Supporting article P: A graphic depiction of the Biogeochemical Cycles
Biogeochemical Cycle : the cycling of chemical elements required by life between the living and nonliving parts of the environment. Some examples of these chemical elements are H2O, P, S, N2, O2 and C.
These elements cycle in either a gas cycle or a sedimentary cycle; some cycle as both a gas and sediment.
In a gas cycle elements move through the atmosphere. Main reservoirs are the atmosphere and the ocean.
In a sedimentary cycle elements move from land to water to sediment. Main reservoirs are the soil and sedimentary rocks.
Gas Cycles: Sedimentary Cycles:
Image above obtained from http://www.cotf.edu/ete/modules/carbon/earthfire.html
– Carbon (C) enters the biosphere during photosynthesis:
CO2 + H2O —> C6H12O6 + O2 + H2O
– Carbon is returned to the biosphere in cellular respiration:
O2 +H2O + C6H12O6 —> CO2 +H2O + energy
Amount of CO2 during the year:
– Every year there is a measurable difference in the concentration of atmospheric CO2 in phase with the seasons.For example, in winter there is almost no photosynthesis therefore there is a high concentration of CO2.
– During the growing season there is a measurable differnece in the concentration of atmospheric CO2 over parts of each day. For example, at sunrise photosynthesis begins with the uptake of CO2, by afternoon plant respiration increases, at sunset photosynthesis stops so the concentration of CO2 in the atmosphere increases.
Human induced changes in the global carbon cycle:
– The Earth is getting warmer.
– The 20th century has been the warmest in the last 600 years.
– This century is about 1 degree Fahrenheit warmer than last century.
– The balance of evidence suggests that burning of fossil fuel (eg. coal, oil, natural gas), which emits CO2 as a waste, is the cause.
– CO2 is a “Green House” gas – it traps heat at the Earth’s surface. (H2O vapor and methane are also examples of green house gases)
Signs that the climate is warming:
– Plants start blooming 8 days earlier in spring than 11 years ago.
– Birds from the United Kingom lay eggs earlier.
– Buds on trees appear earlier and leaves fall later in the Northern Hemisphere.
– Alaska, North West Canada, and Siberia have warmed up as much as 5 degrees Fahrenheit in the last 30 years.
Image obtained from http://muextension.missouri.edu/xplor/waterq/wq0252.htm
– Nitrogen (N) is an essential constituent of protein, DNA, RNA, and chlorophyll.
– N is the most abundant gas in the atmosphere, but it must be fixed or converted into a usable form.
Nitrogen Fixation Methods:
1) High energy fixation- a small amount of atmospheric nitrogen is fixed by lightening. The high energy combines N and H2O resulting in ammonia (NH3) and nitrates (NO3). These forms are carried to Earth in precipitation.
2) Biological fixation: achieves 90% of the nitrogen fixation. Atmospheric nitrogen (N2) is split and combined with hydrogen (H) atoms to form ammonia (NH3).
Who performs nitrogen fixation?
– symbiotic bacteria (eg. Rhizobium spp.) living in association with leguminous ( plants in the pea family), and root-noduled non-leguminous plants (eg. Alnus spp.).
– free-living anaerobic bacteria
– blue-green algae (cyanobacteria)
Once NH3 is in the soil it combines with H+ ions to form ammonium ion (NH4), or without it to form NO3. NH4+ and NO3 are readily absorbed by plants.
Image obtained from http://www.accessexcellence.com/AB/GG/photo_Resp.html
Sources of Oxygen:
1) photodisassociation of H2O vapor
Since oxygen is so reactive its cycling is complex:
1) As a constituent of CO2 it circulates freely throughout the biosphere.
2) Some CO2 combines with Ca to form carbonates.
3) O2 combines with nitrogen compounds to form nitrates.
4) O2 combines with iron compounds to form ferric oxides.
5) Photosynthesis and respiration
6) O2 in the troposphere is reduced to O3 (ozone). Ground level O3 is a pollutant which damages lungs.
Image obtained from http://www.bsi.vt.edu/chagedor/biol_4684/Cycles/Pcycle.html
– Component of DNA, RNA, ATP, proteins and enzymes
– Cycles in a sedimentary cylce
– A good example of how a mineral element becomes part of an organism.
– The source of Phosphorus (P) is rock.
– It is released into the cylce through erosion or mining.
– It is soluble in H2O as phosphate (PO4)
– It is taken up by plant roots, then travels through food chains.
– It is returned to sediment
Image obtained from http://www.agnr.umd.edu/users/agron/nutrient/Factshee/sulfur/Sulfur.html
– Component of protein
– Cycles in both a gas and sedimentary cycle.
– The source of Sulfur is the lithosphere(earth’s crust.
– Sulfur (S) enters the atmosphere as hydrogen sulfide (H2S) during fossil fuel combustion, volcanic eruprtions, gas exchange at ocean surfaces, and decomposition.
– H2S is immediately oxidized to sulfur dioxide (SO2)
– SO2 and water vapor makes H2SO4 ( a weak sulfuric acid), which is then carried to Earth in rainfall.
– Sulfur in soluble form is taken up by plant roots and incorporated into amino acids such as cysteine. It then travels through the food chain and is eventually released through decomposition.