Glossary of Water Well and Groundwater Terminology
Explore words and their meanings common to water wells and groundwater.
Basic Concepts
Abiotic –Non-living chemical and physical factors in the environment.
Adsorption –The adhesion of molecules or particles to a surface.
Aeration –The process of increasing the oxygen saturation of water.
Alluvium –Sediment deposited by flowing water, often containing groundwater.
Anisotropy –Variation in hydraulic conductivity in different directions within an aquifer.
Coliform Bacteria –A group of bacteria commonly found in the environment, used as an indicator of water quality.
Hydraulic Gradient –The slope of the water table or potentiometric surface, driving groundwater flow.
Infiltration –The process by which water on the ground surface enters the soil.
Isotropy –Uniformity in all orientations; opposite of anisotropy.
Percolation –The downward movement of water through soil and rock.
Runoff –Water that flows over the land surface and into streams and rivers.
Seepage –Slow movement of water through soil or rock.
Static Water Level –The static water level is the level of water in a well when the well is not being pumped.
Groundwater and Aquifers
Aquiclude –A geological formation that does not transmit water.
Aquitard –A less permeable layer that restricts the flow of groundwater from one aquifer to another.
Artesian Pressure –The pressure that causes water in a confined aquifer to rise above the top of the aquifer.
Artesian Well –An artesian well is one where water flows to the surface naturally due to pressure in the aquifer.
Confined Aquifer –An aquifer that is bounded above and below by impermeable layers.
Confining Layer –A layer of rock or sediment that restricts the flow of groundwater.
Ephemeral Stream –A stream that flows only during or immediately after rainfall.
Fissures –Cracks in rock formations that can store and transmit groundwater.
Fractured Aquifer –An aquifer where groundwater moves through cracks and fractures in rock.
Groundwater –Groundwater is water stored in the pores and fractures of underground rock formations.
Groundwater Basin –A geographic area that contains a connected groundwater system.
Groundwater Flow –The movement of groundwater through the pore spaces and fractures in rocks and sediments.
Hydraulic Conductivity –Hydraulic conductivity is a measure of how easily water can move through porous materials and is crucial for determining well performance.
Hydraulic Head –The total energy per unit weight of water, comprising elevation, pressure, and velocity heads.
Hydrogeology –The study of groundwater and its interactions with geological formations.
Impermeable Layer –A layer of material through which water cannot pass.
Karst –A type of landscape formed from the dissolution of soluble rocks, often featuring sinkholes and underground streams.
Lateral Flow –Groundwater movement parallel to the Earth's surface.
Overdraft –Overdraft occurs when water is pumped from an aquifer faster than it is recharged.
Perched Aquifer –A localized zone of saturation above the main water table, created by an impermeable layer.
Potentiometric Surface –The level to which water in a confined aquifer would rise if unimpeded.
Recharge –Groundwater recharge is the process where water from precipitation and other sources infiltrates the ground and replenishes aquifers.
Recharge Area –A region where water infiltrates the ground and replenishes an aquifer.
Unconfined Aquifer –An aquifer that is directly open to the surface and whose water table can rise and fall.
Vadose Zone –The area between the ground surface and the water table, also known as the unsaturated zone.
Water Table –The upper surface of the zone of saturation, where groundwater pressure is equal to atmospheric pressure.
Hydrogeological Processes
Capillary Fringe –The subsurface layer where groundwater seeps up from a water table by capillary action.
Catchment Area –The area from which rainfall flows into a river, lake, or reservoir.
Geophysical Logging –The process of recording the physical properties of rocks and sediments in a borehole.
Graben –A depressed block of land bordered by parallel faults, often filled with sediment.
Lithology –The physical characteristics of rock or sediment.
Macropore –A large soil pore that can transmit water rapidly.
Piezometer –An instrument used to measure the pressure of groundwater at a specific point.
Priming –The process of filling a pump with water to remove air and allow it to function.
Tracer Test –The use of a dye or other substance to track the movement of groundwater.
Transmissivity –The ability of an aquifer to transmit water, equal to the hydraulic conductivity times the saturated thickness of the aquifer.
Water Quality
Chlorination –The process of adding chlorine to water to disinfect it.
Dissolved Oxygen –The amount of oxygen dissolved in water, important for aquatic life.
Effluent –Wastewater discharged into the environment from a treatment plant or industrial process.
Leachate –Contaminated water that has percolated through a landfill or other waste material.
Methemoglobinemia –A condition caused by high nitrate levels in water, reducing the blood's ability to carry oxygen.
pH Level –A measure of the acidity or alkalinity of water.