AP ENVIRONMENTAL SCIENCE
Five Causes of Environmental Problems
Population Growth
Unsustainable resource use
Poverty
Excluding environmental costs from prices
Trying to manage nature without knowing enough about it
Formulas
Natural Capital = The natural resources (noun) + natural services (verb)
Doubling time in years = 70 / %growth
% change: (after-before)/before x 100 & (new value - old value)/old value x 100
GDP per capita = GDP / population
Principles of Sustainability
Reliance on solar energy
Biodiversity
Population Control
Nutrient recycling
8 Causes of Collapse in Ancient Civilizations
Deforestation/habitat destruction
Soil problems (erosion, salinization, soil fertility)
Water management problems
Overhunting
Overfishing
Invasive species
Human population growth
Increased per capita impact of people
4 Causes of Collapse in Modern Civilizations
Human-caused climate change
Toxic chemical build-up in the environment
Energy shortages
Full human utilization of Earth’s photosynthetic capacity
The Pathway to Collapse
Food shortages
Starvation
Competition over resources
Political takeovers
War
Factors that Contribute to Societal Collapse (5)
Damages that people inadvertently inflict on their environment.
Climate Change
Hostile Neighbors
Friendly Neighbors
Societal response to problems
Political
Economic
Social
Cultural
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Principles of Sustainability
Reliance on solar energy
Solar capital - a perpetual resource
The sun warms the planet and supports photosynthesis used by plants to provide food for themselves and for us and most other animals.
Biodiversity
The variety of different organisms, the genes they contain, the ecosystems in which they exist, and the natural services they provide
Population Control
Competition for limited resources among different species places a limit on how much their populations can grow.
Nutrient Recycling
Natural processes recycle chemicals that plants and animals need to stay alive and reproduce.
COLLAPSE
8 Causes of Collapse in Ancient Civilizations
Deforestation / habitat destruction
Soil problems (erosion, salinization, soil fertility)
Water management problems
Overhunting
Overfishing
Invasive species
Human population growth
Increased per capita impact of people
4 Additional Causes of Collapse in Modern Civilizations
Human caused climate change
Toxic chemical build-up in the environment
Energy shortages
Full human utilization of Earth’s photosynthetic capacity
Pathway to collapse
Population growth forces people to increase their agricultural production. This involves the use of irrigation, terracing, double-cropping and expanding farming from prime lands to marginal lands.
Unsustainable agricultural practices leads to serious consequences for society to obtain resources:
Food shortages
Starvation
Competition over resources
Political takeovers
War
Societal collapse
Damages that people inadvertently inflict on their environment
People
Environment
Climate change
This may be human induced, or natural fluctuations in climate.
Hostile neighbors
If your neighbors are mightier than you, you can be exterminated.
Often societies collapse by what appears a military conquest, but underlying the conquest was something environmental that weakened the society.
Friendly neighbors
Most every society needs good trading partners.
If your trading partner becomes weakened, you will suffer too.
Societal response to problems
Political
Economic
Social
Cultural
SUSTAINABILITY
Five Causes of Environmental Problems
Population Growth
The world’s population is growing exponentially
Unsustainable resource use
Affluenza is a term used to describe the unsustainable addiction to overconsumption and materialism
Poverty
the inability to meet one’s basic economic needs.
concentrated in the Southern Hemisphere
Excluding environmental costs from prices
Trying to manage nature without knowing enough about it
Environmental Science: Studies interactions between humans and nature.
Worldviews:
Biocentric: All species have equal value.
Ecocentric: Ecosystems and organisms hold equal importance.
Anthropocentric: Focus on human well-being.
Environment: All conditions influencing life.
Sustainability: Using resources without harming future generations.
Conservation: Careful use of resources to prevent depletion.
Preservation: Maintaining ecosystems for continued survival.
Tragedy of the Commons: Overuse of shared resources leads to depletion; requires management solutions like catch-share systems.
Ecosystem Services: Benefits like clean water, timber, and crops.
Environmental Indicators: Metrics for ecosystem health (e.g., biodiversity, CO2).
Feedback Loops:
Positive: Amplifies changes.
Negative: Restores balance.
Closed System: No exchange of matter or energy (rare in nature).
Open System: Energy/matter cross boundaries.
Ecological Footprint: Land/resources needed to support an individual's consumption.
Key Movements:
Agricultural Revolution: Improved soil and crop output.
Industrial Revolution: Increased pollution and fossil fuel use.
Environmental Ethics: Moral responsibility to nature.
Environmental Justice: Equal involvement in environmental policy.
Gifford Pinchot: Advocated for sustainable forestry.
Aldo Leopold: Promoted wilderness conservation.
Thomas Malthus: Warned of overpopulation impacts.
Biotic/Abiotic: Living vs. nonliving elements.
Fossil Fuels: Finite energy sources from ancient biological material.
Millennium Ecosystem Assessment: Evaluated human environmental impacts.
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Reliance on Solar Energy: Solar energy is a perpetual resource, driving processes like photosynthesis that support life.
Biodiversity: The variety of organisms, ecosystems, and natural services essential for ecosystem resilience.
Population Control: Limited resources create competition, naturally regulating population sizes.
Nutrient Recycling: Natural processes recycle essential chemicals for life and reproduction.
Deforestation / habitat destruction
Soil problems (erosion, salinization, fertility loss)
Water management issues
Overhunting
Overfishing
Invasive species
Human population growth
Increased per capita impact
Human-caused climate change
Toxic chemical accumulation
Energy shortages
Full utilization of Earth's photosynthetic capacity
Population growth increases agricultural demands, leading to irrigation, terracing, double-cropping, and farming on marginal lands.
