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.500\,B.C.): First proposed a spherical Earth based on aesthetic grounds rather than physical evidence.
    • Aristotle (384322B.C.384-322\,B.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 1AU1\,AU, which equals 1.496×108km1.496 \times 10^8\,km.
  • Mass of Earth: Approximately 5.974×1024kg5.974 \times 10^{24}\,kg.
  • Diameter Details:
    • Equatorial Diameter: 12,756km12,756\,km.
    • Polar Diameter: 12,714km12,714\,km.
    • Equatorial Bulge: The diameter is wider at the Equator.
  • Circumference Details:
    • Equatorial Circumference: 40,075km40,075\,km.
    • Polar (Meridional) Circumference: 40,008km40,008\,km.
  • Orbital and Rotational Periods:
    • Rotational period: 23.9345hours23.9345\,hours.
    • Orbital period: 365.256days365.256\,days.
  • 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 (N2N_2): 78%78\%.
    • Oxygen (O2O_2): 21%21\%.
    • Carbon dioxide (CO2CO_2): 0.03%0.03\%.
    • Other gases: 0.97%0.97\%.
  • Layers of the Atmosphere:
    1. Troposphere: The lowest layer where humans live. Contains 75%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 (710km7-10\,km at poles, 1718km17-18\,km at the equator).
    2. Stratosphere: Extends to 50km50\,km. Contains the Ozone layer, which absorbs ultraviolet (UV) radiation, causing temperature to increase with height. Upper boundary is the Stratopause.
    3. Mesosphere: Extends from 50km50\,km to 85km85\,km. Temperature decreases with height. Contains the coldest temperatures (approx. 90C-90^{\circ}C) at the Mesopause (boundary with thermosphere).
    4. Thermosphere: Extends from 90km90\,km to 5001,000km500-1,000\,km. Temperature increases with height due to absorption of X-rays and UV radiation. Boundary is the Thermopause.
    5. Exosphere: The highest layer, located between 700km700\,km and 10,000km10,000\,km above the surface.

Structure of the Earth: Internal Structure

  1. The Crust: The coldest, outermost layer made of solid rock (basalt and granite).
    • Oceanic Crust: Denser, 510km5-10\,km thick, mainly basalt.
    • Continental Crust: Less dense, thicker, mainly granite.
  2. 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.
  3. The Core: The hot, dense center composed of iron and nickel alloy. Temperatures reach up to 12,000F12,000^{\circ}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: 23hours23\,hours, 56minutes56\,minutes, and 4seconds4\,seconds (Standard day length: 24hours24\,hours).
    • Effects: Diurnal cycle (day and night); time differences (1hour1\,hour per 1515^{\circ} of longitude); deflection of winds and currents (Coriolis effect); daily rise and fall of tides.
  • Revolution: Motion of Earth around the Sun.
    • Duration: 365.24days365.24\,days.
    • Orbital Path: Elliptical.
    • Perihelion: Closest point to Sun (147millionkm147\,million\,km) on January 3rd.
    • Aphelion: Furthest point from Sun (152millionkm152\,million\,km) on July 4th.
    • Speed: Average 27km/s27\,km/s (faster at perihelion, slower at aphelion).
    • Seasons: Caused by Earth's tilt of 23.523.5^{\circ}. Solstices and Equinoxes define seasonal transitions.

Earth Systems and Cycles

  • Four Main Spheres:
    1. Geosphere (Lithosphere): Land, rocks, minerals, and soil.
    2. Atmosphere: Blanket of gases surrounding the planet.
    3. Hydrosphere: All water (liquid, vapor, and ice).
    4. 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:
    1. Rectilinear Motion: Moving in a straight line (e.g., walking on a straight road, a falling ball).
    2. Curvilinear Motion: Moving along a curved path (e.g., throwing a basketball, moon orbiting Earth). Circular motion is a special case.
    3. Rotatory (Rotational) Motion: An object spinning on its own axis (e.g., spinning top, Earth’s rotation, clock hands).
    4. 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:
    1. Contact Forces: Physical touch (e.g., frictional force, spring force).
    2. Non-contact Forces: Action at a distance (e.g., gravity, magnetism).
  • Gravitational Force (Gravity):
    • Discovered by Sir Isaac Newton (164217271642–1727).
    • 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 (NN).
    • Components: Hook (to hang body), Graduated scale (measurement units), Pointer (indicates weight), Spring (stretchesproportionaltoforcestretches proportional to force).
  • 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):
    1. Reduce: Use less energy and natural resources.
    2. Reuse: Use products more than once.
    3. 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?
    • Answer: The outer core.
  • Exercise 7.7, Question 1: Which is a nonrenewable energy resource?
    • Answer: Coal.
  • 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.