Atomic Structure, Periodicity, and Periodic Trends

Major Milestones in Atomic Theory

  • Democritus (c. 400 BCE400\,\text{BCE}):

    • Proposed that matter could be divided repeatedly until indivisible particles, termed atomos, remained.

    • This proposal was purely philosophical rather than grounded in experimental data.

  • John Dalton (18031803):

    • Developed a scientific atomic theory establishing that elements consist of individual atoms.

    • Stated that chemical compounds form when atoms combine in characteristic whole-number ratios, and chemical reactions involve the rearrangement of these atoms.

    • Successfully explained elemental composition and stoichiometric patterns.

    • Modern Revision: Modern chemistry later modified Dalton's postulate that atoms are indivisible, though his model successfully explained stoichiometric composition.

  • J. J. Thomson (18971897):

    • Utilized cathode-ray tube experiments to discover the electron as a subatomic particle.

    • Recognized that because electrons are negatively charged and atoms are overall electrically neutral, an atom must consist of a diffuse positive background containing embedded electrons (plum pudding model).

  • Ernest Rutherford (19111911):

    • Conducted the gold-foil experiment by firing alpha particles (α\alpha) from an alpha source at a thin piece of gold foil.

    • Observation: The vast majority of alpha particles passed nearly straight through the foil, but a very small fraction underwent large, dramatic deflections.

    • Conclusion: A diffuse positive charge could not account for these rare, powerful electrostatic repulsions. The atom must possess a tiny, extremely dense, positively charged nucleus containing nearly all the atom's mass.

  • Niels Bohr (19131913):

    • Introduced quantized electron energy levels, modeling electrons moving in fixed circular trajectories around the central nucleus.

  • Erwin Schrodinger (19261926):

    • Formulated the quantum-mechanical model of the atom.

    • Replaced exact circular paths with wavefunctions and three-dimensional orbitals, representing mathematical probability distributions for locating electrons.

  • James Chadwick (19321932):

    • Discovered the neutron, an uncharged subatomic particle residing within the atomic nucleus.

  • Fundamental Quantum Model Principle:

    • Electron energy remains strictly quantized, but electrons do not move in fixed circular trajectories.

Development and Modern Organization of the Periodic Table

  • Dmitri Mendeleev:

    • Organized known elements primarily in order of increasing atomic mass while grouping elements that exhibited repeating (periodic) chemical properties.

    • Demonstrated the predictive power of his table by leaving intentional gaps where the periodic pattern indicated undiscovered elements should exist, accurately predicting their chemical and physical properties.

  • Henry Moseley:

    • Used characteristic X-ray spectral measurements to demonstrate that nuclear charge increases in a systematic sequence by integer steps.

    • Replaced atomic mass with atomic number (ZZ) as the fundamental ordering principle of elements.

  • Modern Ordering Principle:

    • Elements are arranged by increasing atomic number (ZZ), which represents the number of protons in the nucleus and uniquely identifies each element.

    • Chemical periodicity directly reflects repeating patterns in valence-electron configurations. Elements within the same representative family share similar valence configurations, dictating similarities in bonding, ion formation, and chemical reactivity.

Fundamental Atomic Properties, Isotopes, and Mass Calculations

  • Key Atomic Quantities and Definitions:

    • Atomic Number (ZZ): Represents the total number of protons in an atom. Uniquely defines the element and measures total nuclear charge.

    • Mass Number (AA): Represents the total sum of protons plus neutrons in a specific isotope or nuclide (A=protons+neutronsA = \text{protons} + \text{neutrons}). Expressed as an integer used in isotope notation.

    • Isotopes: Atoms of the same element containing the identical atomic number (ZZ) but differing numbers of neutrons, resulting in different isotopic masses.

    • Neutral Atom: A state where the number of protons equals the number of electrons, yielding a net charge of zero (Net charge=0\text{Net charge} = 0).

    • Ion Charge: Calculated as the number of protons minus the number of electrons (Ion Charge=protons−electrons\text{Ion Charge} = \text{protons} - \text{electrons}). Positive for cations (electron loss) and negative for anions (electron gain).

