Classification of Elements and Periodicity in Properties - Notes

Classification of Elements and Periodicity in Properties

Objectives

  • Appreciate how grouping elements based on properties led to the Periodic Table.
  • Understand the Periodic Law.
  • Understand the significance of atomic number and electronic configuration for periodic classification.
  • Name elements with Z > 100 using IUPAC nomenclature.
  • Classify elements into s, p, d, f blocks and learn their characteristics.
  • Recognize periodic trends in physical and chemical properties.
  • Compare element reactivity and correlate with their natural occurrence.
  • Explain the relationship between ionization enthalpy and metallic character.
  • Use scientific vocabulary for atomic/ionic radii, ionization enthalpy, electron gain enthalpy, electronegativity, and valence.

Introduction

  • The Periodic Table is a crucial concept in chemistry for students, researchers, and professionals.
  • It demonstrates that elements are not randomly assorted but show trends and form families.
  • Understanding the Periodic Table is essential for comprehending the fundamental building blocks of chemistry.

2.1 Why Classify Elements?

  • Elements are the basic units of matter.
  • In 1800, 31 elements were known; by 1865, the number doubled to 63; currently, 114 elements are known, with ongoing efforts to synthesize more.
  • Studying the chemistry of each element and their compounds individually is challenging due to the large number of elements.
  • Scientists classify elements to organize knowledge, rationalize chemical facts, and predict new ones.

2.2 Genesis of Periodic Classification

  • Classification and the Periodic Law result from systematizing knowledge gained through observations and experiments.

  • Johann Dobereiner (early 1800s) identified trends among element properties, noting similarities within groups of three elements (Triads) by 1829.

  • In Triads, the middle element's atomic weight was approximately halfway between the other two, and its properties were intermediate.

    • Dobereiner's Triads:

      • Lithium (Li): Atomic weight 7

      • Sodium (Na): Atomic weight 23

      • Potassium (K): Atomic weight 39

      • Calcium (Ca): Atomic weight 40

      • Strontium (Sr): Atomic weight 88

      • Barium (Ba): Atomic weight 137

      • Chlorine (Cl): Atomic weight 35.5

      • Bromine (Br): Atomic weight 80

      • Iodine (I): Atomic weight 127

  • The Law of Triads was dismissed as coincidence because it only worked for a few elements.

  • A.E.B. de Chancourtois (1862) arranged elements by increasing atomic weights in a cylindrical table, but this received little attention.

  • John Alexander Newlands (1865) proposed the Law of Octaves, arranging elements by atomic weights and noting that every eighth element had similar properties -- similar to musical octaves.

    • Newlands' Octaves:

      • Li (7), Be (9), B (11), C (12), N (14), O (16), F (19)
      • Na (23), Mg (24), Al (27), Si (29), P (31), S (32), Cl (35.5)
      • K (39), Ca (40)
  • The Law of Octaves was only true for elements up to calcium.

  • Newlands was later awarded the Davy Medal in 1887 by the Royal Society, London, for his work.

  • Dmitri Mendeleev (1834-1907) and Lothar Meyer (1830-1895) independently developed the Periodic Law.

  • In 1869, both chemists proposed that elements arranged by increasing atomic weights show regular intervals in physical and chemical properties.

  • Lothar Meyer plotted physical properties like atomic volume, melting point, and boiling point against atomic weight, observing a periodically repeated pattern with changes in the length of the repeating pattern.

  • By 1868, Meyer had developed a table resembling the Modern Periodic Table, but his work was published after Mendeleev's.

  • Mendeleev is credited with first publishing the Periodic Law:

    • "The properties of the elements are a periodic function of their atomic weights."
  • Mendeleev arranged elements in rows and columns by increasing atomic weights, placing elements with similar properties in the same column or group.

  • Mendeleev's classification was more elaborate than Meyer's and recognized the significance of periodicity, using a broader range of physical and chemical properties.

  • Mendeleev relied on similarities in empirical formulas and compound properties.

  • He sometimes ignored atomic weight order to group similar elements together, assuming atomic weight measurements were incorrect.