Unsustainable agriculture causes resource scarcity, resulting in:
Food shortages
Starvation
Resource competition
Political instability
War
Environmental Damage: Human-induced harm, including climate change.
Hostile Neighbors: Vulnerability to military conquest, often rooted in environmental weakening.
Friendly Neighbors: Collapse of trading partners weakens dependent societies.
Societal Responses: Depend on political, economic, social, and cultural adaptations.
Population Growth: Exponential global population increase.
Unsustainable Resource Use: Overconsumption driven by materialism ("affluenza").
Poverty: Inability to meet basic needs, mainly in the Global South.
Ignoring Environmental Costs: Prices exclude environmental damage.
Poor Environmental Management: Acting without adequate ecological understanding.
Ecosystem Basics
Energy Flow in Ecosystems
The global distribution of fish varies because of some combination of:
Salinity (salt concentration)
Depth
Turbidity (clarity of water)
Nutrient availability
Temperature
Freshwater biomes have low salinity, they include:
Streams and rivers
originate from underground springs
runoff from rain or melting snow.
Streams are narrow and carry small amounts of water
rivers are wider and carry larger amounts of water.
Lakes and ponds
Contain various zones
Lakes have levels of primary productivity
Freshwater wetland
among the most productive biomes on Earth.
Marine biomes have high salinity, they include:
Salt marsh
contains nonwoody emergent vegetation
one of the most productive biomes in the world.
Mangrove swamp
occurs along tropical and subtropical coasts
contains salt-tolerant trees with roots submerged in water
help protect the coastlines from erosion and storm damage
Intertidal zone
narrow band of coastline between the levels of high and low tide
Coral reef
Found in warm, shallow waters beyond the shoreline.
Earth's most diverse marine biome
Coral bleaching: A phenomenon in which algae inside corals die, causing the corals to turn white.
Open ocean
located away from the shoreline where sunlight can no longer reach the ocean bottom
Contains zones
Lakes and Ponds Zones
The littoral zone consists of shallow water with emerging, rooted plants.
The limnetic zone is the deeper water where plants do not emerge.
The profundal zone is the deepest water, where oxygen can be limited because little sunlight penetrates to allow photosynthesis by producers.
The benthic zone consists of the sediments that lie beneath the profundal zone.
Lakes Productivity
Oligotrophic Describes a lake with a low level of productivity.
Mesotrophic Describes a lake with a moderate level of productivity.
Eutrophic Describes a lake with a high level of productivity.
Open Ocean Zones
Photic zone: The upper layer that receives enough sunlight for photosynthesis.
Aphotic zone: The deeper layer that lacks sufficient sunlight for photosynthesis.
Biodiversity
Natural resources
food, water, wood, energy
Natural services
air and water purification, soil fertility, waste disposal, pest control
Aesthetic pleasure
Ecosystem services
Provisioning - material or energy outputs from ecosystems
food, water, and other resources
Regulating - services acting as regulators
regulating air and soil quality, flood control
Cultural - recreation, tourism, aesthetic appreciation
Supporting - habitats for species, maintenance of genetic diversity
Measures of Biodiversity
Species richness
Number of species in an area
Species evenness
Relative proportion of individuals within the different species in an area
Theory of Island Biogeography
Species richness increases as…
size of the habitat increases.
distance to the mainland decreases.
Gene Flow
Process by which individuals move from one population to another and thereby alter the genetic composition of both populations.
Arrival of individuals from adjacent populations alters the frequency of alleles in the population.
Gene flow can help bring in genetic variation to a population.
Genetic drift
A change in genetic composition of a population as a result of random mating.
genetic drift is a nonadaptive, random process.
Important role in altering the genetic composition of small populations.
Bottleneck Effect
Reduction in genetic diversity of a population caused by a reduction in its size.
Reduced population numbers mean reduced genetic variation.
Low genetic variation in a population can cause an increased risk of disease and low fertility.
Resulting low diversity can lead to decline and extinction.
Founder effect
Change in genetic composition of a population as a result of descending from a small number of colonizing individuals.
Threats to Biodiversity: HIPPCO
Habitat destruction
Invasive species
Pollution
Population growth
Climate change
Overexploitation (overhunting, overfishing, overconsumption)
BIOGEOCHEMICAL CYCLES
Hydrologic Cycle
Carbon cycle
Nitrogen cycle
Phosphorus cycle
Sulfur cycle
Hydrologic Cycle
Water moves from the atmosphere to Earth’s surface and back to the atmosphere.
Effects
Withdrawing large amounts of freshwater.
Clearing vegetation and eroding soil.
Polluting surface and underground water.
Carbon Cycle
Producers take up carbon from the atmosphere via photosynthesis and pass it to consumers and decomposers.
Respiration by organisms returns carbon to the atmosphere and water.
Effects
We alter the carbon cycle by adding excess CO2 to the atmosphere through:
Burning fossil fuels.
Clearing vegetation faster than it is replaced.
Nitrogen Cycle
Moves atmospheric nitrogen (N2) into soils through several nitrogen fixation pathways.
Denitrifying bacteria release nitrogen gas back into the atmosphere.
Effects
Human activities (i.e., fertilizers) fix more nitrogen than all natural sources combined.
Adding nitrous oxide to the atmosphere through farming practices warms the atmosphere and depletes ozone.
Contaminating groundwater from nitrate ions in inorganic fertilizers.
Phosphorus Cycle
There is no atmospheric component in the phosphorus cycle.
Effects
Large amounts of phosphate removed from earth to make fertilizer.
Reduction of phosphorus in tropical soils by clearing forests.
Addition of excess phosphates to aquatic systems from runoff of animal wastes and fertilizers.
Sulfur Cycle
Sulfur exists as rocks and as they get weathered, they release sulfate ions (SO42−) that producers take up and pass through the food web.
