
Course Title: General Chemistry I (Physical & Inorganic Chemistry)
General Chemistry I provides students with a foundational understanding of the fundamental principles of chemistry, with emphasis on physical chemistry and inorganic chemistry concepts. The course introduces atomic structure, chemical bonding, stoichiometry, states of matter, periodicity, and the quantitative relationships that govern chemical reactions. Students will develop problem-solving skills, analytical reasoning, and an appreciation for the role of chemistry in scientific and technological advancements. This course is essential for students in science, engineering, medical, agricultural, and environmental disciplines.
By the end of this course, students should be able to:
Chemistry is often described as the “central science” because it links the physical sciences with the life sciences and applied sciences such as engineering, agriculture, medicine, pharmacy, and environmental studies. Every substance around you—air, water, soil, foods, metals, plastics, even your own body—is made of chemicals. Understanding chemistry means understanding matter, its composition, structure, and the changes it undergoes.
Chapter One introduces the basic foundations of chemistry: what chemistry is, how chemists study matter, the measurement systems used in scientific work, the classification of matter, the laws that govern chemical behavior, and the quantitative relationships known as stoichiometry. These ideas form the backbone of all higher-level chemistry topics, from physical chemistry to inorganic chemistry, biochemistry, organic chemistry, and analytical chemistry.
Chemistry is the scientific study of matter—its composition, structure, properties—and the changes it undergoes during chemical reactions. It attempts to answer fundamental questions such as:
In essence, chemistry helps us understand the building blocks of everything around us.
Chemistry is broadly divided into several branches:
Chemistry influences nearly every aspect of modern life:
From cooking to breathing, everything involves chemistry.
Chemists rely on the scientific method—a systematic approach to studying natural phenomena.
This method ensures that chemical knowledge is based on evidence.
Chemical science depends heavily on accurate measurements, since chemistry is quantitative.
Chemists use the International System of Units (SI) for standardization.
Some basic SI units:
| Quantity | SI Unit | Symbol |
|---|---|---|
| Length | meter | m |
| Mass | kilogram | kg |
| Time | second | s |
| Temperature | kelvin | K |
| Amount of Substance | mole | mol |
| Volume | cubic meter | m³ |
Commonly used derived units include liters (L), milliliters (mL), and grams (g).
Significant figures reflect the precision of a measurement.
Rules:
Example:
If a scale consistently gives values close to the same number but far from the true value → precise but not accurate.
Large and small numbers are expressed conveniently using scientific notation:
Density is the mass per unit volume:
\text{Density (ρ)} = \frac{\text{Mass}}{\text{Volume}}Units: g/cm³ or kg/m³
Density helps identify substances and predict how they interact (e.g., floating, mixing).
Matter is anything that has mass and occupies space. It exists in different states:
| State | Characteristics |
|---|---|
| Solid | Fixed shape and volume; particles tightly packed |
| Liquid | Fixed volume, takes shape of container; particles less rigid |
| Gas | No fixed shape or volume; particles far apart and fast-moving |
| Plasma | Ionized gas (e.g., lightning, stars) |
Physical changes
Chemical changes
Matter is divided into:
Pure Substances
Mixtures
Chemistry is governed by foundational laws that describe how substances combine.
Matter is neither created nor destroyed during chemical reactions.
Example:
2H₂ + O₂ → 2H₂O
Mass of reactants = Mass of products.
A chemical compound always contains the same elements in the same proportion by mass.
Example:
Water always contains H and O in a mass ratio of 1:8.
If two elements form more than one compound, the masses combine in simple whole-number ratios.
Example: Carbon & oxygen:
Ratio 16:32 = 1:2 (simple whole numbers)
Dalton proposed that:
Although modern modifications exist, the theory remains foundational.
A chemical equation represents a chemical reaction:
Reactants → Products
Example:
2H₂ + O₂ → 2H₂O
Equations must obey the Law of Conservation of Mass.
Balance using coefficients, not subscripts.
Steps:
Stoichiometry is the quantitative relationship between reactants and products in a chemical reaction.
It allows chemists to calculate:
A mole (mol) is the amount of substance containing 6.022 × 10²³ particles (Avogadro’s number).
1 mole of:
The molar mass is the mass of 1 mole of a substance.
Examples:
\text{Moles} = \frac{\text{Mass}}{\text{Molar Mass}}\text{Mass} = \text{Moles} \times \text{Molar Mass}Example:
Glucose: C₆H₁₂O₆
Empirical formula: CH₂O
If the equation is:
N₂ + 3H₂ → 2NH₃
The mole ratios are:
These ratios help determine the required quantities.
