1887

Abstract

Summary

Offshore groundwater systems have been suggested as alternative sources of potable water in islands and coastal regions. In this study, we integrate offshore controlled-source electromagnetic (CSEM) with borehole data to identify an offshore groundwater system in the Canterbury Bight, New Zealand. CSEM data were acquired with a seafloor-towed system along four profiles and 2-D inversion was carried out using MARE2DEM to derive resistivity models along each profile. Moreover, a trans-dimensional Bayesian inversion was conducted to assess the distribution of plausible resistivity-depth models. The study area was previously investigated during IODP Expedition 317 in which a pore-fluid salinity anomaly (24 psu at 40 mbsf) was recorded in borehole U1353. A comparison between the CSEM resistivity model and the resistivity-depth profile converted from pore-water salinity within the borehole shows a strong correlation between CSEM and borehole data at the closest waypoint to site U1353. We show through a Markov-Chain Monte Carlo approach that our estimates of seafloor resistivity agree with the measured borehole data. The computed resistivity distributions at the borehole provide significant evidence that the CSEM inversion models can be used to extrapolate groundwater inferences from the borehole onto a basin scale providing improved geophysical imaging capabilities for offshore freshened groundwater.

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/content/papers/10.3997/2214-4609.202211048
2022-06-06
2024-04-29
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References

  1. Archie, G.E., 1942. The electrical resistivity log as an aid in determining some reservoir characteristics.Journal of Petroleum Technology, 5, 1–8.
    [Google Scholar]
  2. Browne, G.H., Naish, T.R., 2003. Facies development and sequence architecture of a late Quaternary fluvial-marine transition, Canterbury Plains and shelf, New Zealand: implications for forced regressive deposits.Sedimentary Geology, 158, 57–86.
    [Google Scholar]
  3. Fulthorpe, C.S., Hoyanagi, K., Blum, M., Expedition 317 Scientists, 2011. IODP Expedition 317: Exploring the Record of Sea-Level Change off New Zealand. Scientific Drilling, 12, 4–14.
    [Google Scholar]
  4. Gehrmann, R.A.S., Dettmer, J., Schwalenberg, K., Engels, M., Ozmaral, A., Dosso, S.E., 2015. Trans-dimensional Bayesian inversion of controlled-source electromagnetic data in the German North Sea.Geophysical Prospecting, 63, 1314–1333.
    [Google Scholar]
  5. Key, K., 2016. MARE2DEM: a 2-D inversion code for controlled-source electromagnetic and magnetotelluric data, Geophys. J. Int., 207(1), 571–588.
    [Google Scholar]
  6. Lu, H., Fulthorpe, C.S., 2004. Controls on sequence stratigraphy of a middle Miocene–Holocene, current-swept, passive margin: Offshore Canterbury Basin, New Zealand.Geological Society of America Bulletin, 116(11/12), 1345–1366.
    [Google Scholar]
  7. Micallef, A., Person, M., Haroon, A., Weymer, B. A., Jegen, M., Schwalenberg, K. et al., 2020. 3D characterization and quantification of an offshore freshened groundwater system in the Canterbury Bight.Nature Communications, 11, 1372.
    [Google Scholar]
  8. Mountjoy, J., Micallef, A., Jegen, M., Woelz, S., Cunarro Otero, D., Eton, N., Gerring, P., Hart, A., Luebben, N., Mueller, C., Quinn, W., Schwalenberg, K., Spatola, D., Weymer, B., 2017. Voyage Report RV Tangaroa Voyage TAN1703, 5 April – 1 May 2017, NIWA, Wellington, New Zealand.
    [Google Scholar]
  9. Villasenor, T., Jaeger, J.M., Marsaglia, K.M., Browne, G.H., 2015. Evaluation of the relative roles of global versus local sedimentary controls on Middle to Late Pleistocene formation of continental margin strata, Canterbury Basin, New Zealand.Sedimentology, 62, 1118–1148.
    [Google Scholar]
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