    • For example, iodine (lower atomic weight) was placed with fluorine, chlorine, and bromine due to similar properties, despite tellurium having a higher atomic weight.
  • Mendeleev left gaps in the table, predicting undiscovered elements such as gallium and germanium, which he called Eka-Aluminium and Eka-Silicon, respectively.

  • Mendeleev predicted the properties of these elements, which were later discovered.

    • Mendeleev’s Predictions for Eka-aluminium (Gallium) and Eka-silicon (Germanium):

      • Eka-aluminium (predicted):

        • Atomic weight: 68
        • Density: 5.9 g/cm³
        • Melting point: Low
        • Formula of oxide: E<em>2O</em>3E<em>2O</em>3
        • Formula of chloride: ECl3ECl_3
      • Gallium (found):

        • Atomic weight: 70
        • Density: 5.94 g/cm³
        • Melting point: 302.93 K
        • Formula of oxide: Ga<em>2O</em>3Ga<em>2O</em>3
        • Formula of chloride: GaCl3GaCl_3
      • Eka-silicon (predicted):

        • Atomic weight: 72
        • Density: 5.5 g/cm³
        • Melting point: High
        • Formula of oxide: EO2EO_2
        • Formula of chloride: ECl4ECl_4
      • Germanium (found):

        • Atomic weight: 72.6
        • Density: 5.36 g/cm³
        • Melting point: High
        • Formula of oxide: GeO2GeO_2
        • Formula of chloride: GeCl4GeCl_4
  • Mendeleev's quantitative predictions and their accuracy made him and his Periodic Table famous.

2.3 Modern Periodic Law and the Present Form of the Periodic Table

  • When Mendeleev developed his table, the internal structure of the atom was unknown.

  • In 1913, Henry Moseley observed regularities in the X-ray spectra of elements.

  • Plotting v\sqrt{v} (where vv is the frequency of X-rays emitted) against atomic number (Z) yielded a straight line, unlike plots against atomic mass.

  • Moseley demonstrated that atomic number is a more fundamental element property than atomic mass.

  • The Modern Periodic Law states:

    • "The physical and chemical properties of the elements are periodic functions of their atomic numbers."
  • The Periodic Law revealed analogies among the 94 naturally occurring elements and stimulated interest in inorganic chemistry, leading to the creation of artificial elements.

  • Atomic number equals nuclear charge (number of protons) or the number of electrons in a neutral atom.

  • The Periodic Law is a consequence of periodic variation in electronic configurations, which determine physical and chemical properties.

  • Numerous Periodic Table forms exist, some emphasizing chemical reactions and valence, others focusing on electronic configuration.

  • The "long form" of the Periodic Table is most convenient and widely used.

  • Horizontal rows are called periods, and vertical columns are called groups.

  • Elements with similar outer electronic configurations are arranged in vertical columns (groups or families).

  • IUPAC recommends numbering groups from 1 to 18, replacing older notations.

  • There are seven periods; the period number corresponds to the highest principal quantum number (n).

  • The first period has 2 elements; subsequent periods have 8, 8, 18, 18, and 32 elements, respectively.

  • The seventh period is incomplete but theoretically has a maximum of 32 elements.

  • 14 elements of the sixth and seventh periods (lanthanoids and actinoids) are placed in separate panels at the bottom.

2.4 Nomenclature of Elements with Atomic Numbers > 100

  • Traditionally, the discoverer names new elements, subject to IUPAC ratification.

  • Controversies have arisen because new elements with high atomic numbers are highly unstable and available in minute quantities.

  • Synthesis and characterization require sophisticated equipment, leading to competition among laboratories.

  • Scientists may prematurely claim discovery before collecting reliable data.

  • For example, both American and Soviet scientists claimed discovery of element 104, naming it Rutherfordium and Kurchatovium, respectively.

  • IUPAC recommends a systematic nomenclature derived from the atomic number using numerical roots until discovery is proven and the name is officially recognized.

  • Roots for digits 0-9 are:

    • 0 = nil (n)
    • 1 = un (u)
    • 2 = bi (b)
    • 3 = tri (t)
    • 4 = quad (q)
    • 5 = pent (p)
    • 6 = hex (h)
    • 7 = sept (s)
    • 8 = oct (o)
    • 9 = enn (e)
  • The roots are combined in the order of the digits in the atomic number, and "ium" is added at the end.