    • Average Atomic Mass: The weighted average of the atomic masses of all naturally occurring isotopes of an element. Explains why atomic weights on the periodic table are non-integer decimal values.

  • Mathematical Formula for Average Atomic Mass:   Average Atomic Mass=∑(Isotope Mass×Fractional Abundance)\text{Average Atomic Mass} = \sum \left( \text{Isotope Mass} \times \text{Fractional Abundance} \right)   Fractional Abundance=Percentage Abundance100\text{Fractional Abundance} = \frac{\text{Percentage Abundance}}{100}

  • Step-by-Step Worked Calculation Example:

    • Problem: An element consists of two naturally occurring isotopes: Isotope 1 with a mass of 62.93 amu62.93\,\text{amu} (69.15%69.15\% abundance) and Isotope 2 with a mass of 64.93 amu64.93\,\text{amu} (30.85%30.85\% abundance). Calculate the average atomic mass.

    • Conversion to Fractional Abundance:     Fractional Abundance1=69.15100=0.6915\text{Fractional Abundance}_1 = \frac{69.15}{100} = 0.6915     Fractional Abundance2=30.85100=0.3085\text{Fractional Abundance}_2 = \frac{30.85}{100} = 0.3085

    • Set Up Equation:     Average Mass=(62.93 amu×0.6915)+(64.93 amu×0.3085)\text{Average Mass} = (62.93\,\text{amu} \times 0.6915) + (64.93\,\text{amu} \times 0.3085)

    • Evaluation:     Average Mass=43.516095 amu+20.030905 amu=63.547 amu≈63.55 amu\text{Average Mass} = 43.516095\,\text{amu} + 20.030905\,\text{amu} = 63.547\,\text{amu} \approx 63.55\,\text{amu}

Representative A-Group Families and Simple Ion Patterns

  • Group 1A — Alkali Metals:

    • Valence Electrons: 11

    • Chemical Character: Highly reactive metals (Hydrogen, H\text{H}, is a nonmetal exception).

    • Simple-Ion Pattern: Commonly forms +1+1 cations.

  • Group 2A — Alkaline-Earth Metals:

    • Valence Electrons: 22

    • Chemical Character: Reactive metals.

    • Simple-Ion Pattern: Commonly forms +2+2 cations.

  • Group 3A — Boron Family:

    • Valence Electrons: 33

    • Chemical Character: Boron (B\text{B}) is a metalloid; heavier members are predominantly metals.

    • Simple-Ion Pattern: Commonly forms +3+3 cations.

  • Group 4A — Carbon Family:

    • Valence Electrons: 44

    • Chemical Character: Transitions down the group from nonmetal (Carbon, C\text{C}) to metalloids (Silicon, Si\text{Si}; Germanium, Ge\text{Ge}) to metals (Tin, Sn\text{Sn}; Lead, Pb\text{Pb}).

    • Simple-Ion Pattern: No universal monatomic charge.

  • Group 5A — Nitrogen Family:

    • Valence Electrons: 55

    • Chemical Character: Mixed family containing nonmetals, metalloids, and metals.

    • Simple-Ion Pattern: Commonly forms −3-3 simple anions for lighter nonmetal members.

  • Group 6A — Oxygen Family / Chalcogens:

    • Valence Electrons: 66

    • Chemical Character: Oxygen (O\text{O}) and Sulfur (S\text{S}) are nonmetals; family becomes progressively more metallic downward.

    • Simple-Ion Pattern: Commonly forms −2-2 simple anions.

  • Group 7A — Halogens:

    • Valence Electrons: 77

    • Chemical Character: Highly reactive nonmetals.

    • Simple-Ion Pattern: Commonly forms −1-1 anions.

  • Group 8A — Noble Gases:

    • Valence Electrons: 88 (Helium, He\text{He}, has 22).

    • Chemical Character: Extremely low chemical reactivity / inert in introductory chemistry models.

    • Simple-Ion Pattern: No common simple monatomic ions formed.

  • Critical Application Note on Oxidation States:

    • Simple-ion charge patterns represent predictive trends rather than absolute oxidation-state rules.

    • This distinction is especially critical in the p-block: carbon-family elements do not all exist as 4+4+ monatomic ions, and heavier representative elements frequently exhibit multiple positive oxidation states.

