Course: ESC1000C - Dr. Jackie Miranda
Date: February 16, 2024
60 Second News Update
Hydrologic Cycle
Water Basins and Budgets
Running Water
Water Quality
Florida Water Issues 2025
UNIT 1: Geology
UNIT 2: Oceanography
UNIT 3: Meteorology
UNIT 4: Astronomy
The hydrologic cycle describes the continuous movement of water within the Earth and atmosphere.
Earth is a complex system comprised of various spheres:
Biosphere: life forms
Hydrosphere: water in all forms
Geosphere: land/earth structure
Atmosphere: gases around Earth
Formed approximately 4.5 billion years ago during the early development of the atmosphere.
Initial water vapor likely originated from volcanic eruptions.
Water covers approximately 70% of the Earth's surface.
Query: What percentage is available for human consumption?
68.7% of Earth's freshwater is stored in glaciers and ice caps.
Melting glaciers and ice caps due to global warming result in loss of this freshwater as it mixes with ocean water.
30.1% of freshwater is groundwater, the primary source accessed and utilized by humans.
Water evaporates from oceans, plants, and soil, entering the atmosphere.
Returns to Earth via precipitation.
Infiltration (soaks into ground), runoff (flows over surface), evaporation, or storage as snow/glacier.
The cycle is balanced; water movement occurs between reservoirs, with total amount remaining constant.
The primary driver of the hydrologic cycle is the sun.
Key processes:
Evaporation (oceans)
Transpiration (land)
Condensation
Precipitation
Runoff
Infiltration
Groundwater/aquifers
Origin of water on Earth's surface?
A. Volcanic eruptions
Primary energy source driving the hydrologic cycle?
C. The sun
Process producing water vapor from plants?
A. Transpiration
After rain falls, it may:
C. Infiltrate or evaporate
The U.S. uses 1,344 billion liters (355 billion gallons) of ground and surface water daily.
21% of this, or 88 billion liters (76 billion gallons), is fresh groundwater.
The 100th meridian is the rough boundary between moisture-rich and arid parts of the U.S., affecting agriculture practices (necessity for irrigation).
Water use has decreased over the last 20 years due to:
Improved technologies, such as low-flow toilets and efficient agricultural practices.
A stream drains an area known as a drainage basin or watershed, controlled by elevation and gravity.
Types:
Dendritic: Most common; uniform material
Radial: Found on volcanic cones
Rectangular: Forms in jointed/faulted bedrock
Trellis: Alternating resistant and weak strata
Influenced by:
Rainfall intensity and duration
Soil moisture content
Soil type
Land slope
Vegetative cover
Runoff dominates on impermeable or saturated surfaces, especially urban areas.
Definition: Underground layers of rock holding groundwater.
Aquifers can deplete faster than they refill, termed aquifer depletion.
Rivers significantly influence land drainage, affected by climate and human activity.
Defined as the volume of water flowing past a point over a certain time (Discharge = velocity x area).
Sediment Production: Dominant erosion area in the headwaters.
Sediment Transportation: Balanced transport between erosion and deposition.
Sediment Deposition: Occurs when rivers enter larger bodies of water.
Three load types:
Dissolved Load: Ions from chemical weathering
Suspended Load: Particles sized according to the flow velocity
Bed Load: Larger particles transported by bouncing
Bedrock Channels: Found in steep areas; stable
Alluvial Channels: Changes shape due to erosion and deposition; includes meandering and braided streams
Characterized by sweeping bands with significant erosion on banks with higher velocity.
Composed of diverging and converging channels, typically transporting coarse materials.
Occurs when discharge exceeds channel capacity:
Regional Floods: Caused by rapid snowmelt or storms.
Flash Floods: Rapid rainfall leads to quick water level rise.
Artificial levees: Earth mounds along river banks.
Flood-control dams: Retain floodwater.
Channelization: Altering stream channels for increased flow rate.
Nonstructural methods: Zoning for floodplain management.
Point-source: Single and definable origins (e.g., waste sites).
Nonpoint source: Multiple, diffuse origins (e.g., agriculture).
Organic Chemicals
Inorganic Chemicals
Microbial/Biological
Example sources: herbicides, pesticides, industrial solvents, and pharmaceutical residues.
Examples: heavy metals (lead, mercury), nutrients (nitrates, phosphates).
Includes harmful bacteria like E. coli; groundwater is usually safe unless linked to contaminated surface water.
Bioremediation: Using bacteria to decompose contaminants.
Phytoremediation: Utilizing plants to absorb harmful chemicals.
Chemical remediation: Applying chemicals for harmful material breakdown.
Physical remediation: Filtration methods.
Dissolved Oxygen: Vital for aquatic life.
Nutrients: Monitoring is crucial to prevent eutrophication.
Salinity, Temperature, Bacterial Count: Essential physical parameters for water bodies.
Topics include groundwater depletion, Everglades restoration, saltwater intrusion, and runoff.
Students are to summarize, identify causes, and propose solutions.
Earth Processes and Groundwater: Study on weathering, erosion, soil, and groundwater, with an update due 2/19.
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