Dielectric stratigraphy of ice: A new technique for determining total ionic concentrations in polar ice cores

A 133 m deep Antarctic ice core from Dolleman Island, Antarctic Peninsula, has been profiled by dielectric measurements in the AF‐LF (20 Hz ‐ 100 kHz) frequency range. This has revealed large variations in dielectric relaxation and conductivity down the core. A comparison with the chemical stratigra...

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Veröffentlicht in:Geophysical research letters 1989-10, Vol.16 (10), p.1177-1180
Hauptverfasser: Moore, J. C., Mulvaney, R., Paren, J. G.
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creator Moore, J. C.
Mulvaney, R.
Paren, J. G.
description A 133 m deep Antarctic ice core from Dolleman Island, Antarctic Peninsula, has been profiled by dielectric measurements in the AF‐LF (20 Hz ‐ 100 kHz) frequency range. This has revealed large variations in dielectric relaxation and conductivity down the core. A comparison with the chemical stratigraphy along 45 m of the core demonstrates for the first time the decisive role played by acids and salts in determining the electrical behaviour of natural ice. The total ionic concentration along the ice core can be deduced from the dielectric response. This technique may be applied rapidly in the field and, as it requires no contact between ice core and electrodes, the core is maintained in pristine condition for later chemical analysis.
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ispartof Geophysical research letters, 1989-10, Vol.16 (10), p.1177-1180
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1944-8007
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source Wiley Online Library All Journals
subjects 540320 - Environment, Aquatic- Chemicals Monitoring & Transport- (1990-)
Antarctic Peninsula
ANTARCTIC REGIONS
ANTARCTICA
Chemical analysis
Contact
DEPTH
DIELECTRIC PROPERTIES
Dielectrics
DIMENSIONS
DRILL CORES
ELECTRIC CONDUCTIVITY
ELECTRICAL PROPERTIES
Electrodes
ENVIRONMENTAL SCIENCES
GEOLOGY
HYDROGEN COMPOUNDS
ICE
INORGANIC ACIDS
IONIC CONDUCTIVITY
Islands
Marine
MEASURING METHODS
PHYSICAL PROPERTIES
POLAR REGIONS
Resistivity
SALTS
STRATIGRAPHY
VARIATIONS
title Dielectric stratigraphy of ice: A new technique for determining total ionic concentrations in polar ice cores
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