Use of stable isotopes in rainfall and rivers to explain pathways and speed of water movement through catchments
13 June 2018
Stable hydrogen and oxygen isotopes in rainfall and rivers can provide a powerful tool to explain the pathways and speed of water movement through catchments.
As part of NIWA’s National Hydrological Project, NIWA, GNS and Landcare are establishing a surface water/groundwater hydrological model coupled with water age tracer in collaboration with 3 regional councils. This will enable the project team (i.e. CRIs and regional councils) to relate changes in water sources (e.g. old groundwater or younger, quicker overland flow) to rivers through time as a first step to understanding and then simulating changes in water quality.
Rainfall and river water stable isotope time-series data have shown the sources of water used by trees within the upper reaches of the Waipara catchment in North-Canterbury. Invasive streamside willows were found to remove considerable quantities of groundwater and river water—reducing summertime flows by around 50%.
Rainfall isotope collectors at two sites, designed to reduce evaporation from the rainfall sample once collected. [Photo: Bruce Dudley, NIWA]
Marttila, H., Dudley, B. D., Graham, S., Srinivasan, M.S. 2018. Does transpiration from invasive stream side willows dominate low flow conditions? An investigation using hydrometric and isotopic methods in a headwater catchment. In press - Ecohydrology. DOI: 10.1002/eco.1930
Dudley, B. D., Marttila, H., Graham, S., Evison, R., Srinivasan, M.S. 2018. Water sources for woody shrubs on hillslopes: An investigation using isotopic and sapflow methods. In press - Ecohydrology. DOI: 10.1002/eco.1926