Comprehensive Notes on Global Ecology, Thermodynamics, and Climate Change
The Laws of Thermodynamics in Biological Systems
- First Law of Thermodynamics (Law of Conservation of Energy): Energy can be transferred and transformed, but it cannot be created or destroyed.
- There is a finite amount of energy in the universe.
- Energy changes forms:
- Kinetic motion energy (turning a turbine/rotating a wire around a magnet) transforms into electrical energy.
- Chemical energy in the bonds of wood is released as light and heat energy when ignited.
- Second Law of Thermodynamics: Every energy transfer or transformation increases the disorder or entropy of the universe because no transformation is 100% efficient.
- In biological systems, energy is lost as heat during chemical reactions.
- When organisms burn complex molecules for energy, they produce simpler compounds like CO2 and water.
- Energy Transfer Efficiency (The 10% Rule): In food chains, there is typically a 90% reduction in available energy at each trophic level; only 10% of the energy is assimilated into the next level.
- If a Thompson's gazelle eats 100 units of grass energy, only 10 units become part of the gazelle.
- If a cheetah eats that gazelle, only 1 unit of the original grass energy makes it into the cheetah (1%—calculated as 100×0.1×0.1).
- If a lion eats the cheetah, only 0.1 units are available.
- This inefficiency limits the length of food chains; top predators (like lions eating cheetahs) are rare because of the extreme energy scarcity at the top.
Trophic Levels and Food Systems
- Producers: The base of all food systems. Usually plants, but at the bottom of the ocean, specialized bacteria utilize geothermal heat to synthesize complex compounds.
- Primary Consumers: Organisms that eat producers (e.g., grasshoppers).
- Secondary Consumers: Organisms that eat primary consumers (e.g., mice).
- Tertiary Consumers: Third-order consumers (e.g., snakes).
- Quaternary Consumers: Fourth-order consumers.
- Human Impact and Efficiency: There are approximately 7,500,000,000 humans. Humans are less efficient when eating at the top of the food chain.
- Feeding 1000 calories of corn to a cow produces only 100 calories of beef, which then provides only 10 calories to a human.
- Humans can support a larger population and reduce environmental impact by "eating lower" on the food chain (consuming plants directly).
Industrial Meat Production and CAFOs
- CAFOs (Confined Animal Feeding Operations): Intensive rearing systems where thousands or millions of animals are kept in confined, often windowless, dark conditions.
- High population density requires the use of gas masks by workers due to the smell of waste.
- These operations are often hidden from public view/photographers to obscure production methods.
- Environmental Hazards:
- Waste Management: Waste is stored in massive, non-natural, eutrophic sewage ponds high in Nitrogen and Phosphorus, which can leach into groundwater.
- Habitat Demand: Raising meat requires vast amounts of space and food, displacing native species.
- Human Health: Crowded conditions necessitate the use of antibiotics. This exerts strong selection pressure, leading to virulent bacteria strains (e.g., deadly E.coli).
- Methane Emissions: Livestock, particularly cattle, are the largest emitters of methane (CH4) on Earth.
- Enteric Fermentation: Cows have four stomach chambers where bacteria ferment food, releasing methane through burping.
- One Western cow emits 120kg (250lbs) of methane per year.
- Humans emit about 1,000 times less methane than a cow.
- Non-Western cattle (Africa/Asia) have been selected for higher efficiency and emit less methane.
Biomagnification and Toxins
- Biomagnification: The process whereby toxins become more concentrated at each successive level of a food web.
- Fat-Soluble Toxins: Compounds like mercury, pesticides, and PCBs (used in electronics) are sequestered in fat droplets and not easily excreted.
- Examples of Accumulation (Concentration in Parts Per Million, ppm):
- Phytoplankton (Producers): 0.025ppm of PCB.
- Zooplankton: 0.123ppm.
- Smelt: 1.04ppm.
- Lake Trout: 4.83ppm.
- Herring Gulls: 124ppm.
- Consequences:
- High concentrations in gulls lead to egg failure and species endangerment.
- Overfishing has led to smaller top predators; swordfish today are significantly smaller than specimens from 100 years ago.
- Health advisories warn pregnant women against eating top predators (tuna, swordfish, salmon) because mercury is a neurotoxin that affects fetal brain development.
- Eating lower on the food chain (sardines, herring) reduces toxin exposure.
Biogeochemical Cycles
- Definition: The movement of water, carbon, nitrogen, and phosphorus through the environment.
- Water Cycle: Involves evaporation (gas), condensation, and precipitation (liquid or ice).
- Carbon Cycle: Primarily atmospheric (CO2).
- Released via respiration (animals and plants), decomposition, and combustion of fossil fuels.
