ABSTRACT
Within an 18 month period the Tairāwhiti region was hit with 3 heavy rainfall events and 2 cyclones. This resulted in over 5,200 recorded road faults across its 2,238 km network. The extent of the damage at any site ranged from minor culvert blockages to severe forestry scrag deposition, to minor and sizeable under or over slips taking out culverts, road shoulders and active carriageway.
The immediate response and cost effective final repair of the roading network presented significant challenges for such an extensive road network with limited funding. To ensure the best use of available funding for the road repairs the client, Network Operations Contract (NOC) contractor and designer worked collaboratively to assess, design and construct slip remedial measures. The contractor repaired the majority of the sites during the primary and secondary response phases. Around 380 sites (typically under slips) required specific site assessment to determine the most cost effective design solution and collect sufficient ground and topographic data for design. Remedial solutions for these more complex sites included: – upslope retreats; bench and fills; culvert clearance and repairs; MSE walls; and timber or steel pole walls with anchors. We present the significance, approaches, challenges faced and what we have learnt from them.
INTRODUCTION
Imagine your local river rising over 9 metres for several hours, beaches made of forestry logs and wide spread road closures. This was the reality for residents of the Tairāwhiti Region. Between April 2017 & September 2018 the Tairāwhiti (Gisborne) region was exposed to 3 cyclones and 2 heavy rainfall events. This resulted in over 5,000 reported faults across the 2,563 km of road network. The quantum and magnitude of the problem required several sources of funding and several years work to remediate the reported roading faults.
The road faults were initially managed by the NOC contractor (Downer) and, at the time of the most recent event, the Region’s road network was governed by a collaboration between New Zealand Transport Agency (NZTA) and Gisborne District Council (GDC) known as Tairāwhiti Roads. This partnership was dissolved as of 1 August 2019 and the local road network is now solely managed by GDC and the state highways by the NZTA.
The Tairāwhiti (or Tai Rawhiti) region is located on the East Coast of the North Island and is considered one of the most isolated regions in New Zealand (Figure 1). The topography is mountainous with the Raukumara ranges defining the western boundary.
The southern portion of the region is comprised of Tertiary aged interbedded mudstones and sandstones (weak rocks). To the north the geology also includes Allochthonous Cretaceous aged calcareous mudstone, sandstone, limestone and green sand. All the units have been uplifted and deformed by the East Coast Deformation Belt (Figure 2). The region is capped by a veneer of up to 10 m of rhyolitic volcanic ashes. The upper weathered weak rocks and overlying ashes form the soils of the region. Local shallow slope instability has also created areas of colluvium on the steep hillslopes which remain vulnerable to continued shallow instability. In addition to the ground conditions, historic road formation practices (i.e. sidling cut and fill with minimal compaction) have also created areas vulnerable to shallow slope instability. The interface of the fill with natural ground often becomes the shear surface for shallow failures.
Figure The Tairāwhiti Region (outlined in Red)(source google maps)
Figure 2 Regional geology (source Mazengarb and Speden 2000)
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Rainfall Events Compared to Cyclone Bola
Figure 4 below presents a comparison of the significant peak rainfall events between April 2017 and September 2018 that resulted in so much land damage to Tairāwhiti region. Cyclone Debbie (5 April 2017) produced 85 mm of rain over 16 hours and resulted in the initial saturation of the regions soils. On 12 April 2017, Cyclone Cook hit the region with a peak intensity of 80 mm in 3 hours. Whilst this was a relatively small storm its effects were exacerbated by the preceding Cyclone Debbie. In July 2017 (13-16 and 20-24 July 17) two storm events also impacted the region with peak rainfall of 50 and 80 mm respectively (Cave et al 2017).
The 3-4 June 2018 (Queens Birthday storm) produced a total 266 mm in 24 hours. This was a localised event impacting the Uawa and Pakarae catchments. A second event over 11-12 June 2018 produced 224 mm in 24 hours. This was a region wide event and resulted in flooding and land damage exacerbated by the earlier June event. Flood levels stayed above 9 m for 7 hours (GDC 2018). Finally a rain event over 4-9 September 2018 resulted in a peak rainfall of 100 mm.
