Chemistry · Ch 2 — Structure of Atom
Shapes of Atomic Orbitals
Shapes of Atomic Orbitals
The Shapes of Atomic Orbitals
The quantum mechanical model of the atom tells us that an atomic orbital is a one-electron wave function, . While itself has no direct physical meaning, the square of its magnitude, , gives the probability density of finding the electron at a given point in space. The shape of an orbital is essentially a three-dimensional boundary surface that encloses the region where there is a high probability (typically 90–95%) of finding the electron.
For hydrogen and hydrogen-like species, the solutions to the Schrödinger equation yield orbitals characterized by three quantum numbers: the principal quantum number , the azimuthal quantum number , and the magnetic quantum number . The shape of an orbital is determined primarily by the azimuthal quantum number . For , we get s orbitals; for , p orbitals; for , d orbitals; and for , f orbitals.
The s Orbitals
All s orbitals () are spherically symmetric. This means the probability of finding the electron depends only on its distance from the nucleus, not on the direction. The boundary surface for a 1s orbital is a sphere centred on the nucleus.
Drawn by us to help you understand the concept clearly, and verified to make sure it's accurate. For exams, practice from your textbook's own diagram.
Fig. 2.12 is a set of four plots that show how the wave function (top row) and the probability density (bottom row) behave as you move away from the nucleus along a radial line , for the 1s orbital (left) and the 2s orbital (right).
In the top row, the 1s curve starts at a high positive value right at the nucleus () and then decays smoothly toward zero as increases — no sign change, no bumps. The 2s curve also starts positive, but it does something the 1s curve does not: it crosses zero (the point marked node in the plot), goes negative, and then returns toward zero from below. That crossing point is a radial node — a spherical shell where the wave function is exactly zero.
The bottom row shows for the same orbitals. The 1s curve begins at a very high value at and decays monotonically. The 2s curve starts high, drops to zero at the same radial node, rises to a small local maximum, and then decays to zero. The key point: is never negative — it is always zero or positive, because it is a squared quantity.
The radial node in the 2s orbital is a direct consequence of the wave function changing sign. For an orbital, the number of radial nodes is . So 1s has zero radial nodes, 2s has one, 3s has two, and so on.
The physical idea this figure teaches is that the wave function can have positive and negative regions, but the probability of finding the electron — given by — is always non-negative. The node is a spherical surface where the electron is never found. The 1s orbital has no such surface; the electron can be found anywhere (with decreasing probability as increases). The 2s orbital has one spherical shell of zero probability.
The central formula that the textbook develops with this figure is the relationship between the wave function and probability density:
Here is the probability of finding the electron in a small volume element at a distance from the nucleus. is the probability density — the probability per unit volume. The figure shows that for the 1s orbital, this probability density is maximum at the nucleus and falls off smoothly. For the 2s orbital, it drops to zero at the node, then rises again before finally decaying.
The wave function itself has no direct physical meaning — only does. That is why the textbook plots both: shows the mathematical form (including sign changes), while shows the physically meaningful probability distribution. …
As increases, the size of the s orbital increases. The 2s orbital is larger than the 1s, and the 3s is larger than the 2s. But there is another important feature: s orbitals for have radial nodes — spherical surfaces where the probability of finding the electron is zero. The 2s orbital has one radial node, the 3s has two, and so on. The number of radial nodes for an s orbital is .
The 1s orbital has no radial nodes. The 2s orbital has one radial node, which means there is a spherical shell at a certain distance from the nucleus where . Inside this shell, the probability density is high near the nucleus; outside it, the density rises again to a maximum before decaying.
Drawn by us to help you understand the concept clearly, and verified to make sure it's accurate. For exams, practice from your textbook's own diagram.
Fig. 2.13 is the first visual bridge between the abstract wavefunction and the concrete picture of an orbital that you can hold in your mind. It shows two different ways of representing the same quantum object: the 1s and 2s orbitals of hydrogen.
Panel (a) — Probability density plots. These are electron-cloud pictures: the depth of shading at any point is proportional to , the probability density (the book's own version builds the same picture out of individual dots). For the 1s orbital the cloud is darkest at the nucleus and fades smoothly outward — a single spherical cloud with no gap; the probability is highest at the centre and decreases monotonically.
