Effective diffusivity of sulfuric acid in Antarctic ice cores

• Main Authors: Fudge, Tyler J., Sauvage, Raphael, Vu, Linh, Hills, Benjamin H., Severi, Mirko, Waddington, Edwin D.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: article; Verlagsveröffentlichung; Antarctic; The Antarctic; Antarc*; EPICA; ice core; Ice Sheet
• Online Access: https://doi.org/10.5194/egusphere-2022-1219; https://noa.gwlb.de/receive/cop_mods_00063888; https://egusphere.copernicus.org/preprints/egusphere-2022-1219/egusphere-2022-1219.pdf

Volcanic deposition of sulfuric acid in ice cores is important both for understanding past volcanic activity and for synchronizing ice core timescales. Sulfuric acid has a low eutectic point, so it can potentially exist in liquid at grain boundaries and veins, accelerating chemical diffusion. A high effective diffusivity would allow post-depositional diffusion to obscure the climate history and the peak matching among older portions of ice cores. Here, we use records of sulfate from the EPICA Dome C (EDC) ice core to estimate the effective diffusivity of sulfuric acid in ice. We focus on EDC because multiple glacial-interglacial cycles are preserved, allowing analysis for long timescales and deposition in similar climates. We calculate the mean concentration gradient and the width of prominent volcanic events, and analyze the evolution of each with depth/age. We find the effective diffusivities for interglacials and glacial maximums to be 5 ± 2 × 10-9 m2 a-1, an order of magnitude lower than a previous estimate derived from the Holocene portion of EDC (Barnes et al., 2003). The effective diffusivity may be even smaller if artificial diffusion from the sampling is accounted for. Effective diffusivity is not obviously affected by the ice temperature until about -10 °C, 3000 m depth, which is also where anomalous sulfate peaks begin to be observed (Traversi et al., 2009). Low effective diffusivity suggests that sulfuric acid is not readily diffusing in liquid-like veins in the upper portions of the Antarctic ice sheet and that records may be preserved in deep, old ice if the ice temperature remains well below the pressure melting point.