Universal Solvent: Due to its polarity and Hydrogen bonding (Dilute/Disperse/Dissolve) pollutants
Polar Covalent Molecule with partial charges on H and O
An effective filter of shorter UV wavelengths
Higher density in liquid form than its solid form due to Hydrogen bonding
Polar Covalent Molecule with partial charges on H and O
Melting/Freezing Point 0oC
Boiling Point: 100oC
Universal Solvent: Due to its polarity and Hydrogen bonding (Dilute/Disperse/Dissolve) pollutants
Higher density in liquid form than its solid form due to Hydrogen bonding
Surface water = water on the surface like streams and lakes
Surface Water = Surface runoff and watershed basin (Lake, River, Stream)
Ground water = water that saturates soil, sand, and rock beds, supplying springs and wells, like aquifers
Aquifers = Recharged naturally by rain or by nearby surface water - an underground layer of water-bearing permeable rock
Zone of Saturation - Spaces in soil below a certain depth are filled with water
Water Table - top of the zone of saturation
⅔ of surface runoff are lost due to seasonal flooding and the remaining ⅓ is the reliable runoff
Worldwide Average - freshwater use
70% for Irrigation and Livestock
20% for Industrial use
10% Cities and Residence
Many River Systems are highly stressed
Nile, Jordan, Yangtze, Ganges
30% of Earth’s land area experiences severe drought
Ways to increase Water Supply
Dams and Reservoirs
Saltwater Desalination
Water Transfer/Diversion
dam is a physical structure that retains water; a reservoir is the water body that is created by a dam.
Dams and Reservoirs PROS
Capture and store runoffs which increases reliable runoff
Release runoff for flood control, generate electricity, supply irrigation water, and recreation
Dams and Reservoirs CONS
Habitat destruction displace not just species but also humans
Impair ecological services of rivers such as nutrient distribution
Sediment buildup can fill it within 50 years
Endanger animals and plants
Problems that could arise from using dams
Faulty dams leak water
They can’t work when the water level is too low
flood large areas
force people to relocate
threaten freshwater biodiversity
Environmental impacts of dams
disrupt subsistence fisheries,
leave rivers dry – affecting the ecosystem.
water, soil, air quality
wildlife habitat
Groundwater CONS
Over use leads to depletion or lowering of water tables
Arid countries far from surface water depends on aquifers too much
Limitsfood production which will increase prices
Land Subsidence
Groundwater overdraft in coastal region will risk saltwaterintrusion
Land Subsidence = When the ground sinks, causing buildings to collapse.
Groundwater PROS
Cost-effective
Good for places with high water tables
Irrigation
Industrial and other use
Problems that could arise from using Groundwater
drying up of wells
reduction of water in streams and lakes
deterioration of water quality
increased pumping costs
land subsidence
Environmental impacts of groundwater usage
lowered water tables
saltwater intrusion in aquifers
lower streams and lakes
less biodiversity
Types of desalination methods are Distillation or Reverse osmosis
Reverse osmosis performs water filtration by passing it through multiple stages of filtration stripping off all the minerals. In the final filtration stage, it adds healthy minerals back into the water
Distillation, on the other hand, also purifies water but doesn't add healthy minerals to the water
Cost of desalination: $1000 per cubic meter of water
High cost, high energy usage, and large amounts of salty wastewater
Water Transfer/Diversion = Transfering/diverting water from one place to another through canals or aqueducts
Water Diversion
Loss of water from evaporation and leaks as the water is moved
Environmental Degradation by building them
Aral Sea & Colorado River
There are several similarities and differences between the effects of human alterations on the Colorado River and the Aral Sea. Both have dams and canals, and both fail to reach the ocean. The Colorado River supplies both agriculture and urban areas. And the rivers of the Aral Sea are diverted primarily for agricultural areas. The water levels are depleting and the fish are dying.
The main difference between these two examples is that the Colorado River has been able to maintain some flow while the Aral Sea has not.
Groundwater pumping rates exceed recharge rates leading to declining groundwater tables and reduced availability of this resource
Irrigation is using water for crops that is not rainwater. Irrigated water can be pumpedfrom groundwater, aqueducts and other sources
Waterlogging occurs when too much water is left to sit in the soil. This raises the water table and suffocates plants (prevents gas exchange)
Furrow Irrigation:
Description: Ditches between crop rows that are filled with water.
Benefits: Inexpensive and easy
Drawbacks: 1/3 of the water is lost to evaporation and runoff
Flood Irrigation:
Description: Flooding of a field with water. Sometimes used with furrows.
Benefits: Inexpensive and easy
Drawbacks: 20% loss of water to evaporation and runoff. Can waterlog soil