Remote Detection of Saline Intrusion in a Coastal Aquifer Using Borehole Measurements of Self-Potential

D. J. MacAllister (Corresponding Author), M.D. Jackson, A.P. Butler, J. Vinogradov

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Abstract

Two years of SP measurements were made in a monitoring borehole in the coastal UK Chalk aquifer. The borehole SP data showed a persistent gradient with depth, and temporal variations with a tidal power spectrum consistent with ocean tides. No gradient with depth was observed at a second coastal monitoring borehole c.1 km further inland, and no gradient or tidal power spectrum were observed at an inland site c.80 km from the coast. Numerical modeling suggests that the SP gradient recorded in the coastal monitoring borehole is dominated by the exclusion-diffusion potential, which arises from the concentration gradient across a saline front in close proximity to, but not intersecting, the base of the borehole. No such saline front is present at the two other monitoring sites. Modeling further suggests that the ocean tidal SP response in the borehole, measured prior to breakthrough of saline water, is dominated by the exclusion-diffusion potential across the saline front, and that the SP fluctuations are due to the tidal movement of the remote front. The electrokinetic potential, caused by changes in hydraulic head across the tide, is one order of magnitude too small to explain the observed SP data. The results suggest that in coastal aquifers, the exclusion-diffusion potential plays a dominant role in borehole SP when a saline front is nearby. The SP gradient with depth indicates the close proximity of the saline front to the borehole and changes in SP at the borehole reflect changes in the location of the saline front. Thus, SP monitoring can be used to facilitate more proactive management of abstraction and saline intrusion in coastal aquifers.
Original languageEnglish
Pages (from-to)1669-1687
Number of pages19
JournalWater Resources Research
Volume54
Issue number3
Early online date10 Mar 2018
DOIs
Publication statusPublished - Mar 2018

Fingerprint

self potential
saline intrusion
coastal aquifer
borehole
tidal power
monitoring
detection
ocean tide
hydraulic head
chalk
modeling
tide
temporal variation
aquifer

Keywords

  • self-potential
  • seawater intrusion
  • coastal aquifers
  • exclusion-diffusion potential
  • electrokinetic potential
  • hydrogeophysics

Cite this

Remote Detection of Saline Intrusion in a Coastal Aquifer Using Borehole Measurements of Self-Potential. / MacAllister, D. J. (Corresponding Author); Jackson, M.D.; Butler, A.P. ; Vinogradov, J.

In: Water Resources Research, Vol. 54, No. 3, 03.2018, p. 1669-1687.

Research output: Contribution to journalArticle

MacAllister, D. J. ; Jackson, M.D. ; Butler, A.P. ; Vinogradov, J. / Remote Detection of Saline Intrusion in a Coastal Aquifer Using Borehole Measurements of Self-Potential. In: Water Resources Research. 2018 ; Vol. 54, No. 3. pp. 1669-1687.
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AB - Two years of SP measurements were made in a monitoring borehole in the coastal UK Chalk aquifer. The borehole SP data showed a persistent gradient with depth, and temporal variations with a tidal power spectrum consistent with ocean tides. No gradient with depth was observed at a second coastal monitoring borehole c.1 km further inland, and no gradient or tidal power spectrum were observed at an inland site c.80 km from the coast. Numerical modeling suggests that the SP gradient recorded in the coastal monitoring borehole is dominated by the exclusion-diffusion potential, which arises from the concentration gradient across a saline front in close proximity to, but not intersecting, the base of the borehole. No such saline front is present at the two other monitoring sites. Modeling further suggests that the ocean tidal SP response in the borehole, measured prior to breakthrough of saline water, is dominated by the exclusion-diffusion potential across the saline front, and that the SP fluctuations are due to the tidal movement of the remote front. The electrokinetic potential, caused by changes in hydraulic head across the tide, is one order of magnitude too small to explain the observed SP data. The results suggest that in coastal aquifers, the exclusion-diffusion potential plays a dominant role in borehole SP when a saline front is nearby. The SP gradient with depth indicates the close proximity of the saline front to the borehole and changes in SP at the borehole reflect changes in the location of the saline front. Thus, SP monitoring can be used to facilitate more proactive management of abstraction and saline intrusion in coastal aquifers.

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