B-Group Transition Region and Variable Oxidation States

  • Electronic Characteristics of Transition Elements:

    • Transition metals reside in the d-block of the periodic table.

    • Because dd and ss subshell electrons are close in energy, transition metals frequently lose varying numbers of electrons, forming multiple stable cations.

    • Compound naming requires Roman numerals to denote specific cation oxidation states (e.g., iron(II) chloride, FeCl2\text{FeCl}_2, vs. iron(III) chloride, FeCl3\text{FeCl}_3).

  • Systematic B-Group Classification and Ion Patterns:

    • Group 3B (Sc,Y\text{Sc}, \text{Y}): Commonly forms +3+3 ions.

    • Group 4B (Ti,Zr,Hf\text{Ti}, \text{Zr}, \text{Hf}): Commonly forms +4+4 ions; variable oxidation states occur.

    • Group 5B (V,Nb,Ta\text{V}, \text{Nb}, \text{Ta}): Exhibits variable positive oxidation states.

    • Group 6B (Cr,Mo,W\text{Cr}, \text{Mo}, \text{W}): Chromium (Cr\text{Cr}) is commonly +2+2 or +3+3 in simple salts; +6+6 appears in oxoanions like chromate (CrO42−\text{CrO}_4^{2-}) and dichromate (Cr2O72−\text{Cr}_2\text{O}_7^{2-}).

    • Group 7B (Mn,Tc,Re\text{Mn}, \text{Tc}, \text{Re}): Exhibits variable oxidation states.

    • Group 8B (Fe−Co−Ni\text{Fe}-\text{Co}-\text{Ni} Region): Iron (Fe2+,Fe3+\text{Fe}^{2+}, \text{Fe}^{3+}), Cobalt (Co2+,Co3+\text{Co}^{2+}, \text{Co}^{3+}), and Nickel (Ni2+\text{Ni}^{2+}) are standard examples.

    • Group 1B (Cu,Ag,Au\text{Cu}, \text{Ag}, \text{Au}): Copper commonly forms +1+1 and +2+2; Silver forms +1+1; Gold exhibits variable states.

    • Group 2B (Zn,Cd,Hg\text{Zn}, \text{Cd}, \text{Hg}): Zinc (Zn2+\text{Zn}^{2+}) and Cadmium (Cd2+\text{Cd}^{2+}) commonly form +2+2; Mercury exhibits variable oxidation states (e.g., Hg22+\text{Hg}_2^{2+} and Hg2+\text{Hg}^{2+}).

Electrostatic Principles and Periodic Trends

  • Core Driving Principle: Electrostatic Attraction (Coulombic Law)

    • Electrostatic force between nuclear protons and valence electrons governs periodic trends.

  • Trends Across a Period (Left to Right):

    • Nuclear Charge Dynamics: Protons are added to the nucleus while electrons are added to the same principal energy level (nn).

    • Effective Nuclear Charge (ZeffZ_{\text{eff}}): Core electron shielding does not increase sufficiently to offset the added nuclear protons. Consequently, ZeffZ_{\text{eff}} experienced by valence electrons increases across a period.

    • Atomic Radius: Decreases from left to right because higher ZeffZ_{\text{eff}} exerts a stronger pull on the electron cloud, drawing outer electrons closer to the nucleus.

    • First Ionization Energy (IE): Generally increases across a period because outer electrons experience stronger nuclear attraction, requiring more energy to remove. Exceptions must be justified using subshell energy levels and electron-electron pairing repulsions.

    • Electronegativity: Generally increases toward the upper-right region of the periodic table as smaller atoms with higher ZeffZ_{\text{eff}} attract shared bonding electrons more strongly.

  • Trends Down a Group (Top to Bottom):

    • Shell and Shielding Dynamics: Valence electrons enter higher principal quantum levels (nn), positioning them farther from the nucleus. Inner electron shells multiply, significantly increasing electron shielding.

    • Atomic Radius: Increases down a group because the valence shell has a larger principal quantum number and resides farther from the nucleus.

    • First Ionization Energy: Decreases down a group because increased distance and shielding weaken the net Coulombic pull on valence electrons, making them easier to remove.