Sulfur dioxide combines with water to form sulfuric acid (H2SO4) and is carried back to Earth when it rains or snows.
SUCCESSION
Ecological succession
The predictable replacement of one group of species by another group of species over time.
Primary succession
occurs in areas devoid of soil.
Early-arriving plants and algae colonize bare rock and begin to form soil, making the site more hospitable for other species to colonize later.
Secondary succession
occurs where soil is present, but all plants have been removed
Species
Pioneer species
Moves and colonize into unoccupied habitat and adapt to its particular conditions.
Eg: moss, fungi, bacteria
Keystone species
Species whose activities have a significant role in determining community structure.
Eg: beavers, wolves, elephants
Indicator species
A plant or animal that, by its presence, abundance, or scarcity, demonstrates that some character or quality of an ecosystem is present.
Species that serve as early warnings of damage to a community or an ecosystem.
Eg: frogs, starfish, trout
Foundation Species
create and enhance habitats that can benefit other species in a community.
Eg: elephants pushing/breaking trees to create space
Resistance
Measure of how much a disturbance can affect flows of energy and matter in an ecosystem.
Resilience
Rate at which an ecosystem returns to its original state after a disturbance.
Restoration ecology
Study and implementation of restoring damaged ecosystems.
Ecological Tolerance: the range of environmental conditions that an organism can survive in before becoming stressed or dying
Niche
Niche specialist
A species specialized to live in a specific habitat or feed on a small group of species.
Niche generalist
A species that can live under a wide range of abiotic or biotic conditions.
Watershed
Help us understand how disturbances affect ecosystem processes
All land in a given landscape that drains into a particular stream, river, lake, or wetland.
Intermediate Disturbance Hypothesis
Ecosystems experiencing intermediate levels of disturbance are more diverse than those with high or low disturbance levels.
Productivity
Primary Productivity
Rate at which solar energy (sunlight) is converted into organic compounds via photosynthesis over a unit of time.
Gross primary productivity (GPP)
Total amount of solar energy that producers capture via photosynthesis over a given amount of time.
Net primary productivity (NPP)
Energy captured by producers minus the energy producers respire (R).
NPP = GPP – R
Levels of organization
Individual
One organism
Population
Individuals that belong to the same species and live in a given area at a particular time
Community
All populations of organisms within a given area
Ecosystem
A particular location on Earth with interacting biotic and abiotic components.
Biosphere
Our planet where life resides; combination of all ecosystems.
Levels of organization
Individual
Population
Community
Ecosystem
Biosphere
Symbiotic Relationships
Mutualism
interaction between two species that increases the chances of survival for reproduction for both species.
Commensalism
relationship in which one species benefits and the other species is neither harmed nor helped.
Competition
struggle of individuals to obtain a shared limiting resource.
Predation
interaction in which one animal kills and consumes another animal.
Parasitism
interaction in which one organism lives on or in another organism.
Trophic Levels
Producers
like plants and algae, make their own food using sunlight through photosynthesis.
Primary consumers
such as herbivores, eat producers to gain energy.
Secondary consumers
like carnivores or omnivores, eat primary consumers.
Tertiary consumers
top predators that feed on secondary consumers.
Decomposers
like fungi and bacteria, break down dead organisms, and recycle nutrients back into the ecosystem.
Terrestrial Biomes
Tundra
Boreal forest
Temperate rainforest
Temperate seasonal forest
Woodland/shrubland
Temperate grassland/cold desert
Tropical rainforest
Tropical seasonal forest/savanna
Subtropical desert
Age-Structure Diagrams
Visual representation of the number of individuals within specific age groups for a country
Some are called population pyramids.
Populations with a large proportion of its people in the pre-reproductive stage have a large potential for rapid population growth.
Age Trends
Prereproductive (ages 0 -14)
Reproductive (ages 15 - 44)
Postreproductive (ages 45 and older)
The number of young, middle, and older age groups determines how fast populations grow or decline.
The number younger than age 15 is the major factor determining a country’s population growth.
DEMOGRAPHIC TRANSITION
Theory of demographic transition
As a country moves from a subsistence economy to industrialization and increased affluence, it undergoes a predictable shift in population growth. Generally, both birth and death rates decline.
Phase 1: Pre-industrial
Because high CBR (crude birth rate) and high CDR (crude death rate) offset each other, population growth is slow.
Phase 2: Industrializing
Rapid population growth because CBR remains high but CDR declines due to better sanitation, clean drinking water, availability of food and health care.
Phase 3: Industrialized
Stable population growth as the economy and education system improve and people have fewer children.
Phase 4: Post-industrial
Declining population growth because high levels of affluence and economic development encourages women to delay having children.
Demographic trap
When death rates rise in a developing nation
Occurring in Africa as a result of the HIV/AIDS epidemic.
The nation becomes trapped in Stage 2, and often reverts back to Stage 1.
Solutions
Elevating the social and economic status of women
Fertility is strongly related to female education in many developing countries.
Family control: Regulating the number of offspring through the use of birth control
Reducing poverty
India’s Failed Family Planning Program
Poor planning
Bureaucratic inefficiency
Low status of women
Extreme poverty
Lack of administrative financial support
Disagreement over the best ways to slow population growth
China’s Family Planning Program
One child policy
More food
Larger pensions
Free health care
Salary bonuses
Free school tuition
China’s TFR decreased from 5.7 to 1.6 children.
Negative Effects of the One-Child Policy
Millions had to endure strict enforcement
forced sterilization and forced abortion.
Births of additional children were undocumented
leading to many problems later on for those children
Sons were generally preferred over daughters
China’s birth and fertility rates remained low, leaving the population aging too rapidly and a shrinking workforce.