  • IUPAC names for elements with Z > 100 are listed (see table in the transcript).

  • A new element initially receives a temporary name and symbol consisting of three letters.

  • A permanent name and symbol are later assigned by a vote of IUPAC representatives, reflecting the discovery country or honoring a notable scientist.

  • As of now, elements up to 112, 114, and 116 have been discovered; 113, 115, 117, and 118 are not yet known.

  • Problem: What is the IUPAC name and symbol for element 120?

    • Solution: unbinilium (Ubn)

2.5 Electronic Configurations of Elements and the Periodic Table

  • An electron in an atom is characterized by four quantum numbers; the principal quantum number (n) defines the main energy level or shell.
  • Electrons fill different subshells or orbitals (s, p, d, f) in an atom, resulting in its electronic configuration.
  • An element's position in the Periodic Table reflects the quantum numbers of the last orbital filled.
(a) Electronic Configurations in Periods
  • The period indicates the value of n for the outermost or valence shell.

  • Successive periods correspond to filling the next higher principal energy level (n = 1, n = 2, etc.).

  • The number of elements in each period is twice the number of atomic orbitals available in the energy level being filled.

  • The first period (n = 1) starts with filling the 1s level, with hydrogen (1s11s^1) and helium (1s21s^2) completing the K shell.

  • The second period (n = 2) starts with lithium, and the third electron enters the 2s orbital; beryllium has the configuration 1s22s21s^2 2s^2.

  • From boron, the 2p orbitals fill until neon, which completes the L shell (2s22p62s^2 2p^6). Thus, there are 8 elements in the second period.

  • The third period (n = 3) begins with sodium, where the added electron enters the 3s orbital. Successive filling of 3s and 3p orbitals results in 8 elements, from sodium to argon.

  • The fourth period (n = 4) starts with potassium, and the added electrons fill the 4s orbital. Before the 4p orbital fills, the 3d orbitals become energetically favorable, leading to the 3d transition series.

  • Scandium (Z = 21) has the electronic configuration 3d14s23d^1 4s^2. The 3d orbitals are filled at zinc (Z = 30), with the configuration 3d104s23d^{10} 4s^2.

  • The fourth period ends at krypton with the filling of the 4p orbitals, totaling 18 elements.

  • The fifth period (n = 5) begins with rubidium and is similar to the fourth period, containing the 4d transition series starting at yttrium (Z = 39).

  • This period ends at xenon with the filling of the 5p orbitals.

  • The sixth period (n = 6) contains 32 elements, with electrons successively entering 6s, 4f, 5d, and 6p orbitals.

  • Filling of the 4f orbitals begins with cerium (Z = 58) and ends at lutetium (Z = 71), forming the 4f inner transition series or lanthanide series.

  • The seventh period (n = 7) is similar to the sixth period, with successive filling of the 7s, 5f, 6d, and 7p orbitals, including most man-made radioactive elements.

  • This period will end at element 118, a noble gas. Filling the 5f orbitals after actinium (Z = 89) gives the 5f inner transition series or actinide series.

  • The 4f and 5f inner transition series are placed separately to maintain structure and group elements with similar properties.

  • Problem: How would you justify the presence of 18 elements in the 5th period of the Periodic Table?

    • Solution: For n = 5, l = 0, 1, 2, 3. The order of increasing energy is 5s < 4d < 5p. There are 9 available orbitals, accommodating 18 electrons, thus 18 elements.
(b) Groupwise Electronic Configurations
  • Elements in the same vertical column (group) have similar valence shell electronic configurations, the same number of outer electrons, and similar properties.

  • Group 1 elements (alkali metals) all have ns1ns^1 valence shell electronic configurations.

    • Li: [He\text{He}] 2s12s^1
    • Na: [Ne\text{Ne}] 3s13s^1
    • K: [Ar\text{Ar}] 4s14s^1
    • Rb: [Kr\text{Kr}] 5s15s^1
    • Cs: [Xe\text{Xe}] 6s16s^1
    • Fr: [Rn\text{Rn}] 7s17s^1
  • Element properties have periodic dependence on atomic number, not relative atomic mass.

