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Atoms and Elements: Foundations of General Chemistry

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Atoms: The Essential Building Blocks

Definition and Properties of Atoms

An atom is the smallest unit of an element that retains the unique properties of that element. There are 118 known elements, with 98 occurring naturally on Earth. Atoms combine to form compounds and mixtures, giving rise to the diversity of matter.

  • Element: A pure substance consisting of only one type of atom.

  • Compound: A substance formed when atoms of different elements combine in fixed ratios.

  • Mixture: A physical combination of two or more substances where each retains its own properties.

Microscopic and macroscopic view of matter

Historical Development of Atomic Theory

The concept of the atom dates back to ancient Greece. Democritus (~400 BCE) proposed that matter is composed of indivisible particles called atomos.

Bust of Democritus

Fundamental Laws of Chemistry

The Law of Conservation of Mass

Formulated by Antoine Lavoisier, this law states that mass is neither created nor destroyed in a chemical reaction. The total mass of reactants equals the total mass of products.

  • Key Point: Chemical reactions rearrange atoms but do not change their total mass.

  • Example: Heating mercury in the presence of oxygen forms red mercury oxide, but the total mass remains constant.

Portrait of Lavoisier and his experimentLavoisier's experiment: Mercury and oxygen

The Law of Constant Composition

This law states that a pure compound always contains the same elements in the same proportion by mass, regardless of its source.

  • Example: Water (H2O) always contains two hydrogen atoms and one oxygen atom.

The Law of Multiple Proportions

When two elements form more than one compound, the masses of one element that combine with a fixed mass of the other are in ratios of small whole numbers.

  • Example: Mercury(I) oxide (Hg2O) and Mercury(II) oxide (HgO) have different ratios of mercury to oxygen.

Dalton’s Atomic Theory

Postulates of Dalton’s Atomic Theory

John Dalton (1808) proposed a modern atomic theory based on experimental evidence:

  • Elements are made of tiny, indivisible particles called atoms.

  • Atoms of each element are unique.

  • Atoms combine in whole-number ratios to form compounds.

  • Atoms are unchanged in chemical reactions; only their arrangements change.

Portrait of John Dalton

The Periodic Table of Elements

Organization and Classification

Dmitri Mendeleev organized elements by increasing atomic mass and grouped elements with similar properties. The modern periodic table arranges elements by increasing atomic number and groups them into metals, nonmetals, and metalloids.

  • Groups (families): Vertical columns with similar chemical properties.

  • Periods: Horizontal rows.

  • Metals: Left of the staircase, good conductors.

  • Nonmetals: Right of the staircase, poor conductors.

  • Metalloids: Border the staircase, intermediate properties.

Periodic table of elementsGroups of elements: Alkali metals, alkaline earth metals, halogens, noble gases

Uncovering Atomic Structure

Subatomic Particles

Atoms are composed of three main subatomic particles:

  • Protons: Positively charged, located in the nucleus.

  • Neutrons: Neutral, located in the nucleus.

  • Electrons: Negatively charged, found in the electron cloud surrounding the nucleus.

Structure of an atom showing protons, neutrons, and electrons

Mass and Charge of Subatomic Particles

  • Atomic mass unit (amu):

  • Charge: Measured in coulombs (C). Like charges repel, opposite charges attract.

  • Coulomb’s Law:

Opposite charges attract, like charges repel

Discovery of the Electron: Cathode-Ray Tube Experiments

J.J. Thomson discovered the electron using cathode-ray tubes, determining the charge-to-mass ratio of the electron.

  • Electrons are negatively charged and much lighter than atoms.

  • Deflection in electric and magnetic fields revealed their properties.

Cathode-ray tube experiment

Millikan’s Oil Drop Experiment

Robert Millikan measured the charge of the electron using the oil drop experiment, finding the fundamental unit of electric charge.

  • Charge of electron:

  • Mass of electron:

Millikan oil drop experiment apparatus

Atomic Models: Plum Pudding and Nuclear Model

Early models of the atom included the "plum pudding" model, where electrons were embedded in a positively charged matrix. Rutherford’s gold foil experiment disproved this, showing that atoms have a small, dense, positively charged nucleus.

  • Plum pudding model: Electrons scattered in a sphere of positive charge.

  • Rutherford model: Dense nucleus with electrons orbiting around it.

Plum pudding model (muffin analogy)Rutherford's gold foil experiment setupAlpha particles deflected by gold foil

Summary Table: Subatomic Particles

Subatomic Particle

Location

Mass (amu)

Charge

Proton

Nucleus

1.0073

+1

Neutron

Nucleus

1.0087

0

Electron

Electron cloud

0.0005

-1

Models of the Atom

Development of Atomic Models

  • Dalton’s model (1808): Atoms are indivisible spheres.

  • Plum pudding model (1904): Electrons in a positive matrix.

  • Bohr model (1913): Electrons orbit the nucleus in fixed paths.

  • Quantum model (1920s): Electrons exist in probabilistic clouds (orbitals).

Dalton's solid sphere modelPlum pudding modelBohr model of the atomQuantum model of the atom

Formation of Ions

Neutral Atoms and Ions

Atoms are neutral when the number of protons equals the number of electrons. Ions are formed when atoms gain or lose electrons:

  • Cation: Positively charged ion (loss of electrons).

  • Anion: Negatively charged ion (gain of electrons).

Formation of lithium and fluoride ions

Describing Atoms: Identity and Mass

Atomic Number and Isotopes

The atomic number (Z) is the number of protons in the nucleus and defines the element. Isotopes are atoms of the same element with different numbers of neutrons, resulting in different mass numbers (A).

  • Atomic number (Z): Number of protons.

  • Mass number (A): Number of protons + neutrons.

  • Isotopes: Same Z, different A.

Periodic table entry showing atomic number

Isotopic Mass and Abundance

Isotopes have different masses and natural abundances. The average atomic mass is a weighted average based on isotopic abundance.

  • Example: Hydrogen has three isotopes: protium, deuterium, and tritium.

Calculating Average Atomic Mass

The average atomic mass is calculated as:

  • = mass of isotope i

  • = decimal abundance of isotope i

Calculation of average atomic mass

Atoms in Compounds: Formula Mass and Percent Composition

Formula Mass

The formula mass is the sum of the atomic masses of all atoms in a chemical formula, expressed in amu.

  • Example: For CO2:

Calculation of formula massExample of formula mass calculation

Percent Composition

Percent composition is the percentage by mass of each element in a compound.

  • Example: Oxygen in K2CO3:

The Mole Concept

Avogadro’s Number and the Mole

The mole is a counting unit in chemistry, defined as items (Avogadro’s number). It allows chemists to relate atomic-scale quantities to macroscopic amounts.

Mole concept and Avogadro's number

Molar Mass

The molar mass is the mass of one mole of a substance, numerically equal to the atomic or molecular mass in grams.

  • Example: 1 mole of carbon = 12.01 g; 1 mole of NaCl = 58.44 g

Molar mass and sample calculations

Conversions Between Grams, Moles, and Particles

Conversions use the relationships:

  • 1 mole = particles

  • 1 mole = molar mass in grams

Example Calculations:

  • Atoms in 2.54 mol He: atoms

  • Moles in 1.0 x 1022 C atoms: mol

  • Mass of 1.73 mol Ne: g

  • Moles in 15.3 g NaCl: mol

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