HUMAN POPULATION
Population boom
Expansion of agriculture
Industrial production
Lower death rates from improvements in hygiene, sanitation, and medicine
Factors that drive population growth
Population size
Birth and death rates
Fertility
Life expectancy
Migration
Doubling time
The number of years it takes a population to double.
Crude birth rate (CBR)
Births per 1000
Crude death rate (CDR)
Deaths per 1000
TFR (total fertility rate)
estimate of the average number of children that each woman will bear throughout her childbearing years.
Replacement level fertility
the total fertility rate required to offset the average number of deaths in a population to maintain the current population size.
Developed countries = 2.1
Developing countries = 2.5
Immigration
the movement of people into a country or region, from another country or region.
Emigration
the movement of people out of a country or region
IMPACTS OF POPULATION
Increase in population:
More hunger
More poverty
More disease
More depletion of resources
More habitat destruction
Less living space
Hunger
hunger: an aching desire for food
starvation: suffering or death from being deprived of nourishment
famine: widespread starvation
Poverty Cycle
Poverty → Undernutrition & malnutrition → Decreased energy → Decreased resistance to disease → Reduced ability to learn and work → Results in more poverty
Disease
Diseases spread more rapidly among dense populations
availability of clean water and sanitation
Poor sanitation can lead to cholera, dysentery, hepatitis, etc.
Resources
Freshwater
Energy
for electricity, heating, and transportation
Minerals
Greater demands on mineral resources for manufactured goods.
Living Space
The movement of people from rural areas to the cities is called urbanization.
Emigration out of the city into the suburbs is urban sprawl.
Habitat Destruction
More land cleared for agriculture/grazing destroying forest and grassland habitats.
Water resources drained to provide drinkable water.
Mining destroys other habitats.
POPULATION DYNAMICS
Population size (N)
Total number of individuals within an area at a given time.
N = births + immigration - deaths - emigration
Carrying capacity
maximum population of a given species that a particular habitat can sustain indefinitely without being degraded.
Population density
The number of individuals per unit area at a given time.
Population density = population size ÷ area
Sex ratio
The ratio of males to females in a population.
Population Size Factors
Density-dependent factor
A factor that influences an individual’s probability of survival and reproduction in a manner that depends on the size of the population.
Density-independent factor
A factor that has the same effect on an individual’s probability of survival and the amount of reproduction at any population size.
Population Distribution
How individuals are distributed with respect to one another
Clumped
Better protection from predators
Temporary groups for feeding and caring for their young
Most common
Uniform
Trees in plantation
Adequate sharing of light and water
Random
Dispersed with no pattern
Trees in a natural forest grow where seeds are scattered through wind and birds
Least common
POPULATION GROWTH
Opposing Forces
Biotic potential
Amount the population would grow if there were unlimited resources in its environment
Environmental resistance
Limiting factors that act together to limit the growth of a population
Population Growth Curves
Exponential
Logistic
Exponential Growth Model
Intrinsic growth rate (r)
Maximum potential for growth of a population under ideal conditions with unlimited resources.
Population is not limited by resources
Creates a J-shaped growth curve
Growth is independent of population density
Logistic Growth Model
Carrying capacity (K) = How many individuals the environment can sustain.
As population grows, resources become scarce.
Creates an S-shaped curve
Growth is dependent on population density
Overshoot
When population becomes larger than the environment’s carrying capacity.
Die-off
Rapid decline in a population due to death.
Predator/Prey Cycle
A predator and its prey populations fluctuate with each other.
Boom/Bust Cycle
If there’s a boom in the population beyond the carrying capacity, it’s followed by a bust.
Reproductive Strategies
R-strategists
Species with high intrinsic growth rate- often leads to population overshoots and die-offs.
Large number of small offspring with little parental care
K-strategists
Species with low intrinsic growth rate causing the population to increase slowly until it reaches carrying capacity.
Few, large offspring with invested parental care
Survivorship Curves
A survivorship curve is a graph that represents the distinct patterns of species survival as a function of age.
Type I Survivorship Curve
High survival early in life, with most deaths occurring in old age (eg. humans)
Type II Survivorship Curve
Constant death rate throughout life (eg. birds)
Type III Survivorship Curve
High mortality early in life, but survivors live long (eg. trees)
ATMOSPHERE
The Atmosphere
A fluid ocean of air that surrounds and protects the earth.
99% of the total mass of the atmosphere is within 20 miles of earth’s surface.
It has a weight of 14 psi
The earliest atmosphere of the lighter elements hydrogen and helium likely escaped out into space.
Today’s oxygen-rich atmosphere that sustains life was first produced by bacteria
Nitrogen (78%) and oxygen (21%) make up 99% of the atmosphere.
Aerosols are tiny droplets of liquids.
Layers of Atmosphere
Troposphere
The layer closest to the surface of Earth, extending up to 10 miles
Made up mostly of oxygen and nitrogen
Where all the weather occurs
The temperature decreases as altitude increases
Stratosphere
Stable, very dry, no weather
extending 10–31 miles above the surface of Earth.
Ozone in the stratosphere absorbs some of the sun’s high-energy UV radiation protecting life from the harmful rays.
Mesosphere
The atmosphere’s coldest layer extends about 31-50 miles above earth’s surface.
Meteors burn up in this layer
Thermosphere
Beginnings of outer space
UV radiation reacts with layer of ionized gases and air particles which become electrically charged, creating the “Northern Lights” or aurora borealis.
Exosphere
The outermost layer that blends into outer space.
Only hydrogen, helium, and trace oxygen.
SEASONS
Latitude
The distance north or south of the equator.
Latitude is divided into increments of:
degrees, minutes, and seconds.
