Comprehensive Study Notes: Environmental Science and Global Change

1.1: Introduction to Ecosystems

  • Ecosystem: A community of living (biotic) organisms interacting with the non-living (abiotic) components of their environment as a system through various nutrients and energy cycles.

  • Organism: A living thing that can function on its own.

  • Species: Organisms that resemble each other; are similar in genetic makeup, chemistry, and behavior; and are able to interbreed and produce fertile offspring.     * Interspecific: Means between different species.

  • Population: Organisms of the same species that interact with each other and occupy a specific area.

  • Community: Population of different species.

  • Ecological Niche: A particular area within a habitat occupied by an organism, as well as its function within its community.     * Physical environment: Influences how organisms affect and are affected by resources and competitors.     * Niche: Reflects specific adaptations acquired through evolution.     * Niche Characteristics: Habitat, interactions with living/nonliving factors, role in the food web, and types/amounts of resources available.

  • Symbiosis: Close and long-term biological interaction between two different organisms of the same or different species.     * Amensalism: One species suffers while the other is unaffected (e.g., black walnut tree releasing chemicals that kill neighboring plants).     * Commensalism: One organism benefits while the other is unaffected. Forms include transportation, housing, or using something created by another.     * Competition: Driving force of evolution for food, mating, or territory.         * Intraspecific: Between members of the same species.         * Interspecific: Between members of different species.     * Mutualism: Both species benefit.     * Parasitism: One species benefits while the other is harmed.     * Predation: Predators hunt and kill prey.         * Opportunistic: Kill and eat almost anything.         * Specialist: Prey only upon certain organisms.     * Saprotrophism: Saprotrophs obtain nutrients from dead/decaying matter through absorption of soluble organic compounds.

  • Law of Tolerance: States that the existence, abundance, and distribution of species depend on the tolerance level of each species to physical and chemical factors.

  • Limiting Factor: Any abiotic factor limiting population growth.     * Terrestrial factors: Soil nutrients, water, light, and temperature.     * Aquatic factors: pHpH, dissolved oxygen, light, and degree of salinity.

  • Predator-Prey Cycles: Based on feeding relationships; as prey population multiplies, predators increase until prey populations dwindle.

  • Resource Partitioning:     * Morphological partitioning: Species evolve different structures to use the same resource.     * Spatial partitioning: Competing species use the same resource in different areas.     * Temporal partitioning: Species use the same resource at different times.

1.2: Terrestrial Biomes

  • Biomes: Regional/global biotic communities characterized by dominant plant life and prevailing climate. Temperature and precipitation are the primary determinants.

  • Deserts: Defined by rainfall, not temperature.     * Rainfall: Less than 20inches20\,\text{inches} (50cm50\,cm) per year.     * Location: Between 1515^{\circ} and 3535^{\circ} north and south latitudes.     * Succulents: Store water in fleshy stems/leaves; have deep or shallow roots, open stomata at night, and waxy leaves to minimize transpiration.     * Cactus: Sharp spines for shade/defense; secrete toxins to prevent interspecific competition.     * Wildflowers: Dependent on water for germination; short life spans; store biomass in seeds.     * Animals: Small, nocturnal, and often spend time in underground burrows.     * Aestivation: A summer hibernation.

  • Forests: Cover 33%33\% of Earth's land (primarily North America, Russian Federation, South America); account for 75%75\% of gross primary productivity.     * Closed canopy: Tree crowns cover > 20\% of ground surface (80%80\% of biome).     * Open canopy: Tree crowns cover < 20\% of ground surface.

  • Tropical Rainforests: Near the equator; rainfall exceeds 80inches80\,\text{inches} (200cm200\,cm) annually. Soil is nutrient-poor due to rapid assimilation. Trees have buttressed trunks and large dark green leaves.

  • Temperate Deciduous Forests: Found in eastern North America, NE Asia, Europe. Temperature range: 20F-20^{\circ}F to 85F85^{\circ}F (30C-30^{\circ}C to 30C30^{\circ}C). Precip: 3060inches30-60\,\text{inches} (75150cm75-150\,cm). Fertile soil from decaying leaf litter.

  • Temperate Coniferous Forest: Mild winters, heavy rainfall. Conical trees shed snow; dark green needles absorb light and have thick waxy coatings to reduce transpiration.

  • Taiga (Boreal Forest): Largest terrestrial biome. Southern Taiga is evergreen conifer; Northern Taiga is more barren near the tundra. Soil is thin, acidic, and nutrient-poor.

  • Grasslands:     * Savannas (Tropical): Scattered trees; rainfall 2050inches20-50\,\text{inches} (50130cm50-130\,cm) over 686-8 months, followed by drought.     * Temperate Grasslands: Hot summers, cold winters, moderate rainfall. Examples: veldts (S. Africa), pampas (Argentina), steppes (Russia), plains/prairies (N. America). Fertile soil from deep multi-branched roots.