For the 2s orbital, the picture is strikingly different. Close to the nucleus there is a dense inner cloud. Then, at a certain distance, a spherical shell appears where the shading vanishes completely — the nodal region (labelled in the figure). Beyond that node, a second, outer shell of cloud appears, fainter than the inner region but clearly present. This is the first direct visual evidence that can go to zero at a finite distance from the nucleus, even though the electron is still bound to the atom.
Panel (b) — Boundary surface diagrams. These are simplified, practical representations. Instead of showing every dot, we choose a constant- surface that encloses about 90% of the total probability of finding the electron. For the 1s orbital, that surface is a single sphere. For the 2s orbital, the boundary surface is also a sphere, but it is larger than the 1s sphere. The key point: the boundary surface diagram of the 2s orbital does not show the internal node — it only shows the outer envelope. The node is invisible in this representation, which is why the textbook explicitly labels the "nodal region" in panel (a) but not in panel (b).
A common mistake is to think the 2s boundary surface is hollow or has a gap inside. It does not. The boundary surface is a single continuous sphere. The node is a spherical surface inside that sphere where , but the boundary surface is drawn at a much larger radius, so it hides the node. Always check the dot-density plot to see the node.
The physical idea this figure teaches is profound: orbitals are not fixed paths. The electron does not orbit the nucleus like a planet. Instead, the orbital is a region of space where the electron is likely to be found, and that region can have internal structure — including nodes where the probability is exactly zero. The 2s orbital has one radial node; the 1s orbital has none. In general, an ns orbital has radial nodes.
The central formula that connects the figure to the theory is the definition of probability density:
where is the wavefunction (the atomic orbital) and is the probability density at a distance from the nucleus. The dot-density in panel (a) is a visual representation of . The boundary surface in panel (b) is drawn at a value of such that the volume integral of over the enclosed region equals 0.9 (or 90%).
For the 1s orbital, the wavefunction is:
where is the Bohr radius (). This function is positive everywhere and decays exponentially — no nodes.
For the 2s orbital, the wavefunction has a radial node:
The factor changes sign at , making there. Since is the square, the probability density is zero at that radius — that is the nodal region you see in the dot-density plot. …
The p Orbitals
For , we have p orbitals. Unlike s orbitals, p orbitals are not spherically symmetric. They have a dumbbell shape, consisting of two lobes on opposite sides of the nucleus, separated by a nodal plane (a plane where the probability of finding the electron is zero).
For a given principal quantum number (where ), there are three p orbitals, corresponding to the three possible values of the magnetic quantum number : , , and . These three orbitals are oriented along the x, y, and z axes and are labelled , , and respectively.
Drawn by us to help you understand the concept clearly, and verified to make sure it's accurate. For exams, practice from your textbook's own diagram.
The figure shows three separate coordinate systems, each with a single dumbbell-shaped orbital drawn through the origin. Each dumbbell has two identical lobes, one on each side of the nucleus, and the nucleus sits at the centre where the axes cross. The three orbitals are labelled , , and , and each one is aligned along a different axis: lies along the x-axis, along the y-axis, and along the z-axis. The axes themselves are labelled , , in the usual right-handed orientation.
The key physical idea is that a orbital is not a spherical cloud like an orbital. Instead, it has a directional shape with two lobes and a nodal plane that passes through the nucleus. For , the nodal plane is the -plane; for , it is the -plane; for , it is the -plane. On that plane, the probability of finding the electron is exactly zero. The lobes themselves represent regions where the wave function has opposite signs — one lobe is positive, the other negative — but the probability density is the same in both lobes because squaring removes the sign.
The boundary surface diagram does not show the actual shape of the orbital as a solid object. It encloses the region where there is a high probability (typically 90–95%) of finding the electron. The electron can still be found outside this surface, but the chance is small.
The figure directly illustrates the quantum numbers that arise from solving the Schrödinger equation for the hydrogen atom. The principal quantum number tells us this is the second energy level. The azimuthal quantum number (for a orbital) gives the orbital its dumbbell shape. The magnetic quantum number takes three values: , which correspond to the three orientations , , and respectively. So the three diagrams are not three different kinds of orbitals — they are the same orbital type () pointing in three perpendicular directions.
For a orbital, , , and give the three orientations.
