Understand the methods of scientific inquiry Scientific Method:1. Pose a Question2. Form a Hypothesis3. Test4. Observe/Record Data5. Form a Conclusion (comparing data, making judgements)6. Gather Additional Data7. Write ReportReports should have:-Title-Abstract-Purpose and Hypothesis-Description of Experiment to Prove/Disprove Hypothesis-Supporting Data-Observations-Conclusions
Understand:-Independent Variables-Dependent Variables-Control Variables-Sources of Error
Slide 2
The Nature of Science
The Nature of Scientific Knowledge:-It is subject to change-It is based on evidence-It is based on evidence that can be reproduced
The Nature of Scientific Knowledge:-It is subject to change-
The Common Units of Measurement:Deci: prefix for 1/10th of a unitCenti: prefix for 1/100th of a unitMilli: prefix for 1/1000th of a unitDeca: prefix for 10 times a unitHecto: prefix for 100 times a unitKilo: prefix for 1000 times a unitKnow the Common Units of Measurement for:-Length-Time-Mass-Volume-Energy-Pressure-Force
Slide 3
Organization and Presentation
Understand Scientific Notation and Significant Digits!Data can be Presented and Organized with:-Tables-Charts-GraphsBasic Error Analysis:
Precision
Accuracy
Know the differences between these!
Be Able to Calculate Averages:-Mean-Median-ModeInterpret and Draw Conclusions from Data:
Trends in the data
Relationships between variables
Predictions based on data
Drawing conclusions based on evidence
Slide 4
Safety in the Lab
Be familiar with procedures for:
Safe Storage
Safe Preparation
Proper and Safe Disposal
Use of Equipment like Fume Hood
Use of Safety Equipment: Eyewash Stations and Safety Showers
Appropriate Behavior and Apparel
Minor Burns and Injuries
Mishaps, Fires, and Chemical Spills
Evacuation
Know How to Use Standard Equipment:
Thermometers
Microscopes
Barometers
Graduated Cylinders
Bunsen Burners
Balances
pH Meters
Slide 5
Major Historical Contributions
Understand How Major Concepts Developed Over Time:
Atomic Model
Genetics
Plate Tectonics
Slide 6
Principles of Matter and Energy
Structures and Properties of Matter:Soldis, liquids, gases, and plasmasElements, atoms, compounds, molecules, and mixturesOccurrence and abundance of elements and their isotopesForms of Kinetic and Potential Energy:-Thermal Energy-Chemical Energy-Radiant Energy-Mechanical Energy
Relationships Between Energy and Matter:
Conservation of Energy (First Law of Thermodynamics)
Entropy Changes (Second Law of Thermodynamics)
Conservation of Matter in Chemical Systems
Energy Transformations
Chemical and Physical Property Changes
1st Law of Thermodynamics: Mechanical and internal energy are conserved2nd Law of Thermodynamics: Heat only flows from hot to cold until it reaches equilibrium3rd Law of Thermodynamics: Absolute zero temperature can never be reached
Slide 7
Measurement Scales
Measurement of Temperature:
Celsius
Fahrenheit
Kelvin
Know how to compare and convert these scales!Kelvin Scale: Based on temperatures and volumes of gases
Methods of Heat Transfer:
Convection
Radiation
Conduction
Measurement of Thermal Energy:
Specific Heat Capacity
Joules
Slide 8
Applying Energy and Matter Relationships
Understand the Role of Energy and Matter in:
Trophic levels
Matter cycle/energy flow in ecosystems
Convection currents in atmosphere, ocean, and mantle of the Earth
Conservation of mass in the rock cycle
Nitrogen cycle
Chemical and physical changes in rocks
Solar radiation's impact on Earth and life
Photosynthesis
Cellular respiration
Energy transformations in living systems
Slide 9
Basic Structure of the Atom
Atomic Model
Atomic Structure: Electrons, protons, neutrons
Atomic Number
Atomic Mass
Ions
Electron Arrangements
Radioactivity:
Radioisotopes
Radioactive Decay
Half-Life
Fusion
Fission
Application of Radioactivity:
Carbon Dating
Evidence for Evolution
Medical Imaging
Radioactive Decay: The most common nuclear reaction. This means the nucleus is unstable.
