Groundwater – meltwater coupling in an active proglacial sandur aquifer in southeast Iceland

Brighid Ó Dochartaigh, Alan MacDonald, Paul Wilson, Andrew Black, Jez Everest

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Abstract

The sandur proglacial to Virkisjokull, a rapidly retreating glacier in southeast Iceland, forms a thick (at least 50-100m), high permeability, high storage aquifer that is actively coupled with the meltwater river. The sandur aquifer has been characterised by a combination of piezometer drilling, permeability testing and geophysics, and groundwater-meltwater coupling has been investigated by regular monitoring of hydrochemistry, stable isotopes and dissolved gases and by continuous monitoring of groundwater levels and river stage over two years. The study has demonstrated that active rainfall recharge occurs across the sparsely vegetated sandur, and there is significant river influence on groundwater within at least 50-150m of the river channel, particularly proximal to the glacier. In this zone the river loses to the sandur aquifer throughout most of the year, with high meltwater river flows maintaining high groundwater levels in summer. At~300-400m distance from the river, there is no significant river influence on groundwater: here, groundwater recharge and levels are controlled by the timing and volume of precipitation; groundwater level fluctuations are larger than in the zone near the river; and summer groundwater levels are lower than winter levels. There is significant down-gradient groundwater flow in the sandur aquifer, and from ~3km down-gradient from the upper edge of the sandur there is extensive groundwater discharge via springs that provides baseflow to the river throughout much of the year. This study highlights the important role that groundwater storage will play in regulating meltwater river flows as glaciers retreat globally.
Original languageEnglish
Title of host publication International Symposium on Hydrology of Glaciers and Ice Sheets
Publication statusPublished - 25 Nov 2015
EventInternational Symposium on Hydrology of Glaciers and Ice Sheets - Hotel Vatnajökull at Lindarbakki, Höfn in Hornafjörður, Iceland
Duration: 21 Jun 201526 Jun 2015
http://en.vedur.is/conferences/igs-2015

Conference

ConferenceInternational Symposium on Hydrology of Glaciers and Ice Sheets
CountryIceland
CityHöfn in Hornafjörður
Period21/06/1526/06/15
Internet address

Fingerprint

meltwater
aquifer
groundwater
river
river flow
recharge
glacier
permeability
glacier retreat
dissolved gas
hydrochemistry
piezometer
summer
monitoring
baseflow
river channel
geophysics
groundwater flow
stable isotope
drilling

Keywords

  • GroundwaterBGS
  • Groundwater
  • Groundwater monitoring
  • Catchment processes
  • Surface water interation

Cite this

Ó Dochartaigh, B., MacDonald, A., Wilson, P., Black, A., & Everest, J. (2015). Groundwater – meltwater coupling in an active proglacial sandur aquifer in southeast Iceland. In International Symposium on Hydrology of Glaciers and Ice Sheets
Ó Dochartaigh, Brighid ; MacDonald, Alan ; Wilson, Paul ; Black, Andrew ; Everest, Jez. / Groundwater – meltwater coupling in an active proglacial sandur aquifer in southeast Iceland. International Symposium on Hydrology of Glaciers and Ice Sheets. 2015.
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abstract = "The sandur proglacial to Virkisjokull, a rapidly retreating glacier in southeast Iceland, forms a thick (at least 50-100m), high permeability, high storage aquifer that is actively coupled with the meltwater river. The sandur aquifer has been characterised by a combination of piezometer drilling, permeability testing and geophysics, and groundwater-meltwater coupling has been investigated by regular monitoring of hydrochemistry, stable isotopes and dissolved gases and by continuous monitoring of groundwater levels and river stage over two years. The study has demonstrated that active rainfall recharge occurs across the sparsely vegetated sandur, and there is significant river influence on groundwater within at least 50-150m of the river channel, particularly proximal to the glacier. In this zone the river loses to the sandur aquifer throughout most of the year, with high meltwater river flows maintaining high groundwater levels in summer. At~300-400m distance from the river, there is no significant river influence on groundwater: here, groundwater recharge and levels are controlled by the timing and volume of precipitation; groundwater level fluctuations are larger than in the zone near the river; and summer groundwater levels are lower than winter levels. There is significant down-gradient groundwater flow in the sandur aquifer, and from ~3km down-gradient from the upper edge of the sandur there is extensive groundwater discharge via springs that provides baseflow to the river throughout much of the year. This study highlights the important role that groundwater storage will play in regulating meltwater river flows as glaciers retreat globally.",
keywords = "GroundwaterBGS , Groundwater, Groundwater monitoring, Catchment processes, Surface water interation",
author = "{{\'O} Dochartaigh}, Brighid and Alan MacDonald and Paul Wilson and Andrew Black and Jez Everest",
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Ó Dochartaigh, B, MacDonald, A, Wilson, P, Black, A & Everest, J 2015, Groundwater – meltwater coupling in an active proglacial sandur aquifer in southeast Iceland. in International Symposium on Hydrology of Glaciers and Ice Sheets. International Symposium on Hydrology of Glaciers and Ice Sheets, Höfn in Hornafjörður, Iceland, 21/06/15.