  • Electron Affinity Details:

    • Measures the energy change associated with the addition of an electron to a gaseous atom. Its numerical values contain more local exceptions than the electronegativity trend.

  • Ionic Radii Dynamics:

    • Cations (M+\text{M}^+): Smaller than their neutral parent atoms (M\text{M}) due to loss of valence electrons, reduced electron-electron repulsion, and frequently the loss of an outer principal energy level.

    • Anions (X−\text{X}^-): Larger than their neutral parent atoms (X\text{X}) because added electrons increase electron-electron repulsion, expanding the overall electron cloud.

    • Isoelectronic Series: A group of species containing the identical number of electrons (e.g., O2−,F−,Na+,Mg2+\text{O}^{2-}, \text{F}^-, \text{Na}^+, \text{Mg}^{2+} all contain 10 electrons). Within an isoelectronic series, species with higher atomic numbers (ZZ) have more protons, exerting a stronger nuclear attraction on the electron cloud and resulting in a smaller ionic radius:     O2−(Z=8)>F−(Z=9)>Na+(Z=11)>Mg2+(Z=12)\text{O}^{2-} (Z=8) > \text{F}^- (Z=9) > \text{Na}^+ (Z=11) > \text{Mg}^{2+} (Z=12)

Classifications of Matter and Elemental Radioactivity

  • Structural Categories of Elements:

    • Metals: Occupy the left and central portions of the periodic table; characterized by luster, malleability, conductivity, and a strong tendency to lose electrons to form cations.

    • Nonmetals: Occupy the upper-right region (plus Hydrogen); characterized by high ionization energies/electronegativity and a tendency to gain electrons to form anions or share electrons in covalent bonds.

    • Metalloids (Semimetals): Positioned along the staircase line dividing metals and nonmetals, exhibiting intermediate physical and chemical properties. Standard set:     Boron (B),Silicon (Si),Germanium (Ge),Arsenic (As),Antimony (Sb),Tellurium (Te)\text{Boron (B)}, \text{Silicon (Si)}, \text{Germanium (Ge)}, \text{Arsenic (As)}, \text{Antimony (Sb)}, \text{Tellurium (Te)}

  • Rules Governing Elemental Radioactivity and Nuclear Stability:

    • Lighter Radioisotopes Exceptions: Technetium (Tc\text{Tc}, Z=43Z=43) and Promethium (Pm\text{Pm}, Z=61Z=61) have no stable isotopes.

    • Heavy Element Threshold: All elements with atomic numbers strictly greater than 82 (Z>82Z > 82) possess no stable isotopes. (Bismuth-209, 209Bi^{209}\text{Bi}, Z=83Z=83, is technically radioactive with an extremely long half-life).

    • Inner-Transition Series: The entire Actinide series (Z=89Z=89 to 103103) consists entirely of radioactive elements.

Classified Periodic Table Reference Data

Classified Periodic Table Main BlockLanthanides and Actinides Series
  • Representative Elements (Groups 1A - 8A):

    • Period 1: H (Z=1,1.008)\text{H}\, (Z=1, 1.008), He (Z=2,4.0026)\text{He}\, (Z=2, 4.0026)

    • Period 2: Li (Z=3,6.94)\text{Li}\, (Z=3, 6.94), Be (Z=4,9.0122)\text{Be}\, (Z=4, 9.0122), B (Z=5,10.81)\text{B}\, (Z=5, 10.81), C (Z=6,12.011)\text{C}\, (Z=6, 12.011), N (Z=7,14.007)\text{N}\, (Z=7, 14.007), O (Z=8,15.999)\text{O}\, (Z=8, 15.999), F (Z=9,18.998)\text{F}\, (Z=9, 18.998), Ne (Z=10,20.180)\text{Ne}\, (Z=10, 20.180)

    • Period 3: Na (Z=11,22.990)\text{Na}\, (Z=11, 22.990), Mg (Z=12,24.305)\text{Mg}\, (Z=12, 24.305), Al (Z=13,26.982)\text{Al}\, (Z=13, 26.982), Si (Z=14,28.085)\text{Si}\, (Z=14, 28.085), P (Z=15,30.974)\text{P}\, (Z=15, 30.974), S (Z=16,32.06)\text{S}\, (Z=16, 32.06), Cl (Z=17,35.45)\text{Cl}\, (Z=17, 35.45), Ar (Z=18,39.948)\text{Ar}\, (Z=18, 39.948)