The textbook uses this figure to make a deeper point about the quantum mechanical model. Unlike Bohr's model, which pictured the electron moving in fixed circular orbits, quantum mechanics gives us only a probability distribution. The boundary surface diagram is a visual summary of that distribution: it shows where the electron is most likely to be found, not a path it follows. The nodal plane is a direct consequence of the wave nature of the electron — it is a region where the wave function changes sign and therefore must be zero. …
Each p orbital has one nodal plane. For example, the orbital has its lobes along the z-axis, and the xy-plane is its nodal plane. The orbital has the yz-plane as its nodal plane, and the orbital has the xz-plane as its nodal plane.
A common mistake is to think that the electron is confined to the lobes. The lobes simply represent the region of highest probability. There is a non-zero probability of finding the electron inside the lobes and even, though very small, outside the boundary surface. The nodal plane is the only place where the probability is exactly zero.
The size of p orbitals also increases with . For , the 2p orbitals have no radial nodes (only the angular nodal plane). For , the 3p orbitals have one radial node in addition to the angular nodal plane.
The d Orbitals
For , we have d orbitals. For a given (where ), there are five d orbitals, corresponding to . Their shapes are more complex than p orbitals.
Four of the five d orbitals have a cloverleaf shape, consisting of four lobes arranged in a plane. The fifth, the orbital, has a unique shape: a dumbbell along the z-axis with a donut-shaped ring (a torus) around the middle in the xy-plane.
Drawn by us to help you understand the concept clearly, and verified to make sure it's accurate. For exams, practice from your textbook's own diagram.
The five diagrams in Fig. 2.15 are boundary surface diagrams of the 3d orbitals. They are not photographs of an electron; they are a visual representation of the region in space where there is a 90–95% probability of finding the electron that occupies that orbital. The axes (x, y, z) are drawn through the nucleus at the origin.
Each orbital has a characteristic shape determined by its angular part. The four orbitals , , , and each show four lobes arranged in a cloverleaf pattern. The key difference is the orientation of the lobes relative to the coordinate axes. For , the four lobes lie between the x and y axes; for , between x and z; for , between y and z. The orbital also has four lobes, but they lie along the x and y axes themselves. The orbital is different: it has two lobes along the z-axis (one above, one below the nucleus) and a doughnut-shaped ring (a torus) lying in the xy-plane around the nucleus.
A common mistake is to think the lobes are the electron's path or that the electron is "smeared" across the lobes. The lobes show the region of highest probability — the electron can be found anywhere inside the boundary surface, but it is most likely to be found within the lobes.
The physical idea is that an atomic orbital is not a fixed orbit like a planet's path. It is a probability cloud described by the wave function . The square of the wave function, , gives the probability density at any point. The boundary surface encloses the volume where the probability of finding the electron is, say, 90%. The shape of this surface is determined by the angular part of the wave function, which depends on the quantum numbers and . For (d orbitals), the angular part has a specific mathematical form that produces these cloverleaf and dumbbell-with-ring shapes.
The central formula that connects the figure to the theory is the Schrödinger equation for the hydrogen atom. Its solution yields the wave function , which can be separated into a radial part and an angular part :
Here:
- is the principal quantum number (energy level).
- is the azimuthal quantum number (orbital shape; for d orbitals, ).
- is the magnetic quantum number (orbital orientation; takes values for ).
- , , are the spherical coordinates of the electron relative to the nucleus.
- describes how the probability density varies with distance from the nucleus.
- describes the angular shape — it is this part that gives the cloverleaf or dumbbell-with-ring pattern.
The boundary surface diagram is essentially a plot of the angular part at a fixed radial distance where the probability density is high. The five diagrams correspond to the five possible values of for : . The textbook labels them as , , , , and — these are the real combinations of the complex spherical harmonics that are easier to visualize. …
The five d orbitals are labelled as follows:
- : lobes lie between the x and y axes, in the xy-plane.
- : lobes lie between the y and z axes, in the yz-plane.
- : lobes lie between the z and x axes, in the zx-plane.
- : lobes lie along the x and y axes, in the xy-plane.
- : lobes along the z-axis with a torus in the xy-plane.
Each d orbital has two nodal planes (except , which has two conical nodes). For example, the orbital has the xz-plane and the yz-plane as its nodal planes.
The number of angular nodes (nodal planes or surfaces) for an orbital is equal to the azimuthal quantum number . For s orbitals (): 0 angular nodes. For p orbitals (): 1 angular node. For d orbitals (): 2 angular nodes. The total number of nodes (radial + angular) for an orbital is . …