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Orbitals are the areas outside of the atomic nucleus where electrons are most likely to reside. They are characterized by different energy levels, sha…
Atomic orbitals are three-dimensional regions around the nucleus where an electron is most likely to be found.
The first energy level is nearest to the nucleus and has the lowest energy. It contains a single spherical s orbital.
The second energy level contains four orbitals: one lower-energy 2s orbital and three higher-energy 2p orbitals. Each p orbital is dumbbell-shaped and points along the x-, y-, or z-axis.
The third energy level, along with s and p orbitals, also includes five d orbitals. Four of the 3d orbitals have a cloverleaf shape, while the fifth has two lobes and a ring around the center.
In an orbital diagram, a box represents an orbital, and arrows represent electrons. Each orbital can hold a maximum of two electrons with only opposite spins: one spin-up and one spin-down.
Electrons in the ground state fill atomic orbitals from lowest to highest energy to reach the most stable configuration. For example, sodium has 11 electrons. Two electrons with opposite spins fill the 1s orbital first. Similarly, two electrons fill the 2s orbital. Next, one electron enters each of the three 2p orbitals with the same spin. After that, electrons pair with opposite spins until all three 2p orbitals are filled. Finally, one electron enters the 3s orbital.
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Q1: What are atomic orbitals and where are electrons located?
Atomic orbitals are three-dimensional regions around the nucleus where electrons are most likely to be found. Rather than fixed circular paths, orbitals are cloud-like areas characterized by different energy levels, shapes, and three-dimensional orientations. Electrons occupy these regions based on their energy state and the atom's electron configuration.
Q2: How do electrons fill orbitals in the ground state?
Electrons fill atomic orbitals from lowest to highest energy to reach the most stable configuration. Each orbital can hold a maximum of two electrons with opposite spins. For example, sodium's 11 electrons fill the 1s orbital first with two electrons, then the 2s orbital, followed by the three 2p orbitals, and finally one electron enters the 3s orbital.
Q3: What are the different shapes and characteristics of orbitals?
The first energy level contains a single spherical s orbital. The second level includes one 2s orbital and three dumbbell-shaped 2p orbitals pointing along the x-, y-, or z-axis. The third level adds five d orbitals: four with cloverleaf shapes and one with two lobes and a ring. Higher energy levels contain increasingly complex orbital shapes.
Q4: How many electrons can fit in each energy level?
The first shell holds two electrons in its single 1s orbital. The second shell holds eight total electrons: two in the 2s orbital and two in each of the three 2p orbitals. The third shell can accommodate 18 electrons across s, p, and d subshells. Higher shells accommodate more electrons as d and f subshells become available.
Q5: What is the difference between Bohr's model and Schrödinger's model of orbitals?
Bohr's 1913 model assumed electrons orbited the nucleus in fixed circular paths and accurately predicted hydrogen's behavior. Schrödinger's 1926 quantum mechanical model expanded this by treating electrons as waves affected by the nucleus's positive charge, creating cloud-like orbital regions. Schrödinger's model accurately predicts electron configurations for elements with multiple electrons.
Q6: How do orbital diagrams represent electrons and their energy levels?
In orbital diagrams, boxes represent individual orbitals and arrows represent electrons. Each arrow's direction indicates electron spin: spin-up or spin-down. The diagram's layout shows relative energy levels, with lower-energy orbitals positioned below higher-energy ones, allowing visualization of how electrons distribute across an atom's orbitals.
Q7: What happens when electrons gain or lose energy in atoms?
When electrons gain energy from heat or light, they enter an excited state and jump to higher orbitals. When they lose that energy rapidly, they fall back to lower orbitals and emit a photon of light. The color of the emitted photon corresponds to a specific energy amount that can be measured using a spectroscope.