- Fossil Fuels: Carbon stores from organisms that died hundreds of millions of years ago, covered before they could rot.
- Humans are releasing millions of years of stored carbon into the atmosphere in a span of only 150 to 200 years.
The Greenhouse Effect and Albedo
- Mechanism: The sun sends short-wavelength light and heat energy through the atmosphere. This energy is absorbed by the Earth and re-radiated as long-wavelength infrared light.
- Greenhouse Gases (GHGs): Molecules like CO2, CH4 (methane), and Nitrous Oxide (N2O) trap long-wavelength radiation, bouncing it back to Earth.
- Methane Efficiency: Methane is approximately 20 times more efficient at trapping heat than CO2.
- Albedo Effect: The reflectivity of a surface.
- High Albedo: Ice caps and white clouds reflect radiation back into space, cooling the Earth.
- Low Albedo: Dark vegetation and deep ocean water absorb heat.
- Positive Feedback Loop: As ice melts, it reveals dark ocean, which absorbs more heat, causing more ice to melt.
Climate Change Evidence and Projections
- Mauna Loa Observatory: A remote site in Hawaii used to measure global average CO2. Being far from cities, it provides conservative estimates.
- Historical Trends:
- Historically, CO2 fluctuated between 180ppm and 280ppm over the last 400,000 years.
- In 2015, CO2 reached 400ppm. In November 2016, it was 403ppm. It is currently approaching 410ppm.
- Temperature Anomalies:
- The global average temperature has risen by nearly 1∘F.
- 9 of the last 10 years (as of the early 2000s) were the warmest on record.
- Recent years have seen temperatures 12 to 15 degrees above average in some regions.
- Ice Cores: Scientists measure past atmospheres by analyzing air bubbles trapped in layers of ancient ice (similar to tree rings).
- Impacts:
- Ocean Heating: Warmer surfaces lead to more erratic, powerful, and frequent hurricanes.
- Glacial Melt: Glaciers in Greenland, Iceland, and Africa are disappearing. This reduces freshwater availability for drinking and agriculture.
- Agricultural Shifting: Warm zones are moving north; crops must be moved to higher elevations or latitudes.
Nitrogen and Phosphorus Cycles
- Nitrogen Forms:
- Atmospheric Nitrogen (N2) is inert and unusable by most life.
- Biological Nitrogen: Plants require Nitrates (NO3) or Ammonia (NH4) to build proteins.
- Nitrogen Fixation and Symbiosis:
- Bacteria living in the root nodules of legumes (bean/pea plants) convert N2 into usable forms. This is a mutualism; bacteria get sugars while plants get nitrogen.
- Human Interference:
- The Green Revolution: Synthetic fertilizers (made via high-energy industrial processes) allow for high-yield monocultures.
- Nitrate Runoff: Excess fertilizer runs into rivers (e.g., the Mississippi), accumulating in the Gulf of Mexico.
- Eutrophication: High nitrogen/phosphorus levels cause massive algae blooms. Decomposition of dead algae depletes oxygen, creating "Dead Zones."
- The Phosphorus Cycle: No atmospheric phase. Phosphorus cycles from rocks to water/soil and through organisms.
- Experimental Study: A partitioned lake showed that adding Nitrogen and Carbon did not increase algae, but adding Phosphorus caused massive blooms; thus, phosphorus is often the limiting reagent.
- Law changes now require many detergents to be "phosphate-free."
The Ozone Layer and Air Quality
- Stratospheric Ozone (O3): Forms a layer in the high atmosphere that reflects harmful UVB radiation.
- Ozone Depletion: Caused by Chlorofluorocarbons (CFCs) from aerosol hairsprays.
- One chlorine atom acts as a catalyst, repeatedly breaking down ozone molecules into oxygen without being consumed itself.
- Ground-Level Ozone: Produced by two-stroke motors (lawnmowers, motorbikes). It is toxic and damaging to human lungs.
Mitigation and Personal Action
- Three Choices: Mitigation (reducing the problem), Adaptation (dealing with shifts), and Suffering.
- Mitigation Strategies:
- Energy Efficiency: Replace incandescent bulbs with CFLs or LEDs. LEDs are cheaper, last longer, and run much cooler.
- Renewable Energy: Solar, wind, and geothermal. Solar is particularly viable in Arizona.
- Transportation: Drive less, use public transit, walk, or ride bicycles.
- Dietary Choices: Reduce meat consumption to lower carbon/methane footprints and improve health (reducing risks of cholesterol, high blood pressure, and diabetes).
- Call to Action: Contact congressmen to support subsidies for renewable energy and energy efficiency.