    • Period 4: K (Z=19,39.098)\text{K}\, (Z=19, 39.098), Ca (Z=20,40.078)\text{Ca}\, (Z=20, 40.078), Ga (Z=31,69.723)\text{Ga}\, (Z=31, 69.723), Ge (Z=32,72.630)\text{Ge}\, (Z=32, 72.630), As (Z=33,74.922)\text{As}\, (Z=33, 74.922), Se (Z=34,78.971)\text{Se}\, (Z=34, 78.971), Br (Z=35,79.904)\text{Br}\, (Z=35, 79.904), Kr (Z=36,83.798)\text{Kr}\, (Z=36, 83.798)

    • Period 5: Rb (Z=37,85.468)\text{Rb}\, (Z=37, 85.468), Sr (Z=38,87.62)\text{Sr}\, (Z=38, 87.62), In (Z=49,114.82)\text{In}\, (Z=49, 114.82), Sn (Z=50,118.71)\text{Sn}\, (Z=50, 118.71), Sb (Z=51,121.76)\text{Sb}\, (Z=51, 121.76), Te (Z=52,127.60)\text{Te}\, (Z=52, 127.60), I (Z=53,126.90)\text{I}\, (Z=53, 126.90), Xe (Z=54,131.29)\text{Xe}\, (Z=54, 131.29)

    • Period 6: Cs (Z=55,132.91)\text{Cs}\, (Z=55, 132.91), Ba (Z=56,137.33)\text{Ba}\, (Z=56, 137.33), Tl (Z=81,204.38)\text{Tl}\, (Z=81, 204.38), Pb (Z=82,207.2)\text{Pb}\, (Z=82, 207.2), Bi (Z=83,208.98)\text{Bi}\, (Z=83, 208.98), Po (Z=84,[209])\text{Po}\, (Z=84, [209]) [Radioactive], At (Z=85,[210])\text{At}\, (Z=85, [210]) [Radioactive], Rn (Z=86,[222])\text{Rn}\, (Z=86, [222]) [Radioactive]

    • Period 7: Fr (Z=87,[223])\text{Fr}\, (Z=87, [223]) [Radioactive], Ra (Z=88,[226])\text{Ra}\, (Z=88, [226]) [Radioactive], Nh (Z=113,[286])\text{Nh}\, (Z=113, [286]) [Radioactive], Fl (Z=114,[290])\text{Fl}\, (Z=114, [290]) [Radioactive], Mc (Z=115,[290])\text{Mc}\, (Z=115, [290]) [Radioactive], Lv (Z=116,[293])\text{Lv}\, (Z=116, [293]) [Radioactive], Ts (Z=117,[294])\text{Ts}\, (Z=117, [294]) [Radioactive], Og (Z=118,[294])\text{Og}\, (Z=118, [294]) [Radioactive]

  • Transition Elements (d-Block Groups 3B - 2B):

    • First Transition Series (3d): Sc (Z=21,44.956)\text{Sc}\, (Z=21, 44.956), Ti (Z=22,47.867)\text{Ti}\, (Z=22, 47.867), V (Z=23,50.942)\text{V}\, (Z=23, 50.942), Cr (Z=24,51.996)\text{Cr}\, (Z=24, 51.996), Mn (Z=25,54.938)\text{Mn}\, (Z=25, 54.938), Fe (Z=26,55.845)\text{Fe}\, (Z=26, 55.845), Co (Z=27,58.933)\text{Co}\, (Z=27, 58.933), Ni (Z=28,58.693)\text{Ni}\, (Z=28, 58.693), Cu (Z=29,63.546)\text{Cu}\, (Z=29, 63.546), Zn (Z=30,65.38)\text{Zn}\, (Z=30, 65.38)

