Hydrology, Cryosphere & Earth Surface Editors' Highlights

Revealing Complexity of Groundwater Flow with Hydrogeophysics

A combination of passive seismic and electrical measurements are used to unravel the complex hydrogeology structure and associated groundwater flow paths at a coastal site in O’ahu, Hawai`i.

Source: Water Resources Research


There is growing recognition of the value of combining data from multiple geophysical modalities for improved and unambiguous conceptualization of subsurface flow processes. Grobbe et al. [2021] focus on the use of passive seismic and self-potential measurements near the Kaiwi Coast, O’ahu, Hawai`i.

Analysis of ambient seismic noise from an array of surface geophones, permits the development of a 3D shear wave velocity model, and subsequently a conceptualization of lithology. The addition of self-potential measurements then permits an interpretation of flow pathways within the complex geological setting.

The authors reveal evidence that subsurface flow focuses along paleo-channels on the erosional surface between the basaltic bedrock and the overlying volcanic and sedimentary formations, at roughly 100 to 200 meters depth. This impressive demonstration is likely to prompt many further coupled applications of these two methods.

Citation: Grobbe, N., Mordret, A., Barde‐Cabusson, S., Ellison, L., Lach, M., Seo, Y.‐H., et al. [2021]. A multi‐hydrogeophysical study of a watershed at Kaiwi Coast (Oʻahu, Hawaiʻi), using seismic ambient noise surface wave tomography and self‐potential data. Water Resources Research, 57, e2020WR029057. https://doi.org/10.1029/2020WR029057

—Andrew Binley, Associate Editor, Water Resources Research

Text © 2021. The authors. CC BY-NC-ND 3.0
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