  • Tundra:     * Arctic Tundra: Cold, desert-like around the North Pole. Features permafrost (permanently frozen subsoil). Growing season averages 50days50\,\text{days}. Precipitation 610inches6-10\,\text{inches} (1525cm15-25\,cm).     * Alpine Tundra: High altitudes on mountains where trees cannot grow. Growing season is roughly 180days180\,\text{days}; night temps fall below freezing.

1.3: Aquatic Biomes

  • Water Properties: High thermal capacity; buoyancy reduces need for legs/trunks; screens UV radiation; effective dispersal of gametes.

  • Antarctic: Coldest climate; interior averages 70F-70^{\circ}F (57C-57^{\circ}C). Sea is productive due to summer phytoplankton supporting large krill populations.

  • Marine: Oceans cover 75%75\% of Earth; salt concentration is roughly 3%3\%.

  • Ocean Circulation:     * Convection: Warm liquid rises, cool sinks.     * Thermohaline currents: Conveyor belt driven by temperature and salinity. Cold salty water sinks in the North Atlantic (Norwegian Sea), flows south, and rises in Pacific/Indian Oceans.

  • Ocean Zones:     * Littoral: Intertidal zone near shore.     * Neritic: Extends to continental shelf edge.     * Photic: Upper layer reaching 1%1\% sunlight depth.

  • Corals: Marine invertebrates living in colonies of polyps (exoskeleton made of calcium carbonate (CaCO3CaCO_3)). Energy comes from zooxanthellae dinoflagellates.     * Fringing reefs: Grow near coastlines, narrow lagoons.     * Barrier reefs: Parallel to coast, separated by deep/wide lagoons.     * Atolls: Rings of coral in the middle of the sea around sunken volcanoes.

  • Lakes: Standing freshwater.     * Zones: Benthic (bottom), Limnetic (well-lit open surface), Littoral (shallow near shore), Profundal (deep, dark, low oxygen).     * Oligotrophic: Young, deep, nutrient-poor, clear water.     * Mesotrophic: Middle-aged, moderate nutrients.     * Eutrophic: Old, shallow, nutrient-rich, murky, low oxygen.

  • Lake Stratification:     * Epilimnion: Sun-warmed surface layer.     * Hypolimnion: Cold, dense bottom layer.     * Thermocline: Thin middle layer with rapid temperature change.

  • Seasonal Turnover: Happens twice a year in fall and spring as water reaches its maximum density at 4C4^{\circ}C (39F39^{\circ}F), causing mixing of surface and bottom waters.

  • Wetlands: Areas covered by water part of the year.     * Ecological Services: Absorbing excess flood water, acting as carbon sinks, recharging groundwater, nurseries for fish.     * Degradation: Draining for agriculture (salinization/compaction), damming (blocking sediment), grazing (streambank destabilization), and invasive species (competing with natives).

  • Rivers and Streams:     * Source Zone: Cold, clear headwaters, high oxygen.     * Transition Zone: Slower, warmer, more sediment.     * Floodplain Zone: Murky, warm water; tributaries join to form rivers emptying into estuaries.     * Riparian Areas: Lands adjacent to water with hydrophilic vegetation.

1.4 - 1.7: Biogeochemical Cycles

  • Carbon Cycle: Building block of life (CO_2 < 1\% of atmosphere).     * Sinks: Forests (90%90\% of above-ground carbon), Oceans (phytoplankton/kelp), Sedimentary deposits (Limestone (CaCO3CaCO_3) is the largest reservoir).     * Human Impact: Combustion of fossil fuels/deforestation has increased oceanic acidity, slowing natural precipitation of calcium carbonate.

  • Nitrogen Cycle: Nitrogen makes up 78%78\% of the atmosphere.     * Nitrogen Fixation: N2N_2 converted to ammonia (NH3NH_3) or nitrate (NO3NO_3^-) by bacteria like Rhizobium or lightning.     * Nitrification: Ammonia (NH3NH_3) converted to nitrite (NO2NO_2^-) and nitrate (NO3NO_3^-).     * Assimilation: Plants absorb NH3NH_3, NH4+NH_4^+, and NO3NO_3^- via roots.     * Ammonification: Decomposers convert waste to ammonia (NH3NH_3) and ammonium ions (NH4+NH_4^+).     * Denitrification: Anaerobic bacteria convert ammonia back into N2N_2 and N2ON_2O.

  • Phosphorus Cycle: No atmospheric component. Primary sink is sedimentary rock. Released via weathering. Excess runoff from fertilizers leads to cyanobacteria/algae blooms and hypoxia.

