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Hydraulic Conductivity: Hydraulic conductivity refers to the ability of the aquifer material to transmit water, which in turn, controls the rate at which ground water will flow under a given gradient. It is related to the size and spacing of particles or groins in soils or to the number and size of fractures in rocks Glacial drift: Unstratified deposits laid down directly beneath the ice or dropped from the surface as the ice melted Soil Texture The distribution of soil particle sizes influences the rate of water movement through the soil Soil Permeability Defined as the rate of water movement through the soil Soil Depth Soil Organic Matter The amount of soil organic matter influences the sorption potential of the soil Soil Slope Can influence the amount of water that will infiltrate into a soil.

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Q: What factors influence the hydraulic conductivity of a glacial drift?
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