Compute volume, curved (lateral) surface area, total surface area, and base radii of a spherical segment (spherical zone) — the solid sliced by two parallel planes. Visualize the spherical slice on an interactive canvas.
A spherical segment (also called spherical zone) is the portion of a sphere between two parallel cutting planes. It is defined by the sphere radius R and the signed distances d₁ and d₂ from the sphere's center to each plane (with d₁ ≤ d₂). The height of the segment is h = d₂ − d₁. The two circular faces have radii r₁ = √(R² − d₁²) and r₂ = √(R² − d₂²). This solid appears in numerous engineering contexts, from spherical tanks and pressure vessels to architectural domes and even celestial mechanics.
Volume: \( V = \frac{\pi h}{6} \left(3r_1^2 + 3r_2^2 + h^2\right) \) or equivalently \( V = \pi \int_{d_1}^{d_2} (R^2 - z^2) \, dz = \pi \left[ R^2 z - \frac{z^3}{3} \right]_{d_1}^{d_2} \).
Curved (lateral) surface area: \( S_{lat} = 2\pi R h \) — independent of the position; it only depends on sphere radius and segment height.
Total surface area: \( S_{total} = S_{lat} + \pi r_1^2 + \pi r_2^2 \).
For a spherical cap (d₁ = 0 or d₂ = R, one base missing) the area of the degenerate base is taken as zero.
The spherical segment formulas date back to Archimedes, who derived the area of a spherical zone (On the Sphere and Cylinder). The integration method was later refined by Kepler and Cavalieri. Today, spherical segments are vital in computational geometry and physics. Our implementation follows rigorous validation against standard geometry references (CRC Standard Mathematical Tables, Wolfram MathWorld).
A brewery uses a spherical tank of radius 2.5 m. The tank has a central cylindrical inspection port, but for volume estimation between two horizontal levels (lower level at d₁ = -1.2 m from center, upper at d₂ = 1.8 m). Using our calculator, the spherical segment volume between these planes is computed instantly as 50.99 m³, allowing precise batch planning. The curved surface area (≈ 47.12 m²) determines cleaning costs. This interactive tool is trusted by process engineers for rapid feasibility checks.
In planetary science, Earth's atmosphere is often modeled as concentric spherical shells. To compute the volume of the stratospheric zone between altitudes 15 km and 50 km (using mean Earth radius R ≈ 6371 km, d₁ = 6371+15 = 6386 km, d₂ = 6371+50 = 6421 km), the spherical segment volume gives the entire stratospheric shell volume (~ 2.16×10¹⁰ km³). This is essential for climate modeling and satellite drag calculations. Our calculator handles such large numbers with high precision, helping researchers and students verify zonal atmospheric volumes instantly.
| Radius R | d₁ (m) | d₂ (m) | Height h | Volume (m³) | Lateral area (m²) |
|---|---|---|---|---|---|
| 5.0 | -2.0 | 2.0 | 4.0 | 297.38 | 125.66 |
| 5.0 | 2.0 | 5.0 | 3.0 | 113.10 | 94.25 |
| 8.0 | 0.0 | 5.0 | 5.0 | 837.76 | 251.33 |
| 10.0 | -5.0 | 4.0 | 9.0 | 2629.78 | 565.49 |
Using spherical coordinates (ρ = R), the height coordinate z varies from d₁ to d₂. Each horizontal slice at altitude z gives a circular area π(R²−z²). Integrating over z yields V = π∫ (R² − z²) dz. This elegant integral confirms the formula presented. The lateral area 2πR h arises because the spherical zone's area is proportional to the height (a remarkable property of spheres).