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Awesome Aquifers pt1
Part One of the Vocab
| Term | Defintion |
|---|---|
| Aeration Zone | The zone immediately below the land surface where pores contain both water and air |
| Aquifer | An underground geological formation able to store and yield water |
| Cone of Depression | The zone around a well in an unconfined aquifer that becomes unsaturated as a well is pumped |
| Confining Layer | Geologic Material with little or no permeability |
| Hydraulic Conductivity | The ease with which water can move through pore spaces or fractures |
| Depletion | The loss of water from surface water reservoirs or groundwater aquifers at a rate greater than that of recharge |
| Discharge | An outflow of water from a stream, pipe, aquifer, or watershed. |
| Drawdown | A lowering of the groundwater level caused by pumping |
| Flow Rate | The time required for a volume of groundwater to move between points |
| Groundwater | Water found in the spaces between particles and cracks in rocks underground |
| Hydrologic Cycle | The paths water takes through its carious states |
| Water Cycle | Also known as the Hydrologic Cycle |
| Impermeable Layer | A layer of material in an aquifer through which water can not pass |
| Infiltration | Flow of water from the land surface into the subsurface |
| Infiltration rate | The quantity of water that enters the soil surface in a specified time interval |
| volume of water per unit of soil surface area per unit of time | How infiltration rate is often expressed |
| Monitoring well | A non-pumping well that is used to measure the elevation of a water table or water quality |
| Overwithdrawal | Withdrawal of groundwater over a period of time that exceeds the recharge rate of the supply aquifer |
| Overdraft, Mining the Aquifer | Mainly known as overwithdrawal |
| Permeable/Permeability | capable of transmitting water; the rate at which water moves through rocks or soil |
| Permeable Layer | The layer through which water freely passes as it moves through the ground |
| Plume | An underground pattern of contaminant concentrations created by the movement of groundwater beneath a contaminant source. |