Premium
Controls on the long‐term downward transport of δ²H of water in a regionally extensive, two‐layered aquitard system
Author(s) -
Hendry M. J.,
Barbour S. L.,
Zettl J.,
Chostner V.,
Wassenaar L. I.
Publication year - 2011
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2010wr010044
Subject(s) - geology , aquifer , quaternary , hydrogeology , geomorphology , water table , glacial period , infiltration (hvac) , groundwater , geochemistry , hydrology (agriculture) , petrology , paleontology , geotechnical engineering , physics , thermodynamics
Seven high‐resolution (0.3–0.6 m depth intervals), 1‐D vertical profiles of the δ²H of pore water were collected across a 300 km 2 study area in southern Saskatchewan, Canada, to define the vertical controls on solute transport in a >120 m thick, two‐layered aquitard system. The 1‐D profiles were augmented with an existing δ²H profile collected from a previous study. The surficial aquitard in the area consists of Quaternary deposits (either glacial till or lacustrine deposits; 13 to 128 m thick) underlain by an upper Cretaceous claystone aquitard (80–110 m thick). The shape of the individual δ²H profiles and associated 1‐D transport modeling suggest diffusion is the regionally dominant vertical transport mechanism across the aquitards. The profile shape is controlled by the thickness of the Quaternary deposit and the δ²H value at the upper boundary, which coincides with the depth of the water table. The upper boundary δ²H value varies considerably across the area (−149‰ to −101‰), perhaps due to differences in local hydrological conditions (e.g., slope, aspect, infiltration) across the landscape. Modeling of all profiles shows the timing for till deposition and the timing of climate change during the Holocene are consistent across the area (∼30 ka and 7–10 ka before the present, respectively), corroborating other studies. This study provides insights into the hydrogeologic controls on solute transport in an aquitard system and associated geologic and climatic changes for a prairie region over the past 30 ka, and improves our understanding of initial and time‐dependent transport boundary conditions for the study of aquitards.