Groundwater Flashcards
What is groundwater?
-water found below the Earth’s surface, filling porous spaces in soil and rock
-fresh water from rain or melting snow and ice that is stored between rocks and particles of soil (infiltration)
-provides 25% of the fresh water used in the US
-can stay underground for decades or can come to the surface to fill rivers, streams, lakes, ponds, and wetlands (outcroppings, recharge)
-can move slowly
-also can come to the surface as a spring or be pumped from a well
Relative quantity of groundwater vs surface water
-10 million cubic kilometers of water stored underground
Groundwater zones
unsaturated zone, water table, saturated zone, groundwater
What is surface water?
-surface water is water that collects on the ground or in a stream, river, lake, reservoir or ocean
-surface water is constantly replenished through precipitation and lost through evaporation, plant uptake, ag, DW
-approx 68% of community water system users receive their water from a surface water source
-surface water is any body of water above ground, including streams, rivers, lakes, wetlands, reservoirs, wetlands and creeks
-the ocean, despite being salt water is also considered surface water
-surface water is part of the water cycle, which involves the movement of water to and from the Earth’s surface
-surface water and ground water are reservoirs that can feed into each other. Surface water can seep underground to groundwater and groundwater can resurface on land to replenish surface water
unsaturated zone
the portion of the subsurface above the groundwater table. The soil and rock in this zone contains air as well as water in its pores. In some places the unsaturated zone is absent, as is common where there are lakes and marshes, and in some places it is hundreds of meters thick, as is common in arid regions
water table
the upper surface of the zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with groundwater, which may be fresh, saline, or brackish, depending on the locality. It can also be simply explained as the depth below which the ground is saturated
saturated zone
the part of an aquifer, below the water table, in which relatively all pores and fractures are saturated with water.
unconfined aquifer
the upper layer of an aquifer which does not have a confining layer of solid material above it
confined aquifer
ground water sources under pressure from the weight of rocks that have layers of solid material above and below them causing pressure
artesian well
groundwater aquifers between layers of rock that are confined and under pressure. If tapped by a well, water will rise above the top of the aquifer
What is an aquifer?
an underground layer of water-bearing material, consisting of permeable or fractured rock, or of unconsolidated materials
outcrop
rock walls along roadsides where the rock is exposed and water maybe seen seeping out of the cracks of the rock unit. This rock wall represents an “outcrop” (or location where the rock intersects the land surface) of an aquifer
groundwater recharge: natural
-occurs as precipitation falls on the land surface, infiltrates into soils, and moves through pore spaces down to the water table
- can occur as surface water leakage from rivers, streams, lakes and wetlands
groundwater recharge: artificial
recharge can be done through injection of water through wells
-this has the problem of potentially introducing contaminants
groundwater contamination: point sources
sources that might include wastewater treatment plants, landfills, garages, motor pools and fleet maintenance facilities. other sources include mine discharge water and mine spoil run-off