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Hydrogeologic Units
learn about diff. types of hydrogeologic units
Question | Answer |
---|---|
Aquifer | geologic unit with significant capacity to store and transmit water • water can be pumped economically from a well • medium to high K |
Aquitard | geologic unit with sufficient capacity to store water, but transmits water slowly • will not supply enough water to a well • low K |
Aquiclude | geologic unit that is essentially impermeable |
Water table | the surface where the pore water pressure is equal to atmospheric pressure (Pw = 0 gauge pressure) • essentially the potentiometric surface for an unconfined aquifer |
Potentiometric surface | an imaginary surface that coincides w/ the level of water everywhere in the aquifer • defined by the water level (or hydraulic head) in a series of wells installed in the aquifer does not coincide w/ water table |
Unconfined aquifer | the uppermost aquifer in which the water table defines the upper boundary |
Perched aquifer | special type of unconfined aquifer that forms above the regional water table due to the presence of a low conductivity layer |
Confined aquifer | positioned between two aquitards and the elevation of the potentiometric surface must be above the elevation of the top of the aquifer |
How are aquifers formed? | by geologic processes and consist of lithologic units that have sufficient permeability to transmit water • unconsolidated sands and gravels • glacial, fluvial, alluvial, beach, aeolian • fractured or karst rocks |
Homogeneous | a property (say K) is independent of location in the geologic formation • i.e., K(x,y,z) = constant |
Heterogeneous | K varies with location in the geologic formation • i.e., K(x,y,z) ≠ constant |
Isotropic | K is independent of the direction of measurement at a point in the geologic formation • i.e., Kx = Ky = Kz |
Anisotropic | K varies with the direction of measurement • i.e., Kx ≠ Ky ≠ Kz • K is generally larger in the horizontal direction than the vertical direction |
What are the types of heterogeneity? | layering discontinuities spatial trends |
what are the causes of anisotropy? | grain orientation layering fracture orientation |