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3 Forms of Energy Transfer

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Presentation on theme: "3 Forms of Energy Transfer"— Presentation transcript:

1 3 Forms of Energy Transfer
1. conduction transfer of energy (mostly in solids) by collisions of particles 2. convection transfer of energy by currents moving through liquids or gases (caused by density differences) 3. radiation transfer of energy through empty space (no molecules needed) Ex. energy from the Sun 1. Conduction transfer of energy (mostly in solids) by collisions of molecules or atoms Air touching warm ground, feet touching cold floor, water touching pot 2. Convection transfer of energy by currents moving through liquids or gases (caused by density differences) Convection cells in magma, in atmosphere, boiling water 3. Radiation transfer of energy through empty space (no molecules needed) Ex. energy from the Sun visible light, UV, & other electromagnetic (EM) waves

2 Recycling of Materials Amongst Earth’s Spheres
Earth is constantly recycling materials maintains an overall balance through biogeochemical cycles water carbon etc.

3 Solar Energy Drives the Water Cycle
condensation

4 The Water Cycle 1. precipitation water that falls from clouds to Earth
drizzle, rain, snow, sleet, hail

5 2. infiltration 3. ground water water soaks into soil from the surface
water under the ground; soil is saturated

6 4. evaporation warmth from Sun causes liquid water to turn into water vapor evaporation 5. transpiration when plants give off water vapor through stomata in their leaves

7 6. condensation water vapor cools until it turns back into liquid
forming clouds, fog, or dew condensation

8 Groundwater Pollution
pollutants in soil carried by infiltration into groundwater oil nitrates & phosphates from fertilizers pesticides farm wastes sewage salt to melt ice chemicals & hazardous wastes and more… can be a reason for site to be designated a “brownfield” remediation (clean up )  expensive prevention  best

9 Carbon Cycle Driven chemical & physical processes
Psyn & respiration, combustion

10 Changes in CO2 & Climate CO2 levels have risen steadily since mid-1800s primarily due to human activities combustion of fossil fuels coal gasoline natural gas deforestation decreased photosynthesis

11 Changes in CO2 & Climate avg. global temps have  ~1°C since late 1800s Possible effects: sea-level rise more/stronger storms/hurricanes more frequent heat waves/droughts relocation of major crop-growing areas

12 Common Air Pollutants air pollutant
any airborne gas or particle concentrated enough to harm people or the environment natural causes volcanoes forest fires human causes combustion of fossil fuels (automobiles, factories, etc.)

13 Acid Rain pollutants (SOX & NOX) react w/ H2O vapor in air
acidity measured using pH effects harm to plants/animals damage to structures made of limestone/marble remember… carbonates bubble in acid

14 Weathering breakdown of rocks at Earth’s surface 2 types: chemical
mechanical (physical)

15 Chemical Weathering rock is broken down by chemical action
changed into new substances agents include acids & oxygen

16 rainwater  naturally acidic
Chemical Weathering rainwater  naturally acidic CO2 dissolved in rainwater  carbonic acid can weather carbonate-based rocks ex. marble & limestone (CaCO3) Ex. Marble & Limestone  not best to use for buildings/monuments caves carved out of limestone by chemical weathering

17 other rocks are very resistant to acid and do not weather easily
quartz-based rocks ex. quartzite & sandstone (SiO2) Quartzite & sandstone  more resistant, so better to build w/

18 Mechanical (Physical) Weathering
rock is split, cracked, or broken into smaller pieces of the same material NOT changed into new substances

19 The Rock Cycle Rock Cycle Movie continuous process causing rocks to change from one form to another caused by interactions between water, air, and land

20 3 Major Classes of Rocks sedimentary metamorphic igneous
BrainPop 3 Types of Rocks sedimentary formed by compaction & cementing of layers of sediments metamorphic formed by effects of heat & pressure on other rocks igneous formed by solidification of hot, molten rock sedimentary formed by the compaction and cementing of layers of sediments (rock fragments, plant and animal remains, minerals that settle out of solution onto lake and ocean bottoms) igneous formed by cooling and hardening of hot, molten rock (magma) inside Earth metamorphic formed by the effects of heat and pressure on other rocks

21 Sedimentary Rocks made of sediments cover most of Earth’s surface

22 Metamorphic Rocks metamorphism
process by which a rock’s structure is changed by pressure & heat

23 Examples of Metamorphic Rocks & What They Formed From
granite  gneiss shale  slate  phyllite  schist limestone  marble sandstone  quartzite

24 Igneous Rocks form due to MELTING & solidification Intrusive Extrusive
magma cools slowly deep inside Earth crystals  medium to coarse texture Extrusive lava cools quickly on/above surface of Earth crystals  very small or not seen at all

25 Convection Currents in Magma
drives plate tectonics Convection cells (caused by density differences) in the asthenosphere (mantle) cause hot material to rise, move outward (pushing the plates/ridge push), & sink as the material cools (pulling plates down/slab pull). Convection in the Mantle Animation

26 What Is Plate Tectonics?
theory that describes formation, movements, & interactions of Earth’s lithospheric plates

27 Types of Plate Boundaries
Earth’s lithosphere is broken in to large plates plate boundaries determines type divergent convergent transform

28 Divergent Boundaries plates move apart most are along ocean floor
mid-ocean ridges  molten rock forces through cracks (rifts) in valley

29 Mid-Ocean Ridge Mid-Atlantic Ridge

30 Convergent Boundaries
plates move closer together Oceanic plate subducts (plunges) below another plate Boundary between the 2 plates is called a subduction boundary Features of subduction boundaries Deep-sea (or ocean) trenches Deepest part of the ocean Volcanic activity Island arcs Along the coast of continents Earthquakes

31 Transform Plate Boundary
Transform Boundary--San Andreas Fault Animation plates slide past each other at fault stress released  earthquake Ex. California—San Andreas Fault N

32 Locations of Earthquakes & Volcanoes
occur in concentrated plate boundaries strain builds up  earthquakes molten rock rises  volcanic activity Pacific Ocean  Ring of Fire Ring of Fire Plates & Volcanoes Video


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