  • Hydrologic Cycle:     * Oceans hold 97%97\% of water; source of 78%78\% of precipitation and 86%86\% of evaporation.     * Terms: Condensation, Evaporation, Evapotranspiration, Infiltration, Precipitation, Runoff.     * Aquifers: Confined (artesian) vs. Unsaturated zones. Water table is the level where ground is saturated.

1.8 - 1.10: Energy Flow and Productivity

  • Photosynthesis: Carbon dioxide and light energy used to produce carbohydrates. Plants absorb more CO2CO_2 than they emit, acting as net sinks.

  • Trophic Levels: Position in the food chain.

  • Second Law of Thermodynamics: Energy transfer results in waste (entropy).

  • 10% Rule: Only roughly 10%10\% of energy is transferred to the next trophic level; the rest is lost as heat.

  • Solar Energy Distribution:     * 35%35\% heats water/land and evaporates water.     * 15%15\% reflected to space; 80%80\% absorbed by Earth.     * 1%1\% of available solar energy used for photosynthesis.

  • Productivity:     * Gross Primary Production (GPP): Rate at which plants fix chemical energy as biomass.     * Net Primary Production (NPP): NPP=GPPRNPP = GPP - R (where RR is respiration).

2.1 - 2.7: Biodiversity and Ecosystem Change

  • Biodiversity Levels: Genetic, Species, and Ecosystem diversity.

  • Anthropogenic Loss: Burning fossil fuels (pHpH change from acid rain), Deforestation, Overfishing, Pesticides, and GMOs (decreased genetic variation).

  • Population Bottleneck: Large reduction in population size due to catastrophe, leading to loss of genetic diversity.

  • Species Types:     * Generalist: Varied diet, lives in many environments (e.g., raccoons).     * Specialist: Specific habitat/diet (e.g., giant panda).

  • Island Biogeography: Determined by immigration and extinction. Closer and larger islands have higher biodiversity.

  • Natural Disruptions:     * Volcanoes: Form soil, create early atmosphere, but sulfur gas can cool the troposphere by 23degrees2-3\,\text{degrees}.     * Wildfires: Clear dead vegetation, add nutrients via ash; some plants require fire for life cycles.

  • Sea Level Change: 30%30\% from glacier melt, 30%30\% from thermal expansion, 40%40\% from coastal land subsidence.

  • Ecological Succession:     * Primary: On barren land (e.g., lava) with no soil; takes > 1000\,\text{years}.     * Secondary: Recolonization after disturbance where soil exists; takes 50200years50-200\,\text{years}.     * Pioneer Species: Mature rapidly, short-lived, generalists (rr-strategists).

  • Species Roles:     * Keystone species: Essential for diversity (e.g., sea stars, grizzly bears).     * Indicator species: Reflect environmental health (e.g., lichens for air pollution, mosses for acidic soil).

3.1 - 3.9: Population Dynamics

  • r-Strategists: Many offspring, low parental care, mature rapidly, small, short-lived, Type III survivorship (e.g., insects).

  • K-Strategists: Few offspring, high parental care, stabilize near carrying capacity (KK), larger, long-lived, Type I or II survivorship (e.g., elephants, humans).

  • Survivorship Curves:     * Type I (Late Loss): Most deaths at the end of life span.     * Type II (Constant Loss): Uniform death rates.     * Type III (Early Loss): Prevalent death for young members.

  • Growth Curves:     * J-Curve: Exponential/logarithmic growth in new environments until crash.     * S-Curve: Slows and stabilizes at carrying capacity (KK) due to environmental resistance.

  • Rule of 70: Doubling time dt=70rdt = \frac{70}{r}, where rr is growth rate percentage.

  • Age-Structure Diagrams:     * Pyramid: High birth rates, growing population.     * Bell: Stable population.     * Urn: Declining population (post-reproductive group largest).

  • Demographic Transition:     * Stage 1 (Pre-Industrial): High birth/death rates, low growth.     * Stage 2 (Transitional): Death rates drop, population rises rapidly.     * Stage 3 (Industrial): Birth rate falls, growth slows.     * Stage 4 (Post-Industrial): Zero population growth.

4.1 - 4.9: Earth Systems and Resources

  • Plate Tectonics: Alfred Wegener's Pangaea theory (200million200\,\text{million} years ago).     * Convergent: Plates move together, forming subduction zones or orogenic belts (e.g., Cascade Mountains).     * Divergent: Plates move apart (e.g., Mid-Atlantic Ridge).     * Transform: Plates slide past (e.g., San Andreas fault).

  • Soil Layers: Surface Litter (O), Topsoil (A), Zone of Leaching (E), Subsoil (B), Weathered Parent Material (C).

  • Soil Texture: Gravel, Sand (coarse), Loam (mix of clay/sand/silt/humus), Silt (fine), Clay (very fine, low permeability).

