dc.description.abstract |
Landslide activity is widespread in the Gisborne region of New Zealand’s North Island,
and several investigations have occurred in recent years focused on the spatial pattern
of landsliding, along with triggering factors. High-intensity rainfall, earthquakes, and
land use change (e.g., slope cutting, deforestation) are all triggering factors, with the
weak soils and sedimentary rocks of the region particularly susceptible to slope failure.
Across the region, recent rainfall events in November 2021 and early 2022 have shown
that there is a requirement for slope stability investigations in particularly vulnerable
areas. Such investigations require evaluation of in-situ soil and rock material properties,
and an understanding of process-mechanics of failure and the rate of deformation, to
mitigate future failure at the sites. The focus here is the Kopua coastal landslide at
Wharerata, 21 km southwest of Gisborne. This is a landslide ‘complex’, which was
triggered by rainfall, is ongoing, and is approximately 0.5 km long from the headscarp
to the toe, which is in the ocean. Sediment from cutting of the toe by wave action is
disturbing marine life and shellfish (kai moana) for the local iwi. The methods
employed here include (1) in-situ testing of materials; (2) unpiloted aerial vehicle
(UAVs) surveys for engineering geological mapping and digital elevation model (DEM)
differencing; and (3) laboratory testing of soil index properties and mineralogy. The
landslide can be categorized as a clay/silt rotational coastal landslide caused by
combined effects of drying-fissuring-wetting failure continuum. Recommendations for
mitigation include physical engineering measures such as retaining walls, revetments,
slope coverings and bio-engineering techniques like branch packing and vegetated
gabion walls. Monitoring using global positioning system (GPS), tiltmeters and
extensometers (ExT), inclinometers, shape acceleration arrays (SAA), Acoustic
Emission (AE), piezometers as well as regular UAV surveys would be appropriate. |
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