The limiting reactant is the one that is completely consumed first and determines the amount of product formed.
Steps:
\text{Percentage Yield} = \frac{\text{Actual Yield}}{\text{Theoretical Yield}} \times 100High yield indicates an efficient reaction.
Stoichiometry is crucial in:
Companies calculate exact quantities to avoid waste.
Chapter One provides the foundational building blocks for studying chemistry. Understanding measurements, matter, chemical laws, chemical equations, and stoichiometry enables students to navigate more advanced topics such as chemical bonding, thermodynamics, kinetics, inorganic reactions, gas behavior, and equilibrium. A strong grasp of these basic concepts improves problem-solving skills and prepares students for laboratory work, scientific reasoning, and higher-level courses.
The structure of the atom and the periodic behavior of elements form the theoretical backbone of modern chemistry. Understanding how atoms are built, how electrons are arranged, and how these arrangements influence chemical reactivity enables us to predict and explain a wide range of chemical phenomena. This chapter explores the historical development of atomic theory, the quantum mechanical model of the atom, electron configuration, periodic trends, and how these concepts provide a unified framework for understanding the properties of elements.
While Chapter One dealt with matter in a broad sense, Chapter Two digs deeper into the smallest units that make up matter—the atoms. The journey begins with early models of the atom, transitions into quantum theory, and culminates in our modern interpretation of the periodic table.
Understanding the atom has been a centuries-long scientific endeavor. Each model built upon previous knowledge, moving closer to the modern understanding.
The idea of the atom originated in ancient Greece by philosophers such as Democritus, who proposed that matter was made of tiny, indivisible particles called atomos. However, this idea lacked experimental evidence and was overshadowed by Aristotle’s belief that matter was continuous.
It wasn’t until the 18th and 19th centuries that the atomic theory re-emerged as a result of new experimental data from chemistry.
John Dalton proposed the first scientifically based atomic theory to explain the laws of chemical combination.
Key postulates:
Modern updates:
Regardless, Dalton’s theory laid the foundation for modern chemistry.
Thomson used the cathode ray tube experiment to discover the electron.
Findings:
Thomson proposed the Plum Pudding Model:
This model was revolutionary but later disproven.
Ernest Rutherford’s gold foil experiment involved bombarding thin gold foil with alpha particles.
Observations:
Conclusions:
The Rutherford Model resembled a mini solar system.
Niels Bohr built on Rutherford’s work to address the stability of electron orbits.
Postulates:
Bohr’s model explained the hydrogen emission spectrum perfectly, but failed for multi-electron atoms.
In the early 20th century, scientists like de Broglie, Heisenberg, and Schrödinger revolutionized atomic theory.
Key ideas:
This forms the modern quantum mechanical model, which is more accurate than any previous model.
Atoms consist of three fundamental particles:
| Particle | Symbol | Charge | Mass |
|---|---|---|---|
| Proton | p⁺ | +1 | 1 amu |
| Neutron | n⁰ | 0 | 1 amu |
| Electron | e⁻ | –1 | 1/1836 amu |
The nucleus contains protons and neutrons, with electrons occupying regions around the nucleus called orbitals.
Example:
All are isotopes of carbon.
Atomic mass = weighted average of isotopes.
\text{Average atomic mass} = \sum (\text{mass of isotope} \times \text{abundance})This explains why chlorine’s atomic mass is 35.5 (mixture of Cl-35 and Cl-37).
This model replaced circular orbits with orbitals.
De Broglie proposed that all matter exhibits wave-like properties.
\lambda = \frac{h}{mv}Electrons behave as standing waves, not particles orbiting like planets.
Impossible to know both the exact position and exact momentum of an electron simultaneously.
This principle indicates that electrons are found in probability clouds known as orbitals.
Schrödinger used wave functions (ψ) to describe electrons as wave-like entities.
Solutions to his equation give rise to:
These orbitals describe regions where electrons are most likely found.
Quantum numbers describe the unique address of an electron.
Defines sublevel/orbital shape.
| l | Sublevel | Shape |
|---|---|---|
| 0 | s | spherical |
| 1 | p | dumbbell |
| 2 | d | complex |
| 3 | f | very complex |
Defines orientation in space.
Values: –l → +l
Values: +½ or –½
Electrons must have opposite spins when sharing the same orbital.