Slide 10
The Physical Sciences
Understand Mechanics:
Speed
Velocity
Acceleration
Momentum
Friction
Work, energy, and power
Mass, weight, and gravity
Newton's First Law of InertiaNewton's Second Law (F=MA or Force=Mass times Acceleration) This is also known as "work", action caused by a force. Newton's Third Law: Equal and opposite action-reactionEnergy: The ability to do workMomentum=mass x velocity Understand Simple Machines
Characteristics of Gravitation:
Gravitational Attraction
Acceleration due to Gravity
Mass
Distance
Distinguish Between Mass and Weight! Analyze Motion and Forces in Problems that Involve:-Inclined Planes-Collisions-Projectile Motion-Periodic Motion-Pendulums-Springs-Planetary Objects
Slide 11
Physical Properties
Physical Properties of Fluids:
Buoyancy
Density
Pressure
Electrical Nature of Materials:
Electric Charges
Electrostatic Attraction and Repulsion
Conductivity, Conductors, and Insulators
Analyze Electric Circuits:
DC and AC Current
Current, Resistance, Voltage, and Power
Ohm's Law
Voltage Sources:
Batteries
Generators
Magnetic Fields and Forces:
Magnetic Poles
Attractive and Repulsive Forces
Electromagnets
Ohm's Law: Voltage Difference (V)=Current (I) x Resistance (R)Voltmeter: Measures the Potential Energy (PE) in an electric circuit. Ammeter: Measures current on a circuit. Resistors: Regulate volume-measured in Ohms.
Slide 12
Waves and Light
Characteristics of Light and the Electromagnetic Spectrum:
Nature of Light
Visible Spectrum and Color
Ultraviolet, Infrared, Microwave, and Gamma Rays
Basic Characteristics and Types of Waves:
Transverse and Longitudinal Waves
Frequency
Amplitude
Wavelength
Speed and Intensity
Basic Wave Phenomena:
Reflection, Refraction, Diffraction, and Dispersion
Absorption and Transmission
Interference, Scattering, and Polarization
Doppler Effect
Basic Sound Phenomena:
Pitch/Frequency relationship to Loudness/Intensity
Sound-Wave Production, Air Vibrations, and Resonance
Basic Optics:
Mirrors
Lenses (Human eye, Microscopes, Telescopes)
Prisms
Fiber Optics
Polarized Light: Vibrations are confined to a single plane. Visible Light can be polarized by electric and magnetic fields.Visible Light: Part of the electrostatic spectrum. Contains photons. (Photons can be both waves and particles)
Slide 13
Waves
Longitudinal Waves (Sound):-The disturbance is parallel to the direction of motion, resulting in a spiral look. (Like a slinky)Transverse Waves (Water):-The disturbance is perpendicular to the direction of motion, making up and down swells. Pitch: The frequency of a sound wave. Wave Frequency:-Measured in Hertz-1 hertz=1/seconds
Loudness: The amplitude of the sound wave. The Period of a Wave is the time between disturbances.
Slide 14
The Periodic Table
Be Familiar with the Periodic Table Be Able to Predict the Properties (physical and chemical) of Elements Organization of Periodic Table:
Arranged in columns and rows
Groups/Families, periods
Includes symbol, atomic number, and atomic mass
Trends in chemical reactivity can be seen based on the position of the elements
Metallic and Non-metallic elements
Noble Gases
Trends in the Physical Properties on the Periodic Table:
Atomic Radius
Ionization Energy
Slide 15
Chemical Bonds
Covalent Bonding
Ionic Bonding
Hydrogen Bonding
Chemical Compounds:
Ionic Compounds
Covalent Compounds with Two Elements
Acids and Bases
Interpret Chemical Formulas:
Describe formulas in terms of mols and atoms
Percent composition
Empirical and Molecular formulas
Electron Dot Structure formulas
Know how to Balance Chemical Formulas:
Balance simple chemical reactions
Stoichiometric calculations with balanced equations
Use Chemical Formulas to Identify and Describe Simple Chemical Reactions:
Combustion
Oxidization (Rusting)
Neutralization
Single/Double Replacement
Slide 16
Kinetic Molecular Theory of Matter:
Particles are in constant motion
Speed and energy of gas particles are related to temperature.
