Weathering regime and geochemical conditions in a polar desert environment, Haughton impact structure region, Devon Island, Canada

• Published in: Canadian Journal of Earth Sciences
• Main Authors: Lacelle, Denis, Juneau, Véronique, Pellerin, André, Lauriol, Bernard, Clark, Ian D.
• Other Authors: Hillaire-Marcel, Claude
• Format: Article in Journal/Newspaper
• Language: English
• Published: Canadian Science Publishing 2008
• Subjects: General Earth and Planetary Sciences; Nunavut; Canada; Devon Island; Thumb; Allen Bay; Thumb Mountain; permafrost; polar desert
• Online Access: http://dx.doi.org/10.1139/e08-063; http://www.nrcresearchpress.com/doi/full-xml/10.1139/E08-063; http://www.nrcresearchpress.com/doi/pdf/10.1139/E08-063

This study examines the physical and geochemical properties of near-surface sediments, as well as the geochemical and stable O–H–C isotope composition of (ground)surface waters in and around the Haughton impact structure region (Devon Island, Nunavut) to determine the types of weathering (mechanical, (bio)chemical) and their relative contribution in this polar desert environment. The surface sediments collected from the Allen Bay and Thumb Mountain formations surrounding the impact crater are dominated by sand-sized particles; whereas the impact melt breccias inside the crater have a greater abundance of silt-sized particles. The subsurface sediments in the Allen Bay formation show a near equal amount of sand- and silt-sized particles. However, the micromorphologies of the sand-sized particles collected at the surface revealed that these grains, irrespective of the local geology, were heavily fractured. By contrast, fractures and rounded pits are observed on the surface of the sand grains located within the active layer; whereas those located just above the permafrost table have only rounded cavities on their surface. The (ground)waters also show variations in their solute concentration with depth; the highest concentrations being found in the groundwaters near the top of permafrost. Taken together, these observations suggest that there is a progressive evolution from a mechanically dominated weathering regime near the surface, to increasing chemical weathering with depth. The transition from mechanical weathering near the surface to increasing chemical weathering with depth can be attributed to the decreasing frequency and intensity of mechanical weathering processes (i.e., frost action, wetting–drying, thermal dilation) with depth, and to the presence of permafrost, which allows a greater availability of water for chemical aqueous reactions at the base of the active layer.