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BIOCHEMICAL CYCLES
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The movement of materials through the biotic (living) and abiotic (non-living) parts of an ecosystem BIOCHEMICAL CYCLES
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Biogeochemical Cycles Biogeochemical Cycles are also known as Nutrient Cycles -They are the pathways that 4 materials vital to life follow through an ecosystem - - Carbon - Nitrogen - Phosphorus - Water These materials cycle through both biotic and abiotic reservoirs in an ecosystem -biotic reservoirs are the living things that these materials move through -abiotic reservoirs are the non-living things that these materials move through
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Carbon is the backbone for many of the most important molecules used by living things. carbohydrates, fats, protein, nucleic acid Carbon exists as CO 2 in the atmosphere - CO 2 in the atmosphere can’t be used by living things – it must be converted into a usable form - How does CO 2 get converted? – Photosynthesis in plants - CO 2 is used to make glucose – the carbon in glucose can be used by living things
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CO 2 in atmosphere Photosynthesis Cellular Respiration Combustion Coal Oil Death & Decomposition Fossil Fuels CO 2 is absorbed in water Limestone
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Carbon Cycle Carbon returns to the atmosphere - cellular respiration - combustion All living things are biotic reservoirs The atmosphere and water are abiotic reservoirs Carbon Sink – A sink is a part of the cycle which removes a nutrient from the cycle for long periods of time - Limestone - Fossil Fuels
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Carbon Cycle The carbon in fossil fuels has been stored in the earth for millions of years- Burning them for energy releases the CO 2 back to the atmosphere - causing a rapid increase in CO 2 in the atmosphere - CO 2 is a greenhouse gas which traps heat, warming the Earth - Increasing CO 2 is leading to Global Climate Change
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Nitrogen is used by living things to make proteins and nucleic acids (DNA, RNA & ATP) Nitrogen exists in the atmosphere as N 2. 78% of the atmosphere is N 2 -the N 2 molecule consists of two nitrogen atoms so tightly bonded that they will not react with other elements and so can’t be used by living things. - N 2 can be split, but requires large amounts of energy– lightning can split N 2 -Once split by lightning, the nitrogen atoms bond with other elements and become useable by living things This accounts for 5 – 6 % of all nitrogen available to living things
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Nitrogen Cycle: Nitrogen Fixation - Certain bacteria contain the enzymes necessary to convert N 2 into the nitrogen compound ammonia – NH 3 - these nitrogen fixing bacteria are found in the soil and in symbiotic relationships with certain plants primarily legumes, beans, peas etc…. -The ammonia can enter the food chain when plants assimilate it – take it up and use it or be converted by bacteria into nitrate NO 3 and then assimilated
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Nitrogen Cycle: Man-made Nitrogen The Haber Process –Developed by Fritz Haber in 1909, this process joins N 2 and H 2 together to make ammonia ( NH 3 ) - The elements are driven together under high temperature and high pressure - In the last 60 years the use of ammonia as fertilizer has become wide-spread. - It has allowed humans to produce large quantities of food. However, excess nitrogen leeches into ground water or runs off into lakes and the ocean causing great harm
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