Understanding shapes helps explain bonding and geometries.
Electron configuration indicates how electrons are arranged in orbitals.
Electrons fill orbitals based on three rules:
Electrons fill orbitals from lowest to highest energy.
Order (up to Z = 36):
1s
2s
2p
3s
3p
4s
3d
4p
5s
4d
5p…
No two electrons can have the same set of four quantum numbers.
Hence, an orbital holds a maximum of 2 electrons with opposite spins.
Electrons fill degenerate orbitals singly before pairing occurs.
Example:In the p-sublevel, electrons occupy the three p orbitals one-by-one.
Example: Phosphorus (Z = 15)
Electron configuration:
1s² 2s² 2p⁶ 3s² 3p³
Orbital notation places electrons into orbitals with arrows.
Using noble gases:
P: [Ne] 3s² 3p³
This makes configurations shorter and easier.
Some transition metals have irregular configurations due to stability of half-filled or fully filled orbitals.
Examples:
These exceptions play important roles in inorganic chemistry.
The periodic table organizes elements based on their properties.
Periodic trends arise from electron configuration and effective nuclear charge.
Distance from nucleus to outermost electron shell.
Trend:
Reason: increasing nuclear charge pulls electrons closer.
Isoelectronic ions decrease in radius with increasing nuclear charge.
Energy required to remove one electron.
Trend:
Noble gases have highest IE.
Energy change when an atom gains an electron.
Non-metals (like halogens) have higher EA than metals.
Ability of an atom to attract electrons in a bond.
Most electronegative: Fluorine
Least electronegative: Cesium
Trend:
Metals lose electrons easily.
Trend:
The periodic table is not arbitrary—it reflects electron configuration patterns.
Examples:
Atomic structure explains chemical behavior.
Understanding the atom and periodic trends helps explain:
Predicting which reactions occur and why.
Electron configuration determines bonding type.
Metallic, ionic, and covalent properties depend on atomic structure.
Elements like Na, K, Mg, Ca behave differently due to periodic trends.
Reactivity of pollutants, metals, and gases.
Atomic structure and periodicity form the theoretical basis for understanding all chemical behavior. Whether studying chemical bonding, reactivity, thermodynamics, metals, inorganic complexes, or biochemical systems, these principles remain essential. A solid grasp of these concepts enables students to navigate advanced topics and apply chemical knowledge effectively in scientific and industrial contexts.
Chemical bonding is one of the most important concepts in chemistry because almost all physical and chemical properties of matter—including hardness, melting point, electrical conductivity, solubility, colour, and reactivity—are determined by the type of bonding holding atoms together. Everything around us, from water to diamonds, from proteins to plastics, is the result of atoms bonding in specific ways.
Atoms bond because they achieve greater stability when their outermost (valence) electron shells are either filled or reach a more energetically favorable configuration. Chemical bonding explains why certain elements readily combine while others resist reaction, why molecules adopt particular shapes, and how the forces between molecules determine states of matter.
In this chapter, we explore the different types of chemical bonds, theories that explain bonding, molecular geometry, intermolecular forces, and how molecular structure affects chemical and physical properties.
Atoms form bonds to lower their potential energy and achieve stable electronic configurations, often resembling noble gases.
The main driving forces in bonding are:
Some exceptions exist (H, He, B, expanded octets), but the principle remains a helpful guideline.
Two major categories of bonding include:
Understanding the nature of these interactions is key to explaining molecular behavior.
An ionic bond forms through complete transfer of electrons from one atom to another, resulting in:
The bond arises from the strong electrostatic attraction between these oppositely charged ions.
Ionic bonds usually form between:
Example: Formation of sodium chloride
Na (2,8,1) → loses 1 electron → Na⁺
Cl (2,8,7) → gains 1 electron → Cl⁻
They combine to form NaCl.
Ionic substances have distinct properties:
High melting and boiling points
— result of strong electrostatic attractions.
Hard and brittle
— shifting layers cause repulsion between like charges.
Conduct electricity when molten or dissolved
— ions become mobile.
Soluble in polar solvents (like water)
Form crystal lattice structures
The strength of the ionic bond is measured by lattice energy, which is the energy required to separate one mole of ionic solid into gaseous ions.
Lattice energy increases when:
Ca²⁺ and O²⁻ produce stronger lattice interactions than Na⁺ and Cl⁻.
A covalent bond forms when two atoms share electrons to achieve stable configurations.