Figure 3 Peak rainfall in 24 hours in 2017 and 2018 compared to Cyclone Bola
In March 1988 Cyclone Bola struck the East Coast causing widespread damage from land erosion, downstream flooding and landslips. Damage estimates exceeded $220 million (Cave et al 2017). Bola had a devastating effect on the steep areas at river headwaters that were in pasture or young forestry plantations. Land damage in areas with more mature forestry planting was 16 times less than that of pasture and young forestry (Marden and Rowan 1994). McKelvey and Murton (1991) published on 40 landslide damage sites on State Highway 35 in the Tairāwhiti region following Cyclone Bola. Over $15 million was spent to remediate these 40 sites. There is no other data available to understand the quantum of road damage to SH 2 or the local road network.
As a result of Bola the East Coast Forestry Project was initiated in 1992 with the intent of accelerating the rate of land use change to plantation forestry. By 2016 it was estimated that 141,581 ha of land comprised exotic forest (Cave et al 2017). Harvesting of the East Coast Forestry Project has already commenced with an expected peak in harvesting in the next 13 years (Cave et al 2017). We have not had the data for a direct correlation between damage to the road and forestry activity land. However there is anecdotal evidence that areas that have been harvested in the last 5 years have more localised slope failures and road damage. An example is Tauwhareparae Road near Tologa Bay. In recent years, this area has been heavily deforested and it was the hardest hit road in the region as a result of the 2017 and 2018 storm events. The road recorded over 360 faults from the June 2018 rain event alone.
Whilst the 2017 and 2018 rain events were not as significant in terms of rainfall intensity or flooding duration as the 1988 Cyclone Bola event, the impact on the land, the roading network and the economy has been cumulatively just as significant.
Devastation of the road network
The combination of the rainfall events, steep slopes, saturated soils, recent logging of areas and logging debris created a “perfect storm of circumstances” that resulted in over 5,000 recorded faults on the road network.
Figure 4 below indicates the quantum of sites repaired, evaluated and consented.
Figure 4 Summary of remedial actions
Primary and secondary response to these emergencies by the NOC contractor resulted in the majority of the sites being repaired with minimal engineering design input. At the end of secondary response the remaining 381 sites required engineering assessment and action decisions.
The repair of all the sites could not be made with the available funding and some sites were either classified as “do nothing” or “requiring more funding”. All sites were assessed and 182 sites required investigation, design and consenting.
The types of failures on the roading network are summarised below and illustrated in Figure 5 below.
- Over slips – shallow failures of saturated soils on the uphill side of the road
- Under slips – small failures due to scour at culvert outlets
- scour of the downhill side of the road due to blocked culverts and table drain overtopping
- shallow failure due to saturation of sidling fills
- River bank scour generating loss of road carriageway, undermining bridge abutments
- Forestry scrag damage
- Hillside failures due to saturated conditions
Over slip at Waimata Valley Road, Gisborne | Under slip at Armstrong Road, Whatatutu |
Culvert outlet scour at Moutohora Road, Motu | Under slip at Tarndale Road, Whatatutu |
Forestry scrag damage at Paroa Road, Tolaga | Scour due to culvert blockage and storm water runoff at Arakihi Road, Tolaga |
River bank scour at Tapuaeroa Road, Ruatoria | Hillside failure at Waitahaia Road, Te Puia Springs |
Figure 5 Examples of failure types on the Tairāwhiti roading network.
Consultants response approach
From a consultant’s perspective, we were asked to investigate, design and consent 381 sites in 16 months. From commencement of the programme it was important to understand the level of serviceability the client wanted returned to the local roads, the clients risk appetite and budget constraints. In collaboration, we determined that if a site had 1 m of shoulder, functioning drainage, no risk of undercut or continued failure then a “make safe” or “do minimum” option was applied. Otherwise remedial solutions were identified to create stable solutions to replace lost carriageway, establish 1 m of shoulder, add or fix drainage and provide safety features as needed.
