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Matter and Biogeochemical Cycles

Matter and Biogeochemical Cycles

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Matter and Biogeochemical Cycles. Matter. All material in the universe that has mass and occupies space is called matter. Atoms - smallest unit of an element Example: Oxygen, hydrogen, carbon, gold , etc. Matter. Atom’s nucleus includes: protons (+) n eutrons (+/-) - PowerPoint PPT Presentation

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Page 1: Matter and Biogeochemical  Cycles

Matter and Biogeochemical

Cycles

Page 2: Matter and Biogeochemical  Cycles

Matter• All material in the universe that

has mass and occupies space is called matter.• Atoms- smallest unit of an

elementExample: Oxygen, hydrogen,

carbon, gold, etc

Page 3: Matter and Biogeochemical  Cycles

Matter

• Atom’s nucleus includes:–protons (+)–neutrons (+/-)

Electrons (-) orbiting around the nucleus.

Page 4: Matter and Biogeochemical  Cycles

• Molecules- a cluster of atoms with unique characteristics. Organic compounds have carbon. Inorganic compounds do not have carbon. Hydrocarbons are organic compounds containing ONLY hydrogen and carbon.

Page 5: Matter and Biogeochemical  Cycles

• Macromolecules are the building blocks of life.

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1)Proteins: • made of amino

acids(monomers), • responsible for muscle

contractions, • immunity & carries oxygen in the

body

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2)Carbohydrates: • made of

monosaccharides(monomers); • sugars & starches, • give you short-term energy

Page 8: Matter and Biogeochemical  Cycles

3) Lipids: • made of a glycerol & three fatty

acids (monomer); • fats & oils, • long-term energy, • insulation & cushioning for organs

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4) Nucleic Acids: • nucleotides (monomers), • DNA & RNA, • molecules that store genetic

information• to help create proteins • give you your characteristics

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• Acids, Bases & pH• pH: how basic or acidic a solution

is • pH Scale

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• Biosphere: all the planet’s living, once living and nonliving parts of the environment and how they interact. • Abiotic: non-living• Biotic: living

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• Geosphere – made of all the rock at and below Earth’s surface

• Lithosphere – hard rock just on or below the Earth’s surface

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• Atmosphere – gaseous envelope around the planet

• Hydrosphere – Earth’s supply of water

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Biogeochemical Cycles• BIO – refer to the LIVING organisms

• GEO – refers to the Earth, rock and LAND.

• CHEMICAL – molecules,

REACTIONS and atoms.

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Biogeochemical Cycles• Matter cycles through the

environment. Nutrients are matter that organisms require for life process, circulate throughout the environment in biogeochemical cycles.

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Biogeochemical Cycles• Law of Conservation of Matter: • Matter can be transformed, but

cannot be created or destroyed.

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Water Cycle• The water cycle summarizes how

water plays a role in our environment.

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Unique properties of water 1) Cohesion – water molecule can stick to themselves

2) Expands when freezes 3) Capillary action

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Label the water cycle diagram

• Aquifers• Condensation• Evaporation• Precipitation• Surface runoff• Groundwater• Transpiration

Page 21: Matter and Biogeochemical  Cycles

Label the water cycle diagram

Condensation Precipitation Condensation

Transpiration

Ground water

Surface runoff Evaporation

Aquifers

Page 23: Matter and Biogeochemical  Cycles

Carbon Cycle

Carbon is a building block of life. All organic compounds have carbon.

Carbon is essential for DNA, fats, proteins, carbohydrates & other substances.

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Carbon Cycle

Carbon is gas form is carbon dioxide & it’s a greenhouse gas that helps to maintain earth’s temperature.

Carbon is stored in the ocean, atmosphere & rocks.

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Carbon Cycle

A place where a lot of carbon is stored are called carbon sinks.

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Page 27: Matter and Biogeochemical  Cycles

Pathway 11. Carbon moves between

the atmosphere, oceans & living things.

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2. Through photosynthesis, plants use CO2 from the air & ocean to make glucose (organic compound….C6H12O6)

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3. A consumer eats plants & animals that eat plants & the carbon moves through the food webs.

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4. Respiration is one way carbon is released directly into the air.

Example: exhaling of animals

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5. Decomposition of living things also returns carbon to the soil, water & air in the form of carbon dioxide.

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1. Carbon travels from living things to rocks & back to air or water where living things will use it again.

Pathway 2

Page 33: Matter and Biogeochemical  Cycles

Example: Shells of marine animals contain carbon. These shells fall to bottom of ocean when they die & pile up. They are covered with sediment & compacted to form rock (limestone). Erosion on land eventually dissolve the carbon containing minerals to air & water.

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2. This process takes millions of years.

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Pathway 3

1. This pathway involves the formation & burning of fossil fuels.

2. Oil & natural gas form from the remains of dead organisms.

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3. After buried for a long time, a chemical change takes place & it turns them into petroleum.

