Groundwater significance highlighted through illustrations.
Understand differences between aquifers and aquitards.
Identify various types of wells and springs.
Explain degradation and depletion of groundwater.
Discuss negative consequences of groundwater overuse, dams, and water transport.
Porosity: Ability of rocks to contain fluids.
Permeability: Ability of rocks to allow fluids to pass through.
Groundwater behavior influenced by geology and geometry of rocks/sediments.
Aquifers: High permeability and porosity, facilitating easy water flow.
Aquitards: Low permeability, slowing or preventing water motion.
Visuals show the insufficient vs. sufficient groundwater supply around oceans.
Groundwater accessed via:
Natural springs
Human-made wells
Springs are where the water table meets the surface
Often found in valleys with wetland vegetation and saturated soils year-round.
Ordinary Wells: Holes into an aquifer, requiring pumping.
Artesian Wells: Water rises on its own due to pressure.
Water seeps into ordinary wells up to the water table level, requiring additional means for lifting water.
These wells are specifically designed to access groundwater under pressure, allowing water to reach the surface without pumping.
Engaging illustrations and simulations representing groundwater dynamics.
Freshwater being used unsustainably through
Faster extraction than natural replenishment
Wasting and polluting water resources.
One in ten people lacks access to clean water.
Surface Water: Freshwater from rain and snow.
34% of reliable surface runoff utilized annually.
70% for agriculture, 20% industrial use, and 10% urban usage.
Indirect water usage contributes significantly to global water footprints.
Factors: Dry climate, drought, overuse, inefficient water use.
Freshwater scarcity stress relates to availability versus human demand.
Global water basins often shared among multiple countries, sometimes contentiously.
Different major river basins exhibit varying levels of freshwater scarcity stress.
Global quality and quantity of freshwater supplies are threatened.
1.2 billion people lack access to clean drinking water.
Over-extraction causes lowering of water tables, drying springs, and seawater intrusion.
Rapid population growth leads to high water demand with limited new sources available.
Statistics on average annual precipitation across various regions.
About 70% of rivers engineered to move water between Northern and Southern California.
Key projects: Los Angeles Aqueduct, California Aqueduct, Colorado River Aqueduct.
Groundwater over-extraction threatens food production and urban supply.
Water transfer projects can disrupt ecosystems but expand distribution.
Desalination is an expensive but viable option for augmenting freshwater supplies.
Over-pumping limits food supply and raises prices, impacting affordability.
Lowering water tables necessitates deeper and costlier wells.
Overextraction leads to cone of depression around wells, affecting availability.
Wells may run dry before complete depletion of the water table occurs, prompting deeper installations.
Occurs near coastlines, poisoning wells and rendering them unusable.
Freshwater density compared to saltwater affects intrusion; rapid extraction moves saline boundaries towards wells.
Pumping treated freshwater back into the ground to prevent saltwater intrusion.
Post-extraction, sediments undergo readjustment, leading to compaction and decreasing porosity.
Compaction can cause land subsidence and irreversible damage to infrastructure.
Subsidence leads to destruction of essential structures without hope of recovery.
Illustrative measurements of subsidence in California show significant vertical changes.
Rapid subsidence due to groundwater removal leads to dangerous ground collapses.
Often unnoticed until significant damage occurs; cleanup is slow and expensive.
Common contaminants: fertilizers, animal sewage, industrial waste affecting aquifers.
Dams block river flow, creating reservoirs; vital for water management.
Benefits include flood control, irrigation, electricity generation, and recreation.
Dams displace populations, flood lands, and disrupt ecosystem functions.
Average lifespan limits their effectiveness.
Water transfer diminishes river flow, increases pollution, threatens fisheries, and promotes water wastage.
Encouragement to consider the most impactful advantage and disadvantage concerning dams.
Process of removing soluble salts from seawater; techniques include distillation and reverse osmosis.
High costs, chemical waste harming ecosystems, and significant brine production.
Details of a desalination plant project near Huntington Beach with environmental considerations.
Summary of California's desalination facilities, featuring the Carlsbad project as the largest.
Ongoing challenges related to aquifer depletion, water transfer impacts, and desalination costs.
Factors influencing the assessment of freshwater availability against human consumption.
Three main strategies: conservation, desalination, interbasin transfers to manage water resources effectively.
Overview of a project aimed at enhancing water transport across the state.
Link to further information on water projects.
Concluding content from the course related to water resource management.