Philosophical Origins:
Concept of atoms first suggested by Greek philosophers Leucippus and Democritus (5th century BC).
The term "atomos" means "indivisible" in Greek.
Aristotle proposed that matter was composed of four elements: fire, earth, air, and water.
John Dalton's Contribution:
Dalton introduced his atomic theory in 1807, marking a significant advancement in chemical understanding.
Five Postulates of Dalton’s Atomic Theory:
Matter Composition: Matter is made of exceedingly small particles called atoms; these atoms are the smallest units participating in chemical change.
Element Composition: Each element consists of one type of atom, which has a specific mass unique to that element.
Example: A pre-1982 copper penny is composed of approximately 3 × 10²² copper atoms.
Diversity of Atoms: Atoms of different elements differ in properties from one another.
Compound Formation: A compound is made up of atoms of two or more elements combined in a fixed, whole-number ratio.
Visual Example: Copper(II) oxide exhibits a 1:1 ratio of copper and oxygen atoms.
Chemical Changes: Atoms are neither created nor destroyed in chemical reactions; they are rearranged to form new types of matter.
Visual Example: The reaction of copper and oxygen forms a new compound.
Dalton's theory explains the macroscopic properties of matter:
Atoms remain constant in mass throughout chemical changes, a principle known as the law of conservation of matter.
Assumption: In this section, reactions are treated as completely converting reactants into products.
In Practice: Many reactions are incomplete, leaving some reactants unreacted.
Definition: All samples of a pure compound contain the same elements in the same proportion by mass.
Illustration: Supported by French chemist Joseph Proust's experiments.
For any compound, its elemental composition remains consistent regardless of sample size.
Table Example: Mass ratios of carbon to hydrogen across different samples showing consistent ratios.
Definition: When two elements form multiple compounds, a fixed mass of one element combines with varying masses of the other in ratios of small whole numbers.
Example: Two compounds with copper and chlorine exhibit different mass ratios.
Visual Figures: Illustrate different compounds of copper and chlorine, showing their varied atomic ratios.
J.J. Thomson’s Experiments: Utilized cathode ray tubes to discover cathode rays, which were deflected by positive charges, indicating the presence of a negatively charged particle (the electron).
Cathode ray particles were much lighter than atoms and identical regardless of their source.
Defined as electrons, negatively charged subatomic particles significantly lighter than atoms.
Visual description of the cathode ray tube experiment showing beam deflection and calculation of mass-to-charge ratios.
Overview: Evaluated the charge of individual oil droplets, allowing for the determination of the electron's charge.
Visual Data: Illustrates apparatus used in Millikan’s experiment, highlighting different charge measurements of oil drops.
Established that the charge of an oil drop is always a multiple of 1.6 × 10⁻¹⁹ C, defining the charge of a single electron.
Reiterates Thomson’s mass-to-charge ratio of the electron.
Rutherford’s Gold Foil Experiment: Analyzing alpha particle scattering provided insights into atomic structure.
Focus on the detection of alpha particles scattering through gold foil.
Visual Schematic: Diagram showing how alpha particles interact with gold foil, illustrating scattering patterns.
Atoms contain vast amounts of empty space with a small, dense, positively charged nucleus at their center, which contains most of an atom's mass.
Electrons are dispersed around the nucleus.
Figure Description: Shows α particle behavior in relation to gold nucleus, delineating space occupied by atoms.
Isotopes: Discovered by Frederick Soddy, differing mass atoms of the same element.
Neutrons: Identified by James Chadwick as uncharged particles located in the nucleus, similar in mass to protons.
Write and interpret atomic symbols, including atomic number and mass number.
Define atomic mass unit; calculate average atomic mass and isotopic abundance.
Composition: Nucleus: contains most mass (protons + neutrons).
Structure: Electrons occupy nearly all atomic volume.
Size Ratios: Diameter of a typical atom is ~ 10⁻¹⁰ m; the nucleus is ~ 10⁻¹⁵ m (100,000 times smaller).
Metaphor: If an atom were the size of a football stadium, the nucleus would compare to a blueberry.
Scale: Atoms and particles are extremely lightweight (e.g., carbon weighs less than 2 × 10⁻²³ g).
Defined Atomic Mass Unit (amu): 1 amu = 1.6605 x 10⁻²⁴ g; for example, a carbon-12 atom weighs 12 amu.
Protons: 1.0073 amu, Charge = +1
Neutrons: 1.0087 amu, Charge = 0
Electrons: 0.00055 amu, Charge = -1
Atomic number (Z) indicates the number of protons in an atom's nucleus, defining the element.
Example: An atom with six protons is carbon (Z = 6).
Neutral atoms must have equal numbers of protons and electrons; thus, atomic number also indicates electron count.
Mass number (A) = Total protons + neutrons.
Relationship: A = Z + Neutrons, where Z is atomic number.
Ions form when the number of protons and electrons differ, altering electrical charge.
Charge Calculated: Charge of an atom = Protons - Electrons.
Anions: Mass gain causes negative charge from electron addition.
Example: Oxygen atom gains electrons (2− charge).
Cations: Mass loss results in positive charge from electron removal.
Example: Sodium atom loses an electron (1+ charge).
Symbols denote elements, example: Hg (mercury).
Chemical symbols derived from element names, often with one or two letters; three-letter symbols exist as well.
The chemical symbol represents the element regardless of the quantity (single atom or larger mass).
Table of common elements:
Aluminum (Al), Iron (Fe), Bromine (Br), Lead (Pb), etc.
Isotope notation includes mass number as a left superscript and atomic number as a subscript.
Example: Magnesium isotopes (24Mg, 25Mg, 26Mg) share proton count with differences in neutron count.
Atomic symbol format:
Element symbol (1 or 2 letters), mass number (superscript), atomic number (subscript), and charge
Hydrogen Isotopes:
Protium (99.989%), Deuterium (0.0115%), Tritium (trace).
Atomic mass reflects protons and neutrons’ approximate weight of ~1 amu; varies due to isotopic mixtures.
Weighted averages of isotopes based on natural abundance.
Example: Boron with isotopes 10B (19.9%) and 11B (80.1%).
Mass spectrometry determines isotopes’ occurrences and natural abundances by ionizing atoms and separating them by mass and charge.
Mass Spectrum Sample: Shows different zirconium isotopes detected in a mass spectrometer.