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Eutrophication 2.1 Biogeochemical cycles Alice Newton P. Viaroli
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Important nutrients N:P:Si ~ Ratios N:P and N: Si are especially important ~ N is usually limiting nutrient in coastal waters and estuaries. Can be fixed by cyanobacteria ~ P most important in freshwater lakes. Anoxic sediments release P ~ Si important for phytoplankton composition (diatoms)
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Redfield ratio N:P 16:1 ~ N limited when <16:1 ~ P limited when >16:1 ~ Range of 10 to 25 is “normal” ~ N:P in sewage, manure and fertilizers is different from Redfield ratio.
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N:Si 1:1 ~ Upstream eutrophication in rivers traps Si in sediments before it reaches estuaries ~ Dams: trap Si ~ Si availability controls diatom growth ~ Decrease in Si relative to N & P linked to changes in phytoplankton community and HABs
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Nitrogen cycle
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-3 -1 0 +1 +2 +3 +5 (red-ox) N-cycle Biochemical pathways AnAmOx nitrification Dissimilative Nitrate Reduction to Ammonium denitrification Assimilative reduction N-fix A AR P. Viaroli
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Nitrification total: NH 4 + + 2O 2 NO 3 - + H 2 O+ 2H + Nitrification1: NH 4 + + 0.5 O 2 NH 2 OH + H + NH 2 OH + O 2 NO 2 - + H 2 O + H + Nitrification2: NO 2 - + 0.5 O 2 NO 3 - Nitrogen fixation N 2 +6e - + 6H + 2NH 3 Denitrification (+OM, -O 2 ) Nitrification (+O 2 ) P. Viaroli Ammonium-ammonia equilibrium NH 3 + H 3 O + NH 4 + + H 2 O pKa = 4.75
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NH 4 + NO 2 - NO 3 - N2N2 N - phytoplankton N in zooplankton N-fish N-detrital N - sedimentary Nitrogen cycling in pelagic waters (plankton-dominated) P. Viaroli N in benthos (zoo and phyto)
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Biology of N ~ Gaseous N 2 not useful to most photosynthesizers ~ N fixation ~ eg Trichodesmium can produce NH 4 from N 2 ~ Microbes and BG algae may form NO 2 and NO 3 ~ NH 4, NO 2 and NO 3 can be used as nutrients by photosynthesizers ~ Proteins in Organic matter are excreted or decompose as NH 4
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N org. NH 4 + NO 2 - 3 - Nitrification Nitrosomonas, Nitrobacter N 2 ONO N 2 Ammonification Denitrification Pseudomonas,Thiobacillus Anoxic horizon oxic horizon water DNRA Atmosphere N 2 Nitrogen fixation Cyanobacteria P. Viaroli N-cycle in shallow waters
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dark light Denitrification (mmol m -2 h -1 ) in a Ruppia meadow Denitrification from water nitrate Coupled nitrification-denitrification
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light dark Denitrification rates determined with dark and light incubations
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Quantifying the N cycle ~ N cycle: ~ Natural Sources of N ~ Anthropogenic sources Natural Sources ~ Lightening fixation 5-10Tg pa ~ Natural N fixation (non crop) 90-140 Tg p.a. ~ Marine fixation 30-300 Tg pa??? (Teragrams = 1 million metric tonnes)
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Anthropogenic sources of N ~ Industrial fixation inc Fertilizer 80Tg of N pa (NH 3 & N 2 O) 2020 projection 134 Tg pa ~ Agricultural Legume Fixation 32-53 Tg pa ~ Fossil fuels 20 Tg pa (NO & NH 3 ) 2020 projection 46Tg pa ~ Forests Burning 40 Tg pa (NO, N 2 O & NH 3 ) ~ Loss of wetlands (denitrifying) 10 Tg pa ~ Land clearing for crops 20 Tg pa ~ Domestic and Animal Waste 32 Tg pa (NH 3 ) 1996 Total annual anthropogenic N inputs ~140Tg (Teragrams = 1 million metric tonnes) see text below
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Human alteration to N cycle ~ N has doubled in 50 years (C has only increased 10%) ~ 80 Tg of N pa applied as fertilizer ~ 174 kg/ha/pa Xs ~ Impacts include: ~ Increase N 2 O, (nitrous oxide, a greenhouse gas), due to burning of fossil fuels ~ Increased NO (nitric oxide, photochemical smog formation) ~ Acidification of soils and freshwater ~ Erosion & leaching of N to estuaries and coast (Teragrams = 1 million metric tonnes)
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Changes in N cycle Revised Kates et al. (1990).
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Human-Caused Global N- Emissions
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Atmospheric deposition
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NOx and NHx in the Atmosphere Origins ~ Domestic combustion ~ Industrial processes ~ Traffic ~ Agricultural sources ~ Animal housing ~ Spreading of manure
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A tmospheric D eposition of N in the N orth A tlantic O cean ~ AD-N to the NAO basin arises from pollution sources in North America and Western Europe ~ Sources have increased drastically (5-10-fold) since the Industrial Revolution and continue to increase in both geographic and depositional magnitude. ~ AD-N flux (11.2 Tg N yr -1 ) accounts for 46-57% of the total "new" or anthropogenic nitrogen flux to the NAO. (Teragrams = 1 million metric tonnes)
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Transfers of nitrogen ~ N fixed in industrial areas ~ N transported to agricultural areas ~ N applied to fields, some retained in crops ~ N loss to atmosphere and water ~ Crops transported to livestock producing areas and cities ~ Crops consumed in cities and N enters sewage ~ Animal feed crops consumed in livestock farms ~ Livestock transported to cities ~ Manure spread on fields, enters atmosphere and water
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Industrial areas Agricultural areas Atmosphere Aquatic environment Livestock area Cities
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Natural transfers ~ Sea Birds and guano ~ Salmon migration and death
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N input into Aquatic Systems Modified from Howarth et al. (1996)
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NO 3 in major EU rivers 1980-95 Nitrate concentrations have been largely unchanged since 1980 EEA
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NO 3 in EU coastal waters 1985-98
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P-Cycle ~ P most important in freshwater lakes ~ P limitation has been documented in coastal waters and estuaries: ~ Apalachicola (Gulf of Florida) ~ some Dutch estuaries ~ Tropical systems with carbonate sands ~ P is released from anoxic sediments ~ N-fixing cyanobacteria proliferate when P is abundant, e.g. in the Baltic sea
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P-Cycle P.Viaroli
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Primary producers P-Refractory External load burial/early diagenesis PO 4 Clay Fe P Ad-sorption De-sorption Assimilation Decomposition Organic Detritus Precipitation (es:apatite, hydroxiapatite) Assimilation Ca P P-cycle P. Viaroli
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Human alteration to P cycle ~ 600 Tg applied as fertilizer from 1950 to 1995 ~ ~250 Tg of P harvested as crops ~ ~50 Tg used as feed crops returned to soil as manure ~ Net XS addition 400 Tg in 45 years, ~10 Tg p.a. (Teragrams = 1 million metric tonnes)
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Sources of P in EU 1988-96
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P sources in the UK EA UK
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P in major EU rivers 1980-95 Phosphorus concentrations in some EU rivers have fallen since the mid-1980s, particularly in the largest and most polluted rivers. EEA.
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P in coastal waters 1985-98. EEA
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NO3 & PO4 in EU coastal waters, 1985-1996 Nutrient concentrations in coastal waters show little overall improvement
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