Hydrology Research (Jan 2023)

Surface-groundwater exchange between a wetland, sandur, and lava field in southeastern Iceland

  • Aiesha Aggarwal,
  • Kathy L. Young

DOI
https://doi.org/10.2166/nh.2022.079
Journal volume & issue
Vol. 54, no. 1
pp. 14 – 30

Abstract

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In May 2019, over 50 springs were identified at a sandur-lava field–wetland complex in Southeast Iceland and a subset was selected for further investigation including monitoring water levels, discharge, and water chemistry. Between May and September 2019, springs at the study site had relatively stable water levels and temperatures (4–5 °C), although heavy rains (>10 mm) corresponded with increased water levels and/or temperatures at some springs. Together, the water level, temperature, and stable isotope data suggest that the springs at the study site are fed by older groundwater from an aquifer that is recharged by precipitation. Spikes in water level indicated that at least one spring at the edge of the sandur also received floodwater and shallow subsurface flows from the glacial-fed Brunná River. One wetland spring was further monitored over the water year (October 2019 to October 2020). Like other springs, water levels and temperatures remained relatively stable, fluctuating with inputs of precipitation. Longer-term studies will be needed to gain an improved understanding of seasonal spring vulnerability to climate change and their role in the functioning of a coastal wetland in Southeast Iceland. HIGHLIGHTS Various springs were identified in a sandur, lava field, and wetland landscape in Southeast Iceland.; Wetland springs had stable water levels and temperatures but water levels in other springs were modified by floodwaters of the glacial Brunná River; Baseline hydrological data (water levels, temperature) are provided for springs that warrant long-term monitoring in light of climate warming.; An illustration showing the proposed mechanism of spring discharge at a coastal wetland, Southeast Iceland. Springs in a wetland bordered by a lava field and a sandur have relatively stable hydrology owing to a continuous supply of groundwater. Some springs receive inputs from runoff from the lava field and wetland and shallow surface flows from the sandur as well.

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