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Nitrogen & Phosphorous
Group #3: Neil Mehta Misha Nelson Tristan Jenkins Jenna Colhouer Brendon Esperancilla
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Nitrogen Chemical Reactions
Inorganic and organic reservoirs for the element Pathway of movement Impact of human intervention on the cycle
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Chemical Reactions Nitrogen: (N2) most abundant element in atmosphere (78% of troposphere volume) Combines with atmospheric oxygen to form nitrogen dioxide gas (NO2) (N2) cannot be metabolized as a nutrient Electrical discharges cause N2 & O2 to react Certain bacteria (Rhizobium, etc.) can fix nitrogen for use by plants
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Inorganic and organic reservoirs for the element
Atmospheric gas Organic: Plants are consumed by animals as a source of nitrogen Detritus resulting from decomposition of formerly living organisms
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Pathway of movement Nitrification: ammonia converts to nitrite (NO2-) & nitrate (NO3-) Assimilation: plant roots absorb inorganic ammonia, ammonium ions, and nitrate ions Used for synthesis of DNA, proteins, etc. Ammonification: bacteria decompose dead matter into constituent components, including ammonia and ammonium salts Denitrification: bacteria convert ammonia and ammonium back into nitrite and nitrate, then becoming N2 and nitrogen oxide
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Impact of human intervention on the cycle
When we burn any fuel, it adds large amounts of nitric oxide Acid rain: formed by HNO3 (nitric acid=atmospheric water and nitrogen dioxide) and dissolves in rain or snow Farm animals release methane into atmosphere
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Phosphorous Chemical Reactions
Inorganic and organic reservoirs for the element Pathway of movement Impact of human intervention on the cycle
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Chemical Reactions Very little P circulates in atmosphere
At Earth STP, P is not usually gaseous and mostly mineral P is typically found in terrestrial rock and ocean sediment Helps form structure of bones in animal skeletons Often used in fertilizer Composes ATP for nearly all cellular activities Composes phospholipid bilayer of cell membranes Most abundant form: orthophosphate (PO43-)
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Inorganic and organic reservoirs for the element
Mineral formations Ocean sediment Organic: Aquatic and terrestrial plants Bones of terrestrial animal
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Pathway of movement Starts in mineral form
Weathering deposits it in soils Plants absorb from soil Animals consume plants and their phosphorous Reintegrated into soil after death of animal Can run off into ocean Ocean plants ocean animals Some settles into marine sediment Mined by humans for fertilizer
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Impact of human intervention on the cycle
We harvest phosphorous from sediment to make fertilizer Remove trees from tropical forests No plants, no absorption from soil No plant roots, no soil to begin with! Pollute aquatic environments Overabundance of P promotes algal bloom, which helps bacteria thrive; bacteria consume too much oxygen, and fish drown!?
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HEY!
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