Atoms and the Periodic Table Notes
Section 2.4 Subatomic Particles, Isotopes, and Ions
Learning Objectives:
Identify the mass number of an atom using the count of each type of subatomic particle (protons, electrons, and neutrons) present in that atom, and vice versa.
Identify which specific element an atom represents using the mass number of that atom, or vice versa.
Subatomic Particles and the Atomic Nucleus:
Subatomic Particles: Atoms are composed of three primary particles: neutrons, protons, and electrons.
The Nucleus:
The atomic nucleus is incredibly small, possessing a radius only of the radius of the cell.
The nucleus contains almost all of the mass of the atom.
Electrons:
Electrons possess very little mass.
Despite their low mass, electrons occupy almost the entire volume of the atom.
Properties of Subatomic Particles (Table 2.2):
Proton (p):
Relative Charge (): .
Mass (): .
Location: Inside the nucleus.
Neutron (n):
Relative Charge (): .
Mass (): .
Location: Inside the nucleus.
Electron (e):
Relative Charge (): .
Mass (): .
Location: Outside the nucleus.
Fundamental Unit of Charge: The relative charges are based on the charge of the electron, represented as , where .
Atomic Mass Units: Masses are measured in atomic mass units, abbreviated as .
Relative Sizes and Masses Metaphors:
Mass Comparison: If an electron had the mass of a marble, a proton or neutron would have the mass of a bowling ball.
Size Comparison: If the entire nucleus were the size of a marble, the atom would be the size of a stadium.
Atomic Number, Mass Number, and Isotopes
Atomic Number ():
The atomic number, symbol , is defined by the number of protons in an atom's nucleus: .
The atomic number determines the identity of the element.
On the periodic table, every element is assigned a whole number . For example, is hydrogen and is oxygen.
In an electrically neutral atom, the number of protons equals the number of electrons: .
Isotopes:
Atoms of the same element can have different numbers of neutrons in their nuclei.
Definition: Two atoms with the same number of protons but different numbers of neutrons are called isotopes of the same element.
Isotopes share the same atomic number but differ in mass due to the differing neutron count.
Mass Number ():
The mass number, symbol , is the sum of protons and neutrons in the atom: .
The number of neutrons can be calculated as the difference between the mass number and the atomic number: .
Symbology for Isotopes:
Isotopes are named using the element name or symbol followed by the mass number (e.g., hydrogen-1).
Isotope Symbols: Typically written as , where is the mass number and is the atomic number.
Hydrogen Examples:
Hydrogen-1: (contains 1 proton and 0 neutrons).
Hydrogen-2: (contains 1 proton and 1 neutron).
Examples: Particles and Isotope Notation
Example 2.7: Subatomic Particle Counting:
Question: How many protons, neutrons, and electrons are in a neutral atom of each of the following isotopes?
a.
b.
c.
d.
Solution:
a. Sulfur (): , , (since ).
b. Fluorine (): , , (since ).
c. Neon (): , , (since ).
d. Uranium (): , , (since ).
Example 2.8: Identifying Correct Symbols:
Question: Assuming the element symbols are correct, which of the following isotopic symbols are correct? Explain why.
(Note: Identifying specific correct symbols requires verifying if the atomic number matches the element symbol on the periodic table).
Ions: Cations and Anions
Definition: Atoms can form charged particles called ions by gaining or losing electrons.
Cations:
Formed when an atom loses one or more electrons, resulting in a positive charge.
Example: Sodium reacts to lose an electron: .
This process is termed oxidation.
Anions:
Formed when an atom gains one or more electrons, resulting in a negative charge.
Example: Oxygen reacts to gain electrons: .
This process is termed reduction.
Example 2.11: Identifying Particles in Ions:
Question: How many protons and electrons are in each of the following ions?
a.
b.
c.
d.
Solution:
a. : and .
b. : and .
c. : and .
d. : and .
Section 2.5 Atomic Masses
Learning Objectives:
Calculate the atomic mass of any element using the masses and relative abundances of its naturally occurring mixture of isotopes.
The Atomic Mass Scale:
Atomic masses are measured on a relative scale because they are extremely small. One isotope is assigned a specific value, and all others are measured relative to it.
Historical Standard: Initially, oxygen was the standard, with the naturally occurring mixture of oxygen isotopes assigned a value of exactly ( or ).
Current Standard (1961): Carbon-12 () was designated as the new standard, assigned a mass of exactly .
Modern Determination of Atomic Mass:
The atomic mass displayed on the periodic table is a weighted average of the actual masses of all naturally occurring isotopes of that element.
