Science Notes 2024 T4 PDF

Summary

These notes provide a summary of matter, atoms, atomic structures, and models, including important definitions and concepts, such as atomic models (Dalton, Thomson, Rutherford, and Bohr) and the periodic table. The notes also cover various concepts related to chemical bonding and compounds.

Full Transcript

**Matter, Atoms, and Atomic Structure** 1. **Definitions: Matter, Atom, Element**: - **Matter**: Anything that occupies space and has mass. It exists in various states: solid, liquid, gas, and plasma. - **Atom**: The smallest unit of an element that retains the proper...

**Matter, Atoms, and Atomic Structure** 1. **Definitions: Matter, Atom, Element**: - **Matter**: Anything that occupies space and has mass. It exists in various states: solid, liquid, gas, and plasma. - **Atom**: The smallest unit of an element that retains the properties of that element. An atom consists of a central nucleus made of protons and neutrons, surrounded by electrons in different energy levels or shells. - **Element**: A pure substance consisting of only one type of atom, characterized by a specific number of protons in its nucleus (atomic number). Examples include hydrogen, oxygen, and gold. 2. **Structure of an Atom**: - The atom is composed of three main subatomic particles: - **Protons**: Positively charged particles located in the nucleus. - **Neutrons**: Neutral particles also found in the nucleus. - **Electrons**: Negatively charged particles that orbit the nucleus in energy levels. - **Nucleus**: The dense central part of the atom where protons and neutrons reside. It contains most of the atom\'s mass. - **Electron Cloud**: Electrons move around the nucleus in defined energy levels (or shells). The first shell can hold up to 2 electrons, the second up to 8, and so on. 3. **Development of Atomic Models**: - **Dalton's Model**: Atoms are indivisible solid spheres. Atoms of the same element are identical, and different elements have different atoms. - **Thomson's Model (Plum Pudding Model)**: Discovered the electron and proposed that atoms are composed of a positively charged substance with negatively charged electrons scattered throughout, like \"plums\" in a pudding. - **Rutherford's Model**: Through the gold foil experiment, Rutherford discovered the nucleus. He suggested that atoms have a small, dense, positively charged nucleus with electrons orbiting the nucleus at a distance. - **Bohr's Model**: Bohr refined Rutherford's model by suggesting that electrons move in fixed orbits (energy levels) around the nucleus and that each orbit has a specific energy associated with it. Electrons can jump between these orbits by absorbing or emitting energy. 4. **Models in Science: Benefits and Limitations**: - **Benefits**: - Models simplify complex concepts, making them easier to understand and study. - They help scientists make predictions and develop new experiments. - They are visual aids that can help explain atomic theory to students and professionals. - **Limitations**: - Models are only approximations and do not represent the complete reality. - They often omit finer details to focus on essential features. - The Bohr model, for instance, does not fully explain electron behavior in atoms larger than hydrogen. **Atomic Numbers and Elements** 5. **Differences in Atomic Structure**: - Atoms of different elements vary based on the number of protons in their nucleus (atomic number). - For example, hydrogen has 1 proton, helium has 2 protons, and carbon has 6 protons. 6. **Periodic Table**: - The Periodic Table organizes elements based on their atomic number. - Each element is represented by a symbol (e.g., H for Hydrogen, O for Oxygen), and its atomic number (number of protons) is usually displayed at the top of the element's box. 7. **Mass Number and Neutrons**: - **Mass number** = Number of protons + Number of neutrons. - To determine the number of neutrons: - Subtract the atomic number from the mass number. - Example: Carbon-12 has 6 protons and 6 neutrons (12 -- 6 = 6 neutrons). 8. **Drawing Atomic Configurations**: - Use the periodic table to determine the number of protons, neutrons, and electrons for each element in the first 20. - Draw the nucleus with the correct number of protons and neutrons, then place electrons in their respective energy levels. 