Longitude
The distance east or west of a fixed point.
The lines of longitude are called meridians.
Prime Merdian
imaginary line of longitude that divides the Earth into the Eastern and Western Hemispheres
runs north and south through Greenwich, England.
Parallels
Circles north and south of the equator
0° is the equator. 90°N and 90°S are at the poles.
Movement
Rotation
Spinning on its axis every 24 hours
Revolution
One trip around the sun
It takes 365.24 days for one complete revolution
Earth’s Angle
Its axis is tilted 23.5 °
Earth’s orbit is slightly elliptical so it’s not always the same distance from the sun.
Warming is not across the planet because of it’s angle
Some areas of Earth reflect more solar energy than others.
Earth’s tilt produces predictable seasons.
Tropical regions near the equator receive more solar energy than mid-latitude and polar regions, where the Sun’s rays strike Earth’s surface at an oblique angle.
Reflection
Albedo
percentage of the incoming solar energy reflected
Whiter objects (snow and ice) reflect more solar energy
Darker objects (forests and asphalt) reflect little and absorb much solar energy
This is an example of positive feedback
Day’s
Earth is closest to the sun at perihelion. (Jan. 3)
Earth is farthest from the sun at aphelion. (July 4)
Summer solstice (June 21 or 22) – The day with the most daylight.
Winter solstice (Dec. 21 or 22) – The day with the least daylight.
Autumnal Equinox (September 22 or 23) –Equal day and night.
Vernal Equinox (March 21 or 22) –Equal day and night.
ENSO
Layers
Thermocline
the transition layer between warmer mixed water at the surface and cooler deep water below
Warm water, like warm air, expands and rises.
Ocean Currents
Affected by:
Temperature
Gravity
Prevailing Winds
Coriolis effect
Locations of continents
Gyre
A large-scale pattern of water circulation that moves clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere.
Oceanic circulation patterns
the result of differential heating, gravity, prevailing winds, the Coriolis effect, and the locations of continents.
ENSO
El Niño–Southern Oscillation (ENSO)
A reversal of wind and water currents in the South Pacific Ocean.
Every 3-7 years, the interaction of the Earth's atmosphere and ocean causes surface currents in the tropical Pacific Ocean to reverse direction.
Upwelling
the upward movement of ocean water toward the surface of diverging currents.
Brings cool and nutrient-rich water from the bottom of the ocean to the surface
Disease
Wetter conditions
Increasing mosquito breeding grounds
Flooding creates sanitation problems
Warmer water
bacterial growth increases in warm water
Warmer water increases insect breeding
Higher temperatures
Insects get a longer window of reproductive time
Insects normally killed by cold temperatures continue to live
Drier conditions
Causing streams to become stagnant
Stagnant water increases mosquitos
Drought
Less fresh water
Pollution gets concentrated in shallow ponds increasing diseases like cholera.
Normal Conditions | El Niño Conditions |
(a) In a normal year, trade winds push warm surface waters away from the coast of South America and promote the upwelling from the ocean bottom. | (b) In an El Niño year, trade winds weaken or reverse direction, so warm waters build up along the west coast of Peru. |
Normal Conditions in the Pacific
| El Nino Conditions in the Pacific
|
PLATE TECTONICS
History
Pangea
Alfred Wegener proposed a hypothesis called continental drift in 1912
Began breaking up 200 million years ago
Mesosaurus
Extinct reptile found in South America and Western Africa
Glossopteris
Ancient extinct plant
Earth’s layers+
Core, Mantle, Crust
Convection currents in the mantle produce the force which move the crust
Causes earthquakes and volcanoes
Fault
fracture in rock caused by a movement of Earth’s crust.
Seismic Activity
The frequency and intensity of earthquakes experienced over time.
Fault Zone
A large expanse of rock where a fault has occurred.
Hot Spots
As the Pacific Plate moves over a hot spot under a mantle plume, a series of volcanic eruptions formed the Hawaiian Islands.
Plate Boundaries
Divergent plate boundaries, plates move apart.
Molten rock rises and fills the space between the plates as the plates move apart
This causes mid-ocean ridges
Eg. Mid-Atlantic Ridge.
Transform fault boundaries, plates slide past each other.
Where two plates are grinding past each other.
An earthquake occurs when stress overcomes a locked fault, releasing stored energy.
Eg. San Andreas fault in California
Convergent plate boundaries, plates collide.
Continental crust vs. Continental crust
There is uplifting creating mountains like the Himalayas.
Oceanic crust vs. Continental crust
a subduction zone on the ocean floor.
OC is denser than CC
Oceanic crust vs Oceanic crust
The subducted plate melts, the molten rock rises along the trench
forms a chain of volcanic islands called an island arc.
(e.g. Aleutian Islands in Alaska)
ROCKS
The geologic cycle governing the constant formation, alteration, and destruction of rock material that results from tectonics, weathering, and erosion, among other processes.
Three types of rock are:
Igneous
Directly from molten magma
Intrusive igneous rock: magma rises up and cools in a place underground.
Extrusive igneous rock: magma cools above the surface of Earth.
Sedimentary
Compression of sediments
Hold fossil records
Metamorphic
Exposure to high temperatures and pressures
subjected to high temperature and pressure.
Exposed Rock
Weathering
Physical weathering: mechanical breakdown of rocks and minerals.
Chemical weathering: breakdown of rocks and minerals by chemical reactions the dissolving of chemical elements from rocks, or both.
Erosion
physical removal of rock fragments from a landscape or ecosystem.
result of two processes:
Wind, water, and ice move materials downslope.
Living organisms burrow under the soil.
