https://nova.newcastle.edu.au/vital/access/ /manager/Index en-au 5 https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:13516 Wed 11 Apr 2018 14:42:09 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:1128 Wed 11 Apr 2018 09:58:59 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:21594 Mon 23 Sep 2019 12:25:24 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:52801 50 m and requires specific storage at constant strain of Sϵ ≥ 10−6 m−1, hydraulic conductivity of the aquitard of kl ≤ 5 ⋅ 10−5 ms−1 and aquifer of ka ≥ 10−4 ms−1. We further illustrate that the analytical solution is valid in unconsolidated systems, whereas consolidated systems require additional consideration of the Biot modulus. Overall, a priori knowledge of the subsurface system supports interpretation of the groundwater response. Our results improve understanding of the effect of Earth tides on groundwater systems and its interpretation for subsurface properties.]]> Fri 27 Oct 2023 14:14:33 AEDT ]]>