ecology cycles Flashcards
closed system
- energy exchange
- NO matter exchange
open system
- energy and matter exchange
photosynthesis
6CO2 + 6H2O → C6H12O6 + 6O2
cellular respiration
C6H12O6 (aq) + 6 O2 (g) –> 6 CO2(g) + 6 H2O (l)
* ALL LIVING THINGS DO IT*
1st law of thermodynamics
amount of energy is constant
2nd law of thermodynamics
energy is neither created or destroyed
autotrophs
self feeding
suns energy –> chemical energy
heterotrophs
energy gained by eating producers
decomposers
return nutrients to soil
- also called detritivores
trophic levels
1 - producers, autotrophs
2 - primary consumer, herbivores
3 - secondary consumer, carnivores
4 - tertiary consumer, top carnivores
types of pyramids
- numbers
- biomass
- energy
pyramid of biomass
representation of the total biomass measured in g/m^2
pyramid of energy
- measured in joules of energy
- always pyramid shape
biotic
living
abiotic
non-living
biomagnification
increase in toxin concentrations from one level to another on a food chains
rule of ten
10% of energy goes to the next consumer
homeostasis
a state of balance
properties of water
- polar molecule
- universal solvent
- high specific heat capacity
high specific heat capacity
can absorb or release a LOT energy before changing energy
the hydrologic cycle
evaporation –> condesation –> precipitation
percolation
runoff, trickles through rock picking up ions as it becomes ground water
transpiration
- plants release O2 during photosynthesis
- H2O is lost
anoxic
lack of oxygen
hypoxic
less oxygen
cynobacteria
photosynthesize to release O2
stromatolites
fossilized rocks trapping cynobacteria
carbon cycle
- photosynthesis
- cellular respiration
- combustion
- decomposition
combustion
chemical reaction to oxygen that gives off heat
decomposition
the process of breaking down dead organic substances
carbon sources
any process that releases CO2 into the biosphere
carbon sinks
stores CO2
nitrogen (facts)
- nitrogen is most of our atmosphere
- nitrogen compounds are key components of proteins
nitrogen fixation process
rhizobium (bacteria) complete the reaction
(free nitrogen) N2 –> (ammonia) NH3
ammonification
toxic ammonia (NH3) –> ammonium (NH4)
nitrification
NH3 –> NO2 –> NO3
1. ammonia gets oxidized and becomes nitrite
2. nitrites become nitrates
dentrifying
bacteria convert excess nitrate and nitrite to nitrogen gas
NO3 –> N2
(reverse fixation)
short phosphorus cycle
heterotrophs eat it, release waste, waste decomposes for plants to use
phosphorus is a component of…
DNA, ATP, and RNA
long phosphorus cycle
phosphate dissolves in water, is used by animals to produce rocks (deposit)
rhizobia
nitrogen-fixing bacteria
- energy exchange
- NO matter exchange
closed system
- energy and matter exchange
open system
6CO2 + 6H2O → C6H12O6 + 6O2
photosynthesis
C6H12O6 (aq) + 6 O2 (g) –> 6 CO2(g) + 6 H2O (l)
* ALL LIVING THINGS DO IT*
cellular respiration
amount of energy is constant
1st law of thermodynamics
energy is neither created or destroyed
2nd law of thermodynamics
self feeding
suns energy –> chemical energy
autotrophs
energy gained by eating producers
heterotrophs
return nutrients to soil
- also called detritivores
decomposers
1 - producers, autotrophs
2 - primary consumer, herbivores
3 - secondary consumer, carnivores
4 - tertiary consumer, top carnivores
trophic levels
- numbers
- biomass
- energy
types of pyramids
representation of the total biomass measured in g/m^2
pyramid of biomass
- measured in joules of energy
- always pyramid shape
pyramid of energy
living
biotic
non-living
abiotic
increase in toxin concentrations from one level to another on a food chains
biomagnification
10% of energy goes to the next consumer
rule of ten
a state of balance
homeostasis
- polar molecule
- universal solvent
- high specific heat capacity
properties of water
can absorb or release a LOT energy before changing energy
high specific heat capacity
evaporation –> condesation –> precipitation
the hydrologic cycle
runoff, trickles through rock picking up ions as it becomes ground water
percolation
- plants release O2 during photosynthesis
- H2O is lost
transpiration
lack of oxygen
anoxic
less oxygen
hypoxic
photosynthesize to release O2
cynobacteria
fossilized rocks trapping cynobacteria
stromatolites
- photosynthesis
- cellular respiration
- combustion
- decomposition
carbon cycle
chemical reaction to oxygen that gives off heat
combustion
the process of breaking down dead organic substances
decomposition
any process that releases CO2 into the biosphere
carbon sources
stores CO2
carbon sinks
- nitrogen is most of our atmosphere
- nitrogen compounds are key components of proteins
nitrogen (facts)
rhizobium (bacteria) complete the reaction
(free nitrogen) N2 –> (ammonia) NH3
nitrogen fixation process
toxic ammonia (NH3) –> ammonium (NH4)
ammonification
NH3 –> NO2 –> NO3
1. ammonia gets oxidized and becomes nitrite
2. nitrites become nitrates
nitrification
bacteria convert excess nitrate to nitrogen gas
NO3 –> N2
(reverse fixation)
dentrifying
heterotrophs eat it, release waste, waste decomposes for plants to use
short phosphorus cycle
DNA, ATP, and RNA
phosphorus is a component of…
phosphate dissolves in water, is used by animals to produce rocks (deposit)
long phosphorus cycle
nitrogen-fixing bacteria
rhizobia
biomass production
g/m2/year
rate of energy measurement
J/m2/year