Abstract
A two-dimensional array of electrical conductivity measurements (ECM) has been used to image the acidity of the Siple Dome (Antarctica) ice core in a vertical plane. Annual layering and possible stratigraphic discontinuities are apparent. A brief disruption to the chemical stratigyraphy is detected at 680 m. Below 800 m, weaker layering occurs and is interpreted as the result of post-depositional migration of chemical species. This technique provides a way to observe the horizontal continuity of chemical layers in an ice core and identify some types of flow irregularity.
Cite
CITATION STYLE
Taylor, K. C., & Alley, R. B. (2004). Two-dimensional electrical stratigraphy of the Siple Dome (Antarctica) ice core. Journal of Glaciology, 50(169), 231–235. https://doi.org/10.3189/172756504781830033
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