Articles | Volume 45
https://doi.org/10.5194/adgeo-45-235-2018
https://doi.org/10.5194/adgeo-45-235-2018
30 Aug 2018
 | 30 Aug 2018

Investigation of the influence of earthquakes on the water level in the geothermal reservoir of Waiwera (New Zealand)

Michael Kühn and Tim Schöne

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Latest update: 28 Mar 2024
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Short summary
The water level of the Waiwera geothermal reservoir increased in the hours and days after the Kaikoura earthquake on 14 November 2016. We determined in a continuous time series consisting of monthly means of water level data and pumping rates starting in 1986 if events above a certain strength alter groundwater dynamics at Waiwera. A clear correlation cannot be proven but none of the recorded earthquakes led to such a high energy density in Waiwera as the Kaikoura event did.