Groundwater – meltwater coupling in an active proglacial sandur aquifer in southeast Iceland. / Ó Dochartaigh, Brighid ; MacDonald, Alan; Wilson, Paul; Black, Andrew; Everest, Jez.

International Symposium on Hydrology of Glaciers and Ice Sheets. 2015.

Research output: Chapter in Book/Report/Conference proceedingConference contribution

TY - GEN

T1 - Groundwater – meltwater coupling in an active proglacial sandur aquifer in southeast Iceland

AU - Ó Dochartaigh, Brighid

AU - MacDonald, Alan

AU - Wilson, Paul

AU - Black, Andrew

AU - Everest, Jez

PY - 2015/11/25

Y1 - 2015/11/25

N2 - The sandur proglacial to Virkisjokull, a rapidly retreating glacier in southeast Iceland, forms a thick (at least 50-100m), high permeability, high storage aquifer that is actively coupled with the meltwater river. The sandur aquifer has been characterised by a combination of piezometer drilling, permeability testing and geophysics, and groundwater-meltwater coupling has been investigated by regular monitoring of hydrochemistry, stable isotopes and dissolved gases and by continuous monitoring of groundwater levels and river stage over two years. The study has demonstrated that active rainfall recharge occurs across the sparsely vegetated sandur, and there is significant river influence on groundwater within at least 50-150m of the river channel, particularly proximal to the glacier. In this zone the river loses to the sandur aquifer throughout most of the year, with high meltwater river flows maintaining high groundwater levels in summer. At~300-400m distance from the river, there is no significant river influence on groundwater: here, groundwater recharge and levels are controlled by the timing and volume of precipitation; groundwater level fluctuations are larger than in the zone near the river; and summer groundwater levels are lower than winter levels. There is significant down-gradient groundwater flow in the sandur aquifer, and from ~3km down-gradient from the upper edge of the sandur there is extensive groundwater discharge via springs that provides baseflow to the river throughout much of the year. This study highlights the important role that groundwater storage will play in regulating meltwater river flows as glaciers retreat globally.

AB - The sandur proglacial to Virkisjokull, a rapidly retreating glacier in southeast Iceland, forms a thick (at least 50-100m), high permeability, high storage aquifer that is actively coupled with the meltwater river. The sandur aquifer has been characterised by a combination of piezometer drilling, permeability testing and geophysics, and groundwater-meltwater coupling has been investigated by regular monitoring of hydrochemistry, stable isotopes and dissolved gases and by continuous monitoring of groundwater levels and river stage over two years. The study has demonstrated that active rainfall recharge occurs across the sparsely vegetated sandur, and there is significant river influence on groundwater within at least 50-150m of the river channel, particularly proximal to the glacier. In this zone the river loses to the sandur aquifer throughout most of the year, with high meltwater river flows maintaining high groundwater levels in summer. At~300-400m distance from the river, there is no significant river influence on groundwater: here, groundwater recharge and levels are controlled by the timing and volume of precipitation; groundwater level fluctuations are larger than in the zone near the river; and summer groundwater levels are lower than winter levels. There is significant down-gradient groundwater flow in the sandur aquifer, and from ~3km down-gradient from the upper edge of the sandur there is extensive groundwater discharge via springs that provides baseflow to the river throughout much of the year. This study highlights the important role that groundwater storage will play in regulating meltwater river flows as glaciers retreat globally.

KW - GroundwaterBGS

KW - Groundwater

KW - Groundwater monitoring

KW - Catchment processes

KW - Surface water interation

UR - http://nora.nerc.ac.uk/id/eprint/512297

M3 - Conference contribution

BT - International Symposium on Hydrology of Glaciers and Ice Sheets

ER -

Ó Dochartaigh B, MacDonald A, Wilson P, Black A, Everest J. Groundwater – meltwater coupling in an active proglacial sandur aquifer in southeast Iceland. In International Symposium on Hydrology of Glaciers and Ice Sheets. 2015