.708216372159,-157.09330488281|20.97895794151,-157.09330488281|20.97895794151,-156.77844892578

OSTI Identifier:: 1888759

DOI:: https://doi.org/10.15121/1888759

Project Location:

Citation Formats


                    Lautze, Nicole, Thomas, Donald, and Haskins, Eric. Hawaii Play Fairway: Preliminary Core Box Photos, Lanai Island, Hawaii.  United States: N. p., 2019. 
        Web.  doi:10.15121/1888759.

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                    Lautze, Nicole, Thomas, Donald, & Haskins, Eric. Hawaii Play Fairway: Preliminary Core Box Photos, Lanai Island, Hawaii.  United States.  doi:https://doi.org/10.15121/1888759

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                    Lautze, Nicole, Thomas, Donald, and Haskins, Eric. 2019.  
"Hawaii Play Fairway: Preliminary Core Box Photos, Lanai Island, Hawaii".  United States.  doi:https://doi.org/10.15121/1888759.  https://www.osti.gov/servlets/purl/1888759. Pub date:Mon Jul 01 00:00:00 EDT 2019

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@article{osti_1888759,

  title        = {Hawaii Play Fairway: Preliminary Core Box Photos, Lanai Island, Hawaii},

  author       = {Lautze, Nicole and Thomas, Donald and Haskins, Eric},

  abstractNote = {Photos of core samples from Lanai Island. During the third phase of the Hawaii Play Fairway project, further exploration involved drilling a groundwater well in Lanai's Palawai Basin and performing more geophysical surveys. The project deepened an existing water well on Lanai. Drilling occurred 24/7 the entire month of June 2019 over which time Lanai Well 10 was deepened from 427 m to 1057 m, with continuous core collected. The roughly linear temperature gradient was an average of 42 degC/km, and a maximum bottom hole temperature, 66 degC. This gradient is more than twice the background for Hawaii and within a range of gradients measured in this depth range for some exploration wells within KERZ. The Hawaii Play Fairway project seeks to explore the geologic structures that exist in the caldera region of Hawaiian volcanoes; how those structures influence groundwater storage and flow; and how the magmatic heat from Hawaiian shield volcanoes cools over time. The Hawaii Groundwater and Geothermal Resources Center (Hawaii Institute of Geophysics and Planetology, University of Hawaii at Manoa) executed the Hawaii Play Fairway project. For more information, go to HGGRC's website that is linked in the resources.},

  doi          = {10.15121/1888759},

  journal      = {},

  number       = ,

  volume       = ,

  place        = {United States},

  year         = {Mon Jul 01 00:00:00 EDT 2019},

  month        = {Mon Jul 01 00:00:00 EDT 2019}

}

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DOI: https://doi.org/10.15121/1888759

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