4. This process takes millions of years.

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5. When the oil is removed & we burn it. The combustion releases carbon dioxide into the atmosphere. Then it’s available plants to use for photosynthesis.

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Deforestation: removing trees that absorb carbon dioxide from the atmosphere. Fewer trees mean less carbon dioxide is being absorbed.

Ways HUMANS affect Carbon Cycle

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Burning of fossil fuels in industry & vehicles: Carbon is a by-product of combustion. The amount of carbon dioxide in the atmosphere has been rising. Some say it is contributing to global warming.

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video

Artificial Trees

Page 41: Matter and Biogeochemical  Cycles

Nitrogen Cycle

•Nitrogen is an important element in organic compound such as proteins, DNA, amino acids & chlorophyll.

Page 42: Matter and Biogeochemical  Cycles

Nitrogen is the most abundant gas in the atmosphere. It cycles from the atmosphere to living things & back to atmosphere.

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•But living things cannot use it in its gas form, therefore living things get nitrogen from the food.

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1. Living organisms cannot use simple nitrogen molecules (NH2).

2. Living things take it in as a nitrate (NO3

-).

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3. Nitrate is formed when nitrogen is combined with oxygen. This process is called nitrogen fixation.

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4. Nitrogen-fixing bacteria live on root nodules of legumes & convert the gaseous nitrogen to ammonia (NH4) then to nitrates(NO2 or NO3).

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5. Examples of legumes: clover, peas, soybeans & alfalfa.

6. Plants use nitrates to make proteins. Animals only take in nitrogen by eating plants.

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7. Nitrogen flows through the food web as animals eat plants & animals eat other animals.

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8. During decomposition, nitrogen compound are released. Bacteria will break down ammonia to nitrogen & oxygen & release nitrogen back to soil and atmosphere.

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9. Some aquatic bacteria and lightning can also change nitrogen to nitrates.

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WAYS HUMANS ALTER THE NITROGEN CYCLE

• The rate of nitrogen fixation has doubled since the 1950s.

• Fertilizers: contain nitrogen…place on lawn & farmlands

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WAYS HUMANS ALTER THE NITROGEN CYCLE

• Burning of fossil fuels: releases nitrogen during combustion

• Destruction of forests & wetlands: release nitrogen thru decay

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CONSEQUENCES

• Ecosystems: Nitrogen additions to the soil can lead to changes that favor weeds over native plants, which in turn reduce species diversity and changes ecosystems.

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• Research shows that nitrogen levels are linked with changes in grassland species, from mosses and lichens to grasses and flowers.

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• Precipitation: Nitrogen oxides react with water to form nitric acid, which along with sulfur dioxide is a major component of acid rain.

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• Acid rain can damage and kill aquatic life and vegetation, as well as corrode buildings, bridges, and other structures.

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Air quality: High concentrations of nitrogen oxides in the lower atmosphere are a precursor to tropospheric ozone, which is known to damage living tissues, including human lungs, and decrease plant production.

Page 59: Matter and Biogeochemical  Cycles

Water quality: Adding large amounts of nitrogen to rivers, lakes, and coastal systems results in eutrophication, a condition that occurs in aquatic ecosystems when excessive nutrient concentrations stimulate blooms of algae that deplete oxygen, killing fish and other organisms and ruining water quality.

Page 60: Matter and Biogeochemical  Cycles

PHOSPHORUS CYCLE

•Phosphorus is not a gas and does not enter the atmosphere.

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•Phosphorus cycles from land to ocean and then back to land.

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•Water runs over rocks that contain phosphorus and places it in the water and soil. Plant roots absorb phosphorus.

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•Phosphate makes up DNA. Animals get phosphates thru food. Phosphorus is release by decomposition.

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• Loss of land because of clear cutting and erosion of farmland.

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•When we use soaps and detergents with phosphorus it integrates into our groundwater.• Fertilizers

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Page 67: Matter and Biogeochemical  Cycles

Phosphorus video

Phosphorus cycle video

Page 68: Matter and Biogeochemical  Cycles

Oxygen CycleThis cycle only consists of

photosynthesis & respiration. Photosynthesis & respiration are OPPOSITE reactions & they rely on each other.

Page 69: Matter and Biogeochemical  Cycles

Plants produce OXYGEN through the process of photosynthesis. Animals take in the oxygen from the air & change it into energy & release carbon dioxide through the process of respiration.

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Photosynthesis

• 6CO2 + 6H20 +Sunlight -> C6H12O6 + 6O2

CHLOROPHYLL

Page 71: Matter and Biogeochemical  Cycles

Respiration

C6H12O6 + 6O2 --> 6H2O + 6CO2 + 36 ATP

Page 72: Matter and Biogeochemical  Cycles