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Earthquakes shaking up New Zealand’s water systems - 16/03/2017

Recently published research from GNS Science and Victoria University of Wellington has provided a unique insight into the hydrological effects of earthquakes in New Zealand.

Cromwell Gorge and Lake Dunstan - Aerial view of the Clyde Dam and Lake Dunstan in the Cromwell Gorge, where landslides on the slopes above the lake are engineered for safety.  A dense monitoring network is sensitive to groundwater changes caused by low levels of shaking from earthquakes hundreds of kilometres away. Photo – Lloyd Homer, GNS Science

Cromwell Gorge and Lake Dunstan - Aerial view of the Clyde Dam and Lake Dunstan in the Cromwell Gorge, where landslides on the slopes above the lake are engineered for safety. A dense monitoring network is sensitive to groundwater changes caused by low levels of shaking from earthquakes hundreds of kilometres away. Photo – Lloyd Homer, GNS Science

Led by GNS Science marine geoscience technician Grant O’Brien, the research highlights the impact earthquakes can have on groundwater systems hundreds of kilometres away.

It was based in the Cromwell Gorge in Central Otago and made use of a large amount of hydrological data that has recorded groundwater responses to a series of earthquakes that have occurred in the region over the past few decades.

This is the first time that the landslide monitoring data, provided by Contact Energy Clyde Dam, has been analysed to determine the effects of earthquake shaking on sensitive groundwater systems. 

“The data set used in this study is of rare international size and scope and as far as we can tell is unique in spanning multiple sites and multiple earthquakes over such a long period of time (23 years),” says Mr O’Brien.

“This means we have been able to construct a detailed picture of the behaviour of different groundwater systems in response to earthquakes, ongoing engineering activities and other factors such as intense rainfall.”

The study was supervised by Dr Simon Cox of GNS Science and Professor John Townend from Victoria’s School of Geography, Environment and Earth Sciences, and funded by the Earthquake Commission and the Marsden Fund which is managed by the Royal Society of New Zealand.

Published in the Journal of Geophysical Research, the study shows the sensitivity of groundwater systems to seismic waves at distances well beyond areas of obvious shaking and surface ground damage.

“Our research showed that groundwater systems within seven large landslides in the Cromwell Gorge are surprisingly susceptible to seismic shaking, with the pressures and flow rates responding systematically to large earthquakes at distances of several hundred kilometres,” says Mr O’Brien.

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The different ways groundwater systems respond to the type of earthquake shaking we have observed is critical to understanding how landslides evolve in both the short and long term.

Grant O'brien

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Differences in the type of earthquake shaking—in particular, the duration, amount and frequency of shaking—result in different groundwater responses. The Cromwell Gorge data show that these changes are triggered by stresses associated with the passage of the seismic waves from the earthquake.

“We found that long-duration earthquakes producing seismic waves with a broad range frequencies cause larger groundwater responses that die away more quickly than those produced by short, sharp earthquakes.”

While scientists have yet to examine the effect of the 2016 magnitude 7.8 Kaikoura earthquake on the groundwater systems at Cromwell Gorge, Mr O’Brien expects the monitoring equipment will have recorded a response.

This finding highlights how components of New Zealand’s engineering infrastructure that are dependent on groundwater, such as dams or irrigation schemes, are affected by earthquakes happening in other parts of the country. 

“Although the groundwater changes did not affect the motion of Cromwell Gorge landslides, which are engineered to stop movement, the monitoring by Contact Energy provides an incredible record for application elsewhere.

“The different ways groundwater systems respond to the type of earthquake shaking we have observed is critical to understanding how landslides evolve in both the short and long term.”

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