9. **Position of Metals and Non-metals on the Periodic Table**: - Metals are typically located on the left side and the center of the periodic table (e.g., groups 1-12). - Non-metals are located on the right side of the periodic table (e.g., groups 14-18). - Important groups to remember include: - **Alkali metals** (Group 1) - **Alkaline earth metals** (Group 2) - **Halogens** (Group 17) - **Noble gases** (Group 18) **Chemical Bonding and Compounds** 10. **Covalent vs Ionic Bonds**: - **Covalent Bonds**: Involve the sharing of electrons between two non-metal atoms. Example: Water (H₂O) where oxygen shares electrons with hydrogen. - **Ionic Bonds**: Involve the transfer of electrons from one atom (typically a metal) to another (typically a non-metal), forming ions. Example: Sodium chloride (NaCl) where sodium donates an electron to chlorine. 11. **Valency of Ions and Polyatomic Ions**: - Valency is the combining power of an element or ion. It represents the number of electrons an atom can lose, gain, or share in a chemical bond. - Learn the valencies for common polyatomic ions: - Hydroxide (OH-) = -1 - Nitrate (NO₃-) = -1 - Carbonate (CO₃²⁻) = -2 - Sulfate (SO₄²⁻) = -2 12. **Naming Ionic Compounds and Writing Formulas**: - For ionic compounds, the metal ion is written first, followed by the non-metal or polyatomic ion. - Example: NaCl = Sodium Chloride, MgSO₄ = Magnesium Sulfate. - When given the name of an ionic compound, determine the ions involved and write their respective charges to create the formula. 13. **Salt Formation**: - A salt is formed when a metal ion combines with a non-metal ion or a polyatomic ion. - Example: Sodium chloride (NaCl) is formed by the combination of sodium ions (Na⁺) and chloride ions (Cl⁻). 14. **Naming Covalent Compounds**: - Covalent compounds are named based on the number of atoms and the elements involved, using prefixes such as mono-, di-, tri-, etc. - Example: CO₂ = Carbon Dioxide, H₂O = Dihydrogen Monoxide (commonly known as water). **Acids, Bases, and Chemical Reactions** 15. **Acids and Bases in Everyday Life**: - **Acids**: Common examples include vinegar (acetic acid), lemon juice (citric acid), and stomach acid (hydrochloric acid). - **Bases**: Examples include baking soda (sodium bicarbonate) and household ammonia (ammonium hydroxide). 16. **Properties and Indicators**: - **Acids**: Sour taste, can corrode metals, pH less than 7. - **Bases**: Bitter taste, slippery to the touch, pH greater than 7. - **Indicators**: Substances used to test whether a solution is acidic or basic. - *Litmus paper*: Red in acid, blue in base. - *Universal indicator*: Shows a range of colors based on pH. 17. **Acid Strength**: - *Concentrated*: A large amount of acid in a small volume of water. - *Dilute*: A small amount of acid in a large volume of water. - *Strong Acid*: Completely ionizes in water (e.g., HCl). - *Weak Acid*: Only partially ionizes in water (e.g., acetic acid). 18. **Reactions with Acids**: - Metal + Acid → Salt + Hydrogen gas (e.g., Mg + HCl → MgCl₂ + H₂). - Metal Carbonate + Acid → Salt + Water + Carbon Dioxide (e.g., CaCO₃ + HCl → CaCl₂ + CO₂ + H₂O). - Acid + Base → Salt + Water (neutralization reaction). 19. **Hydrogen Pop Test**: - A lit splint makes a "pop" sound in the presence of hydrogen gas. 20. **Limewater Test for CO₂**: - Limewater turns milky when exposed to carbon dioxide gas, indicating the presence of CO₂. 21. **Chemical Reactions**: - Atoms are rearranged during chemical reactions but are neither created nor destroyed (Law of Conservation of Mass). 22. **pH Scale**: - The pH scale ranges from 0-14, with acids having a pH less than 7, bases having a pH greater than 7, and a pH of 7 being neutral (pure water). 23. **Constructing Word Equations**: - Represent chemical reactions using words rather than symbols. - Example: Hydrogen + Oxygen → Water. 24. **Chemical Reactions in Living Things**: - Respiration is a crucial chemical reaction that occurs in living organisms, converting glucose and oxygen into energy, water, and carbon dioxide. **Alfred Wegener's Theory of Continental Drift and Plate Tectonics** 1. **Wegener's Continental Drift Theory**: - Proposed that continents were once part of a single large landmass (Pangaea) that broke apart and drifted to their current positions. 2. **Evidence for Continental Drift**: - Similarities in the shapes of continents (e.g., South America and Africa appear to fit together). - Fossil evidence showing the same species on continents now separated by oceans. - Similar rock formations and mountain ranges on different continents. 3. **Hess's Seafloor Spreading Hypothesis**: - Harry Hess proposed that new seafloor is created at mid-ocean ridges and spreads outward, pushing older seafloor away from the ridge. 