2.6 Electronic Configurations and Types of Elements: s, p, d, f Blocks

  • The Aufbau principle and electronic configurations give theoretical foundation for periodic classification.
  • Elements in a vertical column constitute a group or family, exhibiting similar chemical behavior due to the same number and distribution of electrons in their outermost orbitals.
  • Elements are classified into s-block, p-block, d-block, and f-block based on the type of atomic orbital being filled with the last electron.
  • Exceptions include helium, which belongs to the s-block but is placed in the p-block due to its filled valence shell (1s21s^2), exhibiting noble gas properties. Hydrogen, with one electron, can be placed in Group 1 or Group 17, but is placed separately at the top of the table because it is a special case.
2.6.1 The s-Block Elements
  • Group 1 (alkali metals) and Group 2 (alkaline earth metals) have ns1ns^1 and ns2ns^2 outermost electronic configurations, respectively.
  • They are reactive metals with low ionization enthalpies, readily losing outermost electrons to form 1+ or 2+ ions.
  • Metallic character and reactivity increase down the group.
  • Due to high reactivity, they are never found pure in nature.
  • Compounds of s-block elements, except those of lithium and beryllium, are predominantly ionic.
2.6.2 The p-Block Elements
  • p-Block elements comprise Groups 13 to 18; together with s-block elements, they are called Representative Elements or Main Group Elements.
  • Outermost electronic configurations vary from ns2np1ns^2np^1 to ns2np6ns^2np^6 in each period.
  • Each period ends with a noble gas element having a closed valence shell ns2np6ns^2np^6 configuration.
  • Noble gases have low chemical reactivity due to the difficulty of altering their stable configuration.
  • Halogens (Group 17) and chalcogens (Group 16) are chemically important non-metals with highly negative electron gain enthalpies, readily adding one or two electrons to attain a stable noble gas configuration.
  • Non-metallic character increases from left to right across a period, while metallic character increases down the group.
2.6.3 The d-Block Elements (Transition Elements)
  • d-Block elements are in Groups 3 to 12 in the center of the Periodic Table, characterized by filling inner d orbitals with electrons.
  • They have the general outer electronic configuration (n1)d110ns12(n-1)d^{1-10} ns^{1-2}.
  • They are all metals, mostly forming colored ions, exhibiting variable valence (oxidation states), paramagnetism, and are often used as catalysts.
  • Zn, Cd, and Hg, with configuration (n1)d10ns2(n-1)d^{10} ns^2, do not show most transition element properties.
  • Transition metals bridge chemically active s-block metals and less active elements of Groups 13 and 14.
2.6.4 The f-Block Elements (Inner-Transition Elements)
  • The two rows at the bottom of the Periodic Table are Lanthanoids (Ce(Z = 58) - Lu(Z = 71)) and Actinoids (Th(Z = 90) - Lr(Z = 103)).

  • They have the outer electronic configuration (n2)f114(n1)d01ns2(n-2)f^{1-14} (n-1)d^{0-1}ns^2, with the last electron entering the f-orbital.

  • These are called Inner-Transition Elements (f-Block Elements) and are all metals.

  • Elements within each series have similar properties.

  • Early actinoid chemistry is more complicated than lanthanoid chemistry due to the large number of possible oxidation states.

  • Actinoid elements are radioactive.

  • Many actinoid elements are made in nanogram quantities or less by nuclear reactions, and their chemistry is not fully studied.

  • Elements after uranium are called Transuranium Elements.

  • Problem: The elements Z = 117 and 120 have not yet been discovered. In which family / group would you place these elements and also give the electronic configuration in each case.

    • Solution: Element Z = 117 belongs to the halogen family (Group 17) with electronic configuration [Rn\text{Rn}] 5f146d107s27p55f^{14}6d^{10}7s^27p^5. Element Z = 120 will be placed in Group 2 (alkaline earth metals) with electronic configuration [Uuo\text{Uuo}] 8s28s^2.