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human influences on biogeochemical cycles
chemical run off leads to eutrophication
atmospheric emissions emit excessive nutrients
deforestation alters water/carbon cycles
urbanisation disrupts ecosystems
description of the carbon cycle
carbon circulated between atmosphere, oceans, soil, and organisms.
forms organic molecules
part of energy transfer and climate regulation
carbon sinks sequester carbon
human activities increase carbon
Carbon dioxide absorbed by plants, animals consume plants
carbon released through respiration and decomposition
carbon returns to atmosphere
definition of nitrogen fixation
Converting atmospheric nitrogen (N2) into ammonia (NH3) to make it accessible.
3 methods of nitrogen fixation
biological fixation: bacteria (Rhizobium/cyanobacteria) fix it; they live in legumes, and exchange carbohydrates and nitrogen.
atmospheric fixation: lighting creates nitrogen oxides that dissolve in rain, forming nitrates.
industrial fixation: Haber-Bosch process synthesises ammonia under high pressure/temperature to create fertilisers
definition of nitrification
nitrifying bacteria convert nitrites into nitrates
description of nitrification of ammonia
nitrosomonas oxidise ammonia to form nitrite; ammonia is toxic to plants in high concentrations
nitrobacter convert nitrite to nitrate, which plants absorb
description of assimilation
plants take it up an convert them into amino acids, proteins, etc.
animals consume plants
description of ammonification
decomposers decompose organisms, turning nitrogen back into ammonia in the soil
description of denitrification
pseudomonas convert nitrates/nitrites in the soil back into nitrogen gas/nitrous oxide, re-releasing it into the atmosphere
human impacts on the Nitrogen cycle
use of fertisilers = excessive nitrogen
irrigation causes leaching into groundwater/water bodies
combustion of fossil fuels releases nitrogen oxides, causing air pollution, acid rain, climate change
Haber-Bosch = excessive nitrogen in biosphere
sewage treatment can release nitogen into oceans/rivers
example: Gulf of Mexico Dead Zone
oxyegn plummets due to excessive nutrient pollution from Mississippi River
agricultural & urban runoff; fertilisers & stormwater/wastewater drainage
hypoxia kills/forces migration of marine life
fisheries impacted
Riparian Buffers = vegetated river banks to aborb/filter excess nutrients
wetland restoration also filters nutrients
why is nitrogen important?
Nitrogen is essential for the formation of amino acids, which are needed to form proteins
sources of energy
energy from insolation is unavailable due to:
being absorbed by inorganic matter
reflected back into the atmosphere
51% energy never reaches producers
energy transfers
coversion of light energy to chemical energy
transfer on chemical energy between trophic levels
10% efficiency
UV & visible light → heat energy
re-radiation of heat energy into atmosphere
definition of gross primary productivity - GPP
total rate of photosynthesis: biomass + respiration; a comprehensive measure of ecosystem's capacity to capture/store energy
definition of net primary productivity - NPP
Energy stored as biomass available to herbivores/decomposers AFTER accounting for respiration; represents energy available for next trophic level
definition of maximum sustainable yield
maximum amount of a renewable natural resource that can be harvested annually without comprommising long term productivity of the resource
equivalent to the net primary productivity (NPP) or net secondary productivity (NSP) of a system (as these values represent the amount of energy stored and new plant or animal biomass per year)
definition of gross secondary productivity - GSP
total energy/biomass assimilated by consumers
GSP = food eaten - fecal loss
definition of net secondary productivity - NSP
total gain in energy/biomass per unit area per unit time by consumers; accounting for respiration
NSP = GSP - R
3 factors affecting secondary productivity
food quality
food quantity
metabolic rate (body size, temperature, activity level)
definition of trophic efficiency
% energy/biomass transferred from one trophic level to the next 10%, but can range between 5-20%
reasons for trophic inefficiency
Not everything is eaten
Digestion is inefficient
Heat is lost in respiration
Some energy assimilated is used in life processes
stores of carbon
solid forms; sedimentary rocks/fossil fuels
oceans (dissolved/shells of crusteaceans)
soil (humus/respiration of soil organisms)
atmosphere
organisms (biomass; cellullose)
fossilized life forms (fossil fuels)
importance of biogeochemical cycles
ensure nutrients/vital elements are consistently available
support biodiversity
ecosystem service; aids soil fertility, water purification, and climate regulation
entwined with energy flow e.g. photosynthesis
food webs transfer nutrients across trophic levels
description of phosphorus cycle
used in ATP, nucleic acids, and cell membranes
cycled through water, soil, organisms; NOT atmosphere
released into environment through rock weathering; accelerated by human activities
description of water cycle
medium for transport of nutrients within ecosystems
precipitation & evaporation are continuous processes
influences climate/weather patterns
translocation/transpiration