SOIL
A renewable resource
Made out of:
Eroded rock
Mineral nutrients
Decaying organic matter
Water
Air
Billions of living organisms (microscopic decomposers)
Function:
A medium for plant growth
A habitat for living organisms
Breaks down organic material
A filter for water
Processes
Infiltration
downward movement of water through soil
Leaching
as water infiltrates down, it dissolves various minerals and organic matter in upper layers and carries them to lower layers
Soil Formation Factors
Parent material
underlying rock material from which the inorganic components of a soil are derived.
Climate
Topography
Organisms
Time
Soil Horizons (5)
O Horizon
Surface litter
Humus: most fully decomposed organic matter in the lowest section of this horizon
A Horizon
Topsoil
E Horizon
Zone of leaching
B Horizon
composed primarily of mineral material with very little organic matter.
C Horizon
Parent material
Least weathered soil horizon
SOIL PROPERTIES
Properties of soil
Physical: texture, porosity
Chemical: pH, N, P, K
Biological: bacteria, snails, insects, earthworms
Physical Properties
Soil Texture
Determined by % of sand, silt, clay
LOAM
40% sand, 40% silt, 20% clay
Soil Permeability
Determined by soil texture
Sand
Drains easily and quickly
Low water-holding capacity, therefore it must be watered more frequently.
Low nutrient-holding capacity, so it must be fertilized more often.
Highly susceptible to wind and water erosion
Silt
Medium size particles
Forms crust, which is often hard.
Created when rock is eroded, or worn away, by water and ice
Promotes water retention and air circulation
Clay
High water-holding capacity
High nutrient-holding capacity
Poor drainage
Waterlogged soil results in the roots being deprived of oxygen and other nutrients
Crusting and cracking are common
Difficult to work because it is so sticky
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Biological Properties
Reflects how well-suited a soil is to support life
Earthworms
Fungi and Bacteria
Microorganisms
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Nitrogen
responsible for plant growth
In Amino acids = make proteins
Required for enzyme reactions
Phosphorus
Major component of DNA & RNA
Root development
Crop maturity
Seed production
Potassium
Indirect role in plant growth (activates over 80 enzymes)
Helps plants withstand extreme temps
Helps plants fight drought and pests
Increases water use efficiency
Transforms sugars into starch
SOIL CONSERVATION
Techniques
Terracing
making “steps” to slow soil erosion down a slope
Contour Planting
plowing and planting crops in rows across the slope rather than up and down the slope
Strip Cropping
planting alternating strips of a row crop and another crop (cover crop) that completely covers the soil.
Alley Cropping
a crop is planted in an alley between trees and shrubs.
Conservation Tillage
involves special machines that drill seeds directly through crop residues into the undisturbed soil
Crop Rotation
plant a nutrient-depleting crop one year and a nutrient-enriching crop the next year
Soil Nutrients
Organic fertilizer: made from plant or animal wastes.
Green manure: growing plants that are plowed back into the soil.
Compost: decayed organic matter
Inorganic fertilizer
Adds no humus (organic matter)
Releases greenhouse gases
Runoff produces water pollution
Salinization
when water evaporates and leaves behind its salts.
Salt tolerant crops = cotton
Desertification
when the productive potential of drylands falls by 10% or more
MEAT & FISH
Meat
Feedlots are used to fatten up cattle before slaughter.
Concentrated Animal Feeding Operation (CAFO)
Large indoor or outdoor structure designed for maximum output.
Less Meat Consumption
Reduce CO₂, methane, and NO2 emissions
Reduce the use of antibiotics and growth hormones
Conserve water
Improve topsoil
Fish
Aquaculture
Farming aquatic organisms such as fish, shellfish, and seaweeds.
Pros:
Provide for more people
Cons:
Concentrate waste
Escaped fish compete/breed with wild fish.
Increase in disease transmission
Fishery
Commercially harvestable population of fish within a particular ecological region.
Fishery Collapse
Decline of a fish population by 90 percent or more.
Bycatch
Unintentional catch of nontarget species while fishing.
WATER
Importance
Global health issue
Economic issue
Women & children issue
National & global security issue
Environmental issue
Freshwater
Only 0.024 % of the earth’s water supply is readily available as liquid freshwater.
Surface water: lakes, rivers, streams, oceans
Groundwater: Underground water (aquifers)
Aquifer = permeable layer of rock and sediment that contains groundwater.
Other Waters
Water table
The uppermost level at which the water in a given area fully saturates rock or soil.
Groundwater recharge
A process by which water percolates through the soil and goes to an aquifer.
Spring
A natural source of water formed when water from an aquifer percolates up to the ground surface.
Artesian well
A well created by drilling a hole into a confined aquifer.
Cone of depression
An area lacking groundwater due to rapid withdrawal by a well.
Saltwater intrusion
Infiltration of salt water in an area where groundwater pressure has been reduced from extensive drilling of wells.
AGRICULTURE
Green Revolution (1950-67)
A shift in agricultural practices that included:
Mechanization
Fertilization
Irrigation
Pesticides
Improved crop varieties
All these increased food output
Crops+
The big three: Wheat, Corn, Rice
Monocropping
large plantings of a single species or variety
Cash crops
cotton, coffee, sugarcane, bananas
Fertilizers
Organic
Organic matter from plants/animals
Synthetic
Made with fossil fuels
Aka inorganic fertilizer
Chemicals
Pesticide
A substance, either natural or synthetic, that kills or controls pests.
Insecticide
A pesticide that targets species of insects that consume crops.
Herbicide
A pesticide that targets plant species that compete with crops.
The pesticide treadmill
pest populations evolve resistance to pesticides, which requires farmers to use higher doses or to develop new pesticides.