    • Second Transition Series (4d): Y (Z=39,88.906)\text{Y}\, (Z=39, 88.906), Zr (Z=40,91.224)\text{Zr}\, (Z=40, 91.224), Nb (Z=41,92.906)\text{Nb}\, (Z=41, 92.906), Mo (Z=42,95.95)\text{Mo}\, (Z=42, 95.95), Tc (Z=43,[98])\text{Tc}\, (Z=43, [98]) [Radioactive], Ru (Z=44,101.07)\text{Ru}\, (Z=44, 101.07), Rh (Z=45,102.91)\text{Rh}\, (Z=45, 102.91), Pd (Z=46,106.42)\text{Pd}\, (Z=46, 106.42), Ag (Z=47,107.87)\text{Ag}\, (Z=47, 107.87), Cd (Z=48,112.41)\text{Cd}\, (Z=48, 112.41)

    • Third Transition Series (5d): La (Z=57,138.91)\text{La}\, (Z=57, 138.91), Hf (Z=72,178.49)\text{Hf}\, (Z=72, 178.49), Ta (Z=73,180.95)\text{Ta}\, (Z=73, 180.95), W (Z=74,183.84)\text{W}\, (Z=74, 183.84), Re (Z=75,186.21)\text{Re}\, (Z=75, 186.21), Os (Z=76,190.23)\text{Os}\, (Z=76, 190.23), Ir (Z=77,192.22)\text{Ir}\, (Z=77, 192.22), Pt (Z=78,195.08)\text{Pt}\, (Z=78, 195.08), Au (Z=79,196.97)\text{Au}\, (Z=79, 196.97), Hg (Z=80,200.59)\text{Hg}\, (Z=80, 200.59)

    • Fourth Transition Series (6d, All Radioactive): Ac (Z=89,[227])\text{Ac}\, (Z=89, [227]) [Radioactive], Rf (Z=104,[267])\text{Rf}\, (Z=104, [267]) [Radioactive], Db (Z=105,[268])\text{Db}\, (Z=105, [268]) [Radioactive], Sg (Z=106,[269])\text{Sg}\, (Z=106, [269]) [Radioactive], Bh (Z=107,[270])\text{Bh}\, (Z=107, [270]) [Radioactive], Hs (Z=108,[269])\text{Hs}\, (Z=108, [269]) [Radioactive], Mt (Z=109,[277])\text{Mt}\, (Z=109, [277]) [Radioactive], Ds (Z=110,[281])\text{Ds}\, (Z=110, [281]) [Radioactive], Rg (Z=111,[282])\text{Rg}\, (Z=111, [282]) [Radioactive], Cn (Z=112,[285])\text{Cn}\, (Z=112, [285]) [Radioactive]

  • Lanthanoids (f-Block, 4f):

    • La (Z=57,138.91)\text{La}\, (Z=57, 138.91), Ce (Z=58,140.12)\text{Ce}\, (Z=58, 140.12), Pr (Z=59,140.91)\text{Pr}\, (Z=59, 140.91), Nd (Z=60,144.24)\text{Nd}\, (Z=60, 144.24), Pm (Z=61,[145])\text{Pm}\, (Z=61, [145]) [Radioactive], Sm (Z=62,150.36)\text{Sm}\, (Z=62, 150.36), Eu (Z=63,151.96)\text{Eu}\, (Z=63, 151.96), Gd (Z=64,157.25)\text{Gd}\, (Z=64, 157.25), Tb (Z=65,158.93)\text{Tb}\, (Z=65, 158.93), Dy (Z=66,162.50)\text{Dy}\, (Z=66, 162.50), Ho (Z=67,164.93)\text{Ho}\, (Z=67, 164.93), Er (Z=68,167.26)\text{Er}\, (Z=68, 167.26), Tm (Z=69,168.93)\text{Tm}\, (Z=69, 168.93), Yb (Z=70,173.05)\text{Yb}\, (Z=70, 173.05), Lu (Z=71,174.97)\text{Lu}\, (Z=71, 174.97)

  • Actinides (f-Block, 5f, All Radioactive):

