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Energy Resources. Renewable vs. Nonrenewable Renewable Resources –Resources that are naturally replenished or regenerated over a short time span – it.

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Presentation on theme: "Energy Resources. Renewable vs. Nonrenewable Renewable Resources –Resources that are naturally replenished or regenerated over a short time span – it."— Presentation transcript:

1 Energy Resources

2 Renewable vs. Nonrenewable Renewable Resources –Resources that are naturally replenished or regenerated over a short time span – it is renewed on a human time scale –i.e. Trees, biofuels (?) Nonrenewable Resources –Resources that are consumed faster than they can be replenished, it is not renewed on a human time scale –i.e. fossil fuels, aluminum, etc.

3 Sources of Energy

4 Nonrenewable sources –Petroleum (38%) –Coal (22%) –Natural Gas (25%) –Nuclear (8%) Renewable sources –Hydroelectric (4%) –Solar –Wind –Tidal –Geothermal –Biofuels

5 Trends in Energy Usage

6 Coal Organic materials that have escaped oxidation in the carbon cycle. Plant material that is rapidly buried

7 Coal Ranking & Formation Rank – amount (%) of carbon (C) in coal, heat content 1.Peat (pre coal) – soft brown mass of compressed, largely non- decomposed plant material, ~50% C 2.Lignite – decomposed peat that has been compressed, ~70% C 3.Bituminous coal – burial increases the pressure and temperature on the lignite and causes a conversion, ~80-90% C 4.Anthracite coal – complete metamorphism, >93% C

8 World-wide distribution of coal

9 U.S. Coal Reserves

10 Illinois Coal Reserves

11 Hydrocarbons Composed of hydrogen and carbon linked together in chains and rings Natural Gas – simple organic molecules Crude Oil – complex chains and rings

12 What is the source of oil? Plankton! 0mm1mm

13 Hydrocarbon Formation Water borne plankton escape oxidation/decomposition before burial Source RockPlankton is deposited in mud (shale) – Source Rock Source rock is overlain by more sediment – increasing the pressure (P) & temperature (T) on the source rock Increase in P & T, breaks down organic debris –Oil forms at 50 o C –Methane (natural gas) at 100 o C reservoir rock (Hydrocarbons migrates upwards (lower density than water) to a reservoir rock (high porosity, high permeability rock) Migration is stopped by either an impermeable rock or a structural trap

14 “Oil Window” Generation of oil requires a specific temperature range 80 – 160 C o (If above this temperature oil will “burn away”) Higher temperatures breakdown oil molecules – generate natural gas Exist in the top most 15-20% of the crust

15 Reservoir Rock Porosity – amount of open (void) space in a rock, ability of a rock to store a fluid Permeability – interconnectedness of the void space, ability of rock to transmit a fluid Reservoir rock – high porosity, high permeability low permeabilityCap (seal) rock – low porosity, low permeability

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17 Structural Traps 4 common types –Anticline Trap –Salt Dome –Fault Trap –Angular Unconformity Trap

18 Fig. 14.28 W. W. Norton

19 Found in rocks less than 500 million years old 85% of oil and gas occur in less than 5% of producing fields Generally, near Tectonic belts, active in the past 60-70 million years Distribution of Oil and Gas

20 Daily Assignment Create a concept map that incorporates the following: OilCoal Plant MaterialPlankton FoldsFaults SandstoneShale Labels the pathways-transition between the components appropriately Additional items may be included if you feel they help understand the concepts.

21 Uranium (U) – used for nuclear power Has a Minimum Concentration Factor > 1000 Source Rock – Igneous U is leached (dissolved) into groundwater Deposit Types –Sandstones that have been enriched with U minerals (groundwater enrichment) –U-bearing minerals in rock fractures –Placer Deposits Nuclear Power - Uranium

22 Hydroelectric and Tidal Power Movement of water drives turbines Dams – gravity key force Tidal – tidal force, need a tidal range of > 8 m (nearly impractical)

23 Geothermal Energy Temperature increases with depth ~ 3 o C/ 100 m Geothermal energy concentrated where magma is near the surface Circulation of groundwater allows water to heat up Hot groundwater drives turbines


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