Unsustainable
Tilling
Slash-and-burn farming
Overuse of fertilizers
Genetic engineering
Greater yield
Greater food quality
Reductions in pesticide use
Reduction of world hunger by increased food production
Increased profits
Integrated Pest Management (IPM)
Cultivation practices: Each year crops are rotated to other locations
Biological methods: Natural predators and parasites are used
Chemical methods: Limited amounts of pesticides can be applied.
Pros
Reduces pesticide use
Reduces pest control costs
Does not reduce crop yield or food quality
Reduces fertilizer needs
Reduces pollution
Cons
Requires expert knowledge of the pest situation
Takes more time to become effective
The control measures in one area may not be effective in another area
Initial costs may be higher, but long-term costs are lower
Resisted by pesticide manufacturers
Solutions
An additional sales tax is applied to pesticides
An IPM demonstration farm is set up in each county
Train USDA personnel in the use of IPM
Green Revolution (1950-67)
Shift in Practices: Mechanization, fertilization, irrigation, pesticides, improved crop varieties → Increased food output.
Crops
Big Three: Wheat, corn, rice.
Monocropping: Single species planting.
Cash Crops: Cotton, coffee, sugarcane, bananas.
Fertilizers
Organic: Plant/animal matter.
Synthetic: Fossil fuel-based (inorganic).
Chemicals
Pesticides: Kill/control pests.
Insecticides: Target insects.
Herbicides: Target weeds.
Pesticide Treadmill: Resistance → higher doses/new pesticides.
Unsustainable Practices
Tilling, slash-and-burn farming, overuse of fertilizers.
Genetic Engineering
Higher yields, better quality, less pesticide use, reduces hunger, higher profits.
Integrated Pest Management (IPM)
Cultivation: Rotate crops yearly.
Biological: Use natural predators/parasites.
Chemical: Minimal pesticide use.
IPM Pros
Less pesticide use/costs.
Maintains yield/quality.
Reduces fertilizer needs/pollution.
IPM Cons
Needs expertise.
Slow effectiveness.
Location-dependent.
Higher initial costs.
Solutions
Pesticide sales tax.
IPM demo farms.
Train USDA personnel
IRRIGATION & CONSERVATION
Methods
The largest human use of freshwater is for irrigation (70%).
Irrigation techniques include:
Drip irrigation
uses perforated hoses to release small amounts of water to roots
This system is the most efficient
Expensive, not used often
Flood irrigation
involves flooding an agricultural field with water
can lead to waterlogging of the soil.
Furrow irrigation
Involves cutting furrows (trenches) between crop rows and filling them with water.
This system is inexpensive
Spray irrigation
pumping groundwater into spray nozzles across an agricultural field
more efficient than flood and furrow irrigation
LEPA (Low Energy Precision Application) sprinklers spray water directly onto crop.
Water Conservation
Tiered water-pricing systems
A water allocation system that charges rates that increase with the amount of water consumed.
Xeriscaping
Landscaping that removes water-intensive vegetation from lawns and replaces it with more water-efficient native landscaping.
Hydroponic agriculture
The cultivation of plants in greenhouse conditions by immersing roots in a nutrient-rich solution.
Requires little or no pesticide use.
Uses up to 95% less water than traditional irrigation.
Crops can be grown year-round.
Graywater: Wastewater from baths, showers, bathrooms, and washing machines.
Saltwater → Freshwater
Desalination The process of removing the salt from ocean water.
Distillation: A process of desalination in which water is boiled and the resulting steam is captured and condensed to yield pure water.
Reverse osmosis: A process of desalination in which water is forced through a thin semi-permeable membrane at high pressure.
Irrigation Methods
Drip Irrigation: Most efficient; perforated hoses deliver water to roots; expensive.
Flood Irrigation: Floods fields; can cause soil waterlogging.
Furrow Irrigation: Trenches between crops filled with water; inexpensive.
Spray Irrigation: Groundwater sprayed via nozzles; more efficient than flood/furrow.
LEPA Sprinklers: Low-energy sprinklers spray water directly onto crops.
Water Conservation
Tiered Pricing: Higher rates for higher water use.
Xeriscaping: Replacing water-intensive lawns with native, drought-resistant plants.
Hydroponics: Plants grown in nutrient solutions; uses 95% less water, no pesticides, year-round growth.
Graywater: Reused water from baths, sinks, and washing machines.
Desalination
Distillation: Boiling water and condensing steam into freshwater.
Reverse Osmosis: Forcing water through semi-permeable membranes to remove salt.
LAND USE
Harvest Practices
Clear-cutting: Removing all or almost all of the trees within an area.
Selective cutting: Removal of single trees or a relatively small number of trees from the larger forest.
Ecologically Sustainable Forestry: Removing trees from forests in ways that do not unduly affect the viability of other noncommercial tree species. The goal is to maintain both plants and animals in as close to a natural state as possible.
Fire
Fires are a natural process for recycling nutrients
Prescribed Burn: fire deliberately set under controlled conditions to reduce the accumulation of dead biomass on a forest floor. Prescribed burns help reduce the risk of uncontrolled natural fires.
Rangeland
Dry open grasslands used for grazing cattle.
Grazing too many animals can quickly denude a region of vegetation.
Loss of vegetation can lead to land exposed to wind and water erosion.
We especially should manage riparian zones (the edges of streams and rivers).
Protected Lands
National WIldlife Refuge: A federal public land managed for the primary purpose of protecting wildlife.
National Wilderness Area: An area set aside with the intent of preserving a large tract of intact ecosystem or landscape.
National Parks: Managed for scientific, educational, and recreational use. Human overuse can harm the environmental features that attract visitors.
Urbanization
Suburb An area surrounding a metropolitan center, with a comparatively low population density.
Exburb An area similar to a suburb, but unconnected to any central city or densely populated area.
