adapted to HTML from lecture notes of Prof. Stephen A. Nelson Tulane
University
Environmental Law
Riparian Doctrine (Bank Doctrine) - Whoever owns the land adjacent
to a body of surface water has the right to use that water. Water must
be used for beneficial or natural uses and must be returned to the
surface water body with the same quality and quantity.
Doctrine of Prior Appropriation Whoever is first has top priority.
Later users are placed in the order that they begin to use the water.
Benefical Uses of Water
Domestic Water Use
Municipal Supply
Irrigation and Watering Livestock
Power Generation
Mining or Drilling for Oil or Gas
Navigation
Recreation
Most Elements in food and water come from the soil.
Seen in areas underlain by limestone. The limestone is easily dissolved by
slightly acid groundwater, and collapses, leaving behind very rugged
topography on the surface.
Sinkholes As caverns become larger the roofs become unstable and collapse
forming large craters or sinkholes . Because water traveling through the
limestone does not pass through sand to clean it, water derived from a
limestone aquifer can be easily contaminated by human activity.
A few links relating to Karst topography can be found below:
Ground Subsidence
Due to withdrawal of groundwater is a problem in some areas when the water
is taken out of mixed clays and sands the remaining empty pore spaces
collapse compacting the soil and making future water retention impossible.
Residence Time
The average time that a substance resides in a reservoir is referred to as
the resident time.
For example, each day over an extended period of time, a hotel has:
100 Guests checking in.
100 Guests checking out.
A steady state - same number leaving as entering.
Average number of resident guests at any one time is 500.
Residence time is the amount in the system divided by the rate of
transport into/out of the system.
T residence = (Amount in system) / (Rate of transport)
= 500 guests / 100 guests/day
= 5 days.
Time of residence is 5, meaning that on average a guest stays for 5
days.
For groundwater:
An aquifer has a volume of 1 billion gallons, with 1,000,000 (1
million) gallons added each year by precipitation.
T residence = 1 billion gallons /(1 million gallons/yr)
= 1000 years.
Therefore, the average length of time of a drop of water remains in
the aquifer is 1000 years. If this aquifer were to be contaminated, it
would take much longer than 1000 years for it to clean itself
naturally.
Water Quality Concentrations
Usually measured in Parts Per Million, or ppm. (Although can also be
expressed as mg/liter)
1 ppm Pb (lead) = 1 part Pb / 1,000,000 parts water, or 1 mg Pb /
1 Liter water
EPA standards for lead in drinking water specify that it can not be
present in concentrations greater than 0.015 ppm or 0.015 mg/Liter.
A number of organic compounds that are carcinogenic have maximum allowed
concentrations of 0.005 ppm, or even less. A very small amount of these
can effect the gorundwater.
For example:
If your septic tank has a volume of 1,000 gallons you need only place
0.00032 ounces of such an organic compound to raise the concentration
level higher than drinking water standards. Some of these materials
include benzene (a common ingredient in gasoline) and dry cleaning
materials.
Dissolved Substances in Water
Calcium and Magnesium
Add "hardness" to water. This hardness is also referred to as Boiler
Scale (from the layer of filmy or scaly deposit found on the insides of
boilers in hard water areas. Good for teeth and bones.
Soft water has from 0 to 60 ppm of Calcium and Magnesium.
Hard water has over 120 ppm of Ca and Mg.
In regions of hard water, people often use water softeners, which
substitute sodium (Na) for calcium.
Fluoride
Should be present in quantities less than 4 ppm.
Too much can mottle the teeth enamel.
Strengthens apatite in bones and teeth.
Ca5(OH,Cl,F)(PO4)3
The increasing presence of Fluoride in the above reaction helps prevent
osteoporosis and tooth decay.