Bethe–Bloch Energy Loss Calculator

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Enter particle and material properties.

Charged Particles and the Energy Loss Puzzle

Whenever a charged particle traverses matter it leaves behind a trail of ionization and excitation. Quantifying how rapidly the particle loses energy as it plows through a medium is crucial for designing detectors, shielding, and accelerators. The Bethe–Bloch formula provides the canonical description of this energy loss for heavy charged particles such as protons, alpha particles, or muons moving at non-relativistic to moderately relativistic speeds. Developed in the 1930s by Hans Bethe and later refined by Felix Bloch, the formula distills the complex electromagnetic interactions between the projectile and atomic electrons into a relatively compact expression.

The energy loss per unit path length, often called the stopping power, depends on the projectile's charge, velocity, and mass as well as on the atomic properties of the absorber. The version implemented here omits density effect and shell corrections, making it most accurate for intermediate energies where the Bethe–Bloch formalism is traditionally applied. Nevertheless, it captures the essential physics and reproduces the famous minimum-ionizing behavior in which particles near βγ ≈ 3 experience the lowest stopping power.

The key parameters entering the formula are the particle's charge number z, its mass m, and its kinetic energy T. From the mass and kinetic energy we compute the Lorentz factor γ = 1 + T/m and the dimensionless velocity β = sqrt(1 − 1/γ²). The material is characterized by its atomic number Z, mass number A, mean excitation energy I, and mass density ρ. The mean excitation energy I encapsulates the average binding energy of electrons in the material and typically ranges from tens to hundreds of electron volts. The density ρ allows us to convert the mass stopping power, expressed in MeV cm²/g, into a linear stopping power in MeV/cm.

The Bethe–Bloch stopping power can be written as

- dE/dx = K z^2 Z/A × (1/β^2) × [1/2 ln(2 m_e c^2 β^2 γ^2 T_max / I^2) − β^2]

where K = 0.307075 MeV mol⁻¹ cm² is a constant derived from fundamental constants, me = 0.511 MeV/c² is the electron mass, and Tmax is the maximum kinetic energy that can be transferred to a free electron in a single collision. For a projectile of mass m and velocity β, the maximum transferable energy is

T_max = (2 m_e c^2 β^2 γ^2) / (1 + 2γ m_e/m + (m_e/m)^2)

Multiplying the mass stopping power by the material density ρ yields the linear stopping power in units of MeV/cm, which is often more directly useful for estimating detector thicknesses or shielding requirements. Dividing the particle's kinetic energy by this linear stopping power gives a crude estimate of the particle's range, assuming a constant stopping power over the energy interval. In reality the stopping power varies with energy, so the calculated range is only an approximation.

To illustrate, consider a 200 MeV proton (z = 1, m = 938 MeV) passing through silicon (Z = 14, A = 28, I = 173 eV, ρ = 2.33 g/cm³). Plugging these values into the formula yields β ≈ 0.565 and γ ≈ 1.21. The resulting mass stopping power is about 4.9 MeV cm²/g, corresponding to a linear stopping power of 11.4 MeV/cm. The proton would therefore travel roughly 17.5 cm before coming to rest if the stopping power remained constant. In reality it would slow down, increasing the stopping power and reducing the range, but the estimate provides a ballpark figure.

The behavior of the stopping power as a function of energy exhibits three main regimes. At low energies the 1/β² factor dominates, leading to the familiar rise in stopping power as the particle slows down—the Bragg peak exploited in proton therapy for cancer treatment. At intermediate energies the logarithmic term balances the 1/β² factor, producing a broad minimum where the particle is said to be minimum ionizing. At very high energies, relativistic effects and density corrections cause the stopping power to rise logarithmically. The calculator here captures the first two regimes but omits the density correction that tempers the high-energy rise.

Historically, the Bethe–Bloch equation marked a milestone in quantum mechanics and particle physics. It combined quantum treatment of electron scattering with classical electrodynamics, providing early evidence that quantum theory could describe phenomena over a huge range of energies. The formula's success in describing cosmic-ray energy loss in the atmosphere and in cloud chambers helped solidify the emerging picture of subatomic particles. Today it remains embedded in detector simulation software such as GEANT and is taught in virtually every course on particle detection.

The implementation below performs the necessary calculations step by step. After computing β and γ from the entered mass and kinetic energy, it evaluates Tmax, plugs everything into the Bethe–Bloch expression, and multiplies by ρ to obtain the linear stopping power. The result displays both the mass stopping power (MeV cm²/g), the linear stopping power (MeV/cm), and the crude range estimate (cm). To help users understand typical values, the table that follows lists sample outputs for a variety of particles and materials.

ProjectileT (MeV)MaterialMass Stop. Power (MeV cm²/g)Linear Stop. Power (MeV/cm)Range Estimate (cm)
Proton200Silicon4.911.417.5
Alpha5Air1500.180.03
Muon3000Lead1.315.0200

While these values offer a glimpse into the rich phenomenology of charged-particle energy loss, the Bethe–Bloch formula has limitations. For very low energies where atomic binding and charge-exchange processes dominate, more sophisticated models are required. At extremely high energies, polarization of the medium reduces the electric field seen by distant electrons, a phenomenon accounted for by the density effect correction δ. Shell corrections become important when the projectile's velocity is comparable to the orbital velocities of the bound electrons. Heavy ions may also necessitate corrections for charge-state evolution as they capture and lose electrons along their path. Nonetheless, within its domain of validity the Bethe–Bloch equation remains a reliable workhorse.

The calculator encourages exploration of how varying parameters influences energy loss. Increasing the charge number z strengthens the electromagnetic interaction and thus raises the stopping power quadratically. Increasing kinetic energy initially lowers the stopping power as β approaches relativistic values, but eventually the logarithmic term takes over and the stopping power rises again. Materials with high Z/A ratios and large mean excitation energies typically lead to greater energy loss. By experimenting with different inputs, users can build intuition for detector design or radiation shielding.

Beyond practical applications, the Bethe–Bloch formula offers insights into fundamental interactions. It illustrates how quantum electrodynamics manifests in macroscopic observables and how collective properties of matter, such as mean excitation energy, emerge from microscopic electron structure. The logarithmic dependence on velocity reflects the long-range nature of the Coulomb force, while the 1/β² factor reveals the diminishing interaction time as particles move faster.

In summary, the Bethe–Bloch energy loss formula stands as a cornerstone of particle physics and detector technology. This calculator distills the core expression into a convenient tool, enabling researchers, students, and enthusiasts to estimate stopping powers and ranges for a variety of scenarios without resorting to lengthy derivations or specialized software. Whether you are planning a beamline experiment, assessing radiation shielding, or simply curious about how particles interact with matter, the Bethe–Bloch calculator provides a window into a classic piece of physics that continues to inform modern science.

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