1. Biogeochemical cycles How matter cycles through systems

2. What are the components of a system? Inputs and outputs One way flow of energy Cycling of matter

3. Water, why is it important? Makes up >50% of mammal body weight Allows molecule move in and between cells Allows for plants to move nutrients Dissolves and removes toxic materials

4. Hydrologic cycle Aka water cycle, cycles water through the hydrosphere

5. Where is the water? 71% of Earth is covered in water but there isn’t enough fresh water to go around

6. Water cycle

7. 1.Evapotranspiration - Evaporation and transpiration that takes place on land. Due to solar energy 2.Condensation - Water in atmosphere cools and condenses around condensation nuclei 3.Precipitation - Downward movement of water from the sky 4.Infiltration and percolation -Conversion of surface water into ground water. I= Movement of water into the soil. -P=Downward movement of water THROUGH water. 5.Runoff -Due to gravity and nonpermeable material 6.Collection - Pooling of surface water

8. Looking closer at human impact Ground water contamination Pollutants get into water and are leached downward through soil to aquifers. Removal of vegetation and plant biomass Flooding and soil erosion Decrease evapotranspiration Increase surface runoff Decrease infiltration Water depletion withdrawal > replenishment

9. Human impact continued… Draining and filling in of wetlands Decrease purification of water and increases runoff Changing permeability of soil Increases runoff and pollutants Decreases amount of groundwater Limits purification of water Change in water quality Nitrogen and phosphates getting into water supple (will get to this later)

10. Question… What are 3 ways in which your lifestyle directly or indirectly affects the hydrologic cycle?

11. Carbon: why is it important Backbone of all organisms and most important element in living things 20% of total biomass Base of organic compounds Carbohydrates Lipids Proteins Nucleic acids

12. Cycling of carbon can be broken down into: FAST Associated with biotic components of cycle Photosynthesis Respiration Exchange SLOW Associated with the abiotic components of cycle Sedimentation and burial Extraction Combustion Without human activity the carbon cycle is at balance. Fast components of removal and input even each other out. Slow components of removal due to fossilization equal the slow process of weathering of carbon containing rocks

15. Question What are 3 ways in which your lifestyle directly or indirectly affects the carbon cycle?

16. Human impact on carbon cycle We have altered the balance of input and output of carbon in the atmosphere Removal of fossilized carbon and combustion of fossil fuels increase amount of CO 2 in atmosphere Increasing temperatures of atmosphere increases the amount of carbon absorbed by oceans creating carbonic acid (H 2 CO 3 ) and lowering the pH of ocean water. This prevents the formation of calcium carbonate (CaCO 3 ) Removal of carbon from biomass adds more Co s into atmosphere

17. Nitrogen cycle Nitrogen is a limiting factor for producers Biotic or abiotic component that controls / prevents growth Without nitrogen plants cannot survive 78% of atmosphere is N 2 but most living organisms cannot utilize this form of nitrogen Vital in the creation of amino acids, proteins, nucleic acids

18. Basic steps of the Nitrogen cycle

20. Human impact on the Nitrogen cycle Burning fossil fuels releases NO into the atmosphere which increases NO 2 in atmosphere (GHG) and can ultimately lead to creation of HNO 3 when mixed with water Production of synthetic fertilizers increases the amount of nitrate Removal of vegetation can deplete nitrogen from soil due to removal of nitrogen fixing bacteria. Too much fertilizer that isn’t assimilated by plants gets into water supply. This leads to increased primary production which ultimately results in fish kills due to hypoxic conditions.

21. Question What are two ways in which the carbon and the nitrogen cycle are linked

22. The Phosphorus Cycle Why do we need it? ATP Major component in Nucleic Acids Phospholipid bilayers Limiting Nutrient Falls below nitrogen in limiting ability but is none the less an important factor.

23. The phosphorus cycle IMPORTANT: THERE IS NO GASEOUS COMPONENT OF PHSOPHORUS. THEREFORE IT IS A VERY SLOW PROCESS AND MAINLY DEPENDENT ON WEATHERING OF ROCKS Since it has a slight negative charge it has the ability to bind positively charged soil particles. Phosphorus also does not dissolve very easily in water, but instead settles into the sediment and is therefore a limiting factor for aquatic locations.

26. Fertilizer use can add additional phosphorus into aquatic systems when moved with runoff This leads to increased algae growth and ultimately leads to hypoxic conditions Phosphates in detergents led to dead zones Manufacturers no longer use this in detergents as of 1994 for laundry and 2010 dishwashing Mining of rocks remove phosphates Deforestation leads to more phosphorus in water supplies Human Impact on P Cycle