Lab 03: The Gamow Peak and the pp-Chain/CNO-Cycle Crossover Temperature

Compute Gamow peak energies and the pp/CNO crossover temperature, then classify the Sun and Sirius A.

Apparatus and Setup

This lab computes the Gamow peak energy (Lecture 05) for proton-proton and CNO-cycle reactions and reproduces the pp-chain/CNO-cycle crossover-temperature calculation (Lecture 06) for the Sun and for Sirius A, using the same schematic power-law energy-generation scalings developed in the lecture.

Materials and Data

StarCore temperature (K)T6
Sun (standard published core temperature)1.570e+0715.70
Sirius A (2.063 M⊙, schematic mass-scaling estimate)2.606e+0726.06

Procedure

  1. Compute the Gamow peak energy E0 for proton-proton reactions (Z1=Z2=1, μ=0.5 amu) at the Sun's core temperature, and compare it to kT at that same temperature.
  2. Compute the Gamow peak energy for a proton-nitrogen-14 reaction (Z1=1, Z2=7, μ=12/13 amu, the CNO cycle's rate-limiting step) at the same temperature, and compare it to the pp-chain Gamow peak from step 1.
  3. Using ε_pp ∝ T6⁴ and ε_CNO ∝ T6²⁰ (both normalized so the Sun is 1000:1 pp-dominated, per Lecture 06), find the crossover T6 at which the two curves are equal, and verify your answer is consistent with the value quoted in Lecture 06.
  4. Using Sirius A's schematic core-temperature estimate, classify Sirius A as pp-dominated or CNO-dominated, and state whether this is consistent with real stellar models for a star of Sirius A's mass and spectral type.

Analysis and Uncertainty

The Sirius A core-temperature estimate uses a schematic mass-scaling relation (T_core ∝ M^0.7), not a precision stellar model; state explicitly why this is sufficient for a qualitative pp-versus-CNO classification but would not be sufficient for a precise nuclear-burning-rate calculation.

Deliverables

Assessment Criteria

References and Provenance