Topic 33 Flashcards
Internal cycling of nutrients
primarily concerned with the flow of nutrients through the ecosystem dominated by the biological processes of primary production and decomposition
Many transformations take place in the..
non living (abiotic) component- atmosphere, water, soil.
Weathering of rocks and minerals releases..
inorganic nutrients into soil and water thins available for plant uptake
Biogeochemical cycle
flow of all nutrients from the nonliving to the living and back to the nonliving components of the ecosystem in a more or less cyclic path
2 major types of cycles (based on primary source of nutrient input)
-gaseous cycles
sedimentary cycles
Gaseous cycles
main pool of nutrients: atmosphere and ocean. ex: nitrogen, oxygen, CO2, dominant components of atmosphere
Sedimentary
main pool of nutrients: soil, socks, minerals. nutrients required by organisms come initially from inorganic source via weathering
All cycles involve..
biological and non biological processes, both driven by flow of energy through the ecosystem
Water is the..
medium in which inorganic nutrient travel through the ecosystem
Without water..
biochemical cycles would stop
Inputs of nutrients into the ecosystem depend on
the type of ecosystem
Terrestrial input
nutrient inputs are supplemented by rain, snow, air currents and animals
Wetfall
precipitation inputs nutrients
Dryfall
airborne particles with associated nutrients fall from the atmosphere
Aquatic input
major source of nutrients are from the surround land in the form of drainage, water, detritus and sediment (also wet and dry fall)
Input of organic carbon from terrestrial ecosystems constitutes the..
majority of energy input into stream and river ecosystem
Output step 1
release into atmosphere
Output step 2
inorganic nutrients released via leaching (dissolved and washed) out of the soil in underground water –> streams
Output step 3
organic matter exported from forest ecosystems by streams and rivers –> lakes
Output step 4
organic matters transferred between ecosystems in form of faces and other rates via movement patterns of consumers
Output step 5
harvesting- nutrients stored in organisms are directly lost during removal from the system but balanced by adding fertilizers because nutrients become limited
Processes of inputs and outputs of nutrients during biochemical cycles link
different ecosystems
The output from one ecosystem represents ..
inputs to another (terrestrial –> aquatic system)
Processes of nutrient exchange among ecosystems requires..
examining biogeochemical cycles from much broader view than single ecosystem. (true of those nutrients w gaseous cycle)
Main pools are the atmosphere and ocean which have..
local circulation patterns because carbon is the basic nutrient in all organic compounds
Terrestrial carbon cycle
photosynthesis: CO2 – organic form – herbivores – carnivores – organic matter – decomposers – plant tissue. CO2 released back into atmosphere via respiration
Swamps and Marshes
dead organic matter falls into water doesn’t completely decompose, carbon stored as humus or peat. buildup of partially decomposed organic mater forms fossil fuels – long terms.
Freshwater and marine ecosystem
CO2 diffuses into the surface water form atmosphere –> carbonates. Phytoplankton uses carbonates – plant tissue – herbivores – carnivores –organic matter – decomposers – plant tissue. CO2 releases via respiration is either reused or released into atmosphere (diffusion)
Diffusion
movement of substance from area of higher to lower concentration
Earths C budget (100,000,000 Gt) most..
buried in sedimentary rocks (not involved in cycle) = 99%
Global cycle is = 55,000 Gt and divided into..
- oceans (major) 38,000 Gt
- fossil fuels (decomposed matter) 10,00 Gt
- atmosphere 750 Gt
- terrestrial 2000 Gt
Oceans Carbon
surface water to atmosphere is main exchange site. exchange rate governed by diffusion gradient between surface waters and atmosphere
Terrestrial Carbon
includes soil and organisms, exchange rate governed by diffusion gradient between plant leaf and atmosphere (photosynthesis) historically exchanges of CO2 between terrestrial environments and the atmosphere were thought t be in equilibrium (has increased)
Atmospheric Carbon
CO2 in atmosphere have increase 25% in last 100 years. industrial revolution CO2 increase steadily by mid 1900s increased exponentially
Historically CO2 is ..
280-290 ppm.
Burning fossil fuels in industrialized nations
adding 6.4 Gt/year in 1990s
Deforestation
forested lands are typically clearly and burned for farming. adding 2.2 Gt / year in 1990s.
Also issues with increased levels of…
methane which is 25x more effective as greenhouse gas
Predictions of global warming
- increases average global temps and precipitation (increase 2-6 C in 100 years)
- changes will not be evenly disturbed over Earths surface (warming is expected to be greater during winter months)
- increased variability in climate (more sever storms and hurricanes, great snowfall increasing variability in rainfall)