Systems
A set of components that function and interact in some regular and theoretically predictable manner and can be isolated for purposes of observation and study
Input
matter
energy
informative flowing into system
Flow/Throughputs
matter
energy
information flowing at a certain rate within a system
stores/storage area
area of accumulation for various lengths of time before being released
Outputs
matter
energy
information that flows out of a system into sinks in the environment
3 Components of a system summary
Matter is a circular system
Energy is linear
Feedback Loops
A runaway cycle in which a change in a certain direction provides further information that causes a system to change further in the same direction
can destabilize a system
Ex: climate change, Hubbard brook experiment
Negative Feedback Loop
One change leads to a lessening of that change
desirable
stabilizes a system
Ex: homeostasis, thermostats, recycling
3 Factors of Life
One way flow of high quality energy from the sun
governed by 1st and 2nd Laws of Thermodynamics
Cycling of matter and nutrients
fixed supply of nutrients needs to constantly be recycled
Gravity
allows the planet to keep the atmosphere
Population
a group of organisms of one type
same species
living in the same area
Community
all populations that live together in a defined location
Ecosystem
communities and abiotic factors
Biosphere
the part of earth that contains all ecosystems
Abiotic factors
soil type
temperature
precipitation
water availability
sunlight
wind
pH
Cell theory
all things are made of one or more cells
cells only come from existing cells
all of an organisms life functions occur within cells
cells contain DNA
needed for regulating all functions
passing hereditary informaion
Biotic Components
living components of an ecosystem
bacteria
protists
fungus
plants
animals
Abiotic components
nonliving components of an ecosystem
determines which organisms can live there
sunlight
temperature
precipitation
pH
soil
nutrient availability
Effects of abiotic factors on biotic factors
each population in an ecosystem has a range of tolerance
range of physical and chemical conditions that must be maintained for a population to stay alive, grow, and function normally
Biomes
terrestrial regions inhabited by certain types of life, especially vegetation
Trophic levels
Levels in the feeding structure of organisms
higher trophic levels consume organisms from lower levels
Trophic pyramid
Represents the distribution of biomass among trophic levels in an ecosystem
Trophic cascade
Ecological phenomenon that occurs when the addition or removal of a top predator affects the population of predators and prey throughout a food web
may lead to significant changes in the structure of an ecosystem and how nutrients cycle
Autotrophs
Plants, algae, and other organisms that use the sun’s energy to produce usable forms of energy
Photosynthesis
Process by which autotrophs trap energy from the sunlight with chlorophyll and use energy to convert carbon dioxide and water into simple sugars
waste product is oxygen
Chemical equation for photosynthesis
6CO₂+6H₂O → C₆H₁₂O₆+6O₂
Heterotrophs
must obtain their energy from consuming other organisms
Primary consumers
heterotrophs (herbivores) that consume producers
Carnivores
heterotrophs that obtain energy by eating other consumers
Tertiary consumers
carnivores/omnivores that eat primary consumers
Scavengers
carnivores that consume dead animals
vultures
Detritivores
organisms that specialize in breaking down dead tissues and waste products into smaller particles
dung beetles
earthworms
Decomposers
organisms that complete the breakdown process by recycling the nutrients from dead tissues and wastes into the ecosystem
fungi
bacteria
Food chain
the sequence of consumption from producers through all levels of consumers
Food web
a complex model of how energy and matter move between trophic levels
more accurate
Ecological efficiency
useable energy that is passed along from one trophic level to the next
Biomass
the energy in an ecosystem can be measured in biomass which is the total mass of all living matter in a specific area
NPP establishes the rate at which biomass is produced over a given amount of time
Gross Primary Productivity (GPP)
the measure of the total amount of solar energy that the producers in an ecosystem capture via photosynthesis over a given amount of time
Net Primary Productivity (NPP)
the energy captured by producers minus the energy that producers respire
allows us to compare the productivity of different ecosystems
NPP equation
GPP - respiration by producers = NPP
Biosphere
the region of our planet where life resides
matter does not enter or leave the biosphere
Earth is a closed system with respect to matter
Biogeochemical cycles
the movement of matter within and between ecosystems involving biological, geological, and chemical processes
Pools/reservoirs
components that contain matter
air
water
organisms
Flows
processes that move matter between pools
The Hydrology Cycle
Solar energy heats Earth and causes evaporation
evaporation from ocean
evaporation from soil
evapotranspiration from plants
Evaporated water condenses into clouds
Water returns to Earth as precipitation
rain
snow
hail
Precipitation falling on land is taken up by plants, run off along the land surface, and enters groundwater
surface water
surface runoff
groundwater
The Carbon Cycle
Producers convert CO₂ into sugars
Sugars are converted back into CO₂
Some carbon is buried
Human extraction of fossil fuels brings carbon to Earth’s surface, where it can be combusted
CO₂ in the atmosphere and CO₂ dissolved in water are constantly exchanged
Combustion converts fossil fuels and plant material into CO₂
The Nitrogen Cycle
Nitrogen fixation
nitrogen fixation converts N₂ from the atmosphere
Biotic processes convert N₂ to ammonia (NH₃)
Abiotic processes convert N₂ to nitrate (NO3- )
Assimilation
producers either take up ammonium (NH4+ ) or nitrate (NH3-)
consumers assimilate nitrogen by eating producers
Ammonification
decomposers in soil and water break down biological nitrogen compounds into ammonium (NH4+)
Nitrification
nitrifying bacteria convert ammonium (NH4+) into nitrate (NO2-) and then into nitrate (NO3-)
Denitrification
denitrifying bacteria in oxygen poor soil and stagnant water (NO2-) into nitrous oxide (N₂O)
eventually becomes nitrogen gas (N₂)
The Phosphorus Cycle
Weathering of uplifted rocks contribute phosphates to the land. Some phosphates make their way back to the ocean
Phosphate fertilizer applied to fields can run off directly into streams, become part of a soil pool or absorbed by plants
Excretion by animals and decomposition of both animals and plants release phosphates on land or in water
Dissolved phosphates precipitate out of solution and contribute to the ocean sediments
conversion of sediments into phosphate rocks is a very slow process
Geologic forces slowly lift up phosphate rocks from the ocean floor to form mountains.