Abstract:Heterogeneous glacial sediments, such as clayey till, dominate large parts of the near-surface geology of the Northern Hemisphere (Houmark-Nielsen, 2010). Sand layers and lenses control water and contaminant flow pathways in the otherwise low-permeable clay matrix. Delineation and characterization of these sand structures and bodies are necessary to determine the timing, the amount and the quality of the water percolating through these sediments (e.g., Gravesen et al., 2014).A method for mapping these sand occ… Show more
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