Weighted averages account for the relative abundance (the number of each type of isotope present in nature).
Example 2.12: Weighted Average Metaphor (Course Grading):
Scenario: Exams = 50%, Quizzes = 25%, Homework = 20%, Participation = 5%.
Student Scores: Exams = 80.2%, Quizzes = 77.3%, Homework = 87.8%, Participation = 100.0%.
Calculation: Overall Grade = .
Calculation of Atomic Mass Formula:
Example 2.13: Calculating Atomic Mass of Copper:
Data:
: 69.17% abundance, mass = .
: 30.83% abundance, mass = .
Steps:
Convert percentages to fractions: 0.6917 and 0.3083.
Calculation: .
Artificial Isotopes and Elements:
Artificial Elements: Elements with Z > 92 are artificial and do not have standard atomic masses based on natural abundance.
Periodic Table Representation: For artificial elements, the mass number of the most stable isotope is provided in parentheses.
Artificial Isotopes: Artificial isotopes of naturally occurring elements are not included in the calculation of the element's atomic mass.
Section 2.6 The Periodic Table
Learning Objectives:
Discuss the historical contributions of Mendeleev and Meyer.
Locate and classify elements based on their position in the table.
Identify periods, groups, and sections by name and number.
Development of the Periodic Table:
History: The table resulted from refining the grouping of elements with similar chemical characteristics over many years.
Early Ordering: Initially, elements were ordered by atomic mass. After reaching Dalton's hypothesis, scientists focused on determining relative atomic masses.
Mendeleev and Meyer: Dimitri Mendeleev and Lothar Meyer independently produced periodic tables combining internal characteristics and atomic masses.
Mendeleev's Innovation: Mendeleev used the table to predict the existence and properties of undiscovered elements. He also prioritized chemical properties over mass when they conflicted, notably swapping Iodine () and Tellurium (). His belief that their masses were incorrectly determined was later validated.
Modern Arrangement:
Elements are arranged horizontally by increasing atomic number () and vertically by similar properties.
Example 2.15: Atomic Mass Inversions: Besides Iodine and Tellurium, other naturally occurring pairs out of order by mass (but correctly ordered by atomic number) include:
Argon () and Potassium ().
Cobalt () and Nickel ().
Structure of the Modern Table:
Periods: Horizontal rows. There are 7 periods. Periods 6 and 7 include the inner transition elements.
Groups/Families: Vertical columns. Elements in a group share similar chemical properties.
Numbering Systems:
Older system: Groups 1–8 with A/B designations.
Modern system: Groups 1–18 (left to right).
Group Names (Figure 2.17):
Group 1 (1A): Alkali metals.
Group 2 (2A): Alkaline earth metals.
Group 11: Coinage metals.
Group 15 (5A): Pnictogens.
Group 16 (6A): Chalcogens.
Group 17 (7A): Halogens.
Group 18 (8A): Noble gases (colorless, odorless, mostly inert; discovered after the initial periodic table development).
Classifications and Categories
Larger Group Classifications:
Main Group Elements: Found in groups 1, 2, and 13–18. These are the most common elements and exhibit predictable chemistry.
Transition Elements: Found in groups 3–12; all are metals.
Inner Transition Elements: Displayed in two rows below the main table.
Lanthanoids: Elements 58–71.
Actinoids: Elements 90–103.
Metals, Nonmetals, and Metalloids (Figure 2.19):
Metals: Make up the majority of elements; located on the left side. Properties: Shiny, malleable, ductile, good conductors of heat and electricity.
Nonmetals: Includes Hydrogen plus elements on the upper-right side. Properties: Brittle as solids.
Metalloids: Border the division between metals and nonmetals; they share properties with both categories.
Example Identifications (Examples 2.16 – 2.20):
Period 4: Starts with Potassium (), ends with Krypton (), contains 18 elements.
Location Identification:
Neon (): Period 2, Group 18.
Rubidium (): Period 5, Group 1 (corrected from transcript slide 41 list).
Tungsten (): Period 6, Group 6.
Francium (): Period 7, Group 1.
Similar Chemical Properties: Rubidium () and Francium () (both are in Group 1).
Classification:
Cesium (): Main group element.
Indium (): Main group element.
Uranium (): Inner transition element (Actinoid).
Element Trivia (Example 2.20):
Fifth element in the first row of transition metals: Manganese ().
Element in Period 4, Group 6: Chromium ().
Seventh transition element: Cobalt ().
First element of Group 8: Iron ().
Third halogen: Bromine ().
First alkaline earth metal: Beryllium ().
First coinage metal: Copper ().