Grade 7 General Science: Units 6 & 7 - Earth in Space, Motion, Force, and Energy
Unit 6: Earth in Space – Introduction and Shape of the Earth
- Definition of Earth: Earth is one of the eight planets in our Solar System and is the only known planet to support life. Geologists study its materials, processes, products, physical nature, and history.
- Ancient Local Ideas (Flat Earth Assumption):
- Early Cultures: Ancient Greeks, Sumerians, Babylonians, Egyptians, and Vikings believed Earth was a flat disc or plane surrounded by water, based on immediate visual observation.
- Ancient Chinese: Believed Earth was a flat square shape surrounded by a round, egg-shaped heaven.
- Flat Earth Society: Claims Antarctica is an ice wall surrounding a disc-shaped Earth.
- Vantage Point Fallacy: Ancient people believed Earth was flat because it looks flat from the ground due to its enormous size.
- Historical Shift to Spherical Assumption:
- Pythagoras (500B.C.): First proposed a spherical Earth based on aesthetic grounds rather than physical evidence.
- Aristotle (384−322B.C.): Provided physical evidence for a sphere, including:
- Ships disappearing "hull first" when sailing over the horizon.
- Different constellations being visible at different latitudes.
- True Shape: Oblate Spheroid:
- Scientists describe the shape as an "Oblate spheroid."
- Oblate: Refers to a slight elliptical appearance.
- Spheroid: Means almost a sphere but not perfectly round.
- Physical Characteristics: Earth is flattened at the poles and bulges in the middle (equatorial bulge).
Evidences Supporting the Spherical Shape of the Earth
- Circumnavigation: Traveling across the world in a straight path (e.g., in a fast plane) leads back to the starting point.
- Earth’s Curved Horizon: Seen from ships, planes, or high cliffs. The horizon widens and becomes circular as altitude increases.
- Ship’s Visibility: When two ships approach at a distance, the front ship is seen before the back ship. On a flat surface, both would appear simultaneously.
- Sunrise and Sunset: Times vary by location. As Earth rotates West to East, Eastern locations see the sun earlier. On a flat Earth, everyone would see sunrise at the same time.
- Lunar Eclipses: The shadow cast by Earth on the moon is always circular. Only a sphere can consistently cast a circular shadow at all angles.
- Space Photographs: Rockets and satellites provide the most modern and convincing proof by capturing the curved edge of Earth.
- Changing Altitude of the Sun: The sun appears at low levels in the morning/evening and high levels at noon due to the curved surface.
Dimensions of the Earth
- Astronomical Unit (AU): The average distance from Earth to the Sun is approximately 1AU, which equals 1.496×108km.
- Mass of Earth: Approximately 5.974×1024kg.
- Diameter Details:
- Equatorial Diameter: 12,756km.
- Polar Diameter: 12,714km.
- Equatorial Bulge: The diameter is wider at the Equator.
- Circumference Details:
- Equatorial Circumference: 40,075km.
- Polar (Meridional) Circumference: 40,008km.
- Orbital and Rotational Periods:
- Rotational period: 23.9345hours.
- Orbital period: 365.256days.
- Angular Distance: Also called angular separation; it is the angle between two sightlines or point objects as viewed from an observer.
Structure of the Earth: External Structure (Atmosphere)
- Atmosphere Definition: A thin layer of gases held by gravitational attraction, containing abiotic (non-living) and biotic (microscopic organisms like bacteria) matter.
- Atmospheric Composition:
- Nitrogen (N2): 78%.
- Oxygen (O2): 21%.
- Carbon dioxide (CO2): 0.03%.
- Other gases: 0.97%.
- Layers of the Atmosphere:
- Troposphere: The lowest layer where humans live. Contains 75% of all air and almost all water vapor. Weather (clouds, rain, snow) occurs here. Temperature decreases with height. The boundary layer is the bottom; the top is the Tropopause (7−10km at poles, 17−18km at the equator).
- Stratosphere: Extends to 50km. Contains the Ozone layer, which absorbs ultraviolet (UV) radiation, causing temperature to increase with height. Upper boundary is the Stratopause.
- Mesosphere: Extends from 50km to 85km. Temperature decreases with height. Contains the coldest temperatures (approx. −90∘C) at the Mesopause (boundary with thermosphere).
- Thermosphere: Extends from 90km to 500−1,000km. Temperature increases with height due to absorption of X-rays and UV radiation. Boundary is the Thermopause.
- Exosphere: The highest layer, located between 700km and 10,000km above the surface.
Structure of the Earth: Internal Structure
- The Crust: The coldest, outermost layer made of solid rock (basalt and granite).
- Oceanic Crust: Denser, 5−10km thick, mainly basalt.
- Continental Crust: Less dense, thicker, mainly granite.
- The Mantle: The thickest layer between the crust and core. Composed of oxygen, silicon, and magnesium. Acts as a viscous liquid. The upper portion is the Asthenosphere.
- Lithosphere: The solid outer part consisting of the crust and the brittle upper portion of the mantle.
- The Core: The hot, dense center composed of iron and nickel alloy. Temperatures reach up to 12,000∘F.
- Outer Core: Liquid state due to high heat.
- Inner Core: Solid state despite higher temperatures because of extreme pressure.
Earth Movements and Their Effects
- Rotation: Motion of Earth around its axis (imaginary line through North and South poles) from West to East.