    • Ac (Z=89,[227])\text{Ac}\, (Z=89, [227]) [Radioactive], Th (Z=90,232.04)\text{Th}\, (Z=90, 232.04), Pa (Z=91,231.04)\text{Pa}\, (Z=91, 231.04), U (Z=92,238.03)\text{U}\, (Z=92, 238.03), Np (Z=93,[237])\text{Np}\, (Z=93, [237]) [Radioactive], Pu (Z=94,[244])\text{Pu}\, (Z=94, [244]) [Radioactive], Am (Z=95,[243])\text{Am}\, (Z=95, [243]) [Radioactive], Cm (Z=96,[247])\text{Cm}\, (Z=96, [247]) [Radioactive], Bk (Z=97,[247])\text{Bk}\, (Z=97, [247]) [Radioactive], Cf (Z=98,[251])\text{Cf}\, (Z=98, [251]) [Radioactive], Es (Z=99,[252])\text{Es}\, (Z=99, [252]) [Radioactive], Fm (Z=100,[257])\text{Fm}\, (Z=100, [257]) [Radioactive], Md (Z=101,[258])\text{Md}\, (Z=101, [258]) [Radioactive], No (Z=102,[259])\text{No}\, (Z=102, [259]) [Radioactive], Lr (Z=103,[266])\text{Lr}\, (Z=103, [266]) [Radioactive]

AP-Style Practice and Conceptual Review Questions

  • Question 1: Rutherford observed that most alpha particles passed through gold foil while a very small fraction were strongly deflected. Explain how both observations support the nuclear model.

  • Question 2: State one idea from the Bohr model retained in modern atomic theory and one idea that the quantum-mechanical model replaced.

  • Question 3: Explain why Mendeleev's predictions of undiscovered elements provided strong evidence for periodicity.

  • Question 4: Explain why atomic number is the fundamental identifier of an element whereas average atomic mass is not.

  • Question 5: A 3+3+ ion contains 2626 protons and 3030 neutrons. Determine ZZ, AA, and the number of electrons.

  • Question 6: Calculate the average atomic mass for isotopes 62.93 amu62.93\,\text{amu} (69.15%69.15\%) and 64.93 amu64.93\,\text{amu} (30.85%30.85\%). Show the setup.

  • Question 7: For groups 1A, 2A, 6A, 7A, and 8A, give the family name, number of valence electrons, and useful simple-ion pattern.

  • Question 8: Explain why 6A is called the oxygen family and why −2-2 is useful for O\text{O} and S\text{S} but should not be treated as the only oxidation state of every 6A element.

  • Question 9: Explain why transition metals are more likely than 1A and 2A metals to require Roman numerals in compound names.

  • Question 10: Rank Na\text{Na}, Mg\text{Mg}, and Al\text{Al} from largest to smallest atomic radius. Justify with effective nuclear charge.

  • Question 11: Rank Na\text{Na}, Mg\text{Mg}, and Cl\text{Cl} from lowest to highest first ionization energy. Explain the general trend.

  • Question 12: Explain why Na+\text{Na}^+ is smaller than Na\text{Na} and why F−\text{F}^- is larger than F\text{F}.

  • Question 13: O2−\text{O}^{2-}, F−\text{F}^-, Na+\text{Na}^+, and Mg2+\text{Mg}^{2+} are isoelectronic. Rank them from largest to smallest and justify using nuclear charge.

  • Question 14: Classify Si\text{Si}, Br\text{Br}, Fe\text{Fe}, Ne\text{Ne}, Tc\text{Tc}, and U\text{U} as specifically as possible using the periodic table.

  • Question 15: Explain why "every 4A element forms a 4+4+ monatomic ion" is incorrect.

  • Question 16: A student says atomic radius increases from left to right because atomic number increases. Evaluate the statement and give the correct AP Chemistry explanation.

  • Question 17: Explain how shielding and principal energy level affect first ionization energy down a group.

  • Question 18: Explain why electronegativity and ionization energy often show similar broad periodic directions but are not the same property.

  • Question 19: Identify the two elements Tc\text{Tc} and Pm\text{Pm} as unusual with respect to stable isotopes, and identify the fully radioactive inner-transition series.

  • Question 20: Write a short AP-style justification for why Mg2+\text{Mg}^{2+} is smaller than O2−\text{O}^{2-} even though both ions have 1010 electrons.