7 - Surface Hydrology 2 Flashcards
Groundwater
All the water that exists in the underground saturated zone
- Water that seeps through soil and does not runoff - stays in ground
30% of freshwater on Earth
Methods groundwater leaves the saturated zone?
Springs (15-20%), river and lake seepage (50-60%), evaporation (10-15%) and submarine groundwater discharge (5-10%)
Submarine groundwater discharge
the natural flow of groundwater from land to ocean or coastal waters through the seabed.
Water table
upper level of an underground surface in which the soil or rocks are permanently saturated with water
What makes the water table move?
Changing precipitation, seasonal variation (lowest in summer), plant uptake and water removal, pumping or human changes
Aquifers
underground layer of water-bearing material consisting of permeable or fractured rock or of unconsolidated materials
Hydraulic head
amount of mechanical energy available in water
How is the hydraulic head determined?
By pressure (weight of overlying water) and elevation (distance from the sea). Flows from areas of high (A) to low (B) head
Hydraulic gradient
movement from one head to another. Tells us the rate and direction of groundwater flow
Darcy’s law
used to calculate speed of groundwater
Hydraulic conductivity
how easily does water move through different substances
Aquitards have low hydraulic conductivity (confining layers) e.g. clay, silt
Hydraulic conductivity is dependent on?
Porosity, permeability, grain size and sorting, material type, degree of saturation and fluid viscosity and temperature
Cone of depression
pumping causes the water table to lower at the well location. For this reason pumps cannot be located too close
Impacts of groundwater pumping?
Subsidence, saltwater intrusion, depleted groundwater, streamflow depletion and dry wells
Subsidence
process by which an area of land sinks to a lower level than the surrounding land
Causes:
- Groundwater extraction
- Mining
- Oil and gas extraction
- Soil compaction