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Chapter 2 - Earth as a System

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1 Chapter 2 - Earth as a System

2 The Earth’s Shape Earth appears to be a sphere.
Rotation causes flattening- called an oblate sphere 1. Centripetal Force –the force required to hold an object in a circular path a. Polar regions flatten b. Equatorial zone bulges

3 Gravity -the force of attraction that exists between all matter
Newton’s Law of Gravitation the force of the attraction between two objects depends on the masses of the objects. The more mass, the greater the attraction The force of attraction decreases as the distance between the objects increases (see figure 4, page 30) The force of gravity is measured in Newtons

4 Earth as a Magnet Earth can be thought of as a dipole (2-pole) magnet.
Earth's magnetic field lines are not as symmetrical as those of the bar magnet. The impact of the solar wind causes the lines facing sunward to compress, while the field lines facing away from the Sun stream back to form Earth's magneto tail. We call this magnetic field surrounding Earth the “magnetosphere”

5 Earth’s Layers Crust- Feldspars Mantle- Magnesium Iron Silicates Compositional Zones are based on the chemical makeup of each layer. These three zones are the layers of the Earth that you learned about in Elementary and Middle School. Core- Nickel and Iron

6 Earth’s Layers Lithosphere- SOLID Structural Zones are based on the state of the matter in each layer. Knowing whether a layer is molten or solid rock can help scientists understand and better predict the behavior of the crust’s movements Asthenosphere- PLASTIC Mesosphere- SOLID Outer Core- LIQUID Inner Core- SOLID

7 Define Compositional Zones:
Crust Two types: Continental Crust: Km thick Oceanic Crust: 5-10 km thick Made of feldspars Mantle 2900 km thick Composed of magnesium iron silicates Core 3500 km thick Composed of Iron and Nickel

8 Define Structural Zones:
Lithosphere km thick Solid and Brittle Asthenosphere km thick Plastic, flows Mesosphere 2400 km thick Solid Outer core Generates earth Magnetic field 2200 km thick Liquid Inner Core 2050 km thick

9 Ch 2-2: Systems Systems- an organized group of related objects or components that interact all systems have boundaries many systems have energy and matter that flow through them closed system- a system in which energy, but not matter is exchanged open system- a system in which energy and matter are exchanged Earth’s system- open, but very limited exchange of matter Meteors manmade space probes Open System Closed System

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11 Earth’s Energy budget Energy exchange on Earth is predictable following scientific laws 1st law of thermodynamics-energy cannot be created or destroyed 2nd law of thermodynamics- when energy is transferred, matter becomes more disorganized (entropy)

12 Sources of energy on Earth
External Sources Solar radiation (heating)- most important source of energy that drives all systems on earth bio- fuels plant growth hydro- drives ocean currents geo- breaks down rocks either though direct heating or erosion atmos- drives winds through uneven heating of Earth’s surface Sun/Moon’s gravity create tides and ocean mixing

13 Internal energy sources
Earth’s interior heated by radioactive decay Earth’s surface is cooler that interior causing hot materials to rise provides limited energy for limited life forms drives motion of tectonic plates

14 Chapter 2-3 Ecology- is the study of the relationship between living (biotic) and non-living (abiotic) things Ecosystems- a community of organisms and their abiotic (non-living) environment Producers: organisms which make their own food Consumers: Organisms which consume other organisms to get their energy Decomposers: organisms that break down decaying material for food

15 Ecological Balance Carrying Capacity- the largest population an environment can support at any given time Responses to change Ecosystems can recover from short term changes Ecosystems have difficulty recovering from long term changes

16 Energy Transfer Ultimate source of energy is SUN As matter cycles through the ecosystem, energy is lost through chemical reactions least amount of energy is available to consumers at the top of the food chain

17 Make a food chain from the food web below:


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