We have investigated the (n, γ) cross sections of p-process isotopes with the activation technique. The measurements were carried out at the Karlsruhe Van de Graaff accelerator using the 7 Li(p, n)7 Be source for simulating a Maxwellian neutron distribution of kT = 25 keV.
I. INTRODUCTIONAstrophysical models can explain the origin of most nuclei beyond the iron group by a combination of processes involving neutron captures on long (s-process) or short (r-process) time scales [1,2].However, 32 proton-rich stable isotopes between 74 Se and 196 Hg cannot be formed in these neutron capture processes, because they are either shielded by stable isotopes from the r-process decay chains or lie outside the s-process flow (Fig. 1). These isotopes, which are ascribed to the so-called "p-process", are 10 to 100 times less abundant than their s-and r-process neighbors. So far, the astrophysical site of the p-process is still under discussion, since the solar p-abundances can not be completely described by current models.Historically, the p-process was thought to proceed via proton captures, but a plausible site with the required amount of free protons could not be identified. Moreover, elements with large Z cannot be produced by proton captures because the temperatures necessary to overcome * Electronic address: iris.dillmann@ph. the Coulomb repulsion favor photodisintegration rather than charged-particle capture.The most plausible astrophysical site is the explosively burning Ne/O layer in core collapse supernovae, which is heated to ignition temperatures by the outgoing shock front [3][4][5]. In this high-temperature environment proton-rich nuclei are produced by sequences of photodissociations and β + decays. In stars 20 times more massive than the sun the p-process temperatures for efficient photo-disintegration are already reached at the end of hydrostatic Ne/O burning [6]. This mechanism is also called "γ process" because proton-rich isotopes are produced by (γ, n) reactions on pre-existing seed nuclei from