4. **Evidence Supporting Seafloor Spreading**: - Magnetic striping on the ocean floor shows alternating patterns of normal and reversed magnetic polarity, recording Earth\'s magnetic field reversals. - The age of rocks increases as you move away from mid-ocean ridges. - The thickness of ocean floor sediments increases with distance from the ridge, suggesting seafloor spreading over time. 5. **Plate Tectonics Theory**: - Earth's lithosphere is divided into tectonic plates that move due to the convection currents in the mantle. - The movement of these plates explains continental drift, earthquakes, volcanic activity, and the formation of mountain ranges. 6. **Mechanisms Driving Plate Movement**: - *Mantle Convection*: Heat from Earth\'s core causes convection currents in the mantle, which move tectonic plates. - *Gravitational Forces*: Ridge push and slab pull also contribute to plate movement. - *Ridge Push*: Newly formed rock at mid-ocean ridges pushes plates apart. - *Slab Pull*: Denser oceanic plates sink into the mantle at subduction zones, pulling the rest of the plate along. 7. **Types of Plate Boundaries**: - *Divergent Boundaries*: Plates move apart. New crust forms at mid-ocean ridges (e.g., Mid-Atlantic Ridge). - *Convergent Boundaries*: Plates move toward each other. This can result in mountain formation or subduction (e.g., Himalayas, Andes). - *Transform Boundaries*: Plates slide past each other, leading to earthquakes (e.g., San Andreas Fault). 8. **Interactions at Plate Boundaries**: - Convergent boundaries can result in the formation of volcanoes, mountain ranges, and ocean trenches. - Divergent boundaries are associated with the creation of new oceanic crust. - Transform boundaries are associated with frequent earthquakes due to friction between plates. 9. **Earthquakes and Plate Boundaries**: - Earthquakes occur when stress builds up along faults or plate boundaries and is suddenly released. - The *focus* is the point inside Earth where the earthquake originates. - The *epicenter* is the point on Earth's surface directly above the focus. 10. **P-Waves and S-Waves**: - **P-Waves (Primary Waves)**: Fastest seismic waves; they compress and expand the ground like sound waves. Travel through both solids and liquids. - **S-Waves (Secondary Waves)**: Slower than P-waves; they move the ground up and down or side to side. Only travel through solids. - The time difference between P-wave and S-wave arrivals helps locate an earthquake's epicenter. 11. **Earthquake Magnitude**: - Measured on the **Richter scale**. Each increase in number represents a tenfold increase in magnitude (energy released). 12. **Volcanic Activity at Hot Spots**: - Hot spots are areas where plumes of hot magma rise through the mantle to create volcanoes, independent of plate boundaries (e.g., Hawaii). 13. **Tsunamis**: - Tsunamis are large sea waves generated by underwater earthquakes or volcanic eruptions, displacing large amounts of water. **Electricity and Circuits** 1. **Conductors, Insulators, and Resistors**: - **Conductors**: Materials that allow electric current to flow easily (e.g., metals like copper and aluminum). - **Insulators**: Materials that resist the flow of electricity (e.g., rubber, plastic). - **Resistors**: Devices that limit the flow of current in a circuit. They convert electrical energy into heat. 2. **Voltage, Current, and Resistance**: - **Voltage (V)**: The potential difference that drives electric current through a circuit. Measured in volts (V). - **Current (I)**: The flow of electric charge through a conductor. Measured in amperes (A). - **Resistance (R)**: The opposition to the flow of current. Measured in ohms (Ω). 3. **Ohm's Law**: - Ohm's law relates voltage (V), current (I), and resistance (R) in a circuit: V = IR. - Example: If a resistor has a resistance of 10Ω and the voltage across it is 5V, the current flowing through the resistor is I = V/R = 5V/10Ω = 0.5A. 4. **Series and Parallel Circuits**: - **Series Circuit**: A single path for current to flow. If one component fails, the entire circuit is interrupted. - **Parallel Circuit**: Multiple paths for current to flow. If one component fails, other parts of the circuit continue to work. 5. **Circuit Components**: - **Ammeter**: Measures the current in a circuit and is connected in series with the circuit. - **Voltmeter**: Measures the voltage across a component and is connected in parallel with the component. 6. **Behaviour of Voltage, Current, and Resistance**: - In a series circuit, the total voltage is divided across the components, while the current remains the same throughout. - In a parallel circuit, the voltage remains the same across all branches, but the current divides among the branches. 7. **Applications of Series and Parallel Circuits**: - **Series Circuits**: Often used in simple applications like flashlights. - **Parallel Circuits**: Used in household wiring to ensure that appliances work independently of each other.

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