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Gain–phase characteristics of groundwater responses to barometric pressure: interpreting subsurface confinement in layered systems

Qin, Zixuan, Guo, Jian, Cleall, Peter J. ORCID: https://orcid.org/0000-0002-4005-5319, Xu, Qiang, Cherry, John A. and Parker, Beth L. 2026. Gain–phase characteristics of groundwater responses to barometric pressure: interpreting subsurface confinement in layered systems. Journal of Hydrology 671 , 135296. 10.1016/j.jhydrol.2026.135296

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Abstract

Aquifer confinement plays a key role in controlling vertical hydraulic connectivity and pressure transmission, yet its identification in heterogeneous systems remains challenging using conventional methods. This study applies frequency-domain barometric response functions (BRF) to analyze groundwater response to atmospheric pressure. A six-port Continuous Multichannel Tubing (CMT) system was installed in a layered aquifer. Long-term groundwater, barometric pressure, and precipitation data were analyzed using cross-correlation, FFT, and BRF methods. Time- and frequency-domain analyses reveal pronounced lithology-controlled differences. Ports screened in sandstone units exhibited stronger barometric signals and shorter response lags, while mudstone-adjacent ports showed attenuated responses. Detailed BRF analysis was performed on two representative ports: Port 1 (upper sandstone above mudstone) and Port 6 (lower sandstone below mudstone). The upper sandstone showed a negative gain-phase co-variation, characteristic of unconfined systems, while the lower sandstone exhibited a positive gain-phase relationship, suggesting functional confinement. These findings highlight the utility of BRF analysis for interpreting pressure transmission and confinement in vertically heterogeneous aquifers.

Item Type: Article
Date Type: Publication
Status: Published
Schools: Schools > Engineering
Additional Information: RRS policy applied
Publisher: Elsevier
ISSN: 0022-1694
Date of First Compliant Deposit: 23 March 2026
Date of Acceptance: 9 March 2026
Last Modified: 23 Mar 2026 10:00
URI: https://orca.cardiff.ac.uk/id/eprint/185788

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