  • Atmosphere Composition: Nitrogen (78%78\%), Oxygen (21%21\%), Water Vapor (04%0-4\%), Carbon Dioxide (< 1\%).

  • Atmosphere Structure:     * Troposphere: 06miles0-6\,\text{miles} (010km0-10\,km); where weather occurs; temperature decreases with height.     * Stratosphere: 630miles6-30\,\text{miles} (1050km10-50\,km); contains ozone (O3O_3); temperature increases with altitude.

  • Wind Patterns:     * Coriolis Effect: Causes winds to spiral clockwise (North) or counterclockwise (South).     * Hadley Cells: Near equator; high humidity and heavy rain.     * Polar Vortex: Low-pressure zone of cold air atop poles.

  • ENSO (El Niño/Southern Oscillation):     * El Niño: Trade winds weaken; warm water piles up off S. America; upwelling decreases/fish die.     * La Niña: Stronger trade winds; increased upwelling; cooler sea temperatures.

5.1 - 5.12: Land and Water Use

  • Tragedy of the Commons: Resource depletion in shared areas (Hardin, 1968).

  • Agriculture:     * Green Revolutions: 1st (fertilizers/pesticides); 2nd (GMOs like BT corn).     * Irrigation: Ditch, Drip (most efficient), Flood (cheap), Furrow, Spray.     * IPM (Integrated Pest Management): Combines biology/chemistry/physics to control pests; reduces bioaccumulation.

  • Meat Production: CAFOs (Concentrated Animal Feeding Operations) house large numbers; cause nitrogen/phosphorus pollution.

  • Urbanization: Movement to cities. Smart growth promotes mixed-use planning and greenbelts.

  • IPAT Formula: I=P×A×TI = P \times A \times T (Impact = Population ×\times Affluence ×\times Technology).

6.1 - 6.12: Energy Resources

  • Units: 1HP=746watts1\,HP = 746\,\text{watts}. kWh is billing unit.

  • Fossil Fuels:     * Coal Types: Lignite (brown coal), Bituminous (electric power), Anthracite (residential heating).     * Fracking: Injecting water/chemicals to fracture bedrock for gas.

  • Nuclear Power: U-235 fission. Control rods absorb neutrons; Moderator slows neutrons.

  • Renewables:     * Biomass: Anaerobic digestion produces methane.     * Solar: Passive (structural features) vs. Active (collectors/pumps).     * Hydroelectric: Dams provide 6.5%6.5\% of US electricity.     * Wind: Most efficient electricity production. One megawatt offsets 2,600tons2,600\,\text{tons} of CO2CO_2.

7.1 - 7.8: Atmospheric Pollution

  • Smog:     * Industrial (Gray): Sulfur-based from coal; forms sulfuric acid (H2SO4H_2SO_4).     * Photochemical (Brown): Nitrogen-based; catalyzed by UV radiation; forms ozone (O3O_3) and PANs.

  • Pollutants: CO, Lead, Nitrogen Oxides, Sulfur Dioxide, Particulate Matter (PMxPM_x), VOCs.

  • Acid Rain: Wet/dry deposition of sulfur/nitrogen oxides. Causes acid shock in lakes.

  • Urban Heat Island: Metropolitan areas warmer than surroundings due to lack of vegetation and heat absorption by asphalt.

8.1 - 8.7: Aquatic and Terrestrial Pollution

  • Eutrophication: Human-induced nutrient increase. Leads to algal blooms and hypoxia (DODO depletion).

  • Oil Spills: Microorganisms, dispersants, or skimming used for cleanup.

  • Water Testing: Alkalinity, BOD (approximate level of biodegradable waste), Coliforms (bacteria from intestines), Turbidity (light scattering).

  • Waste Disposal: MSW (trash), Hazardous, Radioactive.     * Sanitary Landfills: Waste isolated from environment.     * Incineration: Conversion to ash/heat.

9.1 - 9.6: Global Change

  • Ozone Depletion: Caused by CFCs/Halons in stratosphere. Montreal Protocol (1987) phased these out.

  • Greenhouse Gases: CO2CO_2 (fossil fuels), Methane (CH4CH_4 - agriculture/landfills), Nitrous oxide (N2ON_2O - fertilizers).

  • Global Warming Effects: Sea level rise from thermal expansion/melting ice. Arctic release of methane from permafrost creates a positive feedback loop.

  • Ocean Acidification: CO2CO_2 reacts with seawater to form carbonic acid; reduces ocean pHpH.

  • Invasive Species: High dispersal, generalist diet, rapid reproduction (e.g., Zebra mussels, Water hyacinth).

  • Endangered Species: High risk of extinction. Factors include specialized diet (Pandas), slow movement (Tortoises), or commercial value (Elephants, Rhinos).