The client had a strong desire to make the available funding go as far as possible, thus no or minimal intrusive ground investigation was completed. Except for larger road retreats, topographic survey was restricted to zip line, and laser level surveys to develop cross sections to support ground model development and design. GDC accepted the resultant risk of unforeseen ground conditions, the potential for design outcomes with lower life expectancy and the potential for standing time and design changes during construction, To come to this decision the risks were weighed up against the need to have a functional network. An outcome of this approach is that chosen geotechnical design parameters were deliberately conservative.
Borehole drilling or CPT’s were only undertaken for larger and more expensive remedial solutions such as high retaining walls or where rock could not be located in hand augers. Mobilisation of investigation plant into the remote Tairāwhiti regions is expensive. Drone survey was undertaken for larger road retreats. This was especially important to provide better quality geometrics to assist in understanding if private land was affected and to calculate the areas of land disturbance to support consenting.
As we have shown earlier in this paper, the landscape and the roading network of the Tairāwhiti Region is both challenging and relatively fragile. Historically, it has been impacted by a number of flood and rainfall events and may well be subject to seismic activity in the future. Given the size of the roading network and the limited available funding, the road operators have a realistic expectation around the level of resilience that they expect to achieve. For the flood damage repairs, we collaboratively developed a design philosophy which met the clients higher risk appetite and their desire to agree to variations to the design guidance in the NZTA Bridge Manual (2018) requirements. This preference included a 15 year design life, no or minimal seismic design, and larger accepted deformations. Developing this fundamental understanding of the client requirements and basis for design provided a clear pathway of expectations and next steps for the assessment and design teams.
Assessment teams were sent across the region based on an agreed road priority basis. Roads considered to be key access routes, or to have significant importance to the economy such as logging routes were given higher priority. The dedicated assessment teams comprised a geotechnical engineer or an engineering geologist paired with a civil/roading engineer. They were located in the region for 1 week in every 4. These pairings allowed for a pragmatic and holistic approach to the remedial outcomes such that the failure cause was identified, usually storm water related, and allowed for sufficient geotechnical and topographic sections to be collected to support design. Depending on the complexities of the sites and their location, an assessment team could visit and collect data for up to 35 sites in a week and present a summary of remedial solutions to the client on the last day. These client presentations worked well for the less complex sites. We presented the cause of the failure, a range of likely solutions with likely costs and advantages and disadvantages. In collaboration with the client we agreed a design option for each site before the assessment team demobilised from Gisborne. All parties agreed that this was innovative and cost effective.
For all the sites that required assessment and design, a bespoke design was generated. Some were as simple as drainage works, pavement repairs and minor retreats marked up onto site photos. However, the complex over slips, under slips, river and culvert scours required detailed design solutions.
Typical design solutions for these sites included:-
- Timber or steel pole retaining walls with/without anchors
- Retreats
- Reinforced soil slopes
- Mechanically stabilised earth structures
Other design solutions such as rock buttressing, gabion baskets, mass block walls were consider at the early stages of the works. However, local and regional constraints such as excessive cost of quality rock, limited availability of material suitable for gabions, long lead times for concrete block production, long cartage distances and limited number of capable contractors ruled out a number of these options.
For the complex sites, the one size fits all design approach does not work as there are just too many influencing variables. So specific design was completed for each site. To deliver the volume of work and sites, a dedicated team of 21 completed the design and consenting packages. The deliverables for every site included detailed design drawings, supporting design memo, schedule of quantities suitable for contractor pricing, safety in design register, consent assessment, and in some cases consent application. Examples of the types of construction outcomes are presented below in Figure 6.
Accelerating the design consenting programme, wherever possible, was required to ensure that there was a steady flow of sites available for construction and that the funding cash flow could be properly managed.