
Explore the periodic table, unveiling how elements are classified by atomic numbers, moved left to right into blocks and groups, with references to lanthanides and actinides.
Describe how the periodic table classifies elements, from Newlands' octaves and the Devonian approach to modern periodic law and the long-form periodic table, emphasizing atomic number and periodic trends.
Understand the need for classification as the number of elements grew, and see how scientists grouped similar elements into vertical columns to form the periodic table and predict their properties.
Examines early attempts to classify elements, from grouping by similar properties to using atomic masses to predict relationships, and introduces Newlands octaves.
Learn how Dmitri Mendeleev proposed the periodic table and the periodic law, arranging elements by increasing atomic weights to reveal repeating properties and gaps for undiscovered elements.
Analyze the merits of Mendeleev's periodic table: systematic element classification, gaps for undiscovered elements, and predicted properties; and correct atomic weights for elements like beryllium, gold, and platinum.
Defects of Mendeleev's periodic table are explored, including hydrogen placement, isotopes, atomic-mass inversions, and misgrouping of similar and dissimilar elements, motivating a revised periodic table.
Discover how the modern periodic law uses atomic number to explain the periodic recurrence of element properties, yielding the long-form periodic table with 18 groups and s, p, d blocks.
Explore how periodic trends in groups shape atomic properties, including atomic number, valence electrons, ionization energy, electron affinity, electronegativity, and metallic versus nonmetallic character.
Explore how periodic trends arise across a period, including ionization energy, atomic size, electron affinity, electronegativity, and metallic versus nonmetallic character.
Classify elements into s, p, d, and f blocks based on configuration, with alkali metals in the s-block, transition metals in the d-block, and lanthanides and actinides in the f-block.
Explore the merits and demerits of the long form periodic table, including its basis on atomic number and electron configuration, anomaly removal, and ongoing spiral table developments.
Before the nineteenth century, only a few elements were known. These elements could
be easily studied individually.
With the passage of time, many more elements were discovered. More and more of
their compounds were prepared. Study of these elements and compounds individually
became more difficult. So, it was felt that these elements should be classified into a
few groups to make their study systematic and easier. It is expected that a systematic
classification will help us in
• organising the knowledge,
• predicting new elements for undertaking further studies.
One of the earliest attempts towards the classification of elements was to divide these
into metals, and non-metals.
This method of classification failed because most of the elements fell into the
category of metals, whereas only a few elements could be grouped as non-metals.
There were also a few elements which showed the properties of both metals and
non-metals.
Since then, many attempts were made by various scientists to classify elements
in a more systematic way. A few important attempts for the classification of
elements are described over here. There are more than one hundred chemical elements
known today. It is very difficult to study the properties of each element individually, so
these elements were classified on the basis of their similarities in properties. In this
course, we shall discuss the historical development of Mendeleev's periodic table,
modern periodic law and the electronic configuration of atoms as the basis for periodic
classification, the characteristics of s, p, d, f block elements and the periodicity
in physical and chemical properties of the elements.