Ground water

What is ground water and why should we care about it?

      Most important fresh water source

 

Where is ground water found

      Held in pore space of sediments

      Found in fractures and joints of rocks

      Easy to pollute but hard to clean up

 

How is water held in pores of rocks and soils?

      Hygroscopic water

            Thin film of water molecules on soil particles

            Created by polar nature of water and polar nature of clays

            This water bonds to soil and doesn’t move through soil easily

      Capillary water

            Water that is held in pore space due to surface tension of water

            Adheres to soil particles and moves by pressure changes

      Gravitational water

            Associated with large particles such as sand and gravel

            Moves down due to gravity

            Responsible for recharging ground water system

 

Parts of the ground water system

      Zone of aeriation

            Capillary zone

      Zone of saturation

      Water table

      Perched water table

      Spring

 

Ground water motion

      Follows Surface topography

            water flows down hill

      Ground water is always in motion

      How fast does groundwater move?

      Two primary factors

            Porosity

                  The amount of pore spaces in a rock or sediment

                  Determines how much water a rock or sediment can hold

                        Well sorted sediment with low cementation--> good porosity

                        Fractures and joints-->  good porosity

            Permeability

                  how well connected the pore spaces are in a rock or sediment

                  determines how water flows through a system

                        round, well sorted clasts with a random packing

                        poorly cemented or heavily jointed

                  best permeability--> sand and gravel

                  worst permeability--> clay an silt          

      Water movement

            Primary controlΰ permeability

                  low permeability = slow movement of water

            Secondary controlΰ porosity

                  small pores = slow movement of water

 

Aquifer

      A medium that transmits water freely

      What type of material would make a good aquifer?

            Good aquifers

                  Sand, gravel or other permeable and porous material

                  Highly fracture rocks

 

Aquitard

      impermeable layer of material

      What type of material would make a good aquitard?

            Good aquitards

                  Clay

                        Lines aquifers and acts as a pipe

 

Recharging?

      How do water tables recharge?

            Infiltration:   Slow process--> dependent on permeability and porosity of the sediments/rocks

            Influent streams:  streams that feed the water table

 

How long does it take for ground water to recharge?

 

How long does it take to remove water from system?

 

What is a well?

      Man made

            created to harvest ground water

            uses some type of mechanical pump

      Natural well (artesian)

            water rises above the aquifer through hydraulic pressure

            1 aquifer and 2 aquitards

            reaches surface by fracture or pipe

            no pump is required

 

Other ground water exits

What happens when a water table intersects the surface of the earth?

      Springs

      Geysers

      Effluent streams

 

Social issues surrounding water

      Water use in USA (1995)

            surface water  321 billion gal/day

            ground water   77 billion gal/day

                  220 billion gal/day returned to streams after use (55%)

 

What sectors of society use water

      power generation:      39%

      Irrigation:                   39%

      Public supply:            13%

      Industry and mining    7%

      Commerical                 1%

      Livestock                     1%

 

How are water supplies (streams and groundwater) affected by the population

      overuse

      pollution

      climate

 

Overuse (Numbers from the United Nations)

      1950  ~ 2.6 billion people

      2000   ~ 6 billion people

      2050    projected to be ~9 billion people

 

Current over use/mismanagement problems?

      Diversion water from rivers for crop irrigation

      Low water flow to downstream populations

            Rio Grande-->  Mexico and Texas

      Disrupt sediment balance

            Grand Canyon and Colorado River

            Building levees to stop flooding

                  rich sediments not provided to flood plane

            Divert to irrigate fields

                  increases salinity of farmland

      Competition between wells

            overpumping

            draw down and cone of depression

            dry wells

            subsidence

            salt water incursion

      Salt water incursion

     

Mining of water tables

      short term non-renewable

      must apply safe yield concepts

            establish hydrologic equilibrium for each basin

                  how much water is available

                        recharge rate vs withdraw

            long term monitoring

            limit wells

                  drawdown < recharge

 

 

 

 

Pollution?

      Ground water contamination

            dumps

            pesticides and other chemicals

            gas stations

            septic tanks

            farm waste (lagoons)

            industrial

            pipes and tanks leaking

            dumping of toxic material

Why is it so difficult to clean up ground water systems?

 

How can ground water contamination be prevented or mitigated?

      Use sewers not septic systems

      line lagoons

      limit pesticide/chemical use

      rapid response to spills

      monitor wells and tanks

      Natural purification?

            Sediment removes bacteria

            physically

            oxidation

            assimilation

            long resident time required

            small pore spaces