Covalent bonding typically occurs between:
Sharing one pair of electrons
Example: H–H, H–Cl, CH₄
Sharing two pairs of electrons
Example: O=O, C=O
Sharing three pairs of electrons
Example: N≡N, C≡C
Bond order increases → bond strength increases → bond length decreases.
Bond polarity depends on electronegativity difference.
Example:
Polarity creates dipoles, which influence molecular behavior.
Already-shared electron pair comes entirely from one atom.
Example:
NH₃ + H⁺ → NH₄⁺
Here, nitrogen donates both electrons for bonding.
Metal atoms share a “sea of electrons” that move freely throughout the lattice.
Features of metallic bonding:
Metallic bonding explains why metals exhibit unique physical properties.
VSEPR theory predicts molecular shapes based on electron pair repulsion.
Basic principle:
Electron pairs (bonding and lone pairs) around the central atom repel one another and arrange themselves to minimize repulsion.
| Electron Pairs | Shape | Angle |
|---|---|---|
| 2 | Linear | 180° |
| 3 | Trigonal planar | 120° |
| 4 | Tetrahedral | 109.5° |
| 5 | Trigonal bipyramidal | 90°, 120° |
| 6 | Octahedral | 90° |
Lone pairs reduce angles due to greater repulsion.
Examples:
VBT explains covalent bonding as the overlap of atomic orbitals.
When two atomic orbitals overlap:
Bond structure:
Hybridization involves mixing atomic orbitals to form new hybrid orbitals with equal energy.
Hybridization explains molecular shapes more precisely than VSEPR alone.
MOT treats electrons as belonging to the whole molecule, not individual atoms.
When atomic orbitals combine:
Bonding molecular orbital (σ or π)
— lowers energy, stabilizes molecule
Antibonding molecular orbital (σ or π*)*
— higher energy, destabilizing
Bond order:
\text{Bond Order} = \frac{(N_{\text{bonding}} - N_{\text{antibonding}})}{2}Bond order predicts:
Example:
O₂ has bond order 2, and MOT explains its paramagnetism (presence of unpaired electrons).
IMFs determine the physical properties of substances.
Explain:
Example: HCl, SO₂
Strongest IMF
Occurs when H bonds to N, O, or F.
Explains:
Strong interactions between ions and polar molecules.
Example: Na⁺ interacting with water molecules during dissolution.
Molecular polarity depends on:
A molecule can have polar bonds but still be nonpolar if dipoles cancel.
Examples:
Polarity affects:
The type of bonding determines many physical properties:
Lewis structures show valence electrons as dots.
Some molecules cannot be represented by a single structure.
Examples:
Actual structure = resonance hybrid, which is more stable than any single form.
General trends:
This explains differences in reactivity and stability.
Shape and polarity influence how molecules interact.
Examples:
Molecular structure determines:
Bonding theories explain why materials behave as they do and how they can be engineered for specific uses.
Chemical bonding and molecular structure represent the heart of chemical science. They explain why matter forms the structures we observe, why substances have particular properties, and how molecules behave during reactions. A full understanding of bonding prepares students to tackle advanced chemistry topics such as thermodynamics, kinetics, inorganic chemistry, organic chemistry, and biological chemistry.
Mastery of this chapter not only enhances scientific literacy but also provides the conceptual tools needed for careers in medicine, engineering, biotechnology, environmental science, and industrial chemistry.
Matter exists in three major physical states: solid, liquid, and gas, and each state displays distinct properties that arise from the arrangement, motion, and interaction of particles. Understanding the behavior of matter in these states is foundational to physical chemistry, particularly when examining how substances respond to temperature, pressure, and intermolecular forces.
In this chapter, we explore in depth the states of matter, the kinetic molecular theory, the laws governing gases, and the behavior of real vs. ideal gases. We also examine the properties of liquids and solids, phase changes, phase diagrams, and the nature of solutions. The chapter integrates both qualitative explanations and quantitative relationships, giving students a strong conceptual and mathematical understanding of physical changes in matter.
Matter is anything that has mass and occupies space. On a macroscopic level, matter exists in three principal states:
These states differ in molecular arrangement, intermolecular forces, compressibility, and movement of particles.
Solids are substances with definite shape and definite volume. Their particles are held close together in a fixed arrangement due to strong intermolecular forces.
Crystalline solids have particles arranged in an ordered, repeating three-dimensional pattern known as a crystal lattice.
Examples:
Properties of Crystalline Solids
Amorphous solids lack long-range order. Their particles are arranged randomly.
