Early Careers Hydrogeologists’ Network – Past Meetings
15 February 2023 ECHN Event – Christchurch
The ECHN held its second meeting at Tonkin + Taylor office, PwC Centre, Level 3/60 Cashel Street, Ōtautahi/Christchurch, 8013.
Two talks were presented at this event by Alice Sai Louie PhD candidate at University of Canterbury and Cameron Jasper Senior Hydrogeologist at Tonkin + Taylor.
“Quantifying losses from braided rivers using active distributed temperature sensing”
Background: Alice is a PhD candidate at the University of Canterbury researching surface water – groundwater interaction in braided rivers. Her research will utilise heat as a tracer using novel Active-Distributed Temperature Sensing (A-DTS) methods, with an aim to gain insight into how groundwater velocity vectors from alluvial river systems vary spatially and temporally. This study is part of an MBIE Endeavour Fund research programme on braided river research.
Presentation: Globally, braided river systems are a major recharge mechanism for alluvial aquifer systems providing a significant contribution to groundwater, yet this process of surface water – groundwater interaction is a gap in hydrological research. River leakage from braided rivers is the main source of groundwater recharge in the Canterbury Plains of New Zealand (Coluccio & Morgan, 2019). This study investigated surface water – groundwater interaction in the Waikirikiri Selwyn River, in the South Island of New Zealand, using Active-Distributed Temperature Sensing (A-DTS) and estimated groundwater recharge to the alluvial aquifer system, as outlined in Banks et al. (2022).
The field study site is within an ephemeral losing reach of the river and contains two active channels. Braided rivers are dynamic, high-energy environments; therefore, the fibre-optic cables were installed beneath the ground to protect this infrastructure from regular flood events. Novel horizontal Directional Drilling was used to construct two, 100 m long drillholes at a depth of 5 m below ground level and perpendicular to the river channel. Additionally, two vertical A-DTS installations were constructed to 30 m depth. The drillholes were completed with a hybrid fibre optic cable containing four multi-mode fibres and copper conductors.
Groundwater velocities were derived using both analytical and numerical solutions and preliminary results indicate groundwater velocities exceeding 10 m/d. By calculating groundwater velocities, it is possible to quantify groundwater recharge from braided rivers which can aid in informing water allocation and management practices.
References:
Banks, E. W., et al. (2022). “Active distributed temperature sensing to assess surface water–groundwater interaction and river loss in braided river systems.” Journal of Hydrology 615: 128667.
Coluccio, K. and L. K. Morgan (2019). “A review of methods for measuring groundwater-surface water exchange in braided rivers.” Hydrology and Earth System Sciences 23: 4397-4417.
“Managed aquifer recharge: conceptual overview and introduction to sites in New Zealand and abroad”
Presenter 2: Cameron Jasper (Tonkin + Taylor)
Background: Cameron is a hydrogeologist with a range of analytical, modelling, geospatial, survey, and monitoring skills. He joined T+T in October 2021 following his experience across the western US and New Zealand. Experienced in siting, design, and assessment of constructed wetland, managed aquifer recharge, and targeted stream augmentation systems.
Presentation: Managed aquifer recharge is a globally utilized technique to revitalize surface and groundwater resources. This approach leverages a variety of methods tailored to fit specific hydrogeological conditions and goals, including aquifer storage and recovery (injection/abstraction bores) and spreading techniques (infiltration ponds).
In the Canterbury region, efforts are underway to reduce nitrate levels in groundwater through recharge projects at various stages. Alongside this, near river recharge and stream/spring augmentation initiatives aim to boost baseflows and enhance the health of groundwater-fed ecosystems. However, the feasibility of implementing recharge sites across irrigation areas is dependent on water availability, regional planning, changes in land usage, and projected groundwater quality.
Infiltration ponds may play a crucial role in enhancing groundwater quality, quantity, and supporting ecosystems, but their effectiveness at the site level can be hindered by shallow groundwater levels, clogging, and the variability of less permeable alluvial deposits. 
Borehole investigations alone can miss the distribution of restrictive deposits, leading to underperforming recharge rates. By using geophysical techniques including resistivity tomography, electromagnetics, self-potential, and temperature sensing, primary infiltration pathways can be used to improve site selection and design. To mitigate the risk of microbial contamination, it is essential to conduct a thorough assessment of source water quality, transport modelling, and monitoring.
October 2022 Event – Christchurch
The inaugural ECHN Technical meeting was held on 22 October 2020 at GHD, 138 Victoria Street, Christchurch. Two speakers presented to a group of approximately 20 Early Career Hydrogeologists. Details of the presentations are summarised below and can be downloaded in the following link.
‘Investigation of groundwater recharge and irrigation efficiency under loess soil’
Presented by Kate Bailue Senior Groundwater Scientist at Environment Canterbury.
Background: Kate has over 15 years experience as a hydrogeologist with a background in groundwater resource management and modelling. Her current role with Environment Canterbury includes conducting groundwater
investigations and providing advice on groundwater quality and quantity for regional planning, resource consents, compliance monitoring and public enquiries. Prior to joining Environment Canterbury, she was a consultant hydrogeologist where she worked on a range of groundwater projects both in New Zealand and in Australia, including 10 years with Rio Tinto in Western Australia.
Presentation: Loess soils cover approximately 5,606 km2 of land in Canterbury, representing 13% of land in the region. Yet, the hydraulic characteristics of loess soils are poorly understood, even though we know they behave very different from those of the stony and well-draining soils which are common on the Canterbury Plains.
The Collaborative Hillslope Project was established in 2018 to improve understanding of the spatial and temporal controls on water movement through loess soil. The project team consisted of team members from Environment Canterbury, NIWA, Plant & Food Research and Lincoln University. A 4.5 ha single hillslope basin (paddock) dominated by loess soils, located near Otaio, South Canterbury was chosen as the primary field site. The hillslope site was heavily instrumented and characterised with climate and rainfall gauges, surface flumes, piezometers, soil auger holes and soil moisture probes to allow us to measure as many of the water balance variables as possible.
‘Arsenic in the groundwater of Waitaha/Canterbury region’
Presented by Andy Pearson Senior Groundwater Scientist at ESR.
Background: Andy has a PhD in geochemical analysis of speleothems (i.e., secondary cave carbonate deposits) for palaeo-environmental reconstruction (University of Waikato). Since completing his studies in 2020, Andy has primarily worked on groundwater quality; firstly, as a Groundwater Scientist for Environment Canterbury, then at the Institute of Environmental Science & Research (ESR).
Presentation: Arsenic contamination in groundwater affects tens of millions of people worldwide and is also
regarded as a major groundwater issue in Aotearoa New Zealand. Yet, region-wide, the occurrence and causes of arsenic presence are relatively understudied in Canterbury, despite groundwater being the primary source of water for irrigation and drinking. This study was conducted to evaluate the connection between elevated groundwater arsenic concentrations and inferred redox state of aquifers across the Canterbury region using Environment Canterbury data. In total, 2,428 samples from 1,172 wells were analysed for arsenic concentrations, and compared against groundwater redox state, which was inferred using geochemical indicators for each well.