Urban Sprawl Urbanized areas that spread into rural areas, removing clear boundaries between the two.
Urban blight The degradation of built and social environments of a city that accompanies and accelerates migration to the suburbs. Positive feedback loop
Sources of Urban Sprawl
Automobiles and highway construction
Land costs
Governmental policies
Urban Blight
Solutions
Smart Growth A set of principles for community planning that focuses on strategies to encourage the development of sustainable, healthy communities.
Smart Growth Principles
Create mixed land uses.
Create a range of housing opportunities and choices.
Create walkable neighborhoods.
Encourage community and stakeholder collaboration in development decisions.
Take advantage of compact building design.
Foster distinctive, attractive communities with a strong sense of place.
Preserve open space, farmland, natural beauty and critical environmental areas.
Provide a variety of transportation choices.
Strengthen and direct development toward existing communities
Make development decisions predictable, fair and cost-effective
Harvest Practices
Clear-Cutting: Removes nearly all trees in an area.
Selective Cutting: Removes specific trees, minimizing impact.
Ecologically Sustainable Forestry: Maintains biodiversity and natural habitats.
Fire Management
Natural Fires: Recycle nutrients.
Prescribed Burn: Controlled fire to reduce biomass and prevent uncontrolled fires.
Rangelands
Use: Grasslands for grazing cattle.
Risks: Overgrazing causes erosion and vegetation loss, especially near riparian zones.
Protected Lands
National Wildlife Refuge: Protects wildlife.
National Wilderness Area: Preserves ecosystems.
National Parks: Balances recreation, education, and conservation.
Urbanization
Suburb: Low-density areas near cities.
Exurb: Similar to suburbs but not city-connected.
Urban Sprawl: Expansion into rural areas, erasing boundaries.
Urban Blight: City degradation due to suburban migration.
Causes of Urban Sprawl
Automobiles, highways, land costs, urban blight, and policies.
Solutions
Smart Growth: Sustainable, healthy community planning.
Smart Growth Principles
Mixed land uses.
Diverse housing options.
Walkable neighborhoods.
Community collaboration.
Compact design.
Attractive, distinctive communities.
Preserve open spaces.
Transportation variety.
Focus on existing communities.
Predictable, fair development.
MINING
Ore A concentrated accumulation of minerals from which economically valuable materials can be extracted.
Metal An element with properties that allow it to conduct electricity and heat energy, and to perform other important functions.
Reserve In resource management, the known quantity of a resource that can be economically recovered. Where metals are
Smelting Heating the ore to release the mineral; produces air pollutants (especially SO2 which results in acid wastes). Chemical extraction is also done, but it results in many toxic wastes (like cyanide-laden water).
Depletion - the time it takes to use up a certain proportion (usually 80%) of the reserves of a mineral at a given rate.
Types of Mining
Surface mining for shallow deposits
Strip mining
Removal of large portions of soil and rock to expose ore
Mine tailings Unwanted waste material created during mining including mineral and other residues that are left behind after the desired metal or ore is removed.
Open-pit mining
Creates a large visible pit or hole in the ground.
Toxic water can accumulate at the bottom.
Mountaintop removal
A mining technique in which the entire top of a mountain is removed with explosives.
Resulting waste rock and dirt are dumped into the valleys and streams below.
Placer mining
The process of looking for minerals, metals, and precious stones in river sediments.
Subsurface mining for deep deposits (e.g., coal)
Mining techniques used when the desired resource is more than 100 m (328 feet) below the surface of Earth.
Coal, diamonds, and gold are some of the materials extracted by subsurface mining.
Effects of Mining
Enormous amounts of energy
Land disturbance
Toxic wastes
Soil erosion
Subsidence (cave in)
Air and water pollution
Solutions
Industrial Ecosystem
the wastes of one company are the raw materials of another company.
Waste less
Reuse existing supplies
Recycle
Find a substitute
Do without it
Key Terms
Ore: Concentrated minerals for economic extraction.
Metal: Conductive elements used in industry.
Reserve: Known recoverable resources.
Smelting: Heating ore to extract minerals; produces air and toxic waste pollutants.
Depletion: The time it takes to use up a certain proportion (usually 80%)
Types of Mining
Surface Mining: For shallow deposits.
Strip Mining: Removes soil/rock layers to expose ore; leaves waste (tailings).
Open-Pit Mining: Creates large pits; toxic water accumulates.
Mountaintop Removal: Explosives remove mountain tops; waste fills valleys/streams.
Placer Mining: Extracts minerals from river sediments.
Subsurface Mining: For deep deposits (e.g., coal, diamonds); >100 m below surface.
TYPES OF MINING
Surface Mining: For shallow deposits near the Earth’s surface.
Strip Mining: Removes large sections of soil and rock to expose ore; leaves behind mine tailings (unwanted waste materials).
Open-Pit Mining: Creates a large, visible pit or hole in the ground; toxic water often accumulates at the pit’s bottom.
Mountaintop Removal: Entire mountain tops are removed with explosives; waste rock and debris are dumped into nearby valleys and streams, causing environmental damage.
Placer Mining: Extracts metals and precious stones from river sediments using water to separate heavier materials like gold and diamonds.
Subsurface Mining: For deposits more than 100 meters (328 feet) below the surface.
Techniques: Involves creating tunnels or shafts to reach deep resources.
Materials Extracted: Commonly used for coal, diamonds, and gold.
Challenges: Risk of mine collapses, subsidence, and significant energy use.
Effects of Mining
High energy use, land disturbance, soil erosion, toxic wastes, air/water pollution, and subsidence.
Solutions
Industrial Ecosystem: The wastes of one company are the raw materials of another company. .
Conservation: Waste less, reuse, recycle, find substitutes, or do without.