Examples:
Properties
Liquids have definite volume but no definite shape, taking the shape of their container. Intermolecular forces in liquids are moderate—stronger than in gases but weaker than in solids.
Surface tension is the resistance of a liquid surface to external force due to cohesive forces among molecules.
Examples:
Viscosity refers to the resistance to flow.
Viscosity decreases with temperature.
Vapor pressure is the pressure exerted by vapor molecules at equilibrium with their liquid at a given temperature.
High vapor pressure → boils easily (e.g., ether)
Gases have neither definite shape nor definite volume. Their particles are far apart with negligible intermolecular forces, and they move freely at high speeds.
The behavior of gases is best explained by the kinetic molecular theory, discussed later in the chapter.
The kinetic molecular theory (KMT) describes the physical behavior of gases based on molecular motion.
Gas laws relate pressure (P), volume (V), temperature (T), and amount of gas (n). They were discovered through experiments by early scientists such as Boyle, Charles, and Avogadro.
At constant temperature, the volume of a fixed mass of gas is inversely proportional to its pressure.
PV = kP_1V_1 = P_2V_2A gas at 2 atm has a volume of 4 L. What is the volume at 4 atm?
V_2 = \frac{P_1V_1}{P_2} = \frac{2 \times 4}{4} = 2 LAt constant pressure, the volume of a gas is directly proportional to its absolute temperature.
\frac{V}{T} = k\frac{V_1}{T_1} = \frac{V_2}{T_2}Temperature must be in Kelvin (K).
K = ^\circ C + 273At constant volume, pressure is directly proportional to absolute temperature.
\frac{P}{T} = k\frac{P_1}{T_1} = \frac{P_2}{T_2}Equal volumes of gases at the same temperature and pressure contain equal number of molecules.
V \propto n\frac{V_1}{n_1} = \frac{V_2}{n_2}At STP (0°C, 1 atm):
1 \text{ mole of gas} = 22.4 \text{ L}Combining all simple gas laws gives:
PV = nRTWhere:
Values of R:
In a mixture of gases, the total pressure is the sum of partial pressures.
P_{total} = P_1 + P_2 + P_3 + \ldotsPartial pressure is proportional to mole fraction.
P_i = X_i P_{total}The rate of diffusion or effusion of a gas is inversely proportional to the square root of its molar mass.
\frac{r_1}{r_2} = \sqrt{\frac{M_2}{M_1}}Where:
Ideal gases obey gas laws under all conditions—but real gases do not.
These assumptions break down at:
Corrects for non-ideal behavior:
\left(P + \frac{a n^2}{V^2}\right)(V - nb) = nRTWhere:
Gases like CO₂ and NH₃ deviate more due to polarity.
Substances can change from one physical state to another when temperature or pressure changes.
Energy needed for phase transitions without temperature change.
A phase diagram represents the relationship between temperature, pressure, and physical states.
Water and CO₂ have different phase behaviors due to molecular structure.
A solution is a homogeneous mixture of two or more substances.
Solubility is the amount of solute that dissolves in a given amount of solvent at a specific temperature.
C = kPWhere:
Depend only on the number of solute particles.
\Delta T_b = K_b m\Delta T_f = K_f m\Pi = MRT4.7.3 Colligative Properties
Depend only on the number of solute particles.
1. Boiling point elevation
2. Freezing point depression
3. Osmotic pressure
4. Vapor pressure lowering
Boiling Point Elevation
\Delta T_b = K_b m
Freezing Point Depression
\Delta T_f = K_f m
Osmotic Pressure
\Pi = MRT
These properties help determine molar masses of compounds experimentally.
4.8 APPLICATIONS OF GAS LAWS AND STATES OF MATTER
1. Breathing Mechanism
Boyle’s law explains how lungs expand and contract.
2. Refrigeration and Air Conditioning
Phase changes of refrigerants absorb and release heat.
3. Weather and Atmospheric Science
Gas laws describe pressure variations and gas mixing.
4. Industrial Gas Production
Liquefaction of air uses real gas deviations.
5. Medicine
Oxygen cylinders rely on pressure-volume relationships.
4.9 SUMMARY OF KEY POINTS
Matter exists as solid, liquid, and gas, each with unique properties.
Kinetic molecular theory explains gas motion and pressure.
Gas laws relate temperature, pressure, volume, and moles.
Real gases deviate at high pressure and low temperature.
Phase diagrams show equilibrium among phases.
Solutions exhibit colligative properties that depend on particle concentration.