Groundwater 7
Complete List of Terms and Definitions for Groundwater 7
| Terms | Definitions |
|---|---|
| aquitards | groundwater is confined by |
| stalagmites | form from the ground up. |
| Karst topography | irregular terrain, with many depressions |
| recharge | the process of infiltration and migration through which groundwater is replenished, usually by precipitation. |
| aquitard | impermeable layers that hinder or prevent water movement (ex:clay) |
| Diffusion | A way pollution moves (dissolved components move in response to chemical concentration gradients from places of higher concentrations to places of lower concentrations |
| permeable | where water can go through, the ability to transmit a fluid through interconnected pore spaces |
| drawdown | Difference between the water level in a pumped well and the original water-table level |
| Permeability | Connectivity of the pore or empty spaces. How fast water can flow through the pores? |
| Spring | A place where ground water emerges onto the surface |
| deficit | the condition in which stored soil water is gone and the need for moisture is greater than the rainfall. |
| aquifier | permeable rock strata or sediment that transmit groundwater freely (ex: sands/gravels) |
| Groundwater | Water that occurs in soil and rock |
| capacity/load | how much stuff a river can hold |
| Infiltration | The process of water moving into the ground to the water table. |
| groundwater table | separates the zone of aeration from the zone of saturation. It is not flat like a table, but follows the topography (shape of the land). |
| Saturated zone | Below the water table, where water completely fills pores |
| Porosity | holes in rocks, amount of void space in a rock, sandstone, limestone |
| water produced from a confined aquifer will rise to the | pressure surface |
| runoff | water that wont infiltrate the soil or rock |
| zone of saturation | Depth below Earth's surface where all the pores of a material are completely filled with groundwater |
| water table | the upper level of the saturated zone of groundwater |
| flowing artesian well | due to pressure in a confined aquifer |
| meanders | curves cut into a river by the speed of the water's flow |
| unsaturated zone |
(also known as the zone of aeration or vadose zone) has pore spaces filled with air |
| perched water table | a type of spring formation where an aquitard is situated above the main water table, as water percolated downward a portion of it is intercepted by the aquitard, creating a localized zone of saturation and a perched water table |
| cone of depression | inverted cone shaped dip in the water table due to the removal of water from a water table by a well |
| what holds water around sedimentary particles? | the capillary fringe that extends upward from the water table and groundwater is held by surface tension in tiny passages between grains of soil or sediment; (capillus= hair) |
| what does groundwater velocity depend on? | the permeability of the rock and the slope of the water table |