Ideal Gas Laws:
Charles' Law: Volume is proportional to Energy
Boyle's Law: Pressure is inversely proportional to Volume
Phase Changes:
Melting/Freezing
Vaporization/Condensation
Sublimation
Heating/Cooling Curves
States of Matter and Changes
Energy Relationships:
Endothermic Reactions
Exothermic Reactions
Factors that Affect Reaction Rate:
Concentration
Temperature
Pressure
Catalysts/Enzymes
Slide 17
More Chemistry
Acid-Base Chemistry:
Know the chemical and physical properties of acids and bases
pH scale
Neutralization
Buffers
Solutions and Solubility
Diluted and Concentrated
Saturated, Unsaturated, and Supersaturated
Solvent and Solute
Identify different solutions
Concentrations of solutions in terms of molarity
Factors Affecting the Dissolving Process and Solubility of Substances:
Effect of temperature and particle size on dissolving
Effect of temperature on solubility
Polar vs. Nonpolar Solvents and Solutes: Like dissolves like
Ionic compounds dissociate into ions when in a solution (Electrolytes)
Slide 18
Life Sciences
The Structure and Function of Cell Membranes:
Passive/Active Transport
Osmosis
Know the Structure and Function of All Cell Organelles Levels of Organization:
Cells
Tissues
Organs
Organ Systems
Major Cell Types:-Muscle-Nerve-Epithelial
DNA Structure
Replication, Transcription, and Translation
Dominant and Recessive Alleles
Mendelian Inheritance:
Genotype
Phenotype
Punnett Squares
Mutations, Chromosomal Abnormalities, and Common Genetic Disorders Genetic Variation Processes:
Mutation
Sexual Recombination
Slide 20
Taxonomy
Father of Taxonomy: Carolus Linneaus Binomial Nomenclature: Modern Taxonomy uses this classification system. Every species has a two part name (genus and species). King (Kingdom)Phillip (Phylum)Should (Subphylum)Cook (Class)Our (Order)Family (Family)Good (Genus)Spaghetti (Species)There are 5 Kingdoms:1. Animalia2. Monera3. Protista4. Fungi5. Plantae
Kingdom Protista: (First lifeforms on Earth)-Eukaryotic-Unicellular-Some can photosynthesize -Some are consumers Kingdom Monera: (Algae and bacteria)-Prokaryotic-Unicellular-No nucleus Kingdom Fungi: -Eukaryotic-Multicellular-Absorption consumers
Slide 21
Evolution and Ecology
Mechanisms of Evolution:
Natural Selection
Punctuated Equilibrium
Isolation Mechanisms and SpeciationDarwin's 4 Principles:1. Species vary in genetics2. Variations sometimes stem from genetics3. More individuals are produced than will survive4. Certain traits allow for better survival Evidence Supporting Evolution:
Fossil Records
Comparative Genetics
Homologous Structures
Comparative Anatomy
Embryology
Molecular Biology
Observed Changes
Key Aspects of Ecology:Population Dynamics-Growth Curves-Carrying Capacity-Behavior such as Territoriality-Mating Systems-Social SystemsCommunity Ecology-Niche-Succession-Species Diversity-Interspecific Relationships (Predator-Prey, Parasitism)
4 Important Behaviors in Organisms:1. Competitiveness2. Instinctiveness 3. Territoriality 4. Mating
Slide 23
Cell Theory
Robert Hooke: Discovered cell walls in 1665 using a cork.Virchow: Concluded all cells come from pre-existing cells in 1858.
Cell Theory: All living this are composed of 1 or more cells.Modern Cell Theory:
Energy flow occurs in all cells
Cells contain DNA passed down
They grow
They adapt
All organisms share Carbon in common!
Slide 24
Ecosystems
Biomes:1. Marine2. Tropical Rainforest3. Savana4. Desert5. Temperate Deciduous Forest6. Taiga7. Tundra8. Polar/Permafrost Stability and Disturbances-Glaciation-Global Warming EffectsEvidence of Continental Glaciation:1. Abrasive Grooves2. Boulders from North found in South3. Cirques Present (Valleys formed by glaciers)
Theories of Glaciation:-Plate Tectonics-Earth's Orbit-The Changes in Axis Angle Types of Glaciers:-Valley Glaciers (Sharp, peaked mountains)-Continental Glaciers (Smooth mountains)
Energy Flow-Trophic Levels-Food WebsBiogeochemical Cycles
-Water Cycle-Nitrogen Cycle-Carbon Cycle-Biotic/Abiotic InteractionsThe Water Cycle:
Evaporation
Condensation
Precipitation
Runoff
Slide 25
Earth and Space Sciences
Know the Characteristics of Rocks and Their Formation Processes:
Igneous
Metamorphic
Sedimentary
Metamorphic Rocks: Are either Unfoliated (marbled, banded) or Foliated (compressed, striped). They are made under great pressures, and at high temperatures. Igneous Rocks: Known for their texture, composition, and the way they form. Can be Intrusive (below the Earth's surface) or Extrusive (at the surface). Sedimentary Rocks: Made first by compaction, then cementation, and then lithification (sediments transformed into solid rocks).