- Duration: 23hours, 56minutes, and 4seconds (Standard day length: 24hours).
- Effects: Diurnal cycle (day and night); time differences (1hour per 15∘ of longitude); deflection of winds and currents (Coriolis effect); daily rise and fall of tides.
- Revolution: Motion of Earth around the Sun.
- Duration: 365.24days.
- Orbital Path: Elliptical.
- Perihelion: Closest point to Sun (147millionkm) on January 3rd.
- Aphelion: Furthest point from Sun (152millionkm) on July 4th.
- Speed: Average 27km/s (faster at perihelion, slower at aphelion).
- Seasons: Caused by Earth's tilt of 23.5∘. Solstices and Equinoxes define seasonal transitions.
Earth Systems and Cycles
- Four Main Spheres:
- Geosphere (Lithosphere): Land, rocks, minerals, and soil.
- Atmosphere: Blanket of gases surrounding the planet.
- Hydrosphere: All water (liquid, vapor, and ice).
- Biosphere: All living organisms.
- Biogeochemical Cycles:
- Water Cycle: Evaporation (liquid to gas), Condensation (gas to liquid/clouds), Precipitation (rain, snow, hail), and Transpiration (water movement through plants).
- Carbon Cycle: Carbon atoms travel from atmosphere to Earth and back via photosynthesis, consumption, ocean intake, decay, and respiration.
- Nitrogen Cycle: Maintenance of nitrogen balance via Nitrogen fixation, Nitrification, Assimilation, Ammonification, and De-nitrification. Bacteria complete most steps except assimilation.
- Measurement of Large Quantities:
- GPS (Global Positioning System): Network of satellites to determine precise locations and measure continental drift.
- Laser Ranging (Laser Radar): Optical sensing technology for measuring Earth's size and plate motions.
Unit 7: Motion, Force, and Energy
- Definition of Motion: Continuous change of position from a reference frame over time.
- Types of Motion:
- Rectilinear Motion: Moving in a straight line (e.g., walking on a straight road, a falling ball).
- Curvilinear Motion: Moving along a curved path (e.g., throwing a basketball, moon orbiting Earth). Circular motion is a special case.
- Rotatory (Rotational) Motion: An object spinning on its own axis (e.g., spinning top, Earth’s rotation, clock hands).
- Oscillatory Motion: To-and-fro, back-and-forth, or up-down motion (e.g., pendulum, swinging swing, boat tossing on a river).
Force and Gravitational Force
- Definition of Force: A push or pull resulting from interaction with another object. An external agent that changes a body's state of rest or motion.
- Categories of Force:
- Contact Forces: Physical touch (e.g., frictional force, spring force).
- Non-contact Forces: Action at a distance (e.g., gravity, magnetism).
- Gravitational Force (Gravity):
- Discovered by Sir Isaac Newton (1642–1727).
- Attractive force between masses; always a pull, never a push.
- Weight: The measure of the pull of Earth's gravity on an object.
- Effects of Force:
- Move a stationary object.
- Change the speed of a moving object (acceleration/deceleration).
- Stop a moving object.
- Change the direction of motion.
- Change the shape or size of an object (deformation).
Measuring Force and Energy Concepts
- Measuring Device: Newton meter or Spring balance.
- Unit: Newton (N).
- Components: Hook (to hang body), Graduated scale (measurement units), Pointer (indicates weight), Spring (stretchesproportionaltoforce).
- Energy: A property of matter that can be transferred or converted but not created or destroyed.
- Forms of Energy: Chemical, Elastic, Electrical, Gravitational Potential, Heat/Thermal, Kinetic, Light, Sound, Nuclear/Atomic.
- Energy Conversion: Changing one form to another.
- Transducers: Devices that transform energy (e.g., Battery: Chemical to Electrical; Generator: Mechanical to Electrical; Motor: Electrical to Mechanical).
- Energy Sources:
- Renewable: Naturally replenished, inexhaustible (Solar, Wind, Geothermal, Hydropower, Biomass).
- Non-renewable: Finite, take millions of years to form, higher carbon footprint (Coal, Petroleum, Natural Gas, Nuclear).
Conservation and Environmental Issues
- Strategies for Conservation (The 3 R's):
- Reduce: Use less energy and natural resources.
- Reuse: Use products more than once.
- Recycle: Process used materials into new items.
- Resource Depletion: Exhaustion of raw materials (deforestation, overconsumption, mining).
- Environmental Degradation: Deterioration of the environment (air, water, soil) through depletion of resources, habitat destruction, and pollution.
- Human Causes: Urbanization, industrialization, overpopulation.
- Natural Causes: Floods, droughts, fires.
Questions & Discussion
- Activity 7.1 Question: When moving in a bus, are you at rest or in motion?
- Response: You are at rest with respect to the bus seat but in motion with respect to the ground.
- Exercise 6.1, Question 1: The Earth's actual shape is most correctly described as?
- Answer: An oblate sphere.
- Exercise 6.1, Question 2: Which object best represents a scale model of Earth?
- Answer: A Ping-Pong ball (due to being nearly spherical).
- Exercise 6.4, Question 2: Which layer of the earth is liquid?
- Exercise 7.7, Question 1: Which is a nonrenewable energy resource?
- Review Exercise Question: Why does an object thrown upwards come down?
- Response: Because of the force of gravity pulling it toward the center of the Earth.