Porewater Geochemical Assessment of Seismic Indications for Gas Hydrate Presence and Absence: Mahia Slope, East of New Zealand’s North Island

We compare sediment vertical methane flux off the Mahia Peninsula, on the Hikurangi Margin, east of New Zealand’s North Island, with a combination of geochemical, multichannel seismic and sub-bottom profiler data. Stable carbon isotope data provided an overview of methane contributions to shallow se...

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Main Authors: Richard B. Coffin, Gareth Crutchley, Ingo Pecher, Brandon Yoza, Thomas J. Boyd, Joshu Mountjoy
Format: Article
Language:English
Published: MDPI AG 2022-02-01
Series:Energies
Subjects:
Online Access:https://www.mdpi.com/1996-1073/15/3/1233
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author Richard B. Coffin
Gareth Crutchley
Ingo Pecher
Brandon Yoza
Thomas J. Boyd
Joshu Mountjoy
author_facet Richard B. Coffin
Gareth Crutchley
Ingo Pecher
Brandon Yoza
Thomas J. Boyd
Joshu Mountjoy
author_sort Richard B. Coffin
collection DOAJ
description We compare sediment vertical methane flux off the Mahia Peninsula, on the Hikurangi Margin, east of New Zealand’s North Island, with a combination of geochemical, multichannel seismic and sub-bottom profiler data. Stable carbon isotope data provided an overview of methane contributions to shallow sediment carbon pools. Methane varied considerably in concentration and vertical flux across stations in close proximities. At two Mahia transects, methane profiles correlated well with integrated seismic and TOPAS data for predicting vertical methane migration rates from deep to shallow sediment. However, at our “control site”, where no seismic blanking or indications of vertical gas migration were observed, geochemical data were similar to the two Mahia transect lines. This apparent mismatch between seismic and geochemistry data suggests a potential to underestimate gas hydrate volumes based on standard seismic data interpretations. To accurately assess global gas hydrate deposits, multiple approaches for initial assessment, e.g., seismic data interpretation, heatflow profiling and controlled-source electromagnetics, should be compared to geochemical sediment and porewater profiles. A more thorough data matrix will provide better accuracy in gas hydrate volume for modeling climate change and potential available energy content.
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spelling doaj.art-abb7a024297c4fc1a16d3ad08486c17b2023-11-23T16:27:29ZengMDPI AGEnergies1996-10732022-02-01153123310.3390/en15031233Porewater Geochemical Assessment of Seismic Indications for Gas Hydrate Presence and Absence: Mahia Slope, East of New Zealand’s North IslandRichard B. Coffin0Gareth Crutchley1Ingo Pecher2Brandon Yoza3Thomas J. Boyd4Joshu Mountjoy5Department of Physical and Environmental Science, Texas A&M University—Corpus Christi, Corpus Christi, TX 78412, USAGEOMAR Helmholtz Centre for Ocean Research Kiel, 24103 Kiel, GermanyDepartment of Physical and Environmental Science, Texas A&M University—Corpus Christi, Corpus Christi, TX 78412, USAHawai’i Natural Energy Institute, University of Hawai‘i at Mānoa, Honolulu, HI 96822, USAUS Naval Research Laboratory, Code 6181, 4555 Overlook Ave., SW, Washington, DC 20001, USANational Institute of Water and Atmosphere, Wellington 5012, New ZealandWe compare sediment vertical methane flux off the Mahia Peninsula, on the Hikurangi Margin, east of New Zealand’s North Island, with a combination of geochemical, multichannel seismic and sub-bottom profiler data. Stable carbon isotope data provided an overview of methane contributions to shallow sediment carbon pools. Methane varied considerably in concentration and vertical flux across stations in close proximities. At two Mahia transects, methane profiles correlated well with integrated seismic and TOPAS data for predicting vertical methane migration rates from deep to shallow sediment. However, at our “control site”, where no seismic blanking or indications of vertical gas migration were observed, geochemical data were similar to the two Mahia transect lines. This apparent mismatch between seismic and geochemistry data suggests a potential to underestimate gas hydrate volumes based on standard seismic data interpretations. To accurately assess global gas hydrate deposits, multiple approaches for initial assessment, e.g., seismic data interpretation, heatflow profiling and controlled-source electromagnetics, should be compared to geochemical sediment and porewater profiles. A more thorough data matrix will provide better accuracy in gas hydrate volume for modeling climate change and potential available energy content.https://www.mdpi.com/1996-1073/15/3/1233seismic datasub-bottom profiler datamethanevertical migrationcarbon isotope analysis
spellingShingle Richard B. Coffin
Gareth Crutchley
Ingo Pecher
Brandon Yoza
Thomas J. Boyd
Joshu Mountjoy
Porewater Geochemical Assessment of Seismic Indications for Gas Hydrate Presence and Absence: Mahia Slope, East of New Zealand’s North Island
Energies
seismic data
sub-bottom profiler data
methane
vertical migration
carbon isotope analysis
title Porewater Geochemical Assessment of Seismic Indications for Gas Hydrate Presence and Absence: Mahia Slope, East of New Zealand’s North Island
title_full Porewater Geochemical Assessment of Seismic Indications for Gas Hydrate Presence and Absence: Mahia Slope, East of New Zealand’s North Island
title_fullStr Porewater Geochemical Assessment of Seismic Indications for Gas Hydrate Presence and Absence: Mahia Slope, East of New Zealand’s North Island
title_full_unstemmed Porewater Geochemical Assessment of Seismic Indications for Gas Hydrate Presence and Absence: Mahia Slope, East of New Zealand’s North Island
title_short Porewater Geochemical Assessment of Seismic Indications for Gas Hydrate Presence and Absence: Mahia Slope, East of New Zealand’s North Island
title_sort porewater geochemical assessment of seismic indications for gas hydrate presence and absence mahia slope east of new zealand s north island
topic seismic data
sub-bottom profiler data
methane
vertical migration
carbon isotope analysis
url https://www.mdpi.com/1996-1073/15/3/1233
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