Erosion and Deposition
Agents of Erosion
Chemical and Physical (Mechanical) Weathering
Porosity and Permeability
Runoff and Infiltration
Characteristics of Soil:
Types of Soil
Soil Profile
Slide 26
Know the Characteristics of Minerals and Their Formation Processes:
Classes of Minerals
Classes of Crystals
Hardness
Mineral Type Determined By:1. Chemical Composition2. Crystal Structure Polymorphs: 2 or more minerals with the same chemical composition but different crystalline structures. Silicate is the most abundant mineral.
Slide 27
Earth Science
Earth's Layers:
Lithosphere
Mantle
Core
Earth's Shape and SizeGeographical Features:
Mountains
Plateaus
Mid-Ocean Ridges
Earth's Magnetic Field
Plate Tectonics Theory and Evidence to Support:
Folding and Faulting
Continental Drift
Magnetic Reversals
Characteristics of Volcanos:Types of Volcanos-Shield Volcanos (Quiet, Largest Mountains)-Cinder Cone Volcanos (Explosive, Small)-Composite Volcanos (Built by Lava and Ash of Cinder Cone)
Lava
Eruptions
Characteristics of Earthquakes:
Epicenters
Faults
Tsunamis
Seismic Waves and Triangulation
Slide 28
Tectonics
Tectonic Plates: Blocks of Earth's rigid crust on the upper mantle (Lithosphere)Subduction: When a dense plate collides with a less dense plate and slides under the lighter one, plunging into the mantle. (Subduction zones often seen on sea floor as a trench)Rifting: Boundaries form between spreading plates as the crust is pushed apart. Plate Boundaries: Plates that interact through spreading, pressing, and sliding. (Many volcanos, mountain ranges, and earthquake zones are found on plate boundaries.)
Faults: Fractures in the surface crust that are created by tension or compression. Support of Plate Tectonic Theory:
Mesosaur Fossils found in East South America and South Africa
Rocks in East Brazil found in North West Africa
Appalachian Mountains in US match the ranges in Europe
Alfred Wegener: In 1915 he advanced the continental drift theory by suggesting that a Pangea existed 200 million years ago.
Slide 29
Historical Geography
Principles of UniformitarianismBasic Principles of Stratigraphy (classifying rocks by observing their superposition)Law of SuperpositionRelative and Absolute Time:
Index Fossils
Radioactive Dating
Absolute Dating: Radioactivity to accurately determine ages
Geologic Time Scale:
Eons (Most recent is Phanerozoic Eon-beginning of life)
Eras (Paleozoic-ancient life, Mesozoic-middle life, Cenozoic-recent life)
Periods (Cambrian-Paleozoic Era, Triassic, Jurassic, and Cretaceous-Mesozoic Era, Tertiary and Quartenary-Cenozoic Era)
End of an Era:1. Uplifting of Crust2. Extinction of Dominant Plants/Animals3. Appearance of New LifeImportant Events In Earth's Geologic History:
Mass Extinctions
Cambrian Explosion
Ice Ages
Meteor Impacts
Slide 30
Earth's Bodies of Water
Geographic Location of Oceans and SeasTides, Waves, and CurrentsEstuaries and Barrier IslandsIsland, Reef, and Coral FormationPolar Ice Caps, Icebergs, and GlaciersLakes, Ponds, Streams, Rivers, and River DeltasGroundwater, Water Table, Wells, and Aquifers
Properties of Water that Affect Earth's Systems:
Density changes when frozen (ice floats on water)
High high capacity
Polar solvent
Hydrogen bonding
World Weather Influenced By: Ocean surface currents in upper layerSurface Currents-Caused by winds (winds classified by temperature)Ocean Currents-Caused by differences in density Waves-Caused mainly by windsOcean Movement:-Wind-The Sun's heat energy-Earth's rotation-Moon's gravitational pull-Underwater Earthquakes
Slide 31
Basic Meteorology
The SUN:
Core-Place of inner fusion
Photosphere-Surface, sun spots
Chromosphere-Hydrogen gas causes it to be red, solar flares common
Corona- Transparent, only visible during an eclipse
Solar Flares: Excited protons and electrons shoot out from the sun. When they reach Earth they can interfere with radio and magnetic fields. Perihelion: When the Earth is closest to Sun (January)Aphelion: When the Earth is farthest from the Sun (July)
Galaxies: A vast collection of starsStars must have a 7% greater mass than the SunPlanets/Brown Dwarf: Bodies with a mass less than 7% of SunStar Life:1. Mass of gas and dust (Nebula)2. Main Sequence Star3. Red Giant Star4. Nova Star 5. White Dwarf, Neutron (after supernova), or Black Hole Normal Star life requires HEAT and ENERGY. This comes from the conversion of hydrogen into helium. Brightness of Star Measured Through:-Magnitude (how bright the star appears to humans)-Luminosity (intrinsic brightness radiated by star per second, in watts)
Slide 32
Astronomy
3 Ways Astronomers Measure Distance in Space:1. Astronomical Unit (AU)-distance between Earth and Sun (150x10^6 km)2. Light Year (LY)-9.5x10^12 km-63,000 AUs3. Parsec (PC)-3.62 LYsSpectrograph: Photographs the sunSpectroscope: Measures temperature, spectra, pressures, and star movement
Hubble Telescope: Single-reflector mirrorRadio Telescope: Collects invisible radio waves created by the sun and stars.Refracting Telescope: Invented by Galileo. Lenses bend light and focus it. Reflecting Telescope: Invented by Sir Isaac Newton. Mirrors gather light onto a curved mirror, focusing small image.
Slide 33
Space Science
Terrestrial Planets: Have thin atmospheresJovian Planets: Gaseous, thick, atmospheresPlanet's Ability to Retain Atmosphere Depends on:-Mass-TemperatureEarth's Galaxy: Spiral, disc-shaped galaxy in the Milky WayElliptical Galaxy: Contains little gas/dust, millions/trillions of starsIrregular Galaxy: No real structure, early stagesOscillating Universe Model:-Universe will expand and contract-New big bang will happen again
The Big Bang: 20 billion years ago-explosion formed by helium and hydrogen.2 Hypothesis of Solar System Origin:*Condensation Hypothesis-Began with rotating clouds of dust/gas-Condensed in the middle, forming the Sun-Smaller clouds formed the planets-Widely accepted hypothesis*Tidal Hypothesis-Near collision of Sun and large star-Gravity pulled the Sun's hot gases out-Few support this hypothesisBlack Hole: Star with condensed matter and gravity so intense that nothing escapes it, even light.Tilt of Earth's Axis: 23.45 degrees-reason for 4 seasons
Slide 34
Astronomy Terms
Meteoroid: Particles of rock and metalMeteor: Meteoroid burning in the Earth's atmosphereMeteorites: Meteors that strike the surfaceAsteroids: Rocks generally found between Mars and JupiterComets: Frozen gases, cosmic dust, and rocky particles-Nucleus-Coma-Tail (always points away from the sun)Halley's Comet: Returns every 75-76 years
Mercury: Craters, rocks (Terrestrial)Venus: Slow rotation, rotates opposite way, heavy cloud cover (Terrestrial)Mars: Craters, active/extinct volcanoes, red surface from iron oxide, atmosphere similar to Earth, polar regions and ice caps. (Terrestrial)Jupiter: Largest, 16 moons, strong magnetic field, gaseous, Great Red Spot (Jovian)Saturn: 2nd largest, rings of ice/rock/dust, 20 satellites (Jovian)Uranus: 10 dark rings, 15 satellites (Jovian)Neptune: 3 rings, 2 satellites (Jovian)Pluto: Reconsidered as not a planet, rocky, 1 satellite, 250 year revolution around Sun
Slide 35
Moon and Sun
Time between each full moon: 29.53 days The Moon orbits Earth every 27 daysFull Moon, Waning Gibbous, Third Quarter, Waning Crescent, New, Waxing Crescent, First Quarter, Waxing Gibbous, FullWinter Solstice: When the Sun is farthest from Earth's equator. This occurs in December and the Southern Hemisphere leans towards the Sun.Summer Solstice: When the Sun is farthest from Earth's equator. This occurs in June and the Northern Hemisphere leans towards the Sun.
Neap Tides: Weak tides due to the position of the Sun and Moon. They are positioned at a 90 degree angle around Earth.Tidal Bulge: Large tides due